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Mountain chain - Wikipedia
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class="vector-toc-list-item vector-toc-level-1 vector-toc-list-item-expanded"> <a class="vector-toc-link" href="#Literature"> <div class="vector-toc-text"> <span class="vector-toc-numb">5</span> <span>Literature</span> </div> </a> <ul id="toc-Literature-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="Contents" 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="Toggle the table of contents" > <label id="vector-page-titlebar-toc-label" for="vector-page-titlebar-toc-checkbox" class="vector-dropdown-label cdx-button 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Available in 17 languages" > <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-17" 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">17 languages</span> </label> <div class="vector-dropdown-content"> <div class="vector-menu-content"> <ul class="vector-menu-content-list"> <li class="interlanguage-link interwiki-an mw-list-item"><a href="https://an.wikipedia.org/wiki/Sierra" title="Sierra – Aragonese" lang="an" hreflang="an" data-title="Sierra" data-language-autonym="Aragonés" data-language-local-name="Aragonese" class="interlanguage-link-target"><span>Aragonés</span></a></li><li class="interlanguage-link interwiki-de mw-list-item"><a href="https://de.wikipedia.org/wiki/Gebirgszug" title="Gebirgszug – German" lang="de" hreflang="de" data-title="Gebirgszug" data-language-autonym="Deutsch" data-language-local-name="German" class="interlanguage-link-target"><span>Deutsch</span></a></li><li class="interlanguage-link interwiki-et mw-list-item"><a href="https://et.wikipedia.org/wiki/M%C3%A4eahelik" title="Mäeahelik – Estonian" lang="et" hreflang="et" data-title="Mäeahelik" data-language-autonym="Eesti" data-language-local-name="Estonian" class="interlanguage-link-target"><span>Eesti</span></a></li><li class="interlanguage-link interwiki-es mw-list-item"><a href="https://es.wikipedia.org/wiki/Sierra_(geograf%C3%ADa)" title="Sierra (geografía) – Spanish" lang="es" hreflang="es" data-title="Sierra (geografía)" data-language-autonym="Español" data-language-local-name="Spanish" class="interlanguage-link-target"><span>Español</span></a></li><li class="interlanguage-link interwiki-eu mw-list-item"><a href="https://eu.wikipedia.org/wiki/Mendilerro" title="Mendilerro – Basque" lang="eu" hreflang="eu" data-title="Mendilerro" data-language-autonym="Euskara" data-language-local-name="Basque" 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/%D8%B2%D9%86%D8%AC%DB%8C%D8%B1%D9%87_%DA%A9%D9%88%D9%87%DB%8C" title="زنجیره کوهی – Persian" lang="fa" hreflang="fa" data-title="زنجیره کوهی" data-language-autonym="فارسی" data-language-local-name="Persian" class="interlanguage-link-target"><span>فارسی</span></a></li><li class="interlanguage-link interwiki-fr mw-list-item"><a href="https://fr.wikipedia.org/wiki/Massif_de_montagnes" title="Massif de montagnes – French" lang="fr" hreflang="fr" data-title="Massif de montagnes" data-language-autonym="Français" data-language-local-name="French" class="interlanguage-link-target"><span>Français</span></a></li><li class="interlanguage-link interwiki-gl mw-list-item"><a href="https://gl.wikipedia.org/wiki/Serra_(xeograf%C3%ADa)" title="Serra (xeografía) – Galician" lang="gl" hreflang="gl" data-title="Serra (xeografía)" data-language-autonym="Galego" data-language-local-name="Galician" class="interlanguage-link-target"><span>Galego</span></a></li><li class="interlanguage-link interwiki-id badge-Q70893996 mw-list-item" title=""><a href="https://id.wikipedia.org/wiki/Jajaran_gunung" title="Jajaran gunung – Indonesian" lang="id" hreflang="id" data-title="Jajaran gunung" data-language-autonym="Bahasa Indonesia" data-language-local-name="Indonesian" class="interlanguage-link-target"><span>Bahasa Indonesia</span></a></li><li class="interlanguage-link interwiki-li mw-list-item"><a href="https://li.wikipedia.org/wiki/Bergkitting" title="Bergkitting – Limburgish" lang="li" hreflang="li" data-title="Bergkitting" data-language-autonym="Limburgs" data-language-local-name="Limburgish" class="interlanguage-link-target"><span>Limburgs</span></a></li><li class="interlanguage-link interwiki-mg mw-list-item"><a href="https://mg.wikipedia.org/wiki/Tangorom-bohitra" title="Tangorom-bohitra – Malagasy" lang="mg" hreflang="mg" data-title="Tangorom-bohitra" data-language-autonym="Malagasy" data-language-local-name="Malagasy" class="interlanguage-link-target"><span>Malagasy</span></a></li><li class="interlanguage-link interwiki-nl mw-list-item"><a href="https://nl.wikipedia.org/wiki/Bergketen" title="Bergketen – Dutch" lang="nl" hreflang="nl" data-title="Bergketen" data-language-autonym="Nederlands" data-language-local-name="Dutch" class="interlanguage-link-target"><span>Nederlands</span></a></li><li class="interlanguage-link interwiki-oc mw-list-item"><a href="https://oc.wikipedia.org/wiki/Mass%C3%ADs_de_montanha" title="Massís de montanha – Occitan" lang="oc" hreflang="oc" data-title="Massís de montanha" data-language-autonym="Occitan" data-language-local-name="Occitan" class="interlanguage-link-target"><span>Occitan</span></a></li><li class="interlanguage-link interwiki-pl mw-list-item"><a href="https://pl.wikipedia.org/wiki/Pasmo_g%C3%B3rskie" title="Pasmo górskie – Polish" lang="pl" hreflang="pl" data-title="Pasmo górskie" data-language-autonym="Polski" data-language-local-name="Polish" class="interlanguage-link-target"><span>Polski</span></a></li><li class="interlanguage-link interwiki-pt mw-list-item"><a href="https://pt.wikipedia.org/wiki/Serra" title="Serra – Portuguese" lang="pt" hreflang="pt" data-title="Serra" data-language-autonym="Português" data-language-local-name="Portuguese" class="interlanguage-link-target"><span>Português</span></a></li><li class="interlanguage-link interwiki-ru mw-list-item"><a href="https://ru.wikipedia.org/wiki/%D0%93%D1%80%D1%8F%D0%B4%D0%B0_(%D1%80%D0%B5%D0%BB%D1%8C%D0%B5%D1%84)" title="Гряда (рельеф) – Russian" lang="ru" hreflang="ru" data-title="Гряда (рельеф)" data-language-autonym="Русский" data-language-local-name="Russian" class="interlanguage-link-target"><span>Русский</span></a></li><li class="interlanguage-link interwiki-uk mw-list-item"><a href="https://uk.wikipedia.org/wiki/%D0%93%D1%96%D1%80%D1%81%D1%8C%D0%BA%D0%B5_%D0%BF%D0%B0%D1%81%D0%BC%D0%BE" title="Гірське пасмо – Ukrainian" lang="uk" hreflang="uk" data-title="Гірське пасмо" data-language-autonym="Українська" data-language-local-name="Ukrainian" class="interlanguage-link-target"><span>Українська</span></a></li> </ul> <div class="after-portlet after-portlet-lang"><span class="wb-langlinks-edit wb-langlinks-link"><a href="https://www.wikidata.org/wiki/Special:EntityPage/Q2624046#sitelinks-wikipedia" title="Edit interlanguage links" class="wbc-editpage">Edit links</a></span></div> </div> </div> </div> </header> <div class="vector-page-toolbar"> <div class="vector-page-toolbar-container"> <div id="left-navigation"> <nav aria-label="Namespaces"> <div id="p-associated-pages" class="vector-menu vector-menu-tabs mw-portlet mw-portlet-associated-pages" 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data-mw-ve-target-container> <div class="vector-body-before-content"> <div class="mw-indicators"> </div> <div id="siteSub" class="noprint">From Wikipedia, the free encyclopedia</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="en" dir="ltr"><div class="shortdescription nomobile noexcerpt noprint searchaux" style="display:none">Row of high mountain summits</div> <figure class="mw-default-size" typeof="mw:File/Thumb"><a href="/wiki/File:Zell-Pfarre_Peiner_Kobla_01.jpg" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/2/2a/Zell-Pfarre_Peiner_Kobla_01.jpg/260px-Zell-Pfarre_Peiner_Kobla_01.jpg" decoding="async" width="260" height="173" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/2/2a/Zell-Pfarre_Peiner_Kobla_01.jpg/390px-Zell-Pfarre_Peiner_Kobla_01.jpg 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/2/2a/Zell-Pfarre_Peiner_Kobla_01.jpg/520px-Zell-Pfarre_Peiner_Kobla_01.jpg 2x" data-file-width="3008" data-file-height="2000" /></a><figcaption>The <a href="/wiki/Karawanks" title="Karawanks">Karawanks</a>, a single, long mountain chain. This is the <a href="/w/index.php?title=Koschuta&action=edit&redlink=1" class="new" title="Koschuta (page does not exist)">Koschuta</a> ridge near Zell, <a href="/wiki/Carinthia" title="Carinthia">Carinthia</a></figcaption></figure> <p>A <b>mountain chain</b> is a row of high <a href="/wiki/Mountain_summit" class="mw-redirect" title="Mountain summit">mountain summits</a>, a linear sequence of interconnected or related mountains,<sup id="cite_ref-1" class="reference"><a href="#cite_note-1"><span class="cite-bracket">[</span>1<span class="cite-bracket">]</span></a></sup> or a contiguous ridge of mountains within a larger <a href="/wiki/Mountain_range" title="Mountain range">mountain range</a>. The term is also used for elongated <a href="/wiki/Fold_mountain" class="mw-redirect" title="Fold mountain">fold mountains</a> with several parallel chains ("chain mountains"). </p><p>While in mountain ranges, the term mountain chain is common, in hill ranges a sequence of <a href="/wiki/Hill" title="Hill">hills</a> tends to be referred to a <a href="/wiki/Ridge" title="Ridge">ridge</a> or <a href="/wiki/Hill_chain" title="Hill chain">hill chain</a>. </p><p>Elongated mountain chains occur most frequently in the <a href="/wiki/Orogeny" title="Orogeny">orogeny</a> of fold mountains, (that are folded by lateral pressure), and <a href="/wiki/Nappe" title="Nappe">nappe</a> belts (where a sheetlike body of rock has been pushed over another rock mass). Other types of range such as <a href="/wiki/Horst_(geology)" title="Horst (geology)">horst ranges</a>, <a href="/wiki/Fault_block" title="Fault block">fault block</a> mountain or <a href="/wiki/Truncated_upland" title="Truncated upland">truncated uplands</a> rarely form parallel mountain chains. However, if a truncated upland is eroded into a high <a href="/wiki/Table_land" class="mw-redirect" title="Table land">table land</a>, the incision of valleys can lead to the formations of mountain or hill chains. </p> <meta property="mw:PageProp/toc" /> <div class="mw-heading mw-heading2"><h2 id="Formation_of_parallel_mountain_chains">Formation of parallel mountain chains</h2><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Mountain_chain&action=edit&section=1" title="Edit section: Formation of parallel mountain chains"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <figure class="mw-default-size" typeof="mw:File/Thumb"><a href="/wiki/File:Satellitenaufnahme_der_Alpen.jpg" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/1/16/Satellitenaufnahme_der_Alpen.jpg/260px-Satellitenaufnahme_der_Alpen.jpg" decoding="async" width="260" height="201" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/1/16/Satellitenaufnahme_der_Alpen.jpg/390px-Satellitenaufnahme_der_Alpen.jpg 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/1/16/Satellitenaufnahme_der_Alpen.jpg/520px-Satellitenaufnahme_der_Alpen.jpg 2x" data-file-width="1000" data-file-height="773" /></a><figcaption>In this satellite image of the <a href="/wiki/Alps" title="Alps">Alps</a>, the snow limit picks out the individual mountain chains</figcaption></figure> <figure typeof="mw:File/Thumb"><a href="/wiki/File:%D0%A6%D0%B5%D0%BD%D1%82%D1%80%D0%B0%D0%BB%D0%B5%D0%BD_%D0%91%D0%B0%D0%BB%D0%BA%D0%B0%D0%BD.jpg" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/9/9a/%D0%A6%D0%B5%D0%BD%D1%82%D1%80%D0%B0%D0%BB%D0%B5%D0%BD_%D0%91%D0%B0%D0%BB%D0%BA%D0%B0%D0%BD.jpg/260px-%D0%A6%D0%B5%D0%BD%D1%82%D1%80%D0%B0%D0%BB%D0%B5%D0%BD_%D0%91%D0%B0%D0%BB%D0%BA%D0%B0%D0%BD.jpg" decoding="async" width="260" height="174" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/9/9a/%D0%A6%D0%B5%D0%BD%D1%82%D1%80%D0%B0%D0%BB%D0%B5%D0%BD_%D0%91%D0%B0%D0%BB%D0%BA%D0%B0%D0%BD.jpg/390px-%D0%A6%D0%B5%D0%BD%D1%82%D1%80%D0%B0%D0%BB%D0%B5%D0%BD_%D0%91%D0%B0%D0%BB%D0%BA%D0%B0%D0%BD.jpg 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/9/9a/%D0%A6%D0%B5%D0%BD%D1%82%D1%80%D0%B0%D0%BB%D0%B5%D0%BD_%D0%91%D0%B0%D0%BB%D0%BA%D0%B0%D0%BD.jpg/520px-%D0%A6%D0%B5%D0%BD%D1%82%D1%80%D0%B0%D0%BB%D0%B5%D0%BD_%D0%91%D0%B0%D0%BB%D0%BA%D0%B0%D0%BD.jpg 2x" data-file-width="3872" data-file-height="2592" /></a><figcaption>A view of the <a href="/wiki/Balkan_Mountains" title="Balkan Mountains">Balkan Mountains</a> chain</figcaption></figure> <p>The chain-like arrangement of summits and the formation of long, jagged <a href="/wiki/Mountain_crest" class="mw-redirect" title="Mountain crest">mountain crests</a> – known in Spanish as <a href="https://en.wiktionary.org/wiki/sierra#Spanish" class="extiw" title="wikt:sierra">sierras</a> ("saws") – is a consequence of their collective formation by <a href="/wiki/Orogeny" title="Orogeny">mountain building forces</a>. The often linear structure is linked to the direction of these thrust forces and the resulting <a href="/wiki/Folding_(geology)" class="mw-redirect" title="Folding (geology)">mountain folding</a> which in turn relates to the <a href="/wiki/Fault_line" class="mw-redirect" title="Fault line">fault lines</a> in the upper part of the <a href="/wiki/Earth%27s_crust" title="Earth's crust">Earth's crust</a>, that run between the individual mountain chains. In these <a href="/wiki/Fault_zone" class="mw-redirect" title="Fault zone">fault zones</a>, the rock, which has sometimes been pulverised, is easily eroded, so that large <a href="/wiki/River" title="River">river</a> valleys are carved out. These, so called <a href="/wiki/Longitudinal_valley" title="Longitudinal valley">longitudinal valleys</a> reinforce the trend, during the early mountain building phase, towards the formation of parallel chains of mountains. </p><p>The tendency, especially of fold mountains (e. g. the <a href="/wiki/Cordilleras" class="mw-redirect" title="Cordilleras">Cordilleras</a>) to produce roughly parallel chains is due to their rock structure and the propulsive forces of <a href="/wiki/Plate_tectonics" title="Plate tectonics">plate tectonics</a>. The uplifted rock masses are either magmatic <a href="/wiki/Plutonic_rock" class="mw-redirect" title="Plutonic rock">plutonic rocks</a>, easily shaped because of their higher temperature, or <a href="/wiki/Sediment" title="Sediment">sediments</a> or <a href="/wiki/Metamorphic_rock" title="Metamorphic rock">metamorphic rocks</a>, which have a less robust structure, that are deposited in the <a href="/wiki/Syncline" title="Syncline">synclines</a>. As a result of orogenic movements, strata of folded rock are formed that are crumpled out of their original horizontal plane and thrust against one another. The longitudinal stretching of the folds takes place at right angles to the direction of the lateral thrusting. The <a href="/wiki/Overthrust" class="mw-redirect" title="Overthrust">overthrust</a> folds of a <a href="/wiki/Nappe" title="Nappe">nappe</a> belt (e.g. the <a href="/wiki/Central_Alps" class="mw-redirect" title="Central Alps">Central Alps</a>) are formed in a similar way. </p><p>Although the fold mountains, chain mountains and nappe belts around the world were formed at different times in the Earth's history, all during their initial mountain building phases, they are nevertheless morphologically similar. Harder rock forms continuous <a href="/wiki/Ar%C3%AAte" title="Arête">arêtes</a> or ridges that follow the <a href="/wiki/Strike_(geology)" class="mw-redirect" title="Strike (geology)">strike</a> of the beds and folds. The mountain chains or ridges therefore run approximately parallel to one another. They are only interrupted by short, usually narrow, <a href="/wiki/Transverse_valley" title="Transverse valley">transverse valleys</a>, which often form <a href="/wiki/Water_gap" title="Water gap">water gaps</a>. During the course of Earth history, <a href="/wiki/Erosion_(geology)" class="mw-redirect" title="Erosion (geology)">erosion</a> by water, ice and wind carried away the highest points of the mountain crests and carved out individual summits or <a href="/wiki/Double_summit" title="Double summit">summit chains</a>. Between them, notches were formed that, depending on <a href="/wiki/Altitudinal_zonation" title="Altitudinal zonation">altitude</a> and rock-type, form knife-edged <a href="/wiki/Col" title="Col">cols</a> or gentler <a href="/wiki/Mountain_pass" title="Mountain pass">mountain passes</a> and <a href="/wiki/Saddle_(geology)" class="mw-redirect" title="Saddle (geology)">saddles</a>. </p> <div class="mw-heading mw-heading2"><h2 id="Dominant_rocks_and_mountain_forms">Dominant rocks and mountain forms</h2><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Mountain_chain&action=edit&section=2" title="Edit section: Dominant rocks and mountain forms"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <figure class="mw-default-size" typeof="mw:File/Thumb"><a href="/wiki/File:Vedauwoo_Rocks_in_winter.jpg" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/b/b6/Vedauwoo_Rocks_in_winter.jpg/260px-Vedauwoo_Rocks_in_winter.jpg" decoding="async" width="260" height="132" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/b/b6/Vedauwoo_Rocks_in_winter.jpg/390px-Vedauwoo_Rocks_in_winter.jpg 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/b/b6/Vedauwoo_Rocks_in_winter.jpg/520px-Vedauwoo_Rocks_in_winter.jpg 2x" data-file-width="730" data-file-height="371" /></a><figcaption>The remains of an old mountain chain in the <a href="/wiki/Laramie_Mountains" title="Laramie Mountains">Laramie Mountains</a>, Colorado</figcaption></figure> <p>Nappe or fold mountains, with their roughly parallel mountain chains, generally have a common <a href="/wiki/Geological" class="mw-redirect" title="Geological">geological</a> age, but may consist of various types of <a href="/wiki/Rock_(geology)" title="Rock (geology)">rock</a>. For example, in the Central Alps, <a href="/wiki/Granite" title="Granite">granitic</a> rocks, <a href="/wiki/Gneiss" title="Gneiss">gneisses</a> and metamorphic <a href="/wiki/Slate" title="Slate">slate</a> are found, while to the north and south, are the <a href="/wiki/Limestone_Alps" title="Limestone Alps">Limestone Alps</a>. The <a href="/wiki/Northern_Limestone_Alps" title="Northern Limestone Alps">Northern Limestone Alps</a> are, in turn, followed by soft <a href="/wiki/Flysch" title="Flysch">flysch</a> mountains and the <a href="/wiki/Molasse" title="Molasse">molasse</a> zone. </p><p>The type of rock influences the appearance of the mountain ranges very markedly, because <a href="/wiki/Erosion_(geology)" class="mw-redirect" title="Erosion (geology)">erosion</a> leads to very different topography depending on the <a href="/wiki/Hardness" title="Hardness">hardness</a> of the rock and its <a href="/wiki/Petrological" class="mw-redirect" title="Petrological">petrological</a> structure. In addition to height and climate, other factors are the <a href="/wiki/Strata" class="mw-redirect" title="Strata">layering</a> of the rock, its <a href="/wiki/Gradient" title="Gradient">gradient</a> and <a href="/wiki/Aspect_(geography)" title="Aspect (geography)">aspect</a>, the types of <a href="/wiki/Waterbody" class="mw-redirect" title="Waterbody">waterbody</a> and the lines of <a href="/wiki/Dislocation" title="Dislocation">dislocation</a>. For hard rock massifs, rugged rock faces (e.g. in the <a href="/wiki/Dolomites" title="Dolomites">Dolomites</a>) and mighty <a href="/wiki/Scree" title="Scree">scree</a> slopes are typical. By contrast, flysch or slate forms gentler mountain shapes and <i><a href="/wiki/Kuppen" class="mw-redirect" title="Kuppen">kuppen</a></i> or domed mountaintops, because the rock is not porous, but easily shaped. </p> <div class="mw-heading mw-heading2"><h2 id="See_also">See also</h2><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Mountain_chain&action=edit&section=3" title="Edit section: See also"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <ul><li><a href="/wiki/Orogeny" title="Orogeny">Orogeny</a></li> <li><a href="/wiki/Tectonics" title="Tectonics">Tectonics</a></li> <li><a href="/wiki/List_of_highest_mountains_on_Earth" title="List of highest mountains on Earth">List of highest mountains on Earth</a></li> <li><a href="/wiki/List_of_mountain_ranges" title="List of mountain ranges">List of mountain ranges</a></li></ul> <div class="mw-heading mw-heading2"><h2 id="References">References</h2><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Mountain_chain&action=edit&section=4" title="Edit section: References"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <style data-mw-deduplicate="TemplateStyles:r1239543626">.mw-parser-output .reflist{margin-bottom:0.5em;list-style-type:decimal}@media screen{.mw-parser-output .reflist{font-size:90%}}.mw-parser-output .reflist .references{font-size:100%;margin-bottom:0;list-style-type:inherit}.mw-parser-output .reflist-columns-2{column-width:30em}.mw-parser-output .reflist-columns-3{column-width:25em}.mw-parser-output .reflist-columns{margin-top:0.3em}.mw-parser-output .reflist-columns ol{margin-top:0}.mw-parser-output .reflist-columns li{page-break-inside:avoid;break-inside:avoid-column}.mw-parser-output .reflist-upper-alpha{list-style-type:upper-alpha}.mw-parser-output .reflist-upper-roman{list-style-type:upper-roman}.mw-parser-output .reflist-lower-alpha{list-style-type:lower-alpha}.mw-parser-output .reflist-lower-greek{list-style-type:lower-greek}.mw-parser-output .reflist-lower-roman{list-style-type:lower-roman}</style><div class="reflist"> <div class="mw-references-wrap"><ol class="references"> <li id="cite_note-1"><span class="mw-cite-backlink"><b><a href="#cite_ref-1">^</a></b></span> <span class="reference-text">Whittow, John (1984). <i>Dictionary of Physical Geography</i>. London: Penguin, p 87. <style data-mw-deduplicate="TemplateStyles:r1238218222">.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.id-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.id-lock-limited a,.mw-parser-output .id-lock-registration.id-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.id-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}body:not(.skin-timeless):not(.skin-minerva) .mw-parser-output .id-lock-free a,body:not(.skin-timeless):not(.skin-minerva) .mw-parser-output .id-lock-limited a,body:not(.skin-timeless):not(.skin-minerva) .mw-parser-output .id-lock-registration a,body:not(.skin-timeless):not(.skin-minerva) .mw-parser-output .id-lock-subscription a,body:not(.skin-timeless):not(.skin-minerva) .mw-parser-output .cs1-ws-icon a{background-size:contain;padding:0 1em 0 0}.mw-parser-output .cs1-code{color:inherit;background:inherit;border:none;padding:inherit}.mw-parser-output .cs1-hidden-error{display:none;color:var(--color-error,#d33)}.mw-parser-output .cs1-visible-error{color:var(--color-error,#d33)}.mw-parser-output .cs1-maint{display:none;color:#085;margin-left:0.3em}.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}@media screen{.mw-parser-output .cs1-format{font-size:95%}html.skin-theme-clientpref-night .mw-parser-output .cs1-maint{color:#18911f}}@media screen and (prefers-color-scheme:dark){html.skin-theme-clientpref-os .mw-parser-output .cs1-maint{color:#18911f}}</style><a href="/wiki/ISBN_(identifier)" class="mw-redirect" title="ISBN (identifier)">ISBN</a> <a href="/wiki/Special:BookSources/0-14-051094-X" title="Special:BookSources/0-14-051094-X">0-14-051094-X</a>.</span> </li> </ol></div></div> <div class="mw-heading mw-heading2"><h2 id="Literature">Literature</h2><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Mountain_chain&action=edit&section=5" title="Edit section: Literature"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <ul><li><i>Wissen heute: Geologie</i>. Kaiser-Verlag, Florence/Klagenfurt, 1995</li> <li><i>Der geologische Aufbau Österreichs</i>. Geologische Bundesanstalt, Springer-Verlag Vienna/ New York</li> <li>PanGeo, <i>Erdwissenschaften in Österreich</i>. Conference proceedings, 200 pp., Sessions on the Neogene, TRANSALP I and II. Univ. Salzburg, 2005</li> <li><i>Fischer-Lexikon Geographie</i>, pp. 101–129, Frankfurt, 1959</li> <li><i>Großer Weltatlas, Enzyklopädischer Teil</i> (mountain building, folds and faults, the rock cycle). Publ. ÖAMTC, Vienna, ~1980</li> <li>André Cailleux: <i>Der unbekannte Planet: Anatomie der Erde</i>. Kindlers Universitätsbibliothek, Munich, 1968, Chapters 1 and 3</li> <li><i><a rel="nofollow" class="external text" href="http://www.zeno.org/Lueger-1904/A/Gebirge">Gebirge</a></i>, in: Lueger, Otto: <i>Lexikon der gesamten Technik und ihrer Hilfswissenschaften</i>, Vol. 4 Stuttgart, Leipzig, 1906, pp. <a rel="nofollow" class="external text" href="http://www.zeno.org/Lueger-1904/K/lueger-1904-041-0316">316</a>-<a rel="nofollow" class="external text" href="http://www.zeno.org/Lueger-1904/K/lueger-1904-041-0317">317</a>.</li></ul> <div class="navbox-styles"><style data-mw-deduplicate="TemplateStyles:r1129693374">.mw-parser-output .hlist dl,.mw-parser-output .hlist ol,.mw-parser-output .hlist ul{margin:0;padding:0}.mw-parser-output .hlist dd,.mw-parser-output .hlist dt,.mw-parser-output .hlist li{margin:0;display:inline}.mw-parser-output .hlist.inline,.mw-parser-output .hlist.inline dl,.mw-parser-output .hlist.inline ol,.mw-parser-output .hlist.inline ul,.mw-parser-output .hlist dl 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