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Erozija - Wikipedija, prosta enciklopedija

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class="vector-menu-content"> <ul class="vector-menu-content-list"> </ul> </div> </div> <div id="p-vector-user-menu-userpage" class="vector-menu mw-portlet emptyPortlet" > <div class="vector-menu-content"> <ul class="vector-menu-content-list"> </ul> </div> </div> <nav class="vector-appearance-landmark" aria-label="Videz"> <div id="vector-appearance-dropdown" class="vector-dropdown " title="Change the appearance of the page&#039;s font size, width, and color" > <input type="checkbox" id="vector-appearance-dropdown-checkbox" role="button" aria-haspopup="true" data-event-name="ui.dropdown-vector-appearance-dropdown" class="vector-dropdown-checkbox " aria-label="Videz" > <label id="vector-appearance-dropdown-label" for="vector-appearance-dropdown-checkbox" class="vector-dropdown-label cdx-button cdx-button--fake-button cdx-button--fake-button--enabled cdx-button--weight-quiet cdx-button--icon-only " aria-hidden="true" ><span class="vector-icon mw-ui-icon-appearance 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<div id="vector-toc-pinned-container" class="vector-pinned-container"> <div id="vector-toc" class="vector-toc vector-pinnable-element"> <div class="vector-pinnable-header vector-toc-pinnable-header vector-pinnable-header-pinned" data-feature-name="toc-pinned" data-pinnable-element-id="vector-toc" > <h2 class="vector-pinnable-header-label">Vsebina</h2> <button class="vector-pinnable-header-toggle-button vector-pinnable-header-pin-button" data-event-name="pinnable-header.vector-toc.pin">prestavi v stransko letvico</button> <button class="vector-pinnable-header-toggle-button vector-pinnable-header-unpin-button" data-event-name="pinnable-header.vector-toc.unpin">skrij</button> </div> <ul class="vector-toc-contents" id="mw-panel-toc-list"> <li id="toc-mw-content-text" class="vector-toc-list-item vector-toc-level-1"> <a href="#" class="vector-toc-link"> <div class="vector-toc-text">Uvod</div> </a> </li> <li id="toc-Fizični_procesi" class="vector-toc-list-item vector-toc-level-1 vector-toc-list-item-expanded"> <a class="vector-toc-link" href="#Fizični_procesi"> <div class="vector-toc-text"> <span class="vector-toc-numb">1</span> <span>Fizični procesi</span> </div> </a> <button aria-controls="toc-Fizični_procesi-sublist" class="cdx-button cdx-button--weight-quiet cdx-button--icon-only vector-toc-toggle"> <span class="vector-icon mw-ui-icon-wikimedia-expand"></span> <span>Vklopi podrazdelek Fizični procesi</span> </button> <ul id="toc-Fizični_procesi-sublist" class="vector-toc-list"> <li id="toc-Padavine_in_površinsko_odtekanje" class="vector-toc-list-item vector-toc-level-2"> <a class="vector-toc-link" href="#Padavine_in_površinsko_odtekanje"> <div class="vector-toc-text"> <span class="vector-toc-numb">1.1</span> <span>Padavine in površinsko odtekanje</span> </div> </a> <ul id="toc-Padavine_in_površinsko_odtekanje-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-Reke_in_potoki" class="vector-toc-list-item vector-toc-level-2"> <a class="vector-toc-link" href="#Reke_in_potoki"> <div class="vector-toc-text"> <span class="vector-toc-numb">1.2</span> <span>Reke in potoki</span> </div> </a> <ul id="toc-Reke_in_potoki-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-Obalna_erozija" class="vector-toc-list-item vector-toc-level-2"> <a class="vector-toc-link" href="#Obalna_erozija"> <div class="vector-toc-text"> <span class="vector-toc-numb">1.3</span> <span>Obalna erozija</span> </div> </a> <ul id="toc-Obalna_erozija-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-Kemična_erozija" class="vector-toc-list-item vector-toc-level-2"> <a class="vector-toc-link" href="#Kemična_erozija"> <div class="vector-toc-text"> <span class="vector-toc-numb">1.4</span> <span>Kemična erozija</span> </div> </a> <ul id="toc-Kemična_erozija-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-Ledeniki" class="vector-toc-list-item vector-toc-level-2"> <a class="vector-toc-link" href="#Ledeniki"> <div class="vector-toc-text"> <span class="vector-toc-numb">1.5</span> <span>Ledeniki</span> </div> </a> <ul id="toc-Ledeniki-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-Poplave" class="vector-toc-list-item vector-toc-level-2"> <a class="vector-toc-link" href="#Poplave"> <div class="vector-toc-text"> <span class="vector-toc-numb">1.6</span> <span>Poplave</span> </div> </a> <ul id="toc-Poplave-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-Vetrna_erozija" class="vector-toc-list-item vector-toc-level-2"> <a class="vector-toc-link" href="#Vetrna_erozija"> <div class="vector-toc-text"> <span class="vector-toc-numb">1.7</span> <span>Vetrna erozija</span> </div> </a> <ul id="toc-Vetrna_erozija-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-Plazovi" class="vector-toc-list-item vector-toc-level-2"> <a class="vector-toc-link" href="#Plazovi"> <div class="vector-toc-text"> <span class="vector-toc-numb">1.8</span> <span>Plazovi</span> </div> </a> <ul id="toc-Plazovi-sublist" class="vector-toc-list"> </ul> </li> </ul> </li> <li id="toc-Sklici" class="vector-toc-list-item vector-toc-level-1 vector-toc-list-item-expanded"> <a class="vector-toc-link" href="#Sklici"> <div class="vector-toc-text"> <span class="vector-toc-numb">2</span> <span>Sklici</span> </div> </a> <ul id="toc-Sklici-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-Zunanje_povezave" class="vector-toc-list-item vector-toc-level-1 vector-toc-list-item-expanded"> <a class="vector-toc-link" href="#Zunanje_povezave"> <div class="vector-toc-text"> <span class="vector-toc-numb">3</span> <span>Zunanje povezave</span> </div> </a> <ul id="toc-Zunanje_povezave-sublist" class="vector-toc-list"> </ul> </li> </ul> </div> </div> </nav> </div> </div> <div class="mw-content-container"> <main id="content" class="mw-body"> <header class="mw-body-header vector-page-titlebar"> <nav aria-label="Vsebina" class="vector-toc-landmark"> <div id="vector-page-titlebar-toc" class="vector-dropdown vector-page-titlebar-toc vector-button-flush-left" > <input type="checkbox" id="vector-page-titlebar-toc-checkbox" role="button" aria-haspopup="true" data-event-name="ui.dropdown-vector-page-titlebar-toc" class="vector-dropdown-checkbox " aria-label="Vklopi kazalo vsebine" > <label id="vector-page-titlebar-toc-label" for="vector-page-titlebar-toc-checkbox" class="vector-dropdown-label cdx-button cdx-button--fake-button cdx-button--fake-button--enabled cdx-button--weight-quiet cdx-button--icon-only " aria-hidden="true" ><span class="vector-icon mw-ui-icon-listBullet mw-ui-icon-wikimedia-listBullet"></span> <span class="vector-dropdown-label-text">Vklopi kazalo vsebine</span> </label> <div class="vector-dropdown-content"> <div id="vector-page-titlebar-toc-unpinned-container" class="vector-unpinned-container"> </div> </div> </div> </nav> <h1 id="firstHeading" class="firstHeading mw-first-heading"><span class="mw-page-title-main">Erozija</span></h1> <div id="p-lang-btn" class="vector-dropdown mw-portlet mw-portlet-lang" > <input type="checkbox" id="p-lang-btn-checkbox" role="button" aria-haspopup="true" data-event-name="ui.dropdown-p-lang-btn" class="vector-dropdown-checkbox mw-interlanguage-selector" aria-label="P9jdi na članek v drugem jeziku. Na voljo v 93 jezikih." > <label id="p-lang-btn-label" for="p-lang-btn-checkbox" class="vector-dropdown-label cdx-button cdx-button--fake-button cdx-button--fake-button--enabled cdx-button--weight-quiet cdx-button--action-progressive mw-portlet-lang-heading-93" aria-hidden="true" ><span class="vector-icon mw-ui-icon-language-progressive mw-ui-icon-wikimedia-language-progressive"></span> <span class="vector-dropdown-label-text">93 jezikov</span> </label> <div class="vector-dropdown-content"> <div class="vector-menu-content"> <ul class="vector-menu-content-list"> <li class="interlanguage-link interwiki-af mw-list-item"><a href="https://af.wikipedia.org/wiki/Erosie" title="Erosie – afrikanščina" lang="af" hreflang="af" data-title="Erosie" data-language-autonym="Afrikaans" data-language-local-name="afrikanščina" class="interlanguage-link-target"><span>Afrikaans</span></a></li><li class="interlanguage-link interwiki-an mw-list-item"><a href="https://an.wikipedia.org/wiki/Erosi%C3%B3n" title="Erosión – aragonščina" lang="an" hreflang="an" data-title="Erosión" data-language-autonym="Aragonés" data-language-local-name="aragonščina" class="interlanguage-link-target"><span>Aragonés</span></a></li><li class="interlanguage-link interwiki-ar mw-list-item"><a href="https://ar.wikipedia.org/wiki/%D8%AA%D8%B9%D8%B1%D9%8A%D8%A9" title="تعرية – arabščina" lang="ar" hreflang="ar" data-title="تعرية" data-language-autonym="العربية" data-language-local-name="arabščina" class="interlanguage-link-target"><span>العربية</span></a></li><li class="interlanguage-link interwiki-ast mw-list-item"><a href="https://ast.wikipedia.org/wiki/Erosi%C3%B3n" title="Erosión – asturijščina" lang="ast" hreflang="ast" data-title="Erosión" data-language-autonym="Asturianu" data-language-local-name="asturijščina" class="interlanguage-link-target"><span>Asturianu</span></a></li><li class="interlanguage-link interwiki-az mw-list-item"><a href="https://az.wikipedia.org/wiki/Eroziya" title="Eroziya – azerbajdžanščina" lang="az" hreflang="az" data-title="Eroziya" data-language-autonym="Azərbaycanca" data-language-local-name="azerbajdžanščina" class="interlanguage-link-target"><span>Azərbaycanca</span></a></li><li class="interlanguage-link interwiki-be mw-list-item"><a href="https://be.wikipedia.org/wiki/%D0%AD%D1%80%D0%BE%D0%B7%D1%96%D1%8F_(%D0%B3%D0%B5%D0%B0%D0%BB%D0%BE%D0%B3%D1%96%D1%8F)" title="Эрозія (геалогія) – beloruščina" lang="be" hreflang="be" data-title="Эрозія (геалогія)" data-language-autonym="Беларуская" data-language-local-name="beloruščina" class="interlanguage-link-target"><span>Беларуская</span></a></li><li class="interlanguage-link interwiki-bg mw-list-item"><a href="https://bg.wikipedia.org/wiki/%D0%95%D1%80%D0%BE%D0%B7%D0%B8%D1%8F" title="Ерозия – bolgarščina" lang="bg" hreflang="bg" data-title="Ерозия" data-language-autonym="Български" data-language-local-name="bolgarščina" class="interlanguage-link-target"><span>Български</span></a></li><li class="interlanguage-link interwiki-bn mw-list-item"><a href="https://bn.wikipedia.org/wiki/%E0%A6%95%E0%A7%8D%E0%A6%B7%E0%A6%AF%E0%A6%BC%E0%A7%80%E0%A6%AD%E0%A6%AC%E0%A6%A8" title="ক্ষয়ীভবন – bengalščina" lang="bn" hreflang="bn" data-title="ক্ষয়ীভবন" data-language-autonym="বাংলা" data-language-local-name="bengalščina" class="interlanguage-link-target"><span>বাংলা</span></a></li><li class="interlanguage-link interwiki-br mw-list-item"><a href="https://br.wikipedia.org/wiki/Krignerezh" title="Krignerezh – bretonščina" lang="br" hreflang="br" data-title="Krignerezh" data-language-autonym="Brezhoneg" data-language-local-name="bretonščina" class="interlanguage-link-target"><span>Brezhoneg</span></a></li><li class="interlanguage-link interwiki-bs mw-list-item"><a href="https://bs.wikipedia.org/wiki/Erozija" title="Erozija – bosanščina" lang="bs" hreflang="bs" data-title="Erozija" data-language-autonym="Bosanski" data-language-local-name="bosanščina" class="interlanguage-link-target"><span>Bosanski</span></a></li><li class="interlanguage-link interwiki-ca mw-list-item"><a href="https://ca.wikipedia.org/wiki/Erosi%C3%B3" title="Erosió – katalonščina" lang="ca" hreflang="ca" data-title="Erosió" data-language-autonym="Català" data-language-local-name="katalonščina" class="interlanguage-link-target"><span>Català</span></a></li><li class="interlanguage-link interwiki-chr mw-list-item"><a href="https://chr.wikipedia.org/wiki/%E1%8E%A6%E1%8F%93_%E1%8E%A6%E1%8F%93%E1%8E%B6%E1%8F%8D%E1%8E%AC" title="ᎦᏓ ᎦᏓᎶᏍᎬ – čerokeščina" lang="chr" hreflang="chr" data-title="ᎦᏓ ᎦᏓᎶᏍᎬ" data-language-autonym="ᏣᎳᎩ" data-language-local-name="čerokeščina" class="interlanguage-link-target"><span>ᏣᎳᎩ</span></a></li><li class="interlanguage-link interwiki-ckb mw-list-item"><a href="https://ckb.wikipedia.org/wiki/%D9%88%DB%95%D8%B1%DB%8C%D9%86%DB%8C" title="وەرینی – osrednja kurdščina" lang="ckb" hreflang="ckb" data-title="وەرینی" data-language-autonym="کوردی" data-language-local-name="osrednja kurdščina" class="interlanguage-link-target"><span>کوردی</span></a></li><li class="interlanguage-link interwiki-cs mw-list-item"><a href="https://cs.wikipedia.org/wiki/Eroze" title="Eroze – češčina" lang="cs" hreflang="cs" data-title="Eroze" data-language-autonym="Čeština" data-language-local-name="češčina" class="interlanguage-link-target"><span>Čeština</span></a></li><li class="interlanguage-link interwiki-cy mw-list-item"><a href="https://cy.wikipedia.org/wiki/Erydiad" title="Erydiad – valižanščina" lang="cy" hreflang="cy" data-title="Erydiad" data-language-autonym="Cymraeg" data-language-local-name="valižanščina" class="interlanguage-link-target"><span>Cymraeg</span></a></li><li class="interlanguage-link interwiki-da mw-list-item"><a href="https://da.wikipedia.org/wiki/Erosion" title="Erosion – danščina" lang="da" hreflang="da" data-title="Erosion" data-language-autonym="Dansk" data-language-local-name="danščina" class="interlanguage-link-target"><span>Dansk</span></a></li><li class="interlanguage-link interwiki-de mw-list-item"><a href="https://de.wikipedia.org/wiki/Erosion_(Geologie)" title="Erosion (Geologie) – nemščina" lang="de" hreflang="de" data-title="Erosion (Geologie)" data-language-autonym="Deutsch" data-language-local-name="nemščina" class="interlanguage-link-target"><span>Deutsch</span></a></li><li class="interlanguage-link interwiki-el mw-list-item"><a href="https://el.wikipedia.org/wiki/%CE%91%CF%80%CE%BF%CF%83%CE%AC%CE%B8%CF%81%CF%89%CF%83%CE%B7" title="Αποσάθρωση – grščina" lang="el" hreflang="el" data-title="Αποσάθρωση" data-language-autonym="Ελληνικά" data-language-local-name="grščina" class="interlanguage-link-target"><span>Ελληνικά</span></a></li><li class="interlanguage-link interwiki-en mw-list-item"><a href="https://en.wikipedia.org/wiki/Erosion" title="Erosion – angleščina" lang="en" hreflang="en" data-title="Erosion" data-language-autonym="English" data-language-local-name="angleščina" class="interlanguage-link-target"><span>English</span></a></li><li class="interlanguage-link interwiki-eo mw-list-item"><a href="https://eo.wikipedia.org/wiki/Erozio" title="Erozio – esperanto" lang="eo" hreflang="eo" data-title="Erozio" data-language-autonym="Esperanto" data-language-local-name="esperanto" class="interlanguage-link-target"><span>Esperanto</span></a></li><li class="interlanguage-link interwiki-es mw-list-item"><a href="https://es.wikipedia.org/wiki/Erosi%C3%B3n" title="Erosión – španščina" lang="es" hreflang="es" data-title="Erosión" data-language-autonym="Español" data-language-local-name="španščina" class="interlanguage-link-target"><span>Español</span></a></li><li class="interlanguage-link interwiki-et mw-list-item"><a href="https://et.wikipedia.org/wiki/Erosioon" title="Erosioon – estonščina" lang="et" hreflang="et" data-title="Erosioon" data-language-autonym="Eesti" data-language-local-name="estonščina" class="interlanguage-link-target"><span>Eesti</span></a></li><li class="interlanguage-link interwiki-eu mw-list-item"><a href="https://eu.wikipedia.org/wiki/Higadura" title="Higadura – baskovščina" lang="eu" hreflang="eu" data-title="Higadura" data-language-autonym="Euskara" data-language-local-name="baskovščina" class="interlanguage-link-target"><span>Euskara</span></a></li><li class="interlanguage-link interwiki-fa mw-list-item"><a href="https://fa.wikipedia.org/wiki/%D9%81%D8%B1%D8%B3%D8%A7%DB%8C%D8%B4" title="فرسایش – perzijščina" lang="fa" hreflang="fa" data-title="فرسایش" data-language-autonym="فارسی" data-language-local-name="perzijščina" class="interlanguage-link-target"><span>فارسی</span></a></li><li class="interlanguage-link interwiki-fi mw-list-item"><a href="https://fi.wikipedia.org/wiki/Eroosio" title="Eroosio – finščina" lang="fi" hreflang="fi" data-title="Eroosio" data-language-autonym="Suomi" data-language-local-name="finščina" class="interlanguage-link-target"><span>Suomi</span></a></li><li class="interlanguage-link interwiki-fr mw-list-item"><a href="https://fr.wikipedia.org/wiki/%C3%89rosion" title="Érosion – francoščina" lang="fr" hreflang="fr" data-title="Érosion" data-language-autonym="Français" data-language-local-name="francoščina" class="interlanguage-link-target"><span>Français</span></a></li><li class="interlanguage-link interwiki-ga mw-list-item"><a href="https://ga.wikipedia.org/wiki/Cna%C3%AD" title="Cnaí – irščina" lang="ga" hreflang="ga" data-title="Cnaí" data-language-autonym="Gaeilge" data-language-local-name="irščina" class="interlanguage-link-target"><span>Gaeilge</span></a></li><li class="interlanguage-link interwiki-gcr mw-list-item"><a href="https://gcr.wikipedia.org/wiki/%C3%89rozyon" title="Érozyon – Guianan Creole" lang="gcr" hreflang="gcr" data-title="Érozyon" data-language-autonym="Kriyòl gwiyannen" data-language-local-name="Guianan Creole" class="interlanguage-link-target"><span>Kriyòl gwiyannen</span></a></li><li class="interlanguage-link interwiki-gl mw-list-item"><a href="https://gl.wikipedia.org/wiki/Erosi%C3%B3n" title="Erosión – galicijščina" lang="gl" hreflang="gl" data-title="Erosión" data-language-autonym="Galego" data-language-local-name="galicijščina" class="interlanguage-link-target"><span>Galego</span></a></li><li class="interlanguage-link interwiki-gn mw-list-item"><a href="https://gn.wikipedia.org/wiki/Yvysyry" title="Yvysyry – gvaranijščina" lang="gn" hreflang="gn" data-title="Yvysyry" data-language-autonym="Avañe&#039;ẽ" data-language-local-name="gvaranijščina" class="interlanguage-link-target"><span>Avañe'ẽ</span></a></li><li class="interlanguage-link interwiki-ha mw-list-item"><a href="https://ha.wikipedia.org/wiki/Zaizayar_Kasa" title="Zaizayar Kasa – havščina" lang="ha" hreflang="ha" data-title="Zaizayar Kasa" data-language-autonym="Hausa" data-language-local-name="havščina" class="interlanguage-link-target"><span>Hausa</span></a></li><li class="interlanguage-link interwiki-he mw-list-item"><a href="https://he.wikipedia.org/wiki/%D7%A1%D7%97%D7%99%D7%A4%D7%94" title="סחיפה – hebrejščina" lang="he" hreflang="he" data-title="סחיפה" data-language-autonym="עברית" data-language-local-name="hebrejščina" class="interlanguage-link-target"><span>עברית</span></a></li><li class="interlanguage-link interwiki-hi mw-list-item"><a href="https://hi.wikipedia.org/wiki/%E0%A4%85%E0%A4%AA%E0%A4%B0%E0%A4%A6%E0%A4%A8" title="अपरदन – hindijščina" lang="hi" hreflang="hi" data-title="अपरदन" data-language-autonym="हिन्दी" data-language-local-name="hindijščina" class="interlanguage-link-target"><span>हिन्दी</span></a></li><li class="interlanguage-link interwiki-hr mw-list-item"><a href="https://hr.wikipedia.org/wiki/Erozija" title="Erozija – hrvaščina" lang="hr" hreflang="hr" data-title="Erozija" data-language-autonym="Hrvatski" data-language-local-name="hrvaščina" class="interlanguage-link-target"><span>Hrvatski</span></a></li><li class="interlanguage-link interwiki-ht mw-list-item"><a href="https://ht.wikipedia.org/wiki/Ewozyon" title="Ewozyon – haitijska kreolščina" lang="ht" hreflang="ht" data-title="Ewozyon" data-language-autonym="Kreyòl ayisyen" data-language-local-name="haitijska kreolščina" class="interlanguage-link-target"><span>Kreyòl ayisyen</span></a></li><li class="interlanguage-link interwiki-hu mw-list-item"><a href="https://hu.wikipedia.org/wiki/Er%C3%B3zi%C3%B3_(geol%C3%B3gia)" title="Erózió (geológia) – madžarščina" lang="hu" hreflang="hu" data-title="Erózió (geológia)" data-language-autonym="Magyar" data-language-local-name="madžarščina" class="interlanguage-link-target"><span>Magyar</span></a></li><li class="interlanguage-link interwiki-hy mw-list-item"><a href="https://hy.wikipedia.org/wiki/%D4%B7%D6%80%D5%B8%D5%A6%D5%AB%D5%A1" title="Էրոզիա – armenščina" lang="hy" hreflang="hy" data-title="Էրոզիա" data-language-autonym="Հայերեն" data-language-local-name="armenščina" class="interlanguage-link-target"><span>Հայերեն</span></a></li><li class="interlanguage-link interwiki-id mw-list-item"><a href="https://id.wikipedia.org/wiki/Erosi" title="Erosi – indonezijščina" lang="id" hreflang="id" data-title="Erosi" data-language-autonym="Bahasa Indonesia" data-language-local-name="indonezijščina" class="interlanguage-link-target"><span>Bahasa Indonesia</span></a></li><li class="interlanguage-link interwiki-io mw-list-item"><a href="https://io.wikipedia.org/wiki/Erodo" title="Erodo – ido" lang="io" hreflang="io" data-title="Erodo" data-language-autonym="Ido" data-language-local-name="ido" class="interlanguage-link-target"><span>Ido</span></a></li><li class="interlanguage-link interwiki-is mw-list-item"><a href="https://is.wikipedia.org/wiki/Rof" title="Rof – islandščina" lang="is" hreflang="is" data-title="Rof" data-language-autonym="Íslenska" data-language-local-name="islandščina" class="interlanguage-link-target"><span>Íslenska</span></a></li><li class="interlanguage-link interwiki-it mw-list-item"><a href="https://it.wikipedia.org/wiki/Erosione" title="Erosione – italijanščina" lang="it" hreflang="it" data-title="Erosione" data-language-autonym="Italiano" data-language-local-name="italijanščina" class="interlanguage-link-target"><span>Italiano</span></a></li><li class="interlanguage-link interwiki-iu mw-list-item"><a href="https://iu.wikipedia.org/wiki/%E1%93%84%E1%93%87%E1%90%85%E1%91%89_%E1%93%84%E1%96%91%E1%91%95%E1%92%83%E1%90%B8%E1%93%AA%E1%93%95%E1%90%8A%E1%93%82%E1%96%93" title="ᓄᓇᐅᑉ ᓄᖑᑕᒃᐸᓪᓕᐊᓂᖓ – inuktitutščina" lang="iu" hreflang="iu" data-title="ᓄᓇᐅᑉ ᓄᖑᑕᒃᐸᓪᓕᐊᓂᖓ" data-language-autonym="ᐃᓄᒃᑎᑐᑦ / inuktitut" data-language-local-name="inuktitutščina" class="interlanguage-link-target"><span>ᐃᓄᒃᑎᑐᑦ / inuktitut</span></a></li><li class="interlanguage-link interwiki-ja mw-list-item"><a href="https://ja.wikipedia.org/wiki/%E4%BE%B5%E9%A3%9F" title="侵食 – japonščina" lang="ja" hreflang="ja" data-title="侵食" data-language-autonym="日本語" data-language-local-name="japonščina" class="interlanguage-link-target"><span>日本語</span></a></li><li class="interlanguage-link interwiki-jam mw-list-item"><a href="https://jam.wikipedia.org/wiki/Iruojan" title="Iruojan – Jamaican Creole English" lang="jam" hreflang="jam" data-title="Iruojan" data-language-autonym="Patois" data-language-local-name="Jamaican Creole English" class="interlanguage-link-target"><span>Patois</span></a></li><li class="interlanguage-link interwiki-ka mw-list-item"><a href="https://ka.wikipedia.org/wiki/%E1%83%94%E1%83%A0%E1%83%9D%E1%83%96%E1%83%98%E1%83%90" title="ეროზია – gruzijščina" lang="ka" hreflang="ka" data-title="ეროზია" data-language-autonym="ქართული" data-language-local-name="gruzijščina" class="interlanguage-link-target"><span>ქართული</span></a></li><li class="interlanguage-link interwiki-kaa mw-list-item"><a href="https://kaa.wikipedia.org/wiki/Eroziya" title="Eroziya – karakalpaščina" lang="kaa" hreflang="kaa" data-title="Eroziya" data-language-autonym="Qaraqalpaqsha" data-language-local-name="karakalpaščina" class="interlanguage-link-target"><span>Qaraqalpaqsha</span></a></li><li class="interlanguage-link interwiki-kk mw-list-item"><a href="https://kk.wikipedia.org/wiki/%D0%AD%D1%80%D0%BE%D0%B7%D0%B8%D1%8F" title="Эрозия – kazaščina" lang="kk" hreflang="kk" data-title="Эрозия" data-language-autonym="Қазақша" data-language-local-name="kazaščina" class="interlanguage-link-target"><span>Қазақша</span></a></li><li class="interlanguage-link interwiki-kn mw-list-item"><a href="https://kn.wikipedia.org/wiki/%E0%B2%95%E0%B3%8D%E0%B2%B7%E0%B2%B0%E0%B2%A3/%E0%B2%B8%E0%B2%B5%E0%B3%86%E0%B2%A4" title="ಕ್ಷರಣ/ಸವೆತ – kanareščina" lang="kn" hreflang="kn" data-title="ಕ್ಷರಣ/ಸವೆತ" data-language-autonym="ಕನ್ನಡ" data-language-local-name="kanareščina" class="interlanguage-link-target"><span>ಕನ್ನಡ</span></a></li><li class="interlanguage-link interwiki-ko mw-list-item"><a href="https://ko.wikipedia.org/wiki/%EC%B9%A8%EC%8B%9D" title="침식 – korejščina" lang="ko" hreflang="ko" data-title="침식" data-language-autonym="한국어" data-language-local-name="korejščina" class="interlanguage-link-target"><span>한국어</span></a></li><li class="interlanguage-link interwiki-ky mw-list-item"><a href="https://ky.wikipedia.org/wiki/%D0%AD%D1%80%D0%BE%D0%B7%D0%B8%D1%8F" title="Эрозия – kirgiščina" lang="ky" hreflang="ky" data-title="Эрозия" data-language-autonym="Кыргызча" data-language-local-name="kirgiščina" class="interlanguage-link-target"><span>Кыргызча</span></a></li><li class="interlanguage-link interwiki-la mw-list-item"><a href="https://la.wikipedia.org/wiki/Erosio" title="Erosio – latinščina" lang="la" hreflang="la" data-title="Erosio" data-language-autonym="Latina" data-language-local-name="latinščina" class="interlanguage-link-target"><span>Latina</span></a></li><li class="interlanguage-link interwiki-lb mw-list-item"><a href="https://lb.wikipedia.org/wiki/Erosioun" title="Erosioun – luksemburščina" lang="lb" hreflang="lb" data-title="Erosioun" data-language-autonym="Lëtzebuergesch" data-language-local-name="luksemburščina" class="interlanguage-link-target"><span>Lëtzebuergesch</span></a></li><li class="interlanguage-link interwiki-li mw-list-item"><a href="https://li.wikipedia.org/wiki/Erosie" title="Erosie – limburščina" lang="li" hreflang="li" data-title="Erosie" data-language-autonym="Limburgs" data-language-local-name="limburščina" class="interlanguage-link-target"><span>Limburgs</span></a></li><li class="interlanguage-link interwiki-lt mw-list-item"><a href="https://lt.wikipedia.org/wiki/Erozija" title="Erozija – litovščina" lang="lt" hreflang="lt" data-title="Erozija" data-language-autonym="Lietuvių" data-language-local-name="litovščina" class="interlanguage-link-target"><span>Lietuvių</span></a></li><li class="interlanguage-link interwiki-lv mw-list-item"><a href="https://lv.wikipedia.org/wiki/Erozija" title="Erozija – latvijščina" lang="lv" hreflang="lv" data-title="Erozija" data-language-autonym="Latviešu" data-language-local-name="latvijščina" class="interlanguage-link-target"><span>Latviešu</span></a></li><li class="interlanguage-link interwiki-map-bms mw-list-item"><a href="https://map-bms.wikipedia.org/wiki/Erosi" title="Erosi – Banyumasan" lang="jv-x-bms" hreflang="jv-x-bms" data-title="Erosi" data-language-autonym="Basa Banyumasan" data-language-local-name="Banyumasan" class="interlanguage-link-target"><span>Basa Banyumasan</span></a></li><li class="interlanguage-link interwiki-mg mw-list-item"><a href="https://mg.wikipedia.org/wiki/Kaoka" title="Kaoka – malgaščina" lang="mg" hreflang="mg" data-title="Kaoka" data-language-autonym="Malagasy" data-language-local-name="malgaščina" class="interlanguage-link-target"><span>Malagasy</span></a></li><li class="interlanguage-link interwiki-mk mw-list-item"><a href="https://mk.wikipedia.org/wiki/%D0%95%D1%80%D0%BE%D0%B7%D0%B8%D1%98%D0%B0" title="Ерозија – makedonščina" lang="mk" hreflang="mk" data-title="Ерозија" data-language-autonym="Македонски" data-language-local-name="makedonščina" class="interlanguage-link-target"><span>Македонски</span></a></li><li class="interlanguage-link interwiki-ml mw-list-item"><a href="https://ml.wikipedia.org/wiki/%E0%B4%AE%E0%B4%A3%E0%B5%8D%E0%B4%A3%E0%B5%8A%E0%B4%B2%E0%B4%BF%E0%B4%AA%E0%B5%8D%E0%B4%AA%E0%B5%8D" title="മണ്ണൊലിപ്പ് – malajalamščina" lang="ml" hreflang="ml" data-title="മണ്ണൊലിപ്പ്" data-language-autonym="മലയാളം" data-language-local-name="malajalamščina" class="interlanguage-link-target"><span>മലയാളം</span></a></li><li class="interlanguage-link interwiki-mr mw-list-item"><a href="https://mr.wikipedia.org/wiki/%E0%A4%95%E0%A5%8D%E0%A4%B7%E0%A4%B0%E0%A4%A3" title="क्षरण – maratščina" lang="mr" hreflang="mr" data-title="क्षरण" data-language-autonym="मराठी" data-language-local-name="maratščina" class="interlanguage-link-target"><span>मराठी</span></a></li><li class="interlanguage-link interwiki-ms mw-list-item"><a href="https://ms.wikipedia.org/wiki/Penghakisan" title="Penghakisan – malajščina" lang="ms" hreflang="ms" data-title="Penghakisan" data-language-autonym="Bahasa Melayu" data-language-local-name="malajščina" class="interlanguage-link-target"><span>Bahasa Melayu</span></a></li><li class="interlanguage-link interwiki-nl mw-list-item"><a href="https://nl.wikipedia.org/wiki/Erosie" title="Erosie – nizozemščina" lang="nl" hreflang="nl" data-title="Erosie" data-language-autonym="Nederlands" data-language-local-name="nizozemščina" class="interlanguage-link-target"><span>Nederlands</span></a></li><li class="interlanguage-link interwiki-nn mw-list-item"><a href="https://nn.wikipedia.org/wiki/Erosjon" title="Erosjon – novonorveščina" lang="nn" hreflang="nn" data-title="Erosjon" data-language-autonym="Norsk nynorsk" data-language-local-name="novonorveščina" class="interlanguage-link-target"><span>Norsk nynorsk</span></a></li><li class="interlanguage-link interwiki-no mw-list-item"><a href="https://no.wikipedia.org/wiki/Erosjon" title="Erosjon – knjižna norveščina" lang="nb" hreflang="nb" data-title="Erosjon" data-language-autonym="Norsk bokmål" data-language-local-name="knjižna norveščina" class="interlanguage-link-target"><span>Norsk bokmål</span></a></li><li class="interlanguage-link interwiki-oc mw-list-item"><a href="https://oc.wikipedia.org/wiki/Erosion" title="Erosion – okcitanščina" lang="oc" hreflang="oc" data-title="Erosion" data-language-autonym="Occitan" data-language-local-name="okcitanščina" class="interlanguage-link-target"><span>Occitan</span></a></li><li class="interlanguage-link interwiki-pa mw-list-item"><a href="https://pa.wikipedia.org/wiki/%E0%A8%96%E0%A9%8B%E0%A8%B0_(%E0%A8%A7%E0%A8%B0%E0%A8%A4_%E0%A8%B5%E0%A8%BF%E0%A8%97%E0%A8%BF%E0%A8%86%E0%A8%A8)" title="ਖੋਰ (ਧਰਤ ਵਿਗਿਆਨ) – pandžabščina" lang="pa" hreflang="pa" data-title="ਖੋਰ (ਧਰਤ ਵਿਗਿਆਨ)" data-language-autonym="ਪੰਜਾਬੀ" data-language-local-name="pandžabščina" class="interlanguage-link-target"><span>ਪੰਜਾਬੀ</span></a></li><li class="interlanguage-link interwiki-pl mw-list-item"><a href="https://pl.wikipedia.org/wiki/Erozja" title="Erozja – poljščina" lang="pl" hreflang="pl" data-title="Erozja" data-language-autonym="Polski" data-language-local-name="poljščina" class="interlanguage-link-target"><span>Polski</span></a></li><li class="interlanguage-link interwiki-pnb mw-list-item"><a href="https://pnb.wikipedia.org/wiki/%DA%A9%DA%BE%D8%A7%D8%B1" title="کھار – Western Punjabi" lang="pnb" hreflang="pnb" data-title="کھار" data-language-autonym="پنجابی" data-language-local-name="Western Punjabi" class="interlanguage-link-target"><span>پنجابی</span></a></li><li class="interlanguage-link interwiki-ps mw-list-item"><a href="https://ps.wikipedia.org/wiki/%D8%AA%D9%88%DA%96%D9%84_%DA%A9%DB%90%D8%AF%D9%86%D9%87_(%D8%AF_%D8%AA%D9%88%DA%96%D9%86%DB%90_%D8%B9%D9%85%D9%84%D9%8A%D9%87)" title="توږل کېدنه (د توږنې عمليه) – paštunščina" lang="ps" hreflang="ps" data-title="توږل کېدنه (د توږنې عمليه)" data-language-autonym="پښتو" data-language-local-name="paštunščina" class="interlanguage-link-target"><span>پښتو</span></a></li><li class="interlanguage-link interwiki-pt mw-list-item"><a href="https://pt.wikipedia.org/wiki/Eros%C3%A3o" title="Erosão – portugalščina" lang="pt" hreflang="pt" data-title="Erosão" data-language-autonym="Português" data-language-local-name="portugalščina" class="interlanguage-link-target"><span>Português</span></a></li><li class="interlanguage-link interwiki-qu mw-list-item"><a href="https://qu.wikipedia.org/wiki/Allpa_chinkari" title="Allpa chinkari – kečuanščina" lang="qu" hreflang="qu" data-title="Allpa chinkari" data-language-autonym="Runa Simi" data-language-local-name="kečuanščina" class="interlanguage-link-target"><span>Runa Simi</span></a></li><li class="interlanguage-link interwiki-rn mw-list-item"><a href="https://rn.wikipedia.org/wiki/Inkukura" title="Inkukura – rundščina" lang="rn" hreflang="rn" data-title="Inkukura" data-language-autonym="Ikirundi" data-language-local-name="rundščina" class="interlanguage-link-target"><span>Ikirundi</span></a></li><li class="interlanguage-link interwiki-ro mw-list-item"><a href="https://ro.wikipedia.org/wiki/Eroziune" title="Eroziune – romunščina" lang="ro" hreflang="ro" data-title="Eroziune" data-language-autonym="Română" data-language-local-name="romunščina" class="interlanguage-link-target"><span>Română</span></a></li><li class="interlanguage-link interwiki-ru mw-list-item"><a href="https://ru.wikipedia.org/wiki/%D0%AD%D1%80%D0%BE%D0%B7%D0%B8%D1%8F" title="Эрозия – ruščina" lang="ru" hreflang="ru" data-title="Эрозия" data-language-autonym="Русский" data-language-local-name="ruščina" class="interlanguage-link-target"><span>Русский</span></a></li><li class="interlanguage-link interwiki-sh mw-list-item"><a href="https://sh.wikipedia.org/wiki/Erozija" title="Erozija – srbohrvaščina" lang="sh" hreflang="sh" data-title="Erozija" data-language-autonym="Srpskohrvatski / српскохрватски" data-language-local-name="srbohrvaščina" class="interlanguage-link-target"><span>Srpskohrvatski / српскохрватски</span></a></li><li class="interlanguage-link interwiki-simple mw-list-item"><a href="https://simple.wikipedia.org/wiki/Erosion" title="Erosion – Simple English" lang="en-simple" hreflang="en-simple" data-title="Erosion" data-language-autonym="Simple English" data-language-local-name="Simple English" class="interlanguage-link-target"><span>Simple English</span></a></li><li class="interlanguage-link interwiki-sk mw-list-item"><a href="https://sk.wikipedia.org/wiki/Er%C3%B3zia" title="Erózia – slovaščina" lang="sk" hreflang="sk" data-title="Erózia" data-language-autonym="Slovenčina" data-language-local-name="slovaščina" class="interlanguage-link-target"><span>Slovenčina</span></a></li><li class="interlanguage-link interwiki-sq mw-list-item"><a href="https://sq.wikipedia.org/wiki/Abrazioni" title="Abrazioni – albanščina" lang="sq" hreflang="sq" data-title="Abrazioni" data-language-autonym="Shqip" data-language-local-name="albanščina" class="interlanguage-link-target"><span>Shqip</span></a></li><li class="interlanguage-link interwiki-sr mw-list-item"><a href="https://sr.wikipedia.org/wiki/%D0%95%D1%80%D0%BE%D0%B7%D0%B8%D1%98%D0%B0" title="Ерозија – srbščina" lang="sr" hreflang="sr" data-title="Ерозија" data-language-autonym="Српски / srpski" data-language-local-name="srbščina" class="interlanguage-link-target"><span>Српски / srpski</span></a></li><li class="interlanguage-link interwiki-sv mw-list-item"><a href="https://sv.wikipedia.org/wiki/Erosion" title="Erosion – švedščina" lang="sv" hreflang="sv" data-title="Erosion" data-language-autonym="Svenska" data-language-local-name="švedščina" class="interlanguage-link-target"><span>Svenska</span></a></li><li class="interlanguage-link interwiki-sw mw-list-item"><a href="https://sw.wikipedia.org/wiki/Mmomonyoko" title="Mmomonyoko – svahili" lang="sw" hreflang="sw" data-title="Mmomonyoko" data-language-autonym="Kiswahili" data-language-local-name="svahili" class="interlanguage-link-target"><span>Kiswahili</span></a></li><li class="interlanguage-link interwiki-ta mw-list-item"><a href="https://ta.wikipedia.org/wiki/%E0%AE%AE%E0%AE%A3%E0%AF%8D%E0%AE%A3%E0%AE%B0%E0%AE%BF%E0%AE%AA%E0%AF%8D%E0%AE%AA%E0%AF%81" title="மண்ணரிப்பு – tamilščina" lang="ta" hreflang="ta" data-title="மண்ணரிப்பு" data-language-autonym="தமிழ்" data-language-local-name="tamilščina" class="interlanguage-link-target"><span>தமிழ்</span></a></li><li class="interlanguage-link interwiki-th mw-list-item"><a href="https://th.wikipedia.org/wiki/%E0%B8%81%E0%B8%B2%E0%B8%A3%E0%B8%81%E0%B8%A3%E0%B9%88%E0%B8%AD%E0%B8%99" title="การกร่อน – tajščina" lang="th" hreflang="th" data-title="การกร่อน" data-language-autonym="ไทย" data-language-local-name="tajščina" class="interlanguage-link-target"><span>ไทย</span></a></li><li class="interlanguage-link interwiki-tl mw-list-item"><a href="https://tl.wikipedia.org/wiki/Erosyon" title="Erosyon – tagalogščina" lang="tl" hreflang="tl" data-title="Erosyon" data-language-autonym="Tagalog" data-language-local-name="tagalogščina" class="interlanguage-link-target"><span>Tagalog</span></a></li><li class="interlanguage-link interwiki-tr mw-list-item"><a href="https://tr.wikipedia.org/wiki/Erozyon" title="Erozyon – turščina" lang="tr" hreflang="tr" data-title="Erozyon" data-language-autonym="Türkçe" data-language-local-name="turščina" class="interlanguage-link-target"><span>Türkçe</span></a></li><li class="interlanguage-link interwiki-uk mw-list-item"><a href="https://uk.wikipedia.org/wiki/%D0%95%D1%80%D0%BE%D0%B7%D1%96%D1%8F" title="Ерозія – ukrajinščina" lang="uk" hreflang="uk" data-title="Ерозія" data-language-autonym="Українська" data-language-local-name="ukrajinščina" class="interlanguage-link-target"><span>Українська</span></a></li><li class="interlanguage-link interwiki-uz mw-list-item"><a href="https://uz.wikipedia.org/wiki/Eroziya" title="Eroziya – uzbeščina" lang="uz" hreflang="uz" data-title="Eroziya" data-language-autonym="Oʻzbekcha / ўзбекча" data-language-local-name="uzbeščina" class="interlanguage-link-target"><span>Oʻzbekcha / ўзбекча</span></a></li><li class="interlanguage-link interwiki-vi mw-list-item"><a href="https://vi.wikipedia.org/wiki/X%C3%B3i_m%C3%B2n" title="Xói mòn – vietnamščina" lang="vi" hreflang="vi" data-title="Xói mòn" data-language-autonym="Tiếng Việt" data-language-local-name="vietnamščina" class="interlanguage-link-target"><span>Tiếng Việt</span></a></li><li class="interlanguage-link interwiki-war mw-list-item"><a href="https://war.wikipedia.org/wiki/Pagtuno" title="Pagtuno – varajščina" lang="war" hreflang="war" data-title="Pagtuno" data-language-autonym="Winaray" data-language-local-name="varajščina" class="interlanguage-link-target"><span>Winaray</span></a></li><li class="interlanguage-link interwiki-wuu mw-list-item"><a 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data-pinned-container-id="vector-appearance-pinned-container" data-unpinned-container-id="vector-appearance-unpinned-container" > <div class="vector-pinnable-header-label">Videz</div> <button class="vector-pinnable-header-toggle-button vector-pinnable-header-pin-button" data-event-name="pinnable-header.vector-appearance.pin">prestavi v stransko letvico</button> <button class="vector-pinnable-header-toggle-button vector-pinnable-header-unpin-button" data-event-name="pinnable-header.vector-appearance.unpin">skrij</button> </div> </div> </div> </nav> </div> </div> <div id="bodyContent" class="vector-body" aria-labelledby="firstHeading" data-mw-ve-target-container> <div class="vector-body-before-content"> <div class="mw-indicators"> </div> <div id="siteSub" class="noprint">Iz Wikipedije, proste enciklopedije</div> </div> <div id="contentSub"><div id="mw-content-subtitle"></div></div> <div id="mw-content-text" class="mw-body-content"><div class="mw-content-ltr mw-parser-output" lang="sl" dir="ltr"><figure typeof="mw:File/Thumb"><a href="/wiki/Slika:Erosion.jpg" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/7/7b/Erosion.jpg/199px-Erosion.jpg" decoding="async" width="199" height="300" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/7/7b/Erosion.jpg/299px-Erosion.jpg 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/7/7b/Erosion.jpg/398px-Erosion.jpg 2x" data-file-width="1769" data-file-height="2670" /></a><figcaption>Erozija prsti</figcaption></figure> <figure typeof="mw:File/Thumb"><a href="/wiki/Slika:NegevWadi2009.JPG" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/4/46/NegevWadi2009.JPG/199px-NegevWadi2009.JPG" decoding="async" width="199" height="149" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/4/46/NegevWadi2009.JPG/299px-NegevWadi2009.JPG 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/4/46/NegevWadi2009.JPG/398px-NegevWadi2009.JPG 2x" data-file-width="4000" data-file-height="3000" /></a><figcaption></figcaption></figure> <p><b>Erozíja</b> je premikanje <a href="/wiki/Prst_(pedologija)" title="Prst (pedologija)">prsti</a> zaradi <a href="/w/index.php?title=Vetrna_erozija&amp;action=edit&amp;redlink=1" class="new" title="Vetrna erozija (stran ne obstaja)">vetra</a>, <a href="/w/index.php?title=Vodna_erozija&amp;action=edit&amp;redlink=1" class="new" title="Vodna erozija (stran ne obstaja)">vode</a>, <a href="/w/index.php?title=Ledeni%C5%A1ka_erozija&amp;action=edit&amp;redlink=1" class="new" title="Ledeniška erozija (stran ne obstaja)">ledu</a>, <a href="/wiki/Gravitacija" class="mw-redirect" title="Gravitacija">gravitacije</a> ali delovanja živih organizmov, ki neprestano spreminja obliko zemeljskega površja. Erozija sledi <a href="/wiki/Denudacija" title="Denudacija">denudaciji</a>, ko se površinsko spiranje spremeni v tokovno, zaradi česar pride do razjedanja in ne več ploskovnega odnašanja površja. Sodi med eksogene površinotvorne procese, saj za razliko od endogenih (npr. vulkanski izbruhi) znižuje zemeljsko površje. Četudi erozija mnogokrat poteka s <a href="/wiki/Preperevanje" title="Preperevanje">preperevanjem</a>, je treba ta pojma razlikovati, saj slednji pomeni razpadanje <a href="/wiki/Kamnina" title="Kamnina">kamnine</a> in nastajanje prsti, prvi pa odnašanje prsti. Erozija je pomemben naravni proces, danes pa je mnogokrat povečan zaradi človekove aktivnosti in kot tak škodljiv; na tak način ga največkrat povzroča krčenje gozdov, prekomerna pašnja in gradnja prometnih poti. Problem erozije človek skuša odpravljati z gradnjo teras in pogozdovanjem. </p><p>Določena stopnja erozije je naravna in pomembna za zdrav <a href="/wiki/Ekosistem" title="Ekosistem">ekosistem</a>. Tako se npr. prod neprestano premika s pomočjo vodnih tokov. Če pa je odnašanje tega preveliko, lahko pride do težav, kot je mašenje tokov, onesnaževanje čistih voda s <a href="/wiki/Sediment" class="mw-redirect" title="Sediment">sedimenti</a> in posledično zmanjševanje kvalitete vode ter rodnosti prsti. </p><p>Znanost o materialih erozijo definira kot odstopanje površinskih materialov zaradi stalnih mehaničnih poškodb, ki jih povzročajo največkrat strgalni (abrazivni) delci v gibajoči se tekočini. </p> <meta property="mw:PageProp/toc" /> <div class="mw-heading mw-heading2"><h2 id="Fizični_procesi"><span id="Fizi.C4.8Dni_procesi"></span>Fizični procesi</h2><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Erozija&amp;veaction=edit&amp;section=1" title="Uredi razdelek: Fizični procesi" class="mw-editsection-visualeditor"><span>uredi</span></a><span class="mw-editsection-divider"> | </span><a href="/w/index.php?title=Erozija&amp;action=edit&amp;section=1" title="Urejanje izvorne kode razdelka: Fizični procesi"><span>uredi kodo</span></a><span class="mw-editsection-bracket">]</span></span></div> <div class="mw-heading mw-heading3"><h3 id="Padavine_in_površinsko_odtekanje"><span id="Padavine_in_povr.C5.A1insko_odtekanje"></span>Padavine in površinsko odtekanje</h3><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Erozija&amp;veaction=edit&amp;section=2" title="Uredi razdelek: Padavine in površinsko odtekanje" class="mw-editsection-visualeditor"><span>uredi</span></a><span class="mw-editsection-divider"> | </span><a href="/w/index.php?title=Erozija&amp;action=edit&amp;section=2" title="Urejanje izvorne kode razdelka: Padavine in površinsko odtekanje"><span>uredi kodo</span></a><span class="mw-editsection-bracket">]</span></span></div> <figure class="mw-default-size mw-halign-right" typeof="mw:File/Thumb"><a href="/wiki/Slika:Water_and_soil_splashed_by_the_impact_of_a_single_raindrop.jpg" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/7/79/Water_and_soil_splashed_by_the_impact_of_a_single_raindrop.jpg/220px-Water_and_soil_splashed_by_the_impact_of_a_single_raindrop.jpg" decoding="async" width="220" height="157" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/7/79/Water_and_soil_splashed_by_the_impact_of_a_single_raindrop.jpg/330px-Water_and_soil_splashed_by_the_impact_of_a_single_raindrop.jpg 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/7/79/Water_and_soil_splashed_by_the_impact_of_a_single_raindrop.jpg/440px-Water_and_soil_splashed_by_the_impact_of_a_single_raindrop.jpg 2x" data-file-width="800" data-file-height="571" /></a><figcaption> Tla in voda brizgata zaradi udarca ene same dežne kaplje</figcaption></figure> <p><a href="/wiki/Padavine" title="Padavine">Padavine</a> in površinsko odtekanje, ki je lahko posledica padavin, povzročajo štiri glavne vrste erozije tal:<sup id="cite_ref-1" class="reference"><a href="#cite_note-1"><span class="cite-bracket">&#91;</span>1<span class="cite-bracket">&#93;</span></a></sup> </p> <figure class="mw-default-size" typeof="mw:File/Thumb"><a href="/wiki/Slika:Rummu_aherainem%C3%A4gi2.jpg" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/7/7b/Rummu_aherainem%C3%A4gi2.jpg/220px-Rummu_aherainem%C3%A4gi2.jpg" decoding="async" width="220" height="77" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/7/7b/Rummu_aherainem%C3%A4gi2.jpg/330px-Rummu_aherainem%C3%A4gi2.jpg 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/7/7b/Rummu_aherainem%C3%A4gi2.jpg/440px-Rummu_aherainem%C3%A4gi2.jpg 2x" data-file-width="8374" data-file-height="2924" /></a><figcaption> Konica plena, ki je zaradi erozijskih procesov, ki jih povzročijo padavine, pokrita z ruševinami in jarki: Rummu, Estonija</figcaption></figure> <ul><li><b>Površinsko spiranje</b> (medžlebična erozija) je posledica dežne erozije in ploskovne erozije površinskega vodnega toka, ki poteka, preden se voda združi v curke in deluje globinsko. Čeprav gre procesno še za <a href="/wiki/Denudacija" title="Denudacija">denudacijo</a>, ga že štejemo k eroziji prsti. Proces brez stalnega merjenja težko opazimo in ovrednotimo, zato njegove učinke pogosto podcenjujemo.</li> <li><b>Žlebična erozija</b> je globinska erozija, pri kateri voda, združena v curke, vrezuje erozijske žlebiče, majhne, največ do 30 cm globoke in več metrov dolge vdolbine v pobočju.</li> <li><b>Jarkovna erozija</b> je globinska erozija, pri kateri z združevanjem erozijskih žlebičev nastajajo več metrov globoki in več deset metrov dolgi erozijski jarki.</li> <li><b>Cevčenje</b> nastane zaradi tokov vode v preperini, ki so vzporedni s pobočjem. Pri tem voda odnaša delce, v preperini nastajajo vedno večji kanali oziroma »cevi«. Ponavadi nastajajo v manj odpornem spodnjem sloju preperine pod bolj stabilnim zgornjim slojem.</li></ul> <div class="mw-heading mw-heading3"><h3 id="Reke_in_potoki">Reke in potoki</h3><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Erozija&amp;veaction=edit&amp;section=3" title="Uredi razdelek: Reke in potoki" class="mw-editsection-visualeditor"><span>uredi</span></a><span class="mw-editsection-divider"> | </span><a href="/w/index.php?title=Erozija&amp;action=edit&amp;section=3" title="Urejanje izvorne kode razdelka: Reke in potoki"><span>uredi kodo</span></a><span class="mw-editsection-bracket">]</span></span></div> <figure class="mw-default-size" typeof="mw:File/Thumb"><a href="/wiki/Slika:Dobbingstone_Burn_-_geograph.org.uk_-_1291882.jpg" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/a/a4/Dobbingstone_Burn_-_geograph.org.uk_-_1291882.jpg/220px-Dobbingstone_Burn_-_geograph.org.uk_-_1291882.jpg" decoding="async" width="220" height="146" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/a/a4/Dobbingstone_Burn_-_geograph.org.uk_-_1291882.jpg/330px-Dobbingstone_Burn_-_geograph.org.uk_-_1291882.jpg 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/a/a4/Dobbingstone_Burn_-_geograph.org.uk_-_1291882.jpg/440px-Dobbingstone_Burn_-_geograph.org.uk_-_1291882.jpg 2x" data-file-width="640" data-file-height="426" /></a><figcaption> Dobbingstone Burn na Škotskem, ki prikazuje dve različni vrsti erozije, ki vplivata na isto mesto. Erozija doline se pojavi zaradi toka toka, balvani in kamni (ter velik del zemlje), ki ležijo na bregovih potoka, so ledeniški, dokler to ni ostalo, ko so ledeniki v ledeni dobi tekli po terenu.</figcaption></figure> <figure class="mw-default-size" typeof="mw:File/Thumb"><a href="/wiki/Slika:Tauglbach_4.JPG" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/a/ae/Tauglbach_4.JPG/220px-Tauglbach_4.JPG" decoding="async" width="220" height="165" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/a/ae/Tauglbach_4.JPG/330px-Tauglbach_4.JPG 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/a/ae/Tauglbach_4.JPG/440px-Tauglbach_4.JPG 2x" data-file-width="5152" data-file-height="3864" /></a><figcaption> Plasti krede, ki jih razkrije reka, ki teče skozi njih</figcaption></figure> <p>Erozija doline ali toka se pojavi z neprekinjenim pretokom vode vzdolž linearne značilnosti. Erozija je navzdol, poglablja dolino in navzgor, razteza dolino v pobočje, ustvarja prereze in strme brežine. V najzgodnejši fazi erozije potoka je erozivna aktivnost pretežno navpična, doline imajo značilen prerez v obliki črke V, naklon toka je razmeroma strm. Ko je dosežena določena osnovna raven, se erozivna aktivnost preklopi na stransko erozijo, ki razširi dno doline in ustvari ozko poplavno ravnico. Naklon toka postane minimalen, stransko odlaganje sedimentov pa postane pomembno, saj tok vijuga po dnu doline. Na vseh stopnjah erozije potoka se daleč največ erozije pojavi v času poplav, ko je na voljo več in hitreje tekoče vode za prenašanje večje obremenitve sedimenta. V takih procesih ne erodira samo voda: suspendirani abrazivni delci, kamenčki in skale lahko delujejo tudi erozivno, ko prečkajo površino.<sup id="cite_ref-2" class="reference"><a href="#cite_note-2"><span class="cite-bracket">&#91;</span>2<span class="cite-bracket">&#93;</span></a></sup> </p><p>Erozija brega je obraba bregov potoka ali reke. To se razlikuje od sprememb na strugi vodotoka. Erozijo in spremembe v obliki rečnih bregov je mogoče izmeriti.<sup id="cite_ref-3" class="reference"><a href="#cite_note-3"><span class="cite-bracket">&#91;</span>3<span class="cite-bracket">&#93;</span></a></sup> </p><p>Toplotna erozija je posledica taljenja in slabljenja <a href="/wiki/Permafrost" title="Permafrost">permafrosta</a> zaradi premikanja vode.<sup id="cite_ref-nsidc_thermal_4-0" class="reference"><a href="#cite_note-nsidc_thermal-4"><span class="cite-bracket">&#91;</span>4<span class="cite-bracket">&#93;</span></a></sup> Lahko se pojavi tako ob rekah kot ob obali. Hitra migracija rečnih kanalov, opažena v reki <a href="/wiki/Lena" title="Lena">Leni</a> v <a href="/wiki/Sibirija" title="Sibirija">Sibiriji</a>, je posledica toplotne erozije, saj so ti deli brežin sestavljeni iz nekoherentnih materialov, ki so sprijeti z večno zmrzaljo.<sup id="cite_ref-lena_5-0" class="reference"><a href="#cite_note-lena-5"><span class="cite-bracket">&#91;</span>5<span class="cite-bracket">&#93;</span></a></sup> Velik del te erozije se pojavi, ko oslabljeni bregovi propadajo v velikih kosih. Toplotna erozija vpliva tudi na arktično obalo, kjer se delovanje valov in temperature ob obali združujejo, prekinejo permafrost ob obali in povzročijo njihov propad. Letne stopnje erozije vzdolž 100-kilometrskega odseka obale Beaufortovega morja so bile v povprečju 5,6 metra na leto od leta 1955 do 2002.<sup id="cite_ref-jones_arctic_6-0" class="reference"><a href="#cite_note-jones_arctic-6"><span class="cite-bracket">&#91;</span>6<span class="cite-bracket">&#93;</span></a></sup> </p><p>Večina rečne erozije se zgodi bližje ustju reke. Na rečnem ovinku ima najdaljša najmanj ostra stran počasnejšo tekočo vodo. Tu se nabirajo depoziti. Na najožji ostri strani ovinka je hitreje premikajoča se voda, zato ta stran večinoma izgineva. </p><p>Hitra erozija velike reke lahko odstrani dovolj sedimentov, da nastane rečna antiklinala, saj izostatični odboj dvigne kamnine, neobremenjene z erozijo prekrivnih strug. </p> <div class="mw-heading mw-heading3"><h3 id="Obalna_erozija">Obalna erozija</h3><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Erozija&amp;veaction=edit&amp;section=4" title="Uredi razdelek: Obalna erozija" class="mw-editsection-visualeditor"><span>uredi</span></a><span class="mw-editsection-divider"> | </span><a href="/w/index.php?title=Erozija&amp;action=edit&amp;section=4" title="Urejanje izvorne kode razdelka: Obalna erozija"><span>uredi kodo</span></a><span class="mw-editsection-bracket">]</span></span></div> <dl><dd><div class="noprint relarticle mainarticle"><i>Glavni članek&#58; <a href="/w/index.php?title=Obalna_erozija&amp;action=edit&amp;redlink=1" class="new" title="Obalna erozija (stran ne obstaja)">Obalna erozija</a>.</i></div></dd></dl> <figure class="mw-default-size" typeof="mw:File/Thumb"><a href="/wiki/Slika:Wavecut_platform_southerndown_pano.jpg" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/6/63/Wavecut_platform_southerndown_pano.jpg/220px-Wavecut_platform_southerndown_pano.jpg" decoding="async" width="220" height="110" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/6/63/Wavecut_platform_southerndown_pano.jpg/330px-Wavecut_platform_southerndown_pano.jpg 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/6/63/Wavecut_platform_southerndown_pano.jpg/440px-Wavecut_platform_southerndown_pano.jpg 2x" data-file-width="2393" data-file-height="1200" /></a><figcaption>Valovita ploščad, ki jo je povzročila erozija pečin ob morju, v Southerndownu v Južnem Walesu</figcaption></figure> <figure class="mw-default-size" typeof="mw:File/Thumb"><a href="/wiki/Slika:Erosion_of_Boulder_Clay_in_Filey_Bay.JPG" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/6/67/Erosion_of_Boulder_Clay_in_Filey_Bay.JPG/220px-Erosion_of_Boulder_Clay_in_Filey_Bay.JPG" decoding="async" width="220" height="147" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/6/67/Erosion_of_Boulder_Clay_in_Filey_Bay.JPG/330px-Erosion_of_Boulder_Clay_in_Filey_Bay.JPG 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/6/67/Erosion_of_Boulder_Clay_in_Filey_Bay.JPG/440px-Erosion_of_Boulder_Clay_in_Filey_Bay.JPG 2x" data-file-width="3872" data-file-height="2592" /></a><figcaption> Erozija balvanske gline (pleistocenske starosti) vzdolž klifov v zalivu Filey, Yorkshire, Anglija</figcaption></figure> <p>Erozija obale, ki se pojavlja tako na izpostavljeni kot na zaščiteni obali, se pojavi predvsem zaradi delovanja morskih tokov in valov, vendar lahko igrajo vlogo tudi spremembe morske gladine (<a href="/wiki/Plimovanje" class="mw-redirect" title="Plimovanje">plimovanje</a>). </p> <figure class="mw-default-size" typeof="mw:File/Thumb"><span><video id="mwe_player_0" poster="//upload.wikimedia.org/wikipedia/commons/thumb/2/24/Sea_dune_Erosion_at_Talace%2C_Wales.webm/220px--Sea_dune_Erosion_at_Talace%2C_Wales.webm.jpg" controls="" preload="none" data-mw-tmh="" class="mw-file-element" width="220" height="124" data-durationhint="61" data-mwtitle="Sea_dune_Erosion_at_Talace,_Wales.webm" data-mwprovider="wikimediacommons" resource="/wiki/Slika:Sea_dune_Erosion_at_Talace,_Wales.webm"><source src="//upload.wikimedia.org/wikipedia/commons/transcoded/2/24/Sea_dune_Erosion_at_Talace%2C_Wales.webm/Sea_dune_Erosion_at_Talace%2C_Wales.webm.360p.vp9.webm" type="video/webm; codecs=&quot;vp9, opus&quot;" data-transcodekey="360p.vp9.webm" data-width="640" data-height="360" /><source src="//upload.wikimedia.org/wikipedia/commons/transcoded/2/24/Sea_dune_Erosion_at_Talace%2C_Wales.webm/Sea_dune_Erosion_at_Talace%2C_Wales.webm.360p.webm" type="video/webm; codecs=&quot;vp8, vorbis&quot;" data-transcodekey="360p.webm" data-width="640" data-height="360" /><source src="//upload.wikimedia.org/wikipedia/commons/2/24/Sea_dune_Erosion_at_Talace%2C_Wales.webm" type="video/webm; codecs=&quot;vp8, vorbis&quot;" data-width="640" data-height="360" /><source src="//upload.wikimedia.org/wikipedia/commons/transcoded/2/24/Sea_dune_Erosion_at_Talace%2C_Wales.webm/Sea_dune_Erosion_at_Talace%2C_Wales.webm.240p.vp9.webm" type="video/webm; codecs=&quot;vp9, opus&quot;" data-transcodekey="240p.vp9.webm" data-width="426" data-height="240" /></video></span><figcaption> Erozija morskih sipin na plaži Talacre v Walesu</figcaption></figure> <p>Valovanje je najučinkovitejša in najhitrejša oblika erozije obale (ne smemo je zamenjati s <a href="/w/index.php?title=Korozija_(geologija)&amp;action=edit&amp;redlink=1" class="new" title="Korozija (geologija) (stran ne obstaja)">korozijo</a>, ki je raztapljanje kamnine z ogljikovo kislino v morski vodi). Ko se pojavlja na obalah z malo skalami, je erozija veliko bolj izrazita in hitra. Kadar je en material na majhnem območju mehkejši od drugega, najdemo oblike kot so vodnjaki, rovi ali naravna pula. </p><p>Drug pomemben vir erozije, zlasti na karbonatnih obalah, je dolgotrajno strganje in mletje organizmov, postopek, imenovan bioerozija. </p><p>Valovi so elementi, ki neprekinjeno proizvajajo kompresijski in dekompresijski učinek, kar povzroča sesalni učinek in propad obale. Podvodni tok vala ustvarja spodnje tokove, to je gibanje, pravokotno na tok obale. Tokovi lahko povzročijo vzporedno gibanje, ko valovi udarijo poševno na obale. Razlika med plimo in oseko tudi povzroča nepravilne tokove. </p><p>Sediment se prevaža vzdolž obale v smeri prevladujočega toka. Ko je dotok sedimenta manjši od količine odnesene, pride do erozije. Ko je tekoča količina sedimenta večja, se bodo zaradi usedanja nakopičile peščene ali gramozne brežine. Ti bregovi se lahko počasi selijo vzdolž obale v smeri priobalja, izmenično ščitijo in izpostavljajo dele obale. Kjer je na obali ovinek, se pogosto pojavi kopičenje erodiranega materiala, ki tvori dolg ozek breg (rtič, napodalo, kosa). Oklepljene plaže in potopljene obale na morju lahko zaščitijo tudi dele obale pred erozijo. Z leti, ko se plitvine postopoma premikajo, se lahko erozija preusmeri na različne dele obale.<sup id="cite_ref-7" class="reference"><a href="#cite_note-7"><span class="cite-bracket">&#91;</span>7<span class="cite-bracket">&#93;</span></a></sup> </p><p>Erozija obalne površine, ki ji sledi padec gladine morja, lahko povzroči značilno obliko reljefa, imenovano dvignjena plaža.<sup id="cite_ref-Pinter2010_8-0" class="reference"><a href="#cite_note-Pinter2010-8"><span class="cite-bracket">&#91;</span>8<span class="cite-bracket">&#93;</span></a></sup> </p> <div class="mw-heading mw-heading3"><h3 id="Kemična_erozija"><span id="Kemi.C4.8Dna_erozija"></span>Kemična erozija</h3><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Erozija&amp;veaction=edit&amp;section=5" title="Uredi razdelek: Kemična erozija" class="mw-editsection-visualeditor"><span>uredi</span></a><span class="mw-editsection-divider"> | </span><a href="/w/index.php?title=Erozija&amp;action=edit&amp;section=5" title="Urejanje izvorne kode razdelka: Kemična erozija"><span>uredi kodo</span></a><span class="mw-editsection-bracket">]</span></span></div> <dl><dd><div class="noprint relarticle mainarticle"><i>Glavni članek&#58; <a href="/wiki/Kras" title="Kras">Kras</a>.</i></div></dd></dl> <p>Kemična erozija je izguba snovi v pokrajini v obliki topljenja. Kemična erozija se običajno izračuna iz raztopin v potokih. Anders Rapp je pionir v študiji kemijske erozije v svojem delu o Kärkevaggeju, objavljenem leta 1960.<sup id="cite_ref-9" class="reference"><a href="#cite_note-9"><span class="cite-bracket">&#91;</span>9<span class="cite-bracket">&#93;</span></a></sup> </p><p>Nastanek vrtač in druge značilnosti kraške topografije je primer skrajne kemične erozije.<sup id="cite_ref-10" class="reference"><a href="#cite_note-10"><span class="cite-bracket">&#91;</span>10<span class="cite-bracket">&#93;</span></a></sup> </p> <div class="mw-heading mw-heading3"><h3 id="Ledeniki">Ledeniki</h3><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Erozija&amp;veaction=edit&amp;section=6" title="Uredi razdelek: Ledeniki" class="mw-editsection-visualeditor"><span>uredi</span></a><span class="mw-editsection-divider"> | </span><a href="/w/index.php?title=Erozija&amp;action=edit&amp;section=6" title="Urejanje izvorne kode razdelka: Ledeniki"><span>uredi kodo</span></a><span class="mw-editsection-bracket">]</span></span></div> <figure class="mw-default-size mw-halign-left" typeof="mw:File/Thumb"><a href="/wiki/Slika:Pirunpes%C3%A4_Jalasj%C3%A4rvi_8.JPG" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/8/81/Pirunpes%C3%A4_Jalasj%C3%A4rvi_8.JPG/220px-Pirunpes%C3%A4_Jalasj%C3%A4rvi_8.JPG" decoding="async" width="220" height="146" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/8/81/Pirunpes%C3%A4_Jalasj%C3%A4rvi_8.JPG/330px-Pirunpes%C3%A4_Jalasj%C3%A4rvi_8.JPG 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/8/81/Pirunpes%C3%A4_Jalasj%C3%A4rvi_8.JPG/440px-Pirunpes%C3%A4_Jalasj%C3%A4rvi_8.JPG 2x" data-file-width="3584" data-file-height="2376" /></a><figcaption> Hudičevo gnezdo (Pirunpesä), najgloblja erozija tal v Evropi, v Jalasjärviju, Kurikka, Finska<sup id="cite_ref-11" class="reference"><a href="#cite_note-11"><span class="cite-bracket">&#91;</span>11<span class="cite-bracket">&#93;</span></a></sup></figcaption></figure> <figure class="mw-default-size mw-halign-right" typeof="mw:File/Thumb"><a href="/wiki/Slika:MorainesLakeLouise.JPG" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/7/7d/MorainesLakeLouise.JPG/220px-MorainesLakeLouise.JPG" decoding="async" width="220" height="158" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/7/7d/MorainesLakeLouise.JPG/330px-MorainesLakeLouise.JPG 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/7/7d/MorainesLakeLouise.JPG/440px-MorainesLakeLouise.JPG 2x" data-file-width="4000" data-file-height="2874" /></a><figcaption> Ledeniška morena nad jezerom Louise v Alberti v Kanadi</figcaption></figure> <p>Ledeniki razjedajo predvsem s tremi različnimi procesi: drgnjenjem, trganjem in prebijanjem. V procesu drgnjenja ostanki v bazalnem ledu strgajo po postelji, polirajo in izkopavajo spodnje kamnine, podobno kot brusni papir na lesu. Znanstveniki so pokazali, da poleg vloge temperature pri poglabljanju doline tudi drugi glaciološki procesi, kot je erozija, nadzorujejo razlike med dolinami. V homogenem vzorcu erozije temeljnih kamnin nastane ukrivljen prerez kanala pod ledom. Čeprav ledenik še naprej brusi navpično, oblika kanala pod ledom sčasoma ostane konstantna in doseže parabolično ustaljeno stanje v obliki črke U, kot ga vidimo v <a href="/wiki/Ledeni%C5%A1ka_dolina" title="Ledeniška dolina">ledeniških dolinah</a>. Znanstveniki ponujajo tudi numerično oceno časa, ki je potreben za dokončno oblikovanje enakomerno oblikovane doline v obliki črke U-približno 100.000 let. V šibki podlagi (ki vsebuje material, ki je bolj erodibilen od okoliških kamnin), je vzorec erozije nasproten, količina prekomernega poglabljanja je omejena, ker se zmanjšajo hitrosti ledu in stopnje erozije. </p><p>Ledeniki lahko povzročijo tudi razpoke kosov podlage v procesu trganja. Pri vdoru ledu ledenik zmrzne do svoje struge, nato pa, ko se premakne naprej, premakne velike kose zamrznjene usedline na dnu skupaj z ledom. Ta metoda je ustvarila nekaj od tisočih jezerskih kotlin, ki se nahajajo na robu <a href="/w/index.php?title=Kanadski_%C5%A1%C4%8Dit&amp;action=edit&amp;redlink=1" class="new" title="Kanadski ščit (stran ne obstaja)">Kanadskega ščita</a>. Razlike v višini gorskih verig niso le posledica tektonskih sil, kot je dviganje kamnin, ampak tudi lokalne podnebne spremembe. Znanstveniki z globalno analizo topografije dokazujejo, da ledeniška erozija nadzoruje največjo višino gora, saj je relief med gorskimi vrhovi in snežno mejo na splošno omejen na nadmorske višine manj kot 1500 m.<sup id="cite_ref-12" class="reference"><a href="#cite_note-12"><span class="cite-bracket">&#91;</span>12<span class="cite-bracket">&#93;</span></a></sup> Erozija, ki jo povzročajo ledeniki po vsem svetu, tako močno razjeda gore, da se je izraz <i>ledeniška žaga</i> močno razširil, kar opisuje omejevalni učinek ledenikov na višino gorskih verig.<sup id="cite_ref-reference_13-0" class="reference"><a href="#cite_note-reference-13"><span class="cite-bracket">&#91;</span>13<span class="cite-bracket">&#93;</span></a></sup> Ker gore rastejo višje, na splošno omogočajo večjo ledeniško aktivnost (zlasti v akumulacijskem območju nad višino črte ledeniškega ravnovesja), kar povzroča povečano stopnjo erozije gore, in zmanjšuje maso hitreje, kot lahko izostatični odboj povzroči goro.<sup id="cite_ref-14" class="reference"><a href="#cite_note-14"><span class="cite-bracket">&#91;</span>14<span class="cite-bracket">&#93;</span></a></sup> To je dober primer zanke negativnih povratnih zank. Tekoče raziskave kažejo, da lahko ledeniki na nekaterih območjih zmanjšujejo velikost gora, na nekaterih območjih pa ledeniki dejansko lahko zmanjšajo stopnjo erozije in delujejo kot ledeniški oklep. Led ne le lahko uniči gore, ampak jih tudi zaščiti pred erozijo. Odvisno od ledeniškega režima se lahko s pomočjo ledu skozi čas ohranijo tudi strme alpske dežele. Znanstveniki so to teorijo dokazali z vzorčenjem osmih vrhov severozahodnega <a href="/wiki/Svalbard" title="Svalbard">Svalbarda</a> z uporabo Be10 in Al26, ki so pokazali, da se je severozahodni Svalbard preoblikoval iz stanja erozije ledenika pod razmeroma blagimi ledeniškimi maksimumi v stanje ledeniškega oklepa v hladnem zaščitnem ledu, med precej hladnejše ledeniške maksimalne temperature z napredovanjem kvartarne ledene dobe.<sup id="cite_ref-15" class="reference"><a href="#cite_note-15"><span class="cite-bracket">&#91;</span>15<span class="cite-bracket">&#93;</span></a></sup> </p><p>Ti procesi, skupaj z erozijo in transportom po vodnem omrežju pod ledenikom, za seboj puščajo ledeniške oblike, kot so <a href="/wiki/Morena" title="Morena">morene</a>, <a href="/w/index.php?title=Ledeni%C5%A1ki_nanos&amp;action=edit&amp;redlink=1" class="new" title="Ledeniški nanos (stran ne obstaja)">drumlini</a>, prizemne morene ali tili, <a href="/wiki/Balvan" title="Balvan">balvani</a>, običajno na koncu ali med umikom ledenika.<sup id="cite_ref-16" class="reference"><a href="#cite_note-16"><span class="cite-bracket">&#91;</span>16<span class="cite-bracket">&#93;</span></a></sup> </p><p>Morda je najbolje razvita morfologija ledeniške doline omejena na pokrajine z nizkimi stopnjami dviganja kamnin (manjše ali enake 2 mm na leto) in visokim reliefom, kar vodi do dolgih obratov. Kjer stopnje dviganja kamnin presegajo 2 mm na leto, se je morfologija ledeniške doline v postglacialnem času na splošno bistveno spremenila. Medsebojno vplivanje ledeniške erozije in tektonskega narivanja ureja morfološki vpliv poledenitev na aktivne orogene tako z vplivom na njihovo višino kot s spreminjanjem vzorcev erozije v naslednjih ledeniških obdobjih prek povezave med dvigovanjem kamnin in obliko preseka doline.<sup id="cite_ref-17" class="reference"><a href="#cite_note-17"><span class="cite-bracket">&#91;</span>17<span class="cite-bracket">&#93;</span></a></sup> </p> <div class="mw-heading mw-heading3"><h3 id="Poplave">Poplave</h3><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Erozija&amp;veaction=edit&amp;section=7" title="Uredi razdelek: Poplave" class="mw-editsection-visualeditor"><span>uredi</span></a><span class="mw-editsection-divider"> | </span><a href="/w/index.php?title=Erozija&amp;action=edit&amp;section=7" title="Urejanje izvorne kode razdelka: Poplave"><span>uredi kodo</span></a><span class="mw-editsection-bracket">]</span></span></div> <figure class="mw-default-size" typeof="mw:File/Thumb"><a href="/wiki/Slika:Seaton_Beach_after_heavy_rainfall.jpg" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/d/d1/Seaton_Beach_after_heavy_rainfall.jpg/220px-Seaton_Beach_after_heavy_rainfall.jpg" decoding="async" width="220" height="99" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/d/d1/Seaton_Beach_after_heavy_rainfall.jpg/330px-Seaton_Beach_after_heavy_rainfall.jpg 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/d/d1/Seaton_Beach_after_heavy_rainfall.jpg/440px-Seaton_Beach_after_heavy_rainfall.jpg 2x" data-file-width="4000" data-file-height="1800" /></a><figcaption> Ustje reke Seaton v <a href="/wiki/Cornwall" title="Cornwall">Cornwallu</a> je po močnih padavinah povzročilo poplave in erozijo znatne količine plaže; za seboj pusti visoko peščeno brežino</figcaption></figure> <p>Pri izredno visokih pretokih zaradi velikih količin hitro tekoče vode nastajajo podvodni vrtinci ali kolki. Kolki povzročajo ekstremno lokalno erozijo, trgajo podlago in ustvarjajo geografske značilnosti, ki se imenujejo skalna korita. Primeri v poplavnih regijah so posledica ledeniškega <a href="/w/index.php?title=Jezero_Missoula&amp;action=edit&amp;redlink=1" class="new" title="Jezero Missoula (stran ne obstaja)">jezera Missoula</a>, ki je ustvarilo globoke kanale v <a href="/wiki/Pore%C4%8Dje" title="Porečje">porečju</a> reke Columbia na vzhodu države <a href="/wiki/Washington_(zvezna_dr%C5%BEava)" title="Washington (zvezna država)">Washington</a>.<sup id="cite_ref-18" class="reference"><a href="#cite_note-18"><span class="cite-bracket">&#91;</span>18<span class="cite-bracket">&#93;</span></a></sup> </p> <div class="mw-heading mw-heading3"><h3 id="Vetrna_erozija">Vetrna erozija</h3><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Erozija&amp;veaction=edit&amp;section=8" title="Uredi razdelek: Vetrna erozija" class="mw-editsection-visualeditor"><span>uredi</span></a><span class="mw-editsection-divider"> | </span><a href="/w/index.php?title=Erozija&amp;action=edit&amp;section=8" title="Urejanje izvorne kode razdelka: Vetrna erozija"><span>uredi kodo</span></a><span class="mw-editsection-bracket">]</span></span></div> <figure class="mw-default-size" typeof="mw:File/Thumb"><a href="/wiki/Slika:Im_Salar_de_Uyuni.jpg" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/0/09/Im_Salar_de_Uyuni.jpg/220px-Im_Salar_de_Uyuni.jpg" decoding="async" width="220" height="163" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/0/09/Im_Salar_de_Uyuni.jpg/330px-Im_Salar_de_Uyuni.jpg 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/0/09/Im_Salar_de_Uyuni.jpg/440px-Im_Salar_de_Uyuni.jpg 2x" data-file-width="2080" data-file-height="1544" /></a><figcaption> Árbol de Piedra, kamnita formacija v Altiplanu v Boliviji, ki jo je izklesala vetrna erozija</figcaption></figure> <dl><dd><div class="noprint relarticle mainarticle"><i>Glavni članek&#58; <a href="/wiki/Eolsko_delovanje" title="Eolsko delovanje">Eolsko delovanje</a>.</i></div></dd></dl> <p>Vetrna erozija je glavna <a href="/wiki/Geomorfologija" title="Geomorfologija">geomorfološka</a> sila, zlasti v <a href="/wiki/Aridna_klima" title="Aridna klima">sušnih</a> in polsušnih območjih. Je tudi glavni vir degradacije tal, izhlapevanja, dezertifikacije, škodljivega prahu v zraku in poškodb pridelkov - še posebej potem, ko so se s človeškimi dejavnostmi, kot so <a href="/wiki/Kr%C4%8Denje_gozdov" title="Krčenje gozdov">krčenje gozdov</a>, <a href="/wiki/Urbanizacija" title="Urbanizacija">urbanizacija</a> in <a href="/wiki/Kmetijstvo" title="Kmetijstvo">kmetijstvo</a>, te znatno povečale nad naravnimi stopnjami.<sup id="cite_ref-19" class="reference"><a href="#cite_note-19"><span class="cite-bracket">&#91;</span>19<span class="cite-bracket">&#93;</span></a></sup><sup id="cite_ref-20" class="reference"><a href="#cite_note-20"><span class="cite-bracket">&#91;</span>20<span class="cite-bracket">&#93;</span></a></sup> </p><p>Vetrna erozija je dveh glavnih vrst: deflacija, kjer veter pobere in odnese ohlapne delce; in <a href="/wiki/Abrazija" class="mw-disambig" title="Abrazija">abrazija</a>, kjer se površine obrabijo, ko jih udarijo delci v zraku, ki jih prenaša veter. Deflacija je razdeljena v tri kategorije: (1) površinsko plazenje, kjer večji, težji delci drsijo ali se valjajo po tleh; (2) <a href="/wiki/Saltacija_(geologija)" title="Saltacija (geologija)">saltacija</a>, pri katerem se delci velikosti s premerom približno 0,1 do 0,5 mm dvignejo le nekoliko v zrak in odbijajo ter saltirajo po površini tal; in (3) <a href="/wiki/Suspenzija" title="Suspenzija">suspenzija</a>, pri kateri veter zelo majhne in lahke delce dvigne v zrak in jih pogosto nosi na dolge razdalje. Salatacija je odgovorna za večino (50-70&#160;%) vetrne erozije, ki ji sledi suspenzija (30-40&#160;%), nato pa površinsko plazenje (5-25&#160;%).<sup id="cite_ref-BlancoWind_21-0" class="reference"><a href="#cite_note-BlancoWind-21"><span class="cite-bracket">&#91;</span>21<span class="cite-bracket">&#93;</span></a></sup> </p><p>Vetrna erozija je v sušnih območjih in v sušnih obdobjih veliko hujša. Na primer na velikih ravnicah je ocenjeno, da je izguba tal zaradi vetrne erozije lahko v sušnih letih kar 6100-krat večja kot v mokrih letih.<sup id="cite_ref-22" class="reference"><a href="#cite_note-22"><span class="cite-bracket">&#91;</span>22<span class="cite-bracket">&#93;</span></a></sup> </p> <div class="mw-heading mw-heading3"><h3 id="Plazovi">Plazovi</h3><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Erozija&amp;veaction=edit&amp;section=9" title="Uredi razdelek: Plazovi" class="mw-editsection-visualeditor"><span>uredi</span></a><span class="mw-editsection-divider"> | </span><a href="/w/index.php?title=Erozija&amp;action=edit&amp;section=9" title="Urejanje izvorne kode razdelka: Plazovi"><span>uredi kodo</span></a><span class="mw-editsection-bracket">]</span></span></div> <figure class="mw-default-size" typeof="mw:File/Thumb"><a href="/wiki/Slika:NegevWadi2009.JPG" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/4/46/NegevWadi2009.JPG/220px-NegevWadi2009.JPG" decoding="async" width="220" height="165" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/4/46/NegevWadi2009.JPG/330px-NegevWadi2009.JPG 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/4/46/NegevWadi2009.JPG/440px-NegevWadi2009.JPG 2x" data-file-width="4000" data-file-height="3000" /></a><figcaption> Wadi v izraelskem Makhtesh Ramonu, ki na svojih bregovih prikazuje erozijo gravitacijskega kolapsa</figcaption></figure> <p><a href="/wiki/Zemeljski_plaz" title="Zemeljski plaz">Zemeljski plaz</a> je gibanje kamnin in usedlin navzdol in navzven po nagnjeni površini, predvsem zaradi sile teže. </p><p>Plaz je pomemben del erozijskega procesa in je pogosto prva stopnja pri razgradnji in transportu preperelih materialov v gorskih območjih. Je premik materiala z višjih nadmorskih višin na nižje, kjer druga erozivna sredstva, kot so tokovi in ledeniki lahko nato poberejo material in ga premaknejo na še nižje višine. Procesi plazov se vedno pojavljajo neprekinjeno na vseh pobočjih; nekateri procesi delujejo zelo počasi; drugi se pojavijo zelo nenadoma, pogosto s katastrofalnimi posledicami. Plazove je mogoče razvrstiti na veliko bolj podroben način, ki odraža mehanizme, ki so odgovorni za gibanje in hitrost, s katero se gibanje zgodi. Ena od vidnih topografskih manifestacij zelo počasne oblike takšne dejavnosti je <a href="/wiki/Meli%C5%A1%C4%8De" title="Melišče">melišče</a>. </p><p>Plazenje oziroma rušenje se dogaja na strmih pobočjih, ki se pojavljajo vzdolž različnih lomnih območij, pogosto v materialih, kot je glina, ki se lahko, ko se sprostijo, precej hitro premikajo navzdol. Pogosto bodo prikazovali izostatično vdolbino v obliki žlice, pri kateri je material začel drseti navzdol. V nekaterih primerih pride do padca zaradi vode pod pobočjem, ki ga oslabi. V mnogih primerih je to preprosto posledica slabega inženiringa ob cestah, kjer se to redno dogaja.<sup id="cite_ref-P.2007_23-0" class="reference"><a href="#cite_note-P.2007-23"><span class="cite-bracket">&#91;</span>23<span class="cite-bracket">&#93;</span></a></sup> </p><p>Površinsko plazenje je počasno premikanje tal in skalnih ostankov pod vplivom gravitacije, ki jih običajno ni mogoče zaznati, razen z daljšim opazovanjem. Vendar pa izraz lahko opiše tudi valjanje delcev tal s premerom 0,5 do 1,0 mm z vetrom po površini tal. </p> <div class="mw-heading mw-heading2"><h2 id="Sklici">Sklici</h2><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Erozija&amp;veaction=edit&amp;section=10" title="Uredi razdelek: Sklici" class="mw-editsection-visualeditor"><span>uredi</span></a><span class="mw-editsection-divider"> | </span><a href="/w/index.php?title=Erozija&amp;action=edit&amp;section=10" title="Urejanje izvorne kode razdelka: Sklici"><span>uredi kodo</span></a><span class="mw-editsection-bracket">]</span></span></div> <div class="reflist columns references-column-width" style="column-width: 30em; list-style-type: decimal;"> <ol class="references"> <li id="cite_note-1"><span class="mw-cite-backlink"><a href="#cite_ref-1">↑</a></span> <span class="reference-text">Blaž Komac <i>Erozija tal</i><a rel="nofollow" class="external autonumber" href="https://giam.zrc-sazu.si/sites/default/files/komac_erozija_v_sloveniji.pdf">[1]</a>, Geografski inštitut Antona Melika, 2012</span> </li> <li id="cite_note-2"><span class="mw-cite-backlink"><a href="#cite_ref-2">↑</a></span> <span class="reference-text">Ritter, Michael E. (2006) <a rel="nofollow" class="external text" href="http://www4.uwsp.edu/geo/faculty/ritter/geog101/textbook/fluvial_systems/geologic_work_of_streams.html">"Geologic Work of Streams"</a> <a rel="nofollow" class="external text" href="https://web.archive.org/web/20120506040721/http://www4.uwsp.edu/geo/faculty/ritter/geog101/textbook/fluvial_systems/geologic_work_of_streams.html">Arhivirano</a> 2012-05-06 na <a href="/wiki/Wayback_Machine" title="Wayback Machine">Wayback Machine</a>. <i>The Physical Environment: an Introduction to Physical Geography</i> University of Wisconsin, <a href="/wiki/Online_Computer_Library_Center" title="Online Computer Library Center">OCLC</a> <a rel="nofollow" class="external text" href="http://www.worldcat.org/oclc/79006225">79006225</a></span> </li> <li id="cite_note-3"><span class="mw-cite-backlink"><a href="#cite_ref-3">↑</a></span> <span class="reference-text"><style data-mw-deduplicate="TemplateStyles:r5980307">.mw-parser-output cite.citation{font-style:inherit;word-wrap:break-word}.mw-parser-output .citation q{quotes:"»""«""›""‹"}.mw-parser-output .citation:target{background-color:rgba(0,127,255,0.133)}.mw-parser-output .id-lock-free a,.mw-parser-output .citation .cs1-lock-free a{background:url("//upload.wikimedia.org/wikipedia/commons/6/65/Lock-green.svg")right 0.1em center/9px no-repeat}.mw-parser-output .id-lock-limited a,.mw-parser-output .id-lock-registration a,.mw-parser-output .citation .cs1-lock-limited a,.mw-parser-output .citation .cs1-lock-registration a{background:url("//upload.wikimedia.org/wikipedia/commons/d/d6/Lock-gray-alt-2.svg")right 0.1em center/9px no-repeat}.mw-parser-output .id-lock-subscription a,.mw-parser-output .citation .cs1-lock-subscription a{background:url("//upload.wikimedia.org/wikipedia/commons/a/aa/Lock-red-alt-2.svg")right 0.1em center/9px no-repeat}.mw-parser-output .cs1-ws-icon a{background:url("//upload.wikimedia.org/wikipedia/commons/4/4c/Wikisource-logo.svg")right 0.1em center/12px no-repeat}.mw-parser-output .cs1-code{color:inherit;background:inherit;border:none;padding:inherit}.mw-parser-output .cs1-hidden-error{display:none;color:#d33}.mw-parser-output .cs1-visible-error{color:#d33}.mw-parser-output .cs1-maint{display:none;color:#3a3;margin-left:0.3em}.mw-parser-output .cs1-format{font-size:95%}.mw-parser-output .cs1-kern-left{padding-left:0.2em}.mw-parser-output .cs1-kern-right{padding-right:0.2em}.mw-parser-output .citation .mw-selflink{font-weight:inherit}</style><cite id="CITEREFNancy_D._Gordon2004" class="citation book cs1">Nancy D. Gordon (2004). <a rel="nofollow" class="external text" href="https://books.google.com/books?id=_PJHw-hSKGgC&amp;pg=PA113">»Erosion and Scour«</a>. <i>Stream hydrology: an introduction for ecologists</i>. <a href="/wiki/ISBN_(identifikator)" class="mw-redirect" title="ISBN (identifikator)">ISBN</a>&#160;<a href="/wiki/Posebno:ViriKnjig/978-0-470-84357-4" title="Posebno:ViriKnjig/978-0-470-84357-4"><bdi>978-0-470-84357-4</bdi></a>.</cite><span title="ctx_ver=Z39.88-2004&amp;rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Abook&amp;rft.genre=knji%C5%BEni+predmet&amp;rft.atitle=Erosion+and+Scour&amp;rft.btitle=Stream+hydrology%3A+an+introduction+for+ecologists&amp;rft.date=2004&amp;rft.isbn=978-0-470-84357-4&amp;rft.au=Nancy+D.+Gordon&amp;rft_id=https%3A%2F%2Fbooks.google.com%2Fbooks%3Fid%3D_PJHw-hSKGgC%26pg%3DPA113&amp;rfr_id=info%3Asid%2Fsl.wikipedia.org%3AErozija" class="Z3988"></span></span> </li> <li id="cite_note-nsidc_thermal-4"><span class="mw-cite-backlink"><a href="#cite_ref-nsidc_thermal_4-0">↑</a></span> <span class="reference-text"><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r5980307"><cite class="citation web cs1"><a rel="nofollow" class="external text" href="http://nsidc.org/cgi-bin/words/word.pl?thermal%20erosion">»Thermal Erosion«</a>. <i>NSIDC Glossary</i>. National Snow and Ice Data Center. <a rel="nofollow" class="external text" href="https://web.archive.org/web/20101218124656/http://nsidc.org/cgi-bin/words/word.pl?thermal%20erosion">Arhivirano</a> iz spletišča dne 18. decembra 2010<span class="reference-accessdate">. Pridobljeno 21. decembra 2009</span>.</cite><span title="ctx_ver=Z39.88-2004&amp;rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Ajournal&amp;rft.genre=neznano&amp;rft.jtitle=NSIDC+Glossary&amp;rft.atitle=Thermal+Erosion&amp;rft_id=http%3A%2F%2Fnsidc.org%2Fcgi-bin%2Fwords%2Fword.pl%3Fthermal%2520erosion&amp;rfr_id=info%3Asid%2Fsl.wikipedia.org%3AErozija" class="Z3988"></span></span> </li> <li id="cite_note-lena-5"><span class="mw-cite-backlink"><a href="#cite_ref-lena_5-0">↑</a></span> <span class="reference-text"><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r5980307"><cite id="CITEREFCostardDupeyratGautierCarey-Gailhardis2003" class="citation journal cs1">Costard, F.; Dupeyrat, L.; Gautier, E.; Carey-Gailhardis, E. (2003). <a rel="nofollow" class="external text" href="https://archive.org/details/sim_earth-surface-processes-and-landforms_2003-11_28_12/page/1349">»Fluvial thermal erosion investigations along a rapidly eroding river bank: application to the Lena River (central Siberia)«</a>. <i>Earth Surface Processes and Landforms</i>. <b>28</b> (12): 1349–1359. <a href="/wiki/Bibcode_(identifikator)" class="mw-redirect" title="Bibcode (identifikator)">Bibcode</a>:<a rel="nofollow" class="external text" href="https://ui.adsabs.harvard.edu/abs/2003ESPL...28.1349C">2003ESPL...28.1349C</a>. <a href="/wiki/Doi_(identifikator)" class="mw-redirect" title="Doi (identifikator)">doi</a>:<a rel="nofollow" class="external text" href="https://doi.org/10.1002%2Fesp.592">10.1002/esp.592</a>.</cite><span title="ctx_ver=Z39.88-2004&amp;rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Ajournal&amp;rft.genre=%C4%8Dlanek&amp;rft.jtitle=Earth+Surface+Processes+and+Landforms&amp;rft.atitle=Fluvial+thermal+erosion+investigations+along+a+rapidly+eroding+river+bank%3A+application+to+the+Lena+River+%28central+Siberia%29&amp;rft.volume=28&amp;rft.issue=12&amp;rft.pages=1349-1359&amp;rft.date=2003&amp;rft_id=info%3Adoi%2F10.1002%2Fesp.592&amp;rft_id=info%3Abibcode%2F2003ESPL...28.1349C&amp;rft.aulast=Costard&amp;rft.aufirst=F.&amp;rft.au=Dupeyrat%2C+L.&amp;rft.au=Gautier%2C+E.&amp;rft.au=Carey-Gailhardis%2C+E.&amp;rft_id=https%3A%2F%2Farchive.org%2Fdetails%2Fsim_earth-surface-processes-and-landforms_2003-11_28_12%2Fpage%2F1349&amp;rfr_id=info%3Asid%2Fsl.wikipedia.org%3AErozija" class="Z3988"></span></span> </li> <li id="cite_note-jones_arctic-6"><span class="mw-cite-backlink"><a href="#cite_ref-jones_arctic_6-0">↑</a></span> <span class="reference-text"><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r5980307"><cite id="CITEREFJonesHinkel,_K.M.Arp,_C.D.Eisner,_W.R.2008" class="citation journal cs1">Jones, B.M.; Hinkel, K.M.; Arp, C.D.; Eisner, W.R. (2008). <a rel="nofollow" class="external text" href="https://web.archive.org/web/20130517101602/http://arctic.synergiesprairies.ca/arctic/index.php/arctic/article/view/44/115">»Modern Erosion Rates and Loss of Coastal Features and Sites, Beaufort Sea Coastline, Alaska«</a>. <i>Arctic</i>. <b>61</b> (4): 361–372. <a href="/wiki/Doi_(identifikator)" class="mw-redirect" title="Doi (identifikator)">doi</a>:<a rel="nofollow" class="external text" href="https://doi.org/10.14430%2Farctic44">10.14430/arctic44</a>. <a href="/w/index.php?title=Hdl_(identifikator)&amp;action=edit&amp;redlink=1" class="new" title="Hdl (identifikator) (stran ne obstaja)">hdl</a>:<span class="cs1-lock-free" title="Prosto dostopno"><a rel="nofollow" class="external text" href="https://hdl.handle.net/10535%2F5534">10535/5534</a></span>. Arhivirano iz <a rel="nofollow" class="external text" href="http://arctic.synergiesprairies.ca/arctic/index.php/arctic/article/view/44/115">prvotnega spletišča</a> dne 17. maja 2013.</cite><span title="ctx_ver=Z39.88-2004&amp;rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Ajournal&amp;rft.genre=%C4%8Dlanek&amp;rft.jtitle=Arctic&amp;rft.atitle=Modern+Erosion+Rates+and+Loss+of+Coastal+Features+and+Sites%2C+Beaufort+Sea+Coastline%2C+Alaska&amp;rft.volume=61&amp;rft.issue=4&amp;rft.pages=361-372&amp;rft.date=2008&amp;rft_id=info%3Ahdl%2F10535%2F5534&amp;rft_id=info%3Adoi%2F10.14430%2Farctic44&amp;rft.aulast=Jones&amp;rft.aufirst=B.M.&amp;rft.au=Hinkel%2C+K.M.&amp;rft.au=Arp%2C+C.D.&amp;rft.au=Eisner%2C+W.R.&amp;rft_id=http%3A%2F%2Farctic.synergiesprairies.ca%2Farctic%2Findex.php%2Farctic%2Farticle%2Fview%2F44%2F115&amp;rfr_id=info%3Asid%2Fsl.wikipedia.org%3AErozija" class="Z3988"></span></span> </li> <li id="cite_note-7"><span class="mw-cite-backlink"><a href="#cite_ref-7">↑</a></span> <span class="reference-text">Bell, Frederic Gladstone. "Marine action and control." Geological hazards: their assessment, avoidance, and mitigation, Taylor &amp; Francis, 1999, pp. 302–306.</span> </li> <li id="cite_note-Pinter2010-8"><span class="mw-cite-backlink"><a href="#cite_ref-Pinter2010_8-0">↑</a></span> <span class="reference-text"><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r5980307"><cite id="CITEREFPinter,_N2010" class="citation web cs1">Pinter, N (2010). <a rel="nofollow" class="external text" href="https://web.archive.org/web/20101010230028/http://www.geology.siu.edu/people/pinter/pdf/CoastalExercise.pdf">»Coastal Terraces, Sealevel, and Active Tectonics«</a> <span class="cs1-format">(PDF)</span>. Arhivirano iz <a rel="nofollow" class="external text" href="http://www.geology.siu.edu/people/pinter/pdf/CoastalExercise.pdf">prvotnega spletišča</a> <span class="cs1-format">(PDF)</span> dne 10. oktobra 2010<span class="reference-accessdate">. Pridobljeno 21. aprila 2011</span>.</cite><span title="ctx_ver=Z39.88-2004&amp;rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Abook&amp;rft.genre=neznano&amp;rft.btitle=Coastal+Terraces%2C+Sealevel%2C+and+Active+Tectonics&amp;rft.date=2010&amp;rft.au=Pinter%2C+N&amp;rft_id=http%3A%2F%2Fwww.geology.siu.edu%2Fpeople%2Fpinter%2Fpdf%2FCoastalExercise.pdf&amp;rfr_id=info%3Asid%2Fsl.wikipedia.org%3AErozija" class="Z3988"></span> [02/04/2011]</span> </li> <li id="cite_note-9"><span class="mw-cite-backlink"><a href="#cite_ref-9">↑</a></span> <span class="reference-text"><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r5980307"><cite id="CITEREFDixonThorn2005" class="citation journal cs1">Dixon, John C.; Thorn, Colin E. (2005). »Chemical weathering and landscape development in mid-latitude alpine environments«. <i>Geomorphology (journal)</i>. <b>67</b> (1–2): 127–145. <a href="/wiki/Bibcode_(identifikator)" class="mw-redirect" title="Bibcode (identifikator)">Bibcode</a>:<a rel="nofollow" class="external text" href="https://ui.adsabs.harvard.edu/abs/2005Geomo..67..127D">2005Geomo..67..127D</a>. <a href="/wiki/Doi_(identifikator)" class="mw-redirect" title="Doi (identifikator)">doi</a>:<a rel="nofollow" class="external text" href="https://doi.org/10.1016%2Fj.geomorph.2004.07.009">10.1016/j.geomorph.2004.07.009</a>.</cite><span title="ctx_ver=Z39.88-2004&amp;rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Ajournal&amp;rft.genre=%C4%8Dlanek&amp;rft.jtitle=Geomorphology+%28journal%29&amp;rft.atitle=Chemical+weathering+and+landscape+development+in+mid-latitude+alpine+environments&amp;rft.volume=67&amp;rft.issue=1%E2%80%932&amp;rft.pages=127-145&amp;rft.date=2005&amp;rft_id=info%3Adoi%2F10.1016%2Fj.geomorph.2004.07.009&amp;rft_id=info%3Abibcode%2F2005Geomo..67..127D&amp;rft.aulast=Dixon&amp;rft.aufirst=John+C.&amp;rft.au=Thorn%2C+Colin+E.&amp;rfr_id=info%3Asid%2Fsl.wikipedia.org%3AErozija" class="Z3988"></span></span> </li> <li id="cite_note-10"><span class="mw-cite-backlink"><a href="#cite_ref-10">↑</a></span> <span class="reference-text"><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r5980307"><cite id="CITEREFLard,_L.Paull,_C.Hobson,_B.1995" class="citation journal cs1">Lard, L.; Paull, C.; Hobson, B. (1995). <a rel="nofollow" class="external text" href="https://archive.org/details/sim_geology_1995-10_23_10/page/949">»Genesis of a submarine sinkhole without subaerial exposure«</a>. <i>Geology</i>. <b>23</b> (10): 949–951. <a href="/wiki/Bibcode_(identifikator)" class="mw-redirect" title="Bibcode (identifikator)">Bibcode</a>:<a rel="nofollow" class="external text" href="https://ui.adsabs.harvard.edu/abs/1995Geo....23..949L">1995Geo....23..949L</a>. <a href="/wiki/Doi_(identifikator)" class="mw-redirect" title="Doi (identifikator)">doi</a>:<a rel="nofollow" class="external text" href="https://doi.org/10.1130%2F0091-7613%281995%29023%3C0949%3AGOASSW%3E2.3.CO%3B2">10.1130/0091-7613(1995)023&#60;0949:GOASSW&#62;2.3.CO&#59;2</a>.</cite><span title="ctx_ver=Z39.88-2004&amp;rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Ajournal&amp;rft.genre=%C4%8Dlanek&amp;rft.jtitle=Geology&amp;rft.atitle=Genesis+of+a+submarine+sinkhole+without+subaerial+exposure&amp;rft.volume=23&amp;rft.issue=10&amp;rft.pages=949-951&amp;rft.date=1995&amp;rft_id=info%3Adoi%2F10.1130%2F0091-7613%281995%29023%3C0949%3AGOASSW%3E2.3.CO%3B2&amp;rft_id=info%3Abibcode%2F1995Geo....23..949L&amp;rft.au=Lard%2C+L.&amp;rft.au=Paull%2C+C.&amp;rft.au=Hobson%2C+B.&amp;rft_id=https%3A%2F%2Farchive.org%2Fdetails%2Fsim_geology_1995-10_23_10%2Fpage%2F949&amp;rfr_id=info%3Asid%2Fsl.wikipedia.org%3AErozija" class="Z3988"></span></span> </li> <li id="cite_note-11"><span class="mw-cite-backlink"><a href="#cite_ref-11">↑</a></span> <span class="reference-text"><a rel="nofollow" class="external text" href="https://www.pizzatravel.com.ua/eng/finland/117/devils_nest">The Devil's Nest, the deepest ground erosion in Europe</a></span> </li> <li id="cite_note-12"><span class="mw-cite-backlink"><a href="#cite_ref-12">↑</a></span> <span class="reference-text"><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r5980307"><cite id="CITEREFEgholmNielsenPedersenLesemann2009" class="citation journal cs1">Egholm, D. L.; Nielsen, S. B.; Pedersen, V.K.; Lesemann, J.-E. (2009). »Glacial effects limiting mountain height«. <i>Nature</i>. <b>460</b> (7257): 884–887. <a href="/wiki/Bibcode_(identifikator)" class="mw-redirect" title="Bibcode (identifikator)">Bibcode</a>:<a rel="nofollow" class="external text" href="https://ui.adsabs.harvard.edu/abs/2009Natur.460..884E">2009Natur.460..884E</a>. <a href="/wiki/Doi_(identifikator)" class="mw-redirect" title="Doi (identifikator)">doi</a>:<a rel="nofollow" class="external text" href="https://doi.org/10.1038%2Fnature08263">10.1038/nature08263</a>. <a href="/wiki/PMID_(identifikator)" class="mw-redirect" title="PMID (identifikator)">PMID</a>&#160;<a rel="nofollow" class="external text" href="https://pubmed.ncbi.nlm.nih.gov/19675651">19675651</a>. <a href="/wiki/S2CID_(identifikator)" class="mw-redirect" title="S2CID (identifikator)">S2CID</a>&#160;<a rel="nofollow" class="external text" href="https://api.semanticscholar.org/CorpusID:205217746">205217746</a>.</cite><span title="ctx_ver=Z39.88-2004&amp;rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Ajournal&amp;rft.genre=%C4%8Dlanek&amp;rft.jtitle=Nature&amp;rft.atitle=Glacial+effects+limiting+mountain+height&amp;rft.volume=460&amp;rft.issue=7257&amp;rft.pages=884-887&amp;rft.date=2009&amp;rft_id=info%3Adoi%2F10.1038%2Fnature08263&amp;rft_id=https%3A%2F%2Fapi.semanticscholar.org%2FCorpusID%3A205217746%23id-name%3DS2CID&amp;rft_id=info%3Apmid%2F19675651&amp;rft_id=info%3Abibcode%2F2009Natur.460..884E&amp;rft.aulast=Egholm&amp;rft.aufirst=D.+L.&amp;rft.au=Nielsen%2C+S.+B.&amp;rft.au=Pedersen%2C+V.K.&amp;rft.au=Lesemann%2C+J.-E.&amp;rfr_id=info%3Asid%2Fsl.wikipedia.org%3AErozija" class="Z3988"></span></span> </li> <li id="cite_note-reference-13"><span class="mw-cite-backlink"><a href="#cite_ref-reference_13-0">↑</a></span> <span class="reference-text"><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r5980307"><cite id="CITEREFThomsonBrandonTomkinReiners2010" class="citation journal cs1">Thomson, Stuart N.; Brandon, Mark T.; Tomkin, Jonathan H.; Reiners, Peter W.; Vásquez, Cristián; Wilson, Nathaniel J. (2010). »Glaciation as a destructive and constructive control on mountain building«. <i>Nature</i>. <b>467</b> (7313): 313–317. <a href="/wiki/Bibcode_(identifikator)" class="mw-redirect" title="Bibcode (identifikator)">Bibcode</a>:<a rel="nofollow" class="external text" href="https://ui.adsabs.harvard.edu/abs/2010Natur.467..313T">2010Natur.467..313T</a>. <a href="/wiki/Doi_(identifikator)" class="mw-redirect" title="Doi (identifikator)">doi</a>:<a rel="nofollow" class="external text" href="https://doi.org/10.1038%2Fnature09365">10.1038/nature09365</a>. <a href="/w/index.php?title=Hdl_(identifikator)&amp;action=edit&amp;redlink=1" class="new" title="Hdl (identifikator) (stran ne obstaja)">hdl</a>:<span class="cs1-lock-free" title="Prosto dostopno"><a rel="nofollow" class="external text" href="https://hdl.handle.net/10533%2F144849">10533/144849</a></span>. <a href="/wiki/PMID_(identifikator)" class="mw-redirect" title="PMID (identifikator)">PMID</a>&#160;<a rel="nofollow" class="external text" href="https://pubmed.ncbi.nlm.nih.gov/20844534">20844534</a>. <a href="/wiki/S2CID_(identifikator)" class="mw-redirect" title="S2CID (identifikator)">S2CID</a>&#160;<a rel="nofollow" class="external text" href="https://api.semanticscholar.org/CorpusID:205222252">205222252</a>.</cite><span title="ctx_ver=Z39.88-2004&amp;rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Ajournal&amp;rft.genre=%C4%8Dlanek&amp;rft.jtitle=Nature&amp;rft.atitle=Glaciation+as+a+destructive+and+constructive+control+on+mountain+building&amp;rft.volume=467&amp;rft.issue=7313&amp;rft.pages=313-317&amp;rft.date=2010&amp;rft_id=info%3Ahdl%2F10533%2F144849&amp;rft_id=https%3A%2F%2Fapi.semanticscholar.org%2FCorpusID%3A205222252%23id-name%3DS2CID&amp;rft_id=info%3Abibcode%2F2010Natur.467..313T&amp;rft_id=info%3Apmid%2F20844534&amp;rft_id=info%3Adoi%2F10.1038%2Fnature09365&amp;rft.aulast=Thomson&amp;rft.aufirst=Stuart+N.&amp;rft.au=Brandon%2C+Mark+T.&amp;rft.au=Tomkin%2C+Jonathan+H.&amp;rft.au=Reiners%2C+Peter+W.&amp;rft.au=V%C3%A1squez%2C+Cristi%C3%A1n&amp;rft.au=Wilson%2C+Nathaniel+J.&amp;rfr_id=info%3Asid%2Fsl.wikipedia.org%3AErozija" class="Z3988"></span></span> </li> <li id="cite_note-14"><span class="mw-cite-backlink"><a href="#cite_ref-14">↑</a></span> <span class="reference-text">Mitchell, S.G. &amp; Montgomery, D.R. "Influence of a glacial buzzsaw on the height and morphology of the Cascade Range in central Washington State". <i>Quat. Res</i>. 65, 96–107 (2006)</span> </li> <li id="cite_note-15"><span class="mw-cite-backlink"><a href="#cite_ref-15">↑</a></span> <span class="reference-text"><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r5980307"><cite id="CITEREFGjermundsenBrinerAkçarForos2015" class="citation journal cs1">Gjermundsen, Endre F.; Briner, Jason P.; Akçar, Naki; Foros, Jørn; Kubik, Peter W.; Salvigsen, Otto; Hormes, Anne (2015). »Minimal erosion of Arctic alpine topography during late Quaternary glaciation«. <i>Nature Geoscience</i>. <b>8</b> (10): 789. <a href="/wiki/Bibcode_(identifikator)" class="mw-redirect" title="Bibcode (identifikator)">Bibcode</a>:<a rel="nofollow" class="external text" href="https://ui.adsabs.harvard.edu/abs/2015NatGe...8..789G">2015NatGe...8..789G</a>. <a href="/wiki/Doi_(identifikator)" class="mw-redirect" title="Doi (identifikator)">doi</a>:<a rel="nofollow" class="external text" href="https://doi.org/10.1038%2Fngeo2524">10.1038/ngeo2524</a>.</cite><span title="ctx_ver=Z39.88-2004&amp;rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Ajournal&amp;rft.genre=%C4%8Dlanek&amp;rft.jtitle=Nature+Geoscience&amp;rft.atitle=Minimal+erosion+of+Arctic+alpine+topography+during+late+Quaternary+glaciation&amp;rft.volume=8&amp;rft.issue=10&amp;rft.pages=789&amp;rft.date=2015&amp;rft_id=info%3Adoi%2F10.1038%2Fngeo2524&amp;rft_id=info%3Abibcode%2F2015NatGe...8..789G&amp;rft.aulast=Gjermundsen&amp;rft.aufirst=Endre+F.&amp;rft.au=Briner%2C+Jason+P.&amp;rft.au=Ak%C3%A7ar%2C+Naki&amp;rft.au=Foros%2C+J%C3%B8rn&amp;rft.au=Kubik%2C+Peter+W.&amp;rft.au=Salvigsen%2C+Otto&amp;rft.au=Hormes%2C+Anne&amp;rfr_id=info%3Asid%2Fsl.wikipedia.org%3AErozija" class="Z3988"></span></span> </li> <li id="cite_note-16"><span class="mw-cite-backlink"><a href="#cite_ref-16">↑</a></span> <span class="reference-text">Harvey, A.M. "Local-Scale geomorphology – process systems and landforms." <i>Introducing Geomorphology: A Guide to Landforms and Processes</i>. Dunedin Academic Press, 2012, pp. 87–88. EBSCO<i>host</i>.</span> </li> <li id="cite_note-17"><span class="mw-cite-backlink"><a href="#cite_ref-17">↑</a></span> <span class="reference-text"><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r5980307"><cite id="CITEREFPrasicekLarsenMontgomery2015" class="citation journal cs1 cs1-prop-foreign-lang-source">Prasicek, Günther; Larsen, Isaac J.; Montgomery, David R. (14. avgust 2015). <a rel="nofollow" class="external text" href="https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4557346">»Tectonic control on the persistence of glacially sculpted topography«</a>. <i>Nature Communications</i> (v angleščini). <b>6</b>: 8028. <a href="/wiki/Bibcode_(identifikator)" class="mw-redirect" title="Bibcode (identifikator)">Bibcode</a>:<a rel="nofollow" class="external text" href="https://ui.adsabs.harvard.edu/abs/2015NatCo...6.8028P">2015NatCo...6.8028P</a>. <a href="/wiki/Doi_(identifikator)" class="mw-redirect" title="Doi (identifikator)">doi</a>:<a rel="nofollow" class="external text" href="https://doi.org/10.1038%2Fncomms9028">10.1038/ncomms9028</a>. <a href="/wiki/ISSN_(identifikator)" class="mw-redirect" title="ISSN (identifikator)">ISSN</a>&#160;<a rel="nofollow" class="external text" href="https://www.worldcat.org/issn/2041-1723">2041-1723</a>. <a href="/wiki/PMC_(identifikator)" class="mw-redirect" title="PMC (identifikator)">PMC</a>&#160;<span class="cs1-lock-free" title="Prosto dostopno"><a rel="nofollow" class="external text" href="https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4557346">4557346</a></span>. <a href="/wiki/PMID_(identifikator)" class="mw-redirect" title="PMID (identifikator)">PMID</a>&#160;<a rel="nofollow" class="external text" href="https://pubmed.ncbi.nlm.nih.gov/26271245">26271245</a>.</cite><span title="ctx_ver=Z39.88-2004&amp;rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Ajournal&amp;rft.genre=%C4%8Dlanek&amp;rft.jtitle=Nature+Communications&amp;rft.atitle=Tectonic+control+on+the+persistence+of+glacially+sculpted+topography&amp;rft.volume=6&amp;rft.pages=8028&amp;rft.date=2015-08-14&amp;rft_id=https%3A%2F%2Fwww.ncbi.nlm.nih.gov%2Fpmc%2Farticles%2FPMC4557346%23id-name%3DPMC&amp;rft_id=info%3Abibcode%2F2015NatCo...6.8028P&amp;rft_id=info%3Apmid%2F26271245&amp;rft_id=info%3Adoi%2F10.1038%2Fncomms9028&amp;rft.issn=2041-1723&amp;rft.aulast=Prasicek&amp;rft.aufirst=G%C3%BCnther&amp;rft.au=Larsen%2C+Isaac+J.&amp;rft.au=Montgomery%2C+David+R.&amp;rft_id=https%3A%2F%2Fwww.ncbi.nlm.nih.gov%2Fpmc%2Farticles%2FPMC4557346&amp;rfr_id=info%3Asid%2Fsl.wikipedia.org%3AErozija" class="Z3988"></span></span> </li> <li id="cite_note-18"><span class="mw-cite-backlink"><a href="#cite_ref-18">↑</a></span> <span class="reference-text">See, for example: <link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r5980307"><cite id="CITEREFAlt,_David2001" class="citation book cs1">Alt, David (2001). <a rel="nofollow" class="external text" href="https://books.google.com/books?id=s4y3c8fxeEwC"><i>Glacial Lake Missoula &amp; its Humongous Floods</i></a>. Mountain Press. <a href="/wiki/ISBN_(identifikator)" class="mw-redirect" title="ISBN (identifikator)">ISBN</a>&#160;<a href="/wiki/Posebno:ViriKnjig/978-0-87842-415-3" title="Posebno:ViriKnjig/978-0-87842-415-3"><bdi>978-0-87842-415-3</bdi></a>.</cite><span title="ctx_ver=Z39.88-2004&amp;rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Abook&amp;rft.genre=knjiga&amp;rft.btitle=Glacial+Lake+Missoula+%26+its+Humongous+Floods&amp;rft.pub=Mountain+Press&amp;rft.date=2001&amp;rft.isbn=978-0-87842-415-3&amp;rft.au=Alt%2C+David&amp;rft_id=https%3A%2F%2Fbooks.google.com%2Fbooks%3Fid%3Ds4y3c8fxeEwC&amp;rfr_id=info%3Asid%2Fsl.wikipedia.org%3AErozija" class="Z3988"></span></span> </li> <li id="cite_note-19"><span class="mw-cite-backlink"><a href="#cite_ref-19">↑</a></span> <span class="reference-text"><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r5980307"><cite id="CITEREFZheng,_XiaojingHuang,_Ning2009" class="citation book cs1">Zheng, Xiaojing; Huang, Ning (2009). <a rel="nofollow" class="external text" href="https://books.google.com/books?id=R6kYrbA3XSAC&amp;pg=PA7"><i>Mechanics of Wind-Blown Sand Movements</i></a>. <i>Mechanics of Wind-Blown Sand Movements by Xiaojing Zheng. Berlin: Springer</i>. Springer. str.&#160;7–8. <a href="/wiki/Bibcode_(identifikator)" class="mw-redirect" title="Bibcode (identifikator)">Bibcode</a>:<a rel="nofollow" class="external text" href="https://ui.adsabs.harvard.edu/abs/2009mwbs.book.....Z">2009mwbs.book.....Z</a>. <a href="/wiki/ISBN_(identifikator)" class="mw-redirect" title="ISBN (identifikator)">ISBN</a>&#160;<a href="/wiki/Posebno:ViriKnjig/978-3-540-88253-4" title="Posebno:ViriKnjig/978-3-540-88253-4"><bdi>978-3-540-88253-4</bdi></a>.</cite><span title="ctx_ver=Z39.88-2004&amp;rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Abook&amp;rft.genre=knjiga&amp;rft.btitle=Mechanics+of+Wind-Blown+Sand+Movements&amp;rft.pages=7-8&amp;rft.pub=Springer&amp;rft.date=2009&amp;rft_id=info%3Abibcode%2F2009mwbs.book.....Z&amp;rft.isbn=978-3-540-88253-4&amp;rft.au=Zheng%2C+Xiaojing&amp;rft.au=Huang%2C+Ning&amp;rft_id=https%3A%2F%2Fbooks.google.com%2Fbooks%3Fid%3DR6kYrbA3XSAC%26pg%3DPA7&amp;rfr_id=info%3Asid%2Fsl.wikipedia.org%3AErozija" class="Z3988"></span></span> </li> <li id="cite_note-20"><span class="mw-cite-backlink"><a href="#cite_ref-20">↑</a></span> <span class="reference-text"><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r5980307"><cite id="CITEREFCornelis,_Wim_S.2006" class="citation book cs1">Cornelis, Wim S. (2006). <a rel="nofollow" class="external text" href="https://books.google.com/books?id=rUsUPZbFHK8C&amp;pg=PA141">»Hydroclimatology of wind erosion in arid and semi-arid environments«</a>. V D'Odorico, Paolo; Porporato, Amilcare (ur.). <i>Dryland Ecohydrology</i>. Springer. str.&#160;141. <a href="/wiki/ISBN_(identifikator)" class="mw-redirect" title="ISBN (identifikator)">ISBN</a>&#160;<a href="/wiki/Posebno:ViriKnjig/978-1-4020-4261-4" title="Posebno:ViriKnjig/978-1-4020-4261-4"><bdi>978-1-4020-4261-4</bdi></a>.</cite><span title="ctx_ver=Z39.88-2004&amp;rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Abook&amp;rft.genre=knji%C5%BEni+predmet&amp;rft.atitle=Hydroclimatology+of+wind+erosion+in+arid+and+semi-arid+environments&amp;rft.btitle=Dryland+Ecohydrology&amp;rft.pages=141&amp;rft.pub=Springer&amp;rft.date=2006&amp;rft.isbn=978-1-4020-4261-4&amp;rft.au=Cornelis%2C+Wim+S.&amp;rft_id=https%3A%2F%2Fbooks.google.com%2Fbooks%3Fid%3DrUsUPZbFHK8C%26pg%3DPA141&amp;rfr_id=info%3Asid%2Fsl.wikipedia.org%3AErozija" class="Z3988"></span></span> </li> <li id="cite_note-BlancoWind-21"><span class="mw-cite-backlink"><a href="#cite_ref-BlancoWind_21-0">↑</a></span> <span class="reference-text"><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r5980307"><cite id="CITEREFBlanco-CanquiRattan2008" class="citation book cs1">Blanco-Canqui, Humberto; Rattan, Lal (2008). »Wind erosion«. <i>Principles of soil conservation and management</i>. Dordrecht: Springer. str.&#160;54–80. <a href="/wiki/ISBN_(identifikator)" class="mw-redirect" title="ISBN (identifikator)">ISBN</a>&#160;<a href="/wiki/Posebno:ViriKnjig/978-1-4020-8709-7" title="Posebno:ViriKnjig/978-1-4020-8709-7"><bdi>978-1-4020-8709-7</bdi></a>.</cite><span title="ctx_ver=Z39.88-2004&amp;rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Abook&amp;rft.genre=knji%C5%BEni+predmet&amp;rft.atitle=Wind+erosion&amp;rft.btitle=Principles+of+soil+conservation+and+management&amp;rft.place=Dordrecht&amp;rft.pages=54-80&amp;rft.pub=Springer&amp;rft.date=2008&amp;rft.isbn=978-1-4020-8709-7&amp;rft.aulast=Blanco-Canqui&amp;rft.aufirst=Humberto&amp;rft.au=Rattan%2C+Lal&amp;rfr_id=info%3Asid%2Fsl.wikipedia.org%3AErozija" class="Z3988"></span></span> </li> <li id="cite_note-22"><span class="mw-cite-backlink"><a href="#cite_ref-22">↑</a></span> <span class="reference-text"><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r5980307"><cite id="CITEREFWiggs,_Giles_F.S.2011" class="citation book cs1">Wiggs, Giles F.S. (2011). <a rel="nofollow" class="external text" href="https://books.google.com/books?id=swz4rh4KaLYC&amp;pg=PA588">»Geomorphological hazards in drylands«</a>. V Thomas, David S.G. (ur.). <i>Arid Zone Geomorphology: Process, Form and Change in Drylands</i>. John Wiley &amp; Sons. str.&#160;588. <a href="/wiki/ISBN_(identifikator)" class="mw-redirect" title="ISBN (identifikator)">ISBN</a>&#160;<a href="/wiki/Posebno:ViriKnjig/978-0-470-71076-0" title="Posebno:ViriKnjig/978-0-470-71076-0"><bdi>978-0-470-71076-0</bdi></a>.</cite><span title="ctx_ver=Z39.88-2004&amp;rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Abook&amp;rft.genre=knji%C5%BEni+predmet&amp;rft.atitle=Geomorphological+hazards+in+drylands&amp;rft.btitle=Arid+Zone+Geomorphology%3A+Process%2C+Form+and+Change+in+Drylands&amp;rft.pages=588&amp;rft.pub=John+Wiley+%26+Sons&amp;rft.date=2011&amp;rft.isbn=978-0-470-71076-0&amp;rft.au=Wiggs%2C+Giles+F.S.&amp;rft_id=https%3A%2F%2Fbooks.google.com%2Fbooks%3Fid%3Dswz4rh4KaLYC%26pg%3DPA588&amp;rfr_id=info%3Asid%2Fsl.wikipedia.org%3AErozija" class="Z3988"></span></span> </li> <li id="cite_note-P.2007-23"><span class="mw-cite-backlink"><a href="#cite_ref-P.2007_23-0">↑</a></span> <span class="reference-text"><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r5980307"><cite id="CITEREFSivashanmugam,_P.2007" class="citation book cs1">Sivashanmugam, P. (2007). <a rel="nofollow" class="external text" href="https://books.google.com/books?id=aTJ31ycKQeEC&amp;pg=PA43"><i>Basics of Environmental Science and Engineering</i></a>. New India Publishing. str.&#160;43–. <a href="/wiki/ISBN_(identifikator)" class="mw-redirect" title="ISBN (identifikator)">ISBN</a>&#160;<a href="/wiki/Posebno:ViriKnjig/978-81-89422-28-8" title="Posebno:ViriKnjig/978-81-89422-28-8"><bdi>978-81-89422-28-8</bdi></a>.</cite><span title="ctx_ver=Z39.88-2004&amp;rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Abook&amp;rft.genre=knjiga&amp;rft.btitle=Basics+of+Environmental+Science+and+Engineering&amp;rft.pages=43-&amp;rft.pub=New+India+Publishing&amp;rft.date=2007&amp;rft.isbn=978-81-89422-28-8&amp;rft.au=Sivashanmugam%2C+P.&amp;rft_id=https%3A%2F%2Fbooks.google.com%2Fbooks%3Fid%3DaTJ31ycKQeEC%26pg%3DPA43&amp;rfr_id=info%3Asid%2Fsl.wikipedia.org%3AErozija" class="Z3988"></span></span> </li> </ol></div> <div class="mw-heading mw-heading2"><h2 id="Zunanje_povezave">Zunanje povezave</h2><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Erozija&amp;veaction=edit&amp;section=11" title="Uredi razdelek: Zunanje povezave" class="mw-editsection-visualeditor"><span>uredi</span></a><span class="mw-editsection-divider"> | </span><a href="/w/index.php?title=Erozija&amp;action=edit&amp;section=11" title="Urejanje izvorne kode razdelka: Zunanje povezave"><span>uredi kodo</span></a><span class="mw-editsection-bracket">]</span></span></div> <style data-mw-deduplicate="TemplateStyles:r5916282">.mw-parser-output .side-box{margin:4px 0;box-sizing:border-box;border:1px solid #aaa;font-size:88%;line-height:1.25em;background-color:#f9f9f9;display:flow-root}.mw-parser-output .side-box-abovebelow,.mw-parser-output .side-box-text{padding:0.25em 0.9em}.mw-parser-output .side-box-image{padding:2px 0 2px 0.9em;text-align:center}.mw-parser-output .side-box-imageright{padding:2px 0.9em 2px 0;text-align:center}@media(min-width:500px){.mw-parser-output .side-box-flex{display:flex;align-items:center}.mw-parser-output .side-box-text{flex:1}}@media(min-width:720px){.mw-parser-output .side-box{width:238px}.mw-parser-output .side-box-right{clear:right;float:right;margin-left:1em}.mw-parser-output .side-box-left{margin-right:1em}}</style><style data-mw-deduplicate="TemplateStyles:r5922699">.mw-parser-output .sister-box .side-box-abovebelow{padding:0.75em 0;text-align:center}.mw-parser-output .sister-box .side-box-abovebelow>b{display:block}.mw-parser-output .sister-box .side-box-text>ul{border-top:1px solid #aaa;padding:0.75em 0;width:217px;margin:0 auto}.mw-parser-output .sister-box .side-box-text>ul>li{min-height:31px}.mw-parser-output .sister-logo{display:inline-block;width:31px;line-height:31px;vertical-align:middle;text-align:center}.mw-parser-output .sister-link{display:inline-block;margin-left:4px;width:182px;vertical-align:middle}</style><div role="navigation" aria-labelledby="sister-projects" class="side-box metadata side-box-right sister-box sistersitebox plainlinks"><style data-mw-deduplicate="TemplateStyles:r5911185">.mw-parser-output .plainlist ol,.mw-parser-output .plainlist ul{line-height:inherit;list-style:none;margin:0;padding:0}.mw-parser-output .plainlist ol li,.mw-parser-output .plainlist ul li{margin-bottom:0}</style> <div class="side-box-abovebelow"> <b>Erozija</b> v <a href="/wiki/Wikipedija:Sorodni_projekti" title="Wikipedija:Sorodni projekti"><span id="sister-projects">sorodnih projektih</span></a> Wikipedije</div> <div class="side-box-flex"> <div class="side-box-text plainlist"><ul><li><span class="sister-logo"><span class="mw-valign-middle" typeof="mw:File"><span><img alt="" src="//upload.wikimedia.org/wikipedia/commons/thumb/e/ec/Wiktionary-logo.svg/27px-Wiktionary-logo.svg.png" decoding="async" width="27" height="26" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/e/ec/Wiktionary-logo.svg/41px-Wiktionary-logo.svg.png 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/e/ec/Wiktionary-logo.svg/54px-Wiktionary-logo.svg.png 2x" data-file-width="370" data-file-height="350" /></span></span></span><span class="sister-link"><a href="https://sl.wiktionary.org/wiki/Posebno:Iskanje/Erozija" class="extiw" title="wikt:Posebno:Iskanje/Erozija">Opredelitve</a> v Wikislovarju</span></li><li><span class="sister-logo"><span class="mw-valign-middle" typeof="mw:File"><span><img alt="" src="//upload.wikimedia.org/wikipedia/commons/thumb/4/4a/Commons-logo.svg/20px-Commons-logo.svg.png" decoding="async" width="20" height="27" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/4/4a/Commons-logo.svg/30px-Commons-logo.svg.png 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/4/4a/Commons-logo.svg/40px-Commons-logo.svg.png 2x" data-file-width="1024" data-file-height="1376" /></span></span></span><span class="sister-link"><a href="https://commons.wikimedia.org/wiki/Category:Erosion" class="extiw" title="c:Category:Erosion">Predstavnosti</a> v Zbirki</span></li><li><span class="sister-logo"><span class="mw-valign-middle" typeof="mw:File"><span><img alt="" src="//upload.wikimedia.org/wikipedia/commons/thumb/2/24/Wikinews-logo.svg/27px-Wikinews-logo.svg.png" decoding="async" width="27" height="15" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/2/24/Wikinews-logo.svg/41px-Wikinews-logo.svg.png 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/2/24/Wikinews-logo.svg/54px-Wikinews-logo.svg.png 2x" data-file-width="759" data-file-height="415" /></span></span></span><span class="sister-link"><a href="https://sl.wikinews.org/wiki/Posebno:Iskanje/Erozija" class="extiw" title="n:Posebno:Iskanje/Erozija">Novice</a> v Wikinovicah</span></li><li><span class="sister-logo"><span class="mw-valign-middle" typeof="mw:File"><span><img alt="" src="//upload.wikimedia.org/wikipedia/commons/thumb/f/fa/Wikibooks-logo.svg/27px-Wikibooks-logo.svg.png" decoding="async" width="27" height="27" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/f/fa/Wikibooks-logo.svg/41px-Wikibooks-logo.svg.png 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/f/fa/Wikibooks-logo.svg/54px-Wikibooks-logo.svg.png 2x" data-file-width="300" data-file-height="300" /></span></span></span><span class="sister-link"><a href="https://sl.wikibooks.org/wiki/Posebno:Iskanje/Erozija" class="extiw" title="b:Posebno:Iskanje/Erozija">Učbeniki</a> v Wikiknjigah</span></li></ul></div></div> </div> <ul><li><a rel="nofollow" class="external text" href="http://www.soilerosion.net/">The Soil Erosion Site</a></li> <li><a rel="nofollow" class="external text" href="https://web.archive.org/web/20091108010317/http://www.ieca.org/">International Erosion Control Association</a></li> <li><a rel="nofollow" class="external text" href="http://eusoils.jrc.ec.europa.eu/library/themes/erosion/">Soil Erosion Data</a> in the European Soil Portal</li> <li><a rel="nofollow" class="external text" href="https://www.ars.usda.gov/main/site_main.htm?modecode=36021500">USDA National Soil Erosion Laboratory</a></li> <li><a rel="nofollow" class="external text" href="http://www.swcs.org/">The Soil and Water Conservation Society</a></li> <li>Encarta Reference Library Premium 2005, različica 14.0.0.0603</li></ul> <div role="navigation" class="navbox" aria-labelledby="Normativna_kontrola_frameless&amp;#124;text-top&amp;#124;10px&amp;#124;alt=Uredite_to_na_Wikipodatkih&amp;#124;link=https&amp;#58;//www.wikidata.org/wiki/Q80026#identifiers&amp;#124;class=noprint&amp;#124;Uredite_to_na_Wikipodatkih" style="padding:3px"><table class="nowraplinks hlist mw-collapsible autocollapse navbox-inner" style="border-spacing:0;background:transparent;color:inherit"><tbody><tr><th scope="col" class="navbox-title" colspan="2"><div id="Normativna_kontrola_frameless&amp;#124;text-top&amp;#124;10px&amp;#124;alt=Uredite_to_na_Wikipodatkih&amp;#124;link=https&amp;#58;//www.wikidata.org/wiki/Q80026#identifiers&amp;#124;class=noprint&amp;#124;Uredite_to_na_Wikipodatkih" style="font-size:114%;margin:0 4em"><a href="/wiki/Wikipedija:Normativna_kontrola" title="Wikipedija:Normativna kontrola">Normativna kontrola</a> <span class="mw-valign-text-top noprint" typeof="mw:File/Frameless"><a href="https://www.wikidata.org/wiki/Q80026#identifiers" title="Uredite to na Wikipodatkih"><img alt="Uredite to na Wikipodatkih" src="//upload.wikimedia.org/wikipedia/commons/thumb/8/8a/OOjs_UI_icon_edit-ltr-progressive.svg/10px-OOjs_UI_icon_edit-ltr-progressive.svg.png" decoding="async" width="10" height="10" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/8/8a/OOjs_UI_icon_edit-ltr-progressive.svg/15px-OOjs_UI_icon_edit-ltr-progressive.svg.png 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/8/8a/OOjs_UI_icon_edit-ltr-progressive.svg/20px-OOjs_UI_icon_edit-ltr-progressive.svg.png 2x" data-file-width="20" data-file-height="20" /></a></span></div></th></tr><tr><th scope="row" class="navbox-group" style="width:1%">Narodne knjižnice</th><td class="navbox-list navbox-odd" style="text-align:left;border-left-width:2px;border-left-style:solid;width:100%;padding:0px"><div style="padding:0em 0.25em"> <ul><li><span class="uid"><a rel="nofollow" class="external text" href="https://catalogue.bnf.fr/ark:/12148/cb11944123k">Francija</a> <a rel="nofollow" class="external text" href="https://data.bnf.fr/ark:/12148/cb11944123k">(data)</a></span></li> <li><span class="uid"><a rel="nofollow" class="external text" href="http://esu.com.ua/search_articles.php?id=18003">Ukrajina</a></span></li> <li><span class="uid"><a rel="nofollow" class="external text" href="https://d-nb.info/gnd/4015366-6">Nemčija</a></span></li> <li><span class="uid"><a rel="nofollow" class="external text" href="http://uli.nli.org.il/F/?func=find-b&amp;local_base=NLX10&amp;find_code=UID&amp;request=987007553184905171">Izrael</a></span></li> <li><span class="uid"><a rel="nofollow" class="external text" href="https://id.loc.gov/authorities/subjects/sh85044667">ZDA</a></span></li> <li><span class="uid"><a rel="nofollow" class="external text" href="https://id.ndl.go.jp/auth/ndlna/00571149">Japonska</a></span></li> <li><span class="uid"><a rel="nofollow" class="external text" href="https://aleph.nkp.cz/F/?func=find-c&amp;local_base=aut&amp;ccl_term=ica=ph170599&amp;CON_LNG=ENG">Češka republika</a></span></li></ul> </div></td></tr><tr><th scope="row" class="navbox-group" style="width:1%">Drugo</th><td class="navbox-list navbox-even" style="text-align:left;border-left-width:2px;border-left-style:solid;width:100%;padding:0px"><div style="padding:0em 0.25em"> <ul><li><span class="uid"><a rel="nofollow" class="external text" href="http://id.worldcat.org/fast/914754/">Faceted Application of Subject Terminology</a></span></li> <li><span class="uid"><a rel="nofollow" class="external text" href="https://hls-dhs-dss.ch/fr/articles/007784">Zgodovinski leksikon Švice</a></span></li> <li><span class="uid"><a rel="nofollow" class="external text" href="https://catalog.archives.gov/id/10637801">National Archives (ZDA)</a></span></li></ul> </div></td></tr></tbody></table></div> <!-- NewPP limit report Parsed by mw‐web.eqiad.main‐5476bd94cd‐jdqvw Cached time: 20241111130608 Cache expiry: 2592000 Reduced expiry: false Complications: [show‐toc] CPU time usage: 0.334 seconds Real time usage: 0.762 seconds Preprocessor visited node count: 1338/1000000 Post‐expand include size: 47587/2097152 bytes Template argument size: 89/2097152 bytes Highest expansion depth: 8/100 Expensive parser function count: 10/500 Unstrip recursion depth: 1/20 Unstrip post‐expand size: 59725/5000000 bytes Lua time usage: 0.193/10.000 seconds Lua 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