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Hornfels - Wikipedia
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class="vector-toc-link" href="#Mafic"> <div class="vector-toc-text"> <span class="vector-toc-numb">2.3</span> <span>Mafic</span> </div> </a> <ul id="toc-Mafic-sublist" class="vector-toc-list"> </ul> </li> </ul> </li> <li id="toc-Facies" class="vector-toc-list-item vector-toc-level-1 vector-toc-list-item-expanded"> <a class="vector-toc-link" href="#Facies"> <div class="vector-toc-text"> <span class="vector-toc-numb">3</span> <span>Facies</span> </div> </a> <ul id="toc-Facies-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-Acoustic_properties" class="vector-toc-list-item vector-toc-level-1 vector-toc-list-item-expanded"> <a class="vector-toc-link" href="#Acoustic_properties"> <div class="vector-toc-text"> <span class="vector-toc-numb">4</span> <span>Acoustic properties</span> </div> </a> <ul id="toc-Acoustic_properties-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-See_also" class="vector-toc-list-item vector-toc-level-1 vector-toc-list-item-expanded"> <a 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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" title="Table of Contents" > <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 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">Toggle the table of contents</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">Hornfels</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="Go to an article in another language. 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href="https://cs.wikipedia.org/wiki/Kontaktn%C3%AD_rohovec" title="Kontaktní rohovec – Czech" lang="cs" hreflang="cs" data-title="Kontaktní rohovec" data-language-autonym="Čeština" data-language-local-name="Czech" class="interlanguage-link-target"><span>Čeština</span></a></li><li class="interlanguage-link interwiki-de mw-list-item"><a href="https://de.wikipedia.org/wiki/Hornfels" title="Hornfels – German" lang="de" hreflang="de" data-title="Hornfels" 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/Sarvkivi" title="Sarvkivi – Estonian" lang="et" hreflang="et" data-title="Sarvkivi" 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/Corneana" title="Corneana – Spanish" lang="es" hreflang="es" data-title="Corneana" data-language-autonym="Español" data-language-local-name="Spanish" class="interlanguage-link-target"><span>Español</span></a></li><li class="interlanguage-link interwiki-fa mw-list-item"><a href="https://fa.wikipedia.org/wiki/%D9%87%D9%88%D8%B1%D9%86%D9%81%D9%84%D8%B3" title="هورنفلس – Persian" lang="fa" hreflang="fa" data-title="هورنفلس" 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/Corn%C3%A9enne" title="Cornéenne – French" lang="fr" hreflang="fr" data-title="Cornéenne" data-language-autonym="Français" data-language-local-name="French" class="interlanguage-link-target"><span>Français</span></a></li><li class="interlanguage-link interwiki-ko mw-list-item"><a href="https://ko.wikipedia.org/wiki/%ED%98%BC%ED%8E%A0%EC%8A%A4" title="혼펠스 – Korean" lang="ko" hreflang="ko" data-title="혼펠스" data-language-autonym="한국어" data-language-local-name="Korean" class="interlanguage-link-target"><span>한국어</span></a></li><li class="interlanguage-link interwiki-id mw-list-item"><a href="https://id.wikipedia.org/wiki/Batutanduk" title="Batutanduk – Indonesian" lang="id" hreflang="id" data-title="Batutanduk" 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-it mw-list-item"><a href="https://it.wikipedia.org/wiki/Cornubianite" title="Cornubianite – Italian" lang="it" hreflang="it" data-title="Cornubianite" data-language-autonym="Italiano" data-language-local-name="Italian" class="interlanguage-link-target"><span>Italiano</span></a></li><li class="interlanguage-link interwiki-he mw-list-item"><a href="https://he.wikipedia.org/wiki/%D7%94%D7%95%D7%A8%D7%A0%D7%A4%D7%9C%D7%A1" title="הורנפלס – Hebrew" lang="he" hreflang="he" data-title="הורנפלס" data-language-autonym="עברית" data-language-local-name="Hebrew" class="interlanguage-link-target"><span>עברית</span></a></li><li class="interlanguage-link interwiki-ka mw-list-item"><a href="https://ka.wikipedia.org/wiki/%E1%83%A0%E1%83%A5%E1%83%90%E1%83%A3%E1%83%9A%E1%83%90" title="რქაულა – Georgian" lang="ka" hreflang="ka" data-title="რქაულა" data-language-autonym="ქართული" data-language-local-name="Georgian" class="interlanguage-link-target"><span>ქართული</span></a></li><li class="interlanguage-link interwiki-kw mw-list-item"><a href="https://kw.wikipedia.org/wiki/Hornven" title="Hornven – Cornish" lang="kw" hreflang="kw" data-title="Hornven" data-language-autonym="Kernowek" data-language-local-name="Cornish" class="interlanguage-link-target"><span>Kernowek</span></a></li><li class="interlanguage-link interwiki-ky mw-list-item"><a href="https://ky.wikipedia.org/wiki/%D0%A0%D0%BE%D0%B3%D0%BE%D0%B2%D0%B8%D0%BA" title="Роговик – Kyrgyz" lang="ky" hreflang="ky" data-title="Роговик" data-language-autonym="Кыргызча" data-language-local-name="Kyrgyz" class="interlanguage-link-target"><span>Кыргызча</span></a></li><li class="interlanguage-link interwiki-hu mw-list-item"><a href="https://hu.wikipedia.org/wiki/Szaruszirt" title="Szaruszirt – Hungarian" lang="hu" hreflang="hu" data-title="Szaruszirt" data-language-autonym="Magyar" data-language-local-name="Hungarian" class="interlanguage-link-target"><span>Magyar</span></a></li><li class="interlanguage-link interwiki-nl mw-list-item"><a href="https://nl.wikipedia.org/wiki/Hoornrots" title="Hoornrots – Dutch" lang="nl" hreflang="nl" data-title="Hoornrots" data-language-autonym="Nederlands" data-language-local-name="Dutch" class="interlanguage-link-target"><span>Nederlands</span></a></li><li class="interlanguage-link interwiki-ja mw-list-item"><a href="https://ja.wikipedia.org/wiki/%E3%83%9B%E3%83%AB%E3%83%B3%E3%83%95%E3%82%A7%E3%83%AB%E3%82%B9" title="ホルンフェルス – Japanese" lang="ja" hreflang="ja" data-title="ホルンフェルス" data-language-autonym="日本語" data-language-local-name="Japanese" class="interlanguage-link-target"><span>日本語</span></a></li><li class="interlanguage-link interwiki-no mw-list-item"><a href="https://no.wikipedia.org/wiki/Hornfels" title="Hornfels – Norwegian Bokmål" lang="nb" hreflang="nb" data-title="Hornfels" data-language-autonym="Norsk bokmål" data-language-local-name="Norwegian Bokmål" class="interlanguage-link-target"><span>Norsk bokmål</span></a></li><li class="interlanguage-link interwiki-nn mw-list-item"><a href="https://nn.wikipedia.org/wiki/Hornfels" title="Hornfels – Norwegian Nynorsk" lang="nn" hreflang="nn" data-title="Hornfels" data-language-autonym="Norsk nynorsk" data-language-local-name="Norwegian Nynorsk" class="interlanguage-link-target"><span>Norsk nynorsk</span></a></li><li class="interlanguage-link interwiki-pl mw-list-item"><a href="https://pl.wikipedia.org/wiki/Hornfels" title="Hornfels – Polish" lang="pl" hreflang="pl" data-title="Hornfels" 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/Corneana" title="Corneana – Portuguese" lang="pt" hreflang="pt" data-title="Corneana" 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%A0%D0%BE%D0%B3%D0%BE%D0%B2%D0%B8%D0%BA" title="Роговик – Russian" lang="ru" hreflang="ru" data-title="Роговик" data-language-autonym="Русский" data-language-local-name="Russian" class="interlanguage-link-target"><span>Русский</span></a></li><li class="interlanguage-link interwiki-sk mw-list-item"><a href="https://sk.wikipedia.org/wiki/Kontaktn%C3%BD_rohovec" title="Kontaktný rohovec – Slovak" lang="sk" hreflang="sk" data-title="Kontaktný rohovec" data-language-autonym="Slovenčina" data-language-local-name="Slovak" class="interlanguage-link-target"><span>Slovenčina</span></a></li><li class="interlanguage-link interwiki-fi mw-list-item"><a href="https://fi.wikipedia.org/wiki/Hornfels" title="Hornfels – Finnish" lang="fi" hreflang="fi" data-title="Hornfels" data-language-autonym="Suomi" data-language-local-name="Finnish" class="interlanguage-link-target"><span>Suomi</span></a></li><li class="interlanguage-link interwiki-sv mw-list-item"><a href="https://sv.wikipedia.org/wiki/Hornfels" title="Hornfels – Swedish" lang="sv" hreflang="sv" data-title="Hornfels" data-language-autonym="Svenska" data-language-local-name="Swedish" class="interlanguage-link-target"><span>Svenska</span></a></li><li class="interlanguage-link interwiki-uk mw-list-item"><a href="https://uk.wikipedia.org/wiki/%D0%A0%D0%BE%D0%B3%D0%BE%D0%B2%D0%B8%D0%BA_(%D0%BF%D0%BE%D1%80%D0%BE%D0%B4%D0%B0)" title="Роговик (порода) – Ukrainian" lang="uk" hreflang="uk" data-title="Роговик (порода)" data-language-autonym="Українська" data-language-local-name="Ukrainian" class="interlanguage-link-target"><span>Українська</span></a></li><li class="interlanguage-link interwiki-vi mw-list-item"><a href="https://vi.wikipedia.org/wiki/%C4%90%C3%A1_s%E1%BB%ABng" title="Đá sừng – Vietnamese" lang="vi" hreflang="vi" data-title="Đá sừng" data-language-autonym="Tiếng Việt" data-language-local-name="Vietnamese" class="interlanguage-link-target"><span>Tiếng Việt</span></a></li><li class="interlanguage-link interwiki-zh mw-list-item"><a href="https://zh.wikipedia.org/wiki/%E8%A7%92%E5%B2%A9" title="角岩 – Chinese" lang="zh" hreflang="zh" data-title="角岩" data-language-autonym="中文" data-language-local-name="Chinese" class="interlanguage-link-target"><span>中文</span></a></li> </ul> <div class="after-portlet after-portlet-lang"><span class="wb-langlinks-edit wb-langlinks-link"><a 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class="vector-pinnable-header-toggle-button vector-pinnable-header-pin-button" data-event-name="pinnable-header.vector-appearance.pin">move to sidebar</button> <button class="vector-pinnable-header-toggle-button vector-pinnable-header-unpin-button" data-event-name="pinnable-header.vector-appearance.unpin">hide</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">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">Group of metamorphic rocks</div> <figure class="mw-default-size" typeof="mw:File/Thumb"><a href="/wiki/File:Hornfels.jpg" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/7/71/Hornfels.jpg/220px-Hornfels.jpg" decoding="async" width="220" height="241" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/7/71/Hornfels.jpg/330px-Hornfels.jpg 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/7/71/Hornfels.jpg/440px-Hornfels.jpg 2x" data-file-width="1184" data-file-height="1296" /></a><figcaption>A sample of banded hornfels, formed by contact metamorphism of <a href="/wiki/Sandstone" title="Sandstone">sandstones</a> and <a href="/wiki/Shale" title="Shale">shales</a> by a <a href="/wiki/Granite" title="Granite">granite</a> <a href="/wiki/Intrusion" class="mw-redirect" title="Intrusion">intrusion</a></figcaption></figure> <p><b>Hornfels</b> is the group name for a set of <a href="/wiki/Metamorphism#Contact_.28thermal.29" title="Metamorphism">contact metamorphic</a> rocks that have been baked and hardened by the heat of <a href="/wiki/Intrusive_rock" title="Intrusive rock">intrusive igneous</a> masses and have been rendered massive, hard, splintery, and in some cases exceedingly tough and durable.<sup id="cite_ref-eb1911_1-0" class="reference"><a href="#cite_note-eb1911-1"><span class="cite-bracket">[</span>1<span class="cite-bracket">]</span></a></sup> These properties are caused by fine grained non-aligned crystals with platy or prismatic <a href="/wiki/Crystal_habit" title="Crystal habit">habits</a>, characteristic of metamorphism at high temperature but without accompanying deformation.<sup id="cite_ref-yardley-1989-12_2-0" class="reference"><a href="#cite_note-yardley-1989-12-2"><span class="cite-bracket">[</span>2<span class="cite-bracket">]</span></a></sup><sup id="cite_ref-blatt-tracy-1996-367-512_3-0" class="reference"><a href="#cite_note-blatt-tracy-1996-367-512-3"><span class="cite-bracket">[</span>3<span class="cite-bracket">]</span></a></sup><sup id="cite_ref-philpotts-ague-2009-422-428_4-0" class="reference"><a href="#cite_note-philpotts-ague-2009-422-428-4"><span class="cite-bracket">[</span>4<span class="cite-bracket">]</span></a></sup> The term is derived from the German word <i>Hornfels</i>, meaning "hornstone", because of its exceptional toughness and texture both reminiscent of animal horns. These rocks were referred to by miners in northern <a href="/wiki/England" title="England">England</a> as <a href="/wiki/Sharpening_stone" title="Sharpening stone">whetstones</a>.<sup id="cite_ref-5" class="reference"><a href="#cite_note-5"><span class="cite-bracket">[</span>5<span class="cite-bracket">]</span></a></sup><sup id="cite_ref-6" class="reference"><a href="#cite_note-6"><span class="cite-bracket">[</span>6<span class="cite-bracket">]</span></a></sup> </p><p>Most hornfels are fine-grained, and while the original rocks (such as <a href="/wiki/Sandstone" title="Sandstone">sandstone</a>, <a href="/wiki/Shale" title="Shale">shale</a>, <a href="/wiki/Slate" title="Slate">slate</a> and <a href="/wiki/Limestone" title="Limestone">limestone</a>) may have been more or less fissile owing to the presence of bedding or <a href="/wiki/Cleavage_(geology)" title="Cleavage (geology)">cleavage</a> planes, this structure is effaced or rendered inoperative in the hornfels. Though many hornfels show vestiges of the original bedding,<sup id="cite_ref-yardley-1989-12_2-1" class="reference"><a href="#cite_note-yardley-1989-12-2"><span class="cite-bracket">[</span>2<span class="cite-bracket">]</span></a></sup> they break across this as readily as along it; in fact, they tend to separate into cubical fragments rather than into thin plates.<sup id="cite_ref-eb1911_1-1" class="reference"><a href="#cite_note-eb1911-1"><span class="cite-bracket">[</span>1<span class="cite-bracket">]</span></a></sup> Sheet minerals may be abundant but are aligned at random.<sup id="cite_ref-nesse-2000-195_7-0" class="reference"><a href="#cite_note-nesse-2000-195-7"><span class="cite-bracket">[</span>7<span class="cite-bracket">]</span></a></sup> </p><p>Hornfels most commonly form in the <a href="/wiki/Metamorphic_aureole" class="mw-redirect" title="Metamorphic aureole">aureole</a> of <a href="/wiki/Granitoid" title="Granitoid">granitic</a> intrusions in the upper or middle crust. Hornfels formed from contact metamorphism by volcanic activity very close to the surface can produce unusual and distinctive minerals.<sup id="cite_ref-yardley-1989-12_2-2" class="reference"><a href="#cite_note-yardley-1989-12-2"><span class="cite-bracket">[</span>2<span class="cite-bracket">]</span></a></sup><sup id="cite_ref-blatt-tracy-1996-367-512_3-1" class="reference"><a href="#cite_note-blatt-tracy-1996-367-512-3"><span class="cite-bracket">[</span>3<span class="cite-bracket">]</span></a></sup> Changes in composition caused by fluids given off by the <a href="/wiki/Magmatic" class="mw-redirect" title="Magmatic">magmatic</a> body (<a href="/wiki/Metasomatism" title="Metasomatism">metasomatism</a>) sometimes take place.<sup id="cite_ref-harry-1952_8-0" class="reference"><a href="#cite_note-harry-1952-8"><span class="cite-bracket">[</span>8<span class="cite-bracket">]</span></a></sup> The <i>hornfels facies</i> is the <a href="/wiki/Metamorphic_facies" title="Metamorphic facies">metamorphic facies</a> which occupies the lowest pressure portion of the metamorphic pressure-temperature space.<sup id="cite_ref-blatt-tracy-1996-378-380-512_9-0" class="reference"><a href="#cite_note-blatt-tracy-1996-378-380-512-9"><span class="cite-bracket">[</span>9<span class="cite-bracket">]</span></a></sup> </p><p>The most common hornfels (the <a href="/wiki/Biotite" title="Biotite">biotite</a> hornfels) are dark-brown to black with a somewhat velvety <a href="/wiki/Lustre_(mineralogy)" title="Lustre (mineralogy)">luster</a> owing to the abundance of small <a href="/wiki/Crystal" title="Crystal">crystals</a> of shining black <a href="/wiki/Mica" title="Mica">mica</a>. Also, most common hornfels have a black streak. The <a href="/wiki/Lime_(mineral)" class="mw-redirect" title="Lime (mineral)">lime</a> hornfels are often white, yellow, pale-green, brown and other colors. Green and dark-green are the prevalent tints of the hornfels produced by the alteration of <a href="/wiki/Igneous_rock" title="Igneous rock">igneous rocks</a>. Although for the most part the constituent grains are too small to be determined by the unaided eye, there are often larger crystals (<a href="/wiki/Porphyroblast" title="Porphyroblast">porphyroblasts</a>) of <a href="/wiki/Cordierite" title="Cordierite">cordierite</a>, <a href="/wiki/Garnet" title="Garnet">garnet</a> or <a href="/wiki/Andalusite" title="Andalusite">andalusite</a> scattered through the fine matrix, and these may become very prominent on the <a href="/wiki/Weathering" title="Weathering">weathered</a> faces of the rock.<sup id="cite_ref-eb1911_1-2" class="reference"><a href="#cite_note-eb1911-1"><span class="cite-bracket">[</span>1<span class="cite-bracket">]</span></a></sup><sup id="cite_ref-yardley-1989-161_10-0" class="reference"><a href="#cite_note-yardley-1989-161-10"><span class="cite-bracket">[</span>10<span class="cite-bracket">]</span></a></sup> </p> <meta property="mw:PageProp/toc" /> <div class="mw-heading mw-heading2"><h2 id="Structure">Structure</h2><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Hornfels&action=edit&section=1" title="Edit section: Structure"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <p>The structure of the hornfels is very characteristic. Very rarely do any of the minerals show crystalline form, but the small grains fit closely together like the fragments of a mosaic; they are usually of nearly equal dimensions. This has been called pflaster or pavement structure from the resemblance to rough pavement work. Each <a href="/wiki/Mineral" title="Mineral">mineral</a> may also enclose particles of the others; in <a href="/wiki/Quartz" title="Quartz">quartz</a>, for example, small crystals of <a href="/wiki/Graphite" title="Graphite">graphite</a>, biotite, <a href="/wiki/Iron_oxide" title="Iron oxide">iron oxides</a>, sillimanite or feldspar may appear in great numbers. Often the whole of the grains are rendered semi-opaque in this way. The minutest crystals may show traces of crystalline outlines; undoubtedly they are of new formation and have originated <i>in situ</i>. This leads us to believe that the whole rock has been <a href="/wiki/Recrystallization_(geology)" title="Recrystallization (geology)">recrystallized</a> at a high temperature and in the solid state so that there was little freedom for the mineral <a href="/wiki/Molecule" title="Molecule">molecules</a> to build up well-individualized crystals. The regeneration of the rock has been sufficient to efface most of the original structures and to replace the former minerals more-or-less completely by new ones. But crystallization has been hampered by the solid condition of the mass and the new minerals are formless and have been unable to reject impurities, but have grown around them.<sup id="cite_ref-eb1911_1-3" class="reference"><a href="#cite_note-eb1911-1"><span class="cite-bracket">[</span>1<span class="cite-bracket">]</span></a></sup> </p> <div class="mw-heading mw-heading2"><h2 id="Compositions">Compositions</h2><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Hornfels&action=edit&section=2" title="Edit section: Compositions"><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:Corneenne_dielette_manche.jpg" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/8/8e/Corneenne_dielette_manche.jpg/220px-Corneenne_dielette_manche.jpg" decoding="async" width="220" height="165" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/8/8e/Corneenne_dielette_manche.jpg/330px-Corneenne_dielette_manche.jpg 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/8/8e/Corneenne_dielette_manche.jpg/440px-Corneenne_dielette_manche.jpg 2x" data-file-width="2592" data-file-height="1944" /></a><figcaption>Hornfels sample (Normandy, France)</figcaption></figure> <div class="mw-heading mw-heading3"><h3 id="Pelitic">Pelitic</h3><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Hornfels&action=edit&section=3" title="Edit section: Pelitic"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <p><a href="/wiki/Clay" title="Clay">Clays</a>, sedimentary slates and shales yield biotite hornfels in which the most conspicuous mineral is biotite mica, the small scales of which are transparent under the microscope and have a dark reddish-brown color and strong <a href="/wiki/Dichroism" title="Dichroism">dichroism</a>. There is also quartz, and often a considerable amount of feldspar, while graphite, <a href="/wiki/Tourmaline" title="Tourmaline">tourmaline</a> and iron oxides frequently occur in lesser quantity. In these biotite hornfels the minerals, which consist of aluminium silicates, are commonly found; they are usually andalusite and <a href="/wiki/Sillimanite" title="Sillimanite">sillimanite</a>, but <a href="/wiki/Kyanite" title="Kyanite">kyanite</a> appears also in hornfels, especially in those that have a <a href="/wiki/Schist" title="Schist">schistose</a> character. The andalusite may be pink and is then often <a href="/wiki/Pleochroic" class="mw-redirect" title="Pleochroic">pleochroic</a> in thin sections, or it may be white with the cross-shaped dark enclosures of the matrix that are characteristic of <a href="/wiki/Chiastolite" title="Chiastolite">chiastolite</a>. Sillimanite usually forms exceedingly minute needles embedded in quartz.<sup id="cite_ref-eb1911_1-4" class="reference"><a href="#cite_note-eb1911-1"><span class="cite-bracket">[</span>1<span class="cite-bracket">]</span></a></sup> </p><p>In the rocks of this group cordierite also occurs, not rarely, and may have the outlines of imperfect hexagonal prisms that are divided up into six sectors when seen in polarized light. In biotite hornfels, a faint striping may indicate the original bedding of the unaltered rock and corresponds to small changes in the nature of the <a href="/wiki/Sediment" title="Sediment">sediment</a> deposited. More commonly there is a distinct spotting, visible on the surfaces of the hand specimens. The spots are round or elliptical, and may be paler or darker than the rest of the rock.<sup id="cite_ref-eb1911_1-5" class="reference"><a href="#cite_note-eb1911-1"><span class="cite-bracket">[</span>1<span class="cite-bracket">]</span></a></sup> In some cases they are rich in graphite or carbonaceous matter;<sup id="cite_ref-dickey-obata-1974_11-0" class="reference"><a href="#cite_note-dickey-obata-1974-11"><span class="cite-bracket">[</span>11<span class="cite-bracket">]</span></a></sup> in others they are full of brown mica; some spots consist of rather coarser grains of quartz than occur in the matrix. The frequency with which this feature reappears in the less altered slates and hornfels is rather remarkable, especially as it seems certain that the spots are not always of the same nature or origin. Tourmaline hornfels are found sometimes near the margins of tourmaline granites; they are black with small needles of <a href="/wiki/Schorl" class="mw-redirect" title="Schorl">schorl</a> that under the microscope are dark brown and richly pleochroic. As the tourmaline contains <a href="/wiki/Boron" title="Boron">boron</a>, there must have been some permeation of vapors from the granite into the sediments. Rocks of this group are often seen in the Cornish <a href="/wiki/Tin" title="Tin">tin</a>-mining districts, especially near the lodes.<sup id="cite_ref-eb1911_1-6" class="reference"><a href="#cite_note-eb1911-1"><span class="cite-bracket">[</span>1<span class="cite-bracket">]</span></a></sup> </p> <div class="mw-heading mw-heading3"><h3 id="Carbonate">Carbonate</h3><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Hornfels&action=edit&section=4" title="Edit section: Carbonate"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <p>A second great group of hornfels are the <a href="/wiki/Calc%E2%80%93silicate_rock" title="Calc–silicate rock">calc–silicate</a> hornfels that arise from the thermal alteration of impure <a href="/wiki/Limestone" title="Limestone">limestone</a>. The purer beds <a href="/wiki/Recrystallization_(geology)" title="Recrystallization (geology)">recrystallize</a> as <a href="/wiki/Marble" title="Marble">marbles</a>, but where there has been originally an admixture of <a href="/wiki/Sand" title="Sand">sand</a> or clay lime-bearing silicates are formed, such as <a href="/wiki/Diopside" title="Diopside">diopside</a>, <a href="/wiki/Epidote" title="Epidote">epidote</a>, <a href="/wiki/Garnet" title="Garnet">garnet</a>, <a href="/wiki/Sphene" class="mw-redirect" title="Sphene">sphene</a>, <a href="/wiki/Vesuvianite" title="Vesuvianite">vesuvianite</a> and <a href="/wiki/Scapolite" title="Scapolite">scapolite</a>; with these <a href="/wiki/Phlogopite" title="Phlogopite">phlogopite</a>, various feldspars, <a href="/wiki/Pyrite" title="Pyrite">pyrites</a>, quartz and <a href="/wiki/Actinolite" title="Actinolite">actinolite</a> often occur. These rocks are fine-grained, and though often banded, are tough and much harder than the original limestones. They are excessively variable in their mineralogical composition, and very often alternate in thin seams with biotite hornfels and indurated <a href="/wiki/Quartzite" title="Quartzite">quartzites</a>. When perfused with boric and fluoric vapors from the granite they may contain much <a href="/wiki/Axinite" title="Axinite">axinite</a>, <a href="/wiki/Fluorite" title="Fluorite">fluorite</a> and <a href="/wiki/Datolite" title="Datolite">datolite</a>, but the altiminous silicates are absent from these rocks.<sup id="cite_ref-eb1911_1-7" class="reference"><a href="#cite_note-eb1911-1"><span class="cite-bracket">[</span>1<span class="cite-bracket">]</span></a></sup> </p> <div class="mw-heading mw-heading3"><h3 id="Mafic">Mafic</h3><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Hornfels&action=edit&section=5" title="Edit section: Mafic"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <p>From <a href="/wiki/Diabase" title="Diabase">diabases</a>, <a href="/wiki/Basalt" title="Basalt">basalts</a>, <a href="/wiki/Andesite" title="Andesite">andesites</a> and other igneous rocks a third type of hornfels is produced. They consist essentially of feldspar with hornblende (generally of brown color) and pale pyroxene. Sphene, biotite and iron oxides are the other common constituents, but these rocks show much variety of composition and structure. Where the original mass was decomposed and contained calcite, <a href="/wiki/Zeolite" title="Zeolite">zeolites</a>, <a href="/wiki/Chlorite_group" title="Chlorite group">chlorite</a> and other secondary minerals either in veins or in cavities, there are usually rounded areas or irregular streaks containing a suite of new minerals, which may resemble those of the calcium-silicate hornfelses above described. The original <a href="/wiki/Porphyritic" title="Porphyritic">porphyritic</a>, fluidal, vesicular or fragmental structures of the igneous rock are clearly visible in the less advanced stages of hornfelsing, but become less evident as the alteration progresses.<sup id="cite_ref-eb1911_1-8" class="reference"><a href="#cite_note-eb1911-1"><span class="cite-bracket">[</span>1<span class="cite-bracket">]</span></a></sup> </p><p>In some districts hornfelsed rocks occur that have acquired a schistose structure through shearing, and these form transitions to schists and <a href="/wiki/Gneiss" title="Gneiss">gneisses</a> that contain the same minerals as the hornfels, but have a schistose instead of a hornfels structure. Among these may be mentioned cordierite and sillimanite gneisses, andalusite and kyanite mica-schists, and those schistose calcite-silicate rocks that are known as <a href="/wiki/Cipolin" class="mw-redirect" title="Cipolin">cipolins</a>. That these are sediments that have undergone thermal alteration is generally admitted, but the exact conditions under which they were formed are not always clear. The essential features of hornfelsing are ascribed to the action of heat, <a href="/wiki/Pressure" title="Pressure">pressure</a> and permeating vapors, regenerating a rock mass without the production of fusion (at least on a large scale). It has been argued, however, that often there is extensive chemical change owing to the introduction of matter from the granite into the rocks surrounding it. The formation of new feldspar in the hornfelses is pointed out as evidence of this. While this felspathization may have occurred in a few localities, it seems conspicuously absent from others. Most authorities at the present time regard the changes as being purely of a physical and not of a chemical nature.<sup id="cite_ref-eb1911_1-9" class="reference"><a href="#cite_note-eb1911-1"><span class="cite-bracket">[</span>1<span class="cite-bracket">]</span></a></sup> </p> <div class="mw-heading mw-heading2"><h2 id="Facies">Facies</h2><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Hornfels&action=edit&section=6" title="Edit section: Facies"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <table style="float: right; margin: 10px; border: 1px #CCCCCC solid; background:#F9F9F9"> <tbody><tr> <td><div style="position: relative;"> <p><span typeof="mw:File"><a href="/wiki/File:Metamorphic_facies_blanc.svg" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/a/ad/Metamorphic_facies_blanc.svg/500px-Metamorphic_facies_blanc.svg.png" decoding="async" width="450" height="364" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/a/ad/Metamorphic_facies_blanc.svg/675px-Metamorphic_facies_blanc.svg.png 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/a/ad/Metamorphic_facies_blanc.svg/900px-Metamorphic_facies_blanc.svg.png 2x" data-file-width="744" data-file-height="602" /></a></span> </p> <div style="position:absolute; left:281px; top:44.5px"><small><a href="/wiki/Eclogite_facies" class="mw-redirect" title="Eclogite facies">Eclogite</a></small></div> <div style="position:absolute; left:158.5px; top:160px"><small><a href="/wiki/Blueschist_facies" class="mw-redirect" title="Blueschist facies">Blueschist</a></small></div> <div style="position:absolute; left:179.5px; top:237px"><small><a href="/wiki/Greenschist_facies" class="mw-redirect" title="Greenschist facies">Greenschist</a></small></div> <div style="position:absolute; left:106px; top:223px"><small><a href="/wiki/Prehnite-Pumpellyite_facies" class="mw-redirect" title="Prehnite-Pumpellyite facies">Prehnite-<br />Pumpellyite</a></small></div> <div style="position:absolute; left:95.5px; top:286px"><a href="/wiki/Zeolite_facies" title="Zeolite facies">Zeolite</a></div> <div style="position:absolute; left:379px; top:181px"><a href="/wiki/Granulite_facies" class="mw-redirect" title="Granulite facies">Granulite</a></div> <div style="position:absolute; left:256.5px; top:202px"><a href="/wiki/Amphibolite_facies" class="mw-redirect" title="Amphibolite facies">Amphibolite</a></div> <div style="position:absolute; left:225px; top:303.5px"><small><a href="/wiki/Hornfels_facies" class="mw-redirect" title="Hornfels facies">Hornfels</a></small></div> <div style="position:absolute; left:372px; top:303.5px"><small><a href="/wiki/Sanidinite_facies" class="mw-redirect" title="Sanidinite facies">Sanidinite</a></small></div> <div style="position:absolute; left:1px; top:132px"><a href="/wiki/Pressure" title="Pressure">P</a><br />(<a href="/wiki/Kbar" class="mw-redirect" title="Kbar">kbar</a>)</div> <div style="position:absolute; left:204px; top:345.5px"><a href="/wiki/Temperature" title="Temperature">T</a> (°C)</div> <div style="position:absolute; left:57px; top:331.5px">0</div> <div style="position:absolute; left:85px; top:331.5px">100</div> <div style="position:absolute; left:123.5px; top:331.5px">200</div> <div style="position:absolute; left:162px; top:331.5px">300</div> <div style="position:absolute; left:200.5px; top:331.5px">400</div> <div style="position:absolute; left:239px; top:331.5px">500</div> <div style="position:absolute; left:277.5px; top:331.5px">600</div> <div style="position:absolute; left:312.5px; top:331.5px">700</div> <div style="position:absolute; left:351px; top:331.5px">800</div> <div style="position:absolute; left:389.5px; top:331.5px">900</div> <div style="position:absolute; left:424.5px; top:331.5px">1000</div> <div style="position:absolute; left:39.5px; top:314px">0</div> <div style="position:absolute; left:39.5px; top:282.85px">2</div> <div style="position:absolute; left:39.5px; top:251.7px">4</div> <div style="position:absolute; left:39.5px; top:220.55px">6</div> <div style="position:absolute; left:39.5px; top:189.4px">8</div> <div style="position:absolute; left:32.5px; top:158.25px">10</div> <div style="position:absolute; left:32.5px; top:127.1px">12</div> <div style="position:absolute; left:32.5px; top:95.95px">14</div> <div style="position:absolute; left:32.5px; top:64.8px">16</div> <div style="position:absolute; left:32.5px; top:33.65px">18</div> <div style="position:absolute; left:32.5px; top:2.5px">20</div> </div> </td></tr> <tr> <td><small>Metamorphic facies in <a href="/wiki/Pressure" title="Pressure">pressure</a>-<a href="/wiki/Temperature" title="Temperature">temperature</a> space. The various hornfels facies <br />occupy the low pressure region of the space.</small> </td></tr></tbody></table> <p>The hornfels facies occupies the portion of the metamorphic pressure-temperature space of lowest pressure and low to high temperature. It is subdivided into a low-temperature regime of <a href="/wiki/Albite" title="Albite">albite</a>-<a href="/wiki/Epidote" title="Epidote">epidote</a> hornfels, a medium-temperature regime of <a href="/wiki/Hornblende" title="Hornblende">hornblende</a> hornfels, a high-temperature regime of <a href="/wiki/Pyroxene" title="Pyroxene">pyroxene</a> hornfels, and an ultra-high-temperature sanidinite regime. The latter is sometimes regarded as a separate facies. Maximum pressures are around 2 kbar and temperatures are around 300-500 C for the albite-epidote hornfels facies, 500-650 C for the hornblende hornfels facies, 650-800 C for the pyroxene hornfels facies, and above 800 C for the sanidinite facies.<sup id="cite_ref-blatt-tracy-1996-378-380-512_9-1" class="reference"><a href="#cite_note-blatt-tracy-1996-378-380-512-9"><span class="cite-bracket">[</span>9<span class="cite-bracket">]</span></a></sup><sup id="cite_ref-philpotts-ague-2009-422-428_4-1" class="reference"><a href="#cite_note-philpotts-ague-2009-422-428-4"><span class="cite-bracket">[</span>4<span class="cite-bracket">]</span></a></sup> </p><p>The actual minerals present in each facies depends on the composition of the <a href="/wiki/Protolith" title="Protolith">protolith</a>. For a mafic protolith, the albite-epidote hornfels facies is characterized by albite and epidote or <a href="/wiki/Zoisite" title="Zoisite">zoisite</a> with minor <a href="/wiki/Actinolite" title="Actinolite">actinolite</a> and <a href="/wiki/Chlorite" title="Chlorite">chlorite</a>. This gives way to hornblende, <a href="/wiki/Plagioclase" title="Plagioclase">plagioclase</a>, pyroxene, and <a href="/wiki/Garnet" title="Garnet">garnet</a> in the hornblende hornfels facies, which in turn gives way to <a href="/wiki/Orthopyroxene" class="mw-redirect" title="Orthopyroxene">orthopyroxene</a>, <a href="/wiki/Augite" title="Augite">augite</a>, plagioclase, and characteristic trace garnet in the pyroxene hornfels facies and sanidinite facies, the latter two being indistinguishable for this composition of protolith.<sup id="cite_ref-blatt-tracy-1996-378-380-512_9-2" class="reference"><a href="#cite_note-blatt-tracy-1996-378-380-512-9"><span class="cite-bracket">[</span>9<span class="cite-bracket">]</span></a></sup> </p><p>For an ultramafic protolith, the albite-epidote facies is characterized by <a href="/wiki/Serpentine_subgroup" title="Serpentine subgroup">serpentine</a>, <a href="/wiki/Talc" title="Talc">talc</a>, <a href="/wiki/Tremolite" title="Tremolite">tremolite</a>, and chlorite, giving way to <a href="/wiki/Forsterite" title="Forsterite">forsterite</a>, orthopyroxene, hornblende, chlorite, and characteristic minor aluminum <a href="/wiki/Spinel" title="Spinel">spinel</a> and <a href="/wiki/Magnetite" title="Magnetite">magnetite</a> in the hornblende facies, which in turn gives way to forsterite, orthopyroxene, augite, plagioclase, and aluminum spinel in the pyroxene hornfels facies. The sanidinite facies for this composition differs from the pyroxene hornfels facies only in the disappearance of aluminum spinel.<sup id="cite_ref-blatt-tracy-1996-378-380-512_9-3" class="reference"><a href="#cite_note-blatt-tracy-1996-378-380-512-9"><span class="cite-bracket">[</span>9<span class="cite-bracket">]</span></a></sup> </p><p>For a pelitic protolith, the sequence is <a href="/wiki/Quartz" title="Quartz">quartz</a>, plagioclase, <a href="/wiki/Muscovite" title="Muscovite">muscovite</a>, chlorite, and <a href="/wiki/Cordierite" title="Cordierite">cordierite</a> in the albite-epidote facies; quartz, plagioclase, muscovite, biotite, cordierite, and <a href="/wiki/Andalusite" title="Andalusite">andalusite</a> in the hornblende hornfels facies; and quartz, plagioclase, orthoclase, andalusite, <a href="/wiki/Sillimanite" title="Sillimanite">sillimanite</a>, cordierite, and orthopyroxene in the pyroxene hornfels facies. The sanidinite facies features quartz, plagioclase, sillimanite, cordierite, orthopyroxene, <a href="/wiki/Sapphirine" title="Sapphirine">sapphirine</a>, and aluminum spinel.<sup id="cite_ref-stewart-1942_12-0" class="reference"><a href="#cite_note-stewart-1942-12"><span class="cite-bracket">[</span>12<span class="cite-bracket">]</span></a></sup><sup id="cite_ref-blatt-tracy-1996-378-380-512_9-4" class="reference"><a href="#cite_note-blatt-tracy-1996-378-380-512-9"><span class="cite-bracket">[</span>9<span class="cite-bracket">]</span></a></sup> </p><p>For a calcareous protolith, the sequence is <a href="/wiki/Calcite" title="Calcite">calcite</a>, <a href="/wiki/Dolomite_(mineral)" title="Dolomite (mineral)">dolomite</a>, quartz, tremolite, talc, and forsterite for the albite-epidote hornfels facies; calcite, dolomite, quartz, tremolite, <a href="/wiki/Diopside" title="Diopside">diopside</a>, and forsterite for the hornblende hornfels facies; calcite, quartz, diposide, forsterite, and <a href="/wiki/Wollastonite" title="Wollastonite">wollastonite</a> for the pyroxene hornfels facies; and calcite, quartz, diopside, forsterite, wollastonite, <a href="/wiki/Monticellite" title="Monticellite">monticellite</a>, and <a href="/wiki/Akermanite" class="mw-redirect" title="Akermanite">akermanite</a> for the sanidinite facies.<sup id="cite_ref-blatt-tracy-1996-378-380-512_9-5" class="reference"><a href="#cite_note-blatt-tracy-1996-378-380-512-9"><span class="cite-bracket">[</span>9<span class="cite-bracket">]</span></a></sup> </p> <div class="mw-heading mw-heading2"><h2 id="Acoustic_properties">Acoustic properties</h2><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Hornfels&action=edit&section=7" title="Edit section: Acoustic properties"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <p>Hornfels have the ability to resonate when struck. Michael Tellinger had described these stones in <a href="/wiki/South_Africa" title="South Africa">South Africa</a> also known as "ring-stones" due to their ability to ring like a bell.<sup id="cite_ref-13" class="reference"><a href="#cite_note-13"><span class="cite-bracket">[</span>13<span class="cite-bracket">]</span></a></sup> The <a href="/wiki/Musical_Stones_of_Skiddaw" title="Musical Stones of Skiddaw">Musical Stones of Skiddaw</a> are an example of a <a href="/wiki/Lithophone" title="Lithophone">lithophone</a> made from hornfels.<sup id="cite_ref-14" class="reference"><a href="#cite_note-14"><span class="cite-bracket">[</span>14<span class="cite-bracket">]</span></a></sup> </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=Hornfels&action=edit&section=8" title="Edit section: See also"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <ul><li><a href="/wiki/List_of_rock_types" title="List of rock types">List of rock types</a> – List of rock types recognized by geologists</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=Hornfels&action=edit&section=9" 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 mw-references-columns"><ol class="references"> <li id="cite_note-eb1911-1"><span class="mw-cite-backlink">^ <a href="#cite_ref-eb1911_1-0"><sup><i><b>a</b></i></sup></a> <a href="#cite_ref-eb1911_1-1"><sup><i><b>b</b></i></sup></a> <a href="#cite_ref-eb1911_1-2"><sup><i><b>c</b></i></sup></a> <a href="#cite_ref-eb1911_1-3"><sup><i><b>d</b></i></sup></a> <a href="#cite_ref-eb1911_1-4"><sup><i><b>e</b></i></sup></a> <a href="#cite_ref-eb1911_1-5"><sup><i><b>f</b></i></sup></a> <a href="#cite_ref-eb1911_1-6"><sup><i><b>g</b></i></sup></a> <a href="#cite_ref-eb1911_1-7"><sup><i><b>h</b></i></sup></a> <a href="#cite_ref-eb1911_1-8"><sup><i><b>i</b></i></sup></a> <a href="#cite_ref-eb1911_1-9"><sup><i><b>j</b></i></sup></a></span> <span class="reference-text"><span class="noprint"><span class="noviewer" typeof="mw:File"><span><img alt="" src="//upload.wikimedia.org/wikipedia/commons/thumb/4/4c/Wikisource-logo.svg/20px-Wikisource-logo.svg.png" decoding="async" width="12" height="13" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/4/4c/Wikisource-logo.svg/40px-Wikisource-logo.svg.png 2x" data-file-width="410" data-file-height="430" /></span></span> </span>One or more of the preceding sentences incorporates text from a publication now in the <a href="/wiki/Public_domain" title="Public domain">public domain</a>: <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><cite id="CITEREFFlett1911" class="citation encyclopaedia cs1"><a href="/wiki/John_Smith_Flett" class="mw-redirect" title="John Smith Flett">Flett, John Smith</a> (1911). "<a href="https://en.wikisource.org/wiki/1911_Encyclop%C3%A6dia_Britannica/Hornfels" class="extiw" title="s:1911 Encyclopædia Britannica/Hornfels">Hornfels</a>". In <a href="/wiki/Hugh_Chisholm" title="Hugh Chisholm">Chisholm, Hugh</a> (ed.). <i><a href="/wiki/Encyclop%C3%A6dia_Britannica_Eleventh_Edition" title="Encyclopædia Britannica Eleventh Edition">Encyclopædia Britannica</a></i>. Vol. 13 (11th ed.). Cambridge University Press. pp. <span class="nowrap">710–</span>711.</cite><span title="ctx_ver=Z39.88-2004&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Abook&rft.genre=bookitem&rft.atitle=Hornfels&rft.btitle=Encyclop%C3%A6dia+Britannica&rft.pages=%3Cspan+class%3D%22nowrap%22%3E710-%3C%2Fspan%3E711&rft.edition=11th&rft.pub=Cambridge+University+Press&rft.date=1911&rft.aulast=Flett&rft.aufirst=John+Smith&rfr_id=info%3Asid%2Fen.wikipedia.org%3AHornfels" class="Z3988"></span></span> </li> <li id="cite_note-yardley-1989-12-2"><span class="mw-cite-backlink">^ <a href="#cite_ref-yardley-1989-12_2-0"><sup><i><b>a</b></i></sup></a> <a href="#cite_ref-yardley-1989-12_2-1"><sup><i><b>b</b></i></sup></a> <a href="#cite_ref-yardley-1989-12_2-2"><sup><i><b>c</b></i></sup></a></span> <span class="reference-text"><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1238218222" /><cite id="CITEREFYardley1989" class="citation book cs1">Yardley, Bruce W.D. (1989). <i>An introduction to metamorphic petrology</i>. Harlow, Essex, England: Longman Scientific & Technical. pp. 12, 26. <a href="/wiki/ISBN_(identifier)" class="mw-redirect" title="ISBN (identifier)">ISBN</a> <a href="/wiki/Special:BookSources/0582300967" title="Special:BookSources/0582300967"><bdi>0582300967</bdi></a>.</cite><span title="ctx_ver=Z39.88-2004&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Abook&rft.genre=book&rft.btitle=An+introduction+to+metamorphic+petrology&rft.place=Harlow%2C+Essex%2C+England&rft.pages=12%2C+26&rft.pub=Longman+Scientific+%26+Technical&rft.date=1989&rft.isbn=0582300967&rft.aulast=Yardley&rft.aufirst=Bruce+W.D.&rfr_id=info%3Asid%2Fen.wikipedia.org%3AHornfels" class="Z3988"></span></span> </li> <li id="cite_note-blatt-tracy-1996-367-512-3"><span class="mw-cite-backlink">^ <a href="#cite_ref-blatt-tracy-1996-367-512_3-0"><sup><i><b>a</b></i></sup></a> <a href="#cite_ref-blatt-tracy-1996-367-512_3-1"><sup><i><b>b</b></i></sup></a></span> <span class="reference-text"><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1238218222" /><cite id="CITEREFBlattTracy1996" class="citation book cs1">Blatt, Harvey; Tracy, Robert J. (1996). <i>Petrology : igneous, sedimentary, and metamorphic</i> (2nd ed.). New York: W.H. Freeman. pp. 367, 512. <a href="/wiki/ISBN_(identifier)" class="mw-redirect" title="ISBN (identifier)">ISBN</a> <a href="/wiki/Special:BookSources/0716724383" title="Special:BookSources/0716724383"><bdi>0716724383</bdi></a>.</cite><span title="ctx_ver=Z39.88-2004&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Abook&rft.genre=book&rft.btitle=Petrology+%3A+igneous%2C+sedimentary%2C+and+metamorphic.&rft.place=New+York&rft.pages=367%2C+512&rft.edition=2nd&rft.pub=W.H.+Freeman&rft.date=1996&rft.isbn=0716724383&rft.aulast=Blatt&rft.aufirst=Harvey&rft.au=Tracy%2C+Robert+J.&rfr_id=info%3Asid%2Fen.wikipedia.org%3AHornfels" class="Z3988"></span></span> </li> <li id="cite_note-philpotts-ague-2009-422-428-4"><span class="mw-cite-backlink">^ <a href="#cite_ref-philpotts-ague-2009-422-428_4-0"><sup><i><b>a</b></i></sup></a> <a href="#cite_ref-philpotts-ague-2009-422-428_4-1"><sup><i><b>b</b></i></sup></a></span> <span class="reference-text"><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1238218222" /><cite id="CITEREFPhilpottsAgue2009" class="citation book cs1">Philpotts, Anthony R.; Ague, Jay J. (2009). <i>Principles of igneous and metamorphic petrology</i> (2nd ed.). Cambridge, UK: Cambridge University Press. pp. 422, 428. <a href="/wiki/ISBN_(identifier)" class="mw-redirect" title="ISBN (identifier)">ISBN</a> <a href="/wiki/Special:BookSources/9780521880060" title="Special:BookSources/9780521880060"><bdi>9780521880060</bdi></a>.</cite><span title="ctx_ver=Z39.88-2004&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Abook&rft.genre=book&rft.btitle=Principles+of+igneous+and+metamorphic+petrology&rft.place=Cambridge%2C+UK&rft.pages=422%2C+428&rft.edition=2nd&rft.pub=Cambridge+University+Press&rft.date=2009&rft.isbn=9780521880060&rft.aulast=Philpotts&rft.aufirst=Anthony+R.&rft.au=Ague%2C+Jay+J.&rfr_id=info%3Asid%2Fen.wikipedia.org%3AHornfels" class="Z3988"></span></span> </li> <li id="cite_note-5"><span class="mw-cite-backlink"><b><a href="#cite_ref-5">^</a></b></span> <span class="reference-text"><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1238218222" /><cite class="citation web cs1"><a rel="nofollow" class="external text" href="http://www.explorenorthpennines.org.uk/sites/default/files/activity/downloads/enp052.pdf">"Holwick Scar & Low Force : Pamphlet"</a> <span class="cs1-format">(PDF)</span>. Explorenorthpennines.org.uk<span class="reference-accessdate">. Retrieved <span class="nowrap">2015-03-17</span></span>.</cite><span title="ctx_ver=Z39.88-2004&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Abook&rft.genre=unknown&rft.btitle=Holwick+Scar+%26+Low+Force+%3A+Pamphlet&rft.pub=Explorenorthpennines.org.uk&rft_id=http%3A%2F%2Fwww.explorenorthpennines.org.uk%2Fsites%2Fdefault%2Ffiles%2Factivity%2Fdownloads%2Fenp052.pdf&rfr_id=info%3Asid%2Fen.wikipedia.org%3AHornfels" class="Z3988"></span></span> </li> <li id="cite_note-6"><span class="mw-cite-backlink"><b><a href="#cite_ref-6">^</a></b></span> <span class="reference-text">Lawrence, D. J. D et al 2004 <i>Durham Geodiversity Audit</i>, Durham: Durham County Council p20</span> </li> <li id="cite_note-nesse-2000-195-7"><span class="mw-cite-backlink"><b><a href="#cite_ref-nesse-2000-195_7-0">^</a></b></span> <span class="reference-text"><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1238218222" /><cite id="CITEREFNesse2000" class="citation book cs1">Nesse, William D. (2000). <i>Introduction to mineralogy</i>. New York: Oxford University Press. p. 195. <a href="/wiki/ISBN_(identifier)" class="mw-redirect" title="ISBN (identifier)">ISBN</a> <a href="/wiki/Special:BookSources/9780195106916" title="Special:BookSources/9780195106916"><bdi>9780195106916</bdi></a>.</cite><span title="ctx_ver=Z39.88-2004&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Abook&rft.genre=book&rft.btitle=Introduction+to+mineralogy&rft.place=New+York&rft.pages=195&rft.pub=Oxford+University+Press&rft.date=2000&rft.isbn=9780195106916&rft.aulast=Nesse&rft.aufirst=William+D.&rfr_id=info%3Asid%2Fen.wikipedia.org%3AHornfels" class="Z3988"></span></span> </li> <li id="cite_note-harry-1952-8"><span class="mw-cite-backlink"><b><a href="#cite_ref-harry-1952_8-0">^</a></b></span> <span class="reference-text"><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1238218222" /><cite id="CITEREFHarry1952" class="citation journal cs1">Harry, W. T. (December 1952). "Basic hornfels at a gabbro contact near Carlingford, Eire". <i>Geological Magazine</i>. <b>89</b> (6): <span class="nowrap">411–</span>416. <a href="/wiki/Bibcode_(identifier)" class="mw-redirect" title="Bibcode (identifier)">Bibcode</a>:<a rel="nofollow" class="external text" href="https://ui.adsabs.harvard.edu/abs/1952GeoM...89..411H">1952GeoM...89..411H</a>. <a href="/wiki/Doi_(identifier)" class="mw-redirect" title="Doi (identifier)">doi</a>:<a rel="nofollow" class="external text" href="https://doi.org/10.1017%2FS0016756800068114">10.1017/S0016756800068114</a>.</cite><span title="ctx_ver=Z39.88-2004&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Ajournal&rft.genre=article&rft.jtitle=Geological+Magazine&rft.atitle=Basic+hornfels+at+a+gabbro+contact+near+Carlingford%2C+Eire&rft.volume=89&rft.issue=6&rft.pages=%3Cspan+class%3D%22nowrap%22%3E411-%3C%2Fspan%3E416&rft.date=1952-12&rft_id=info%3Adoi%2F10.1017%2FS0016756800068114&rft_id=info%3Abibcode%2F1952GeoM...89..411H&rft.aulast=Harry&rft.aufirst=W.+T.&rfr_id=info%3Asid%2Fen.wikipedia.org%3AHornfels" class="Z3988"></span></span> </li> <li id="cite_note-blatt-tracy-1996-378-380-512-9"><span class="mw-cite-backlink">^ <a href="#cite_ref-blatt-tracy-1996-378-380-512_9-0"><sup><i><b>a</b></i></sup></a> <a href="#cite_ref-blatt-tracy-1996-378-380-512_9-1"><sup><i><b>b</b></i></sup></a> <a href="#cite_ref-blatt-tracy-1996-378-380-512_9-2"><sup><i><b>c</b></i></sup></a> <a href="#cite_ref-blatt-tracy-1996-378-380-512_9-3"><sup><i><b>d</b></i></sup></a> <a href="#cite_ref-blatt-tracy-1996-378-380-512_9-4"><sup><i><b>e</b></i></sup></a> <a href="#cite_ref-blatt-tracy-1996-378-380-512_9-5"><sup><i><b>f</b></i></sup></a></span> <span class="reference-text">Blatt and Tracy, p.378-380, 512</span> </li> <li id="cite_note-yardley-1989-161-10"><span class="mw-cite-backlink"><b><a href="#cite_ref-yardley-1989-161_10-0">^</a></b></span> <span class="reference-text">Yardley 1989, p.161</span> </li> <li id="cite_note-dickey-obata-1974-11"><span class="mw-cite-backlink"><b><a href="#cite_ref-dickey-obata-1974_11-0">^</a></b></span> <span class="reference-text"><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1238218222" /><cite id="CITEREFDickeyObata1974" class="citation journal cs1">Dickey, John S.; Obata, Masaaki (1974). <a rel="nofollow" class="external text" href="https://pubs.geoscienceworld.org/msa/ammin/article-abstract/59/11-12/1183/541166">"Graphitic hornfels dikes in the Ronda high-temperature peridotite massif"</a>. <i>American Mineralogist</i>. <b>59</b> (<span class="nowrap">11–</span>12): <span class="nowrap">1183–</span>1189<span class="reference-accessdate">. Retrieved <span class="nowrap">23 August</span> 2020</span>.</cite><span title="ctx_ver=Z39.88-2004&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Ajournal&rft.genre=article&rft.jtitle=American+Mineralogist&rft.atitle=Graphitic+hornfels+dikes+in+the+Ronda+high-temperature+peridotite+massif.&rft.volume=59&rft.issue=%3Cspan+class%3D%22nowrap%22%3E11%E2%80%93%3C%2Fspan%3E12&rft.pages=%3Cspan+class%3D%22nowrap%22%3E1183-%3C%2Fspan%3E1189&rft.date=1974&rft.aulast=Dickey&rft.aufirst=John+S.&rft.au=Obata%2C+Masaaki&rft_id=https%3A%2F%2Fpubs.geoscienceworld.org%2Fmsa%2Fammin%2Farticle-abstract%2F59%2F11-12%2F1183%2F541166&rfr_id=info%3Asid%2Fen.wikipedia.org%3AHornfels" class="Z3988"></span></span> </li> <li id="cite_note-stewart-1942-12"><span class="mw-cite-backlink"><b><a href="#cite_ref-stewart-1942_12-0">^</a></b></span> <span class="reference-text"><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1238218222" /><cite id="CITEREFStewart1942" class="citation journal cs1">Stewart, F. H. (September 1942). "Chemical data on a silica-poor argillaceous hornfels and its constituent minerals". <i>Mineralogical Magazine and Journal of the Mineralogical Society</i>. <b>26</b> (178): <span class="nowrap">260–</span>266. <a href="/wiki/Bibcode_(identifier)" class="mw-redirect" title="Bibcode (identifier)">Bibcode</a>:<a rel="nofollow" class="external text" href="https://ui.adsabs.harvard.edu/abs/1942MinM...26..260S">1942MinM...26..260S</a>. <a href="/wiki/Doi_(identifier)" class="mw-redirect" title="Doi (identifier)">doi</a>:<a rel="nofollow" class="external text" href="https://doi.org/10.1180%2Fminmag.1942.026.178.04">10.1180/minmag.1942.026.178.04</a>.</cite><span title="ctx_ver=Z39.88-2004&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Ajournal&rft.genre=article&rft.jtitle=Mineralogical+Magazine+and+Journal+of+the+Mineralogical+Society&rft.atitle=Chemical+data+on+a+silica-poor+argillaceous+hornfels+and+its+constituent+minerals&rft.volume=26&rft.issue=178&rft.pages=%3Cspan+class%3D%22nowrap%22%3E260-%3C%2Fspan%3E266&rft.date=1942-09&rft_id=info%3Adoi%2F10.1180%2Fminmag.1942.026.178.04&rft_id=info%3Abibcode%2F1942MinM...26..260S&rft.aulast=Stewart&rft.aufirst=F.+H.&rfr_id=info%3Asid%2Fen.wikipedia.org%3AHornfels" class="Z3988"></span></span> </li> <li id="cite_note-13"><span class="mw-cite-backlink"><b><a href="#cite_ref-13">^</a></b></span> <span class="reference-text"><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1238218222" /><cite class="citation web cs1"><a rel="nofollow" class="external text" href="https://web.archive.org/web/20160809173935/https://www.youtube.com/watch?v=LUFv4rbBkhg">"2014 Ancient Hidden Technology of the Annunaki (Fallen Angels)"</a>. see from 43 min. Archived from <a rel="nofollow" class="external text" href="https://www.youtube.com/watch?v=LUFv4rbBkhg">the original</a> on 2016-08-09<span class="reference-accessdate">. Retrieved <span class="nowrap">2016-06-02</span></span>.</cite><span title="ctx_ver=Z39.88-2004&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Abook&rft.genre=unknown&rft.btitle=2014+Ancient+Hidden+Technology+of+the+Annunaki+%28Fallen+Angels%29&rft.pub=see+from+43+min.&rft_id=https%3A%2F%2Fwww.youtube.com%2Fwatch%3Fv%3DLUFv4rbBkhg&rfr_id=info%3Asid%2Fen.wikipedia.org%3AHornfels" class="Z3988"></span></span> </li> <li id="cite_note-14"><span class="mw-cite-backlink"><b><a href="#cite_ref-14">^</a></b></span> <span class="reference-text"><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1238218222" /><cite class="citation web cs1"><a rel="nofollow" class="external text" href="https://web.archive.org/web/20100619025947/http://www.allerdale.gov.uk/leisure-and-culture/museums-and-galleries/keswick-museum/the-musical-stones-of-skiddaw.aspx">"The Musical Stones of Skiddaw - Allerdale Borough Council"</a>. Allerdale.gov.uk. Archived from <a rel="nofollow" class="external text" href="http://www.allerdale.gov.uk/leisure-and-culture/museums-and-galleries/keswick-museum/the-musical-stones-of-skiddaw.aspx">the original</a> on 2010-06-19<span class="reference-accessdate">. Retrieved <span class="nowrap">2015-03-17</span></span>.</cite><span title="ctx_ver=Z39.88-2004&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Abook&rft.genre=unknown&rft.btitle=The+Musical+Stones+of+Skiddaw+-+Allerdale+Borough+Council&rft.pub=Allerdale.gov.uk&rft_id=http%3A%2F%2Fwww.allerdale.gov.uk%2Fleisure-and-culture%2Fmuseums-and-galleries%2Fkeswick-museum%2Fthe-musical-stones-of-skiddaw.aspx&rfr_id=info%3Asid%2Fen.wikipedia.org%3AHornfels" class="Z3988"></span></span> </li> </ol></div></div> <ul><li><span class="noprint"><span class="noviewer" typeof="mw:File"><span><img alt="" src="//upload.wikimedia.org/wikipedia/commons/thumb/4/4c/Wikisource-logo.svg/20px-Wikisource-logo.svg.png" decoding="async" width="12" height="13" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/4/4c/Wikisource-logo.svg/40px-Wikisource-logo.svg.png 2x" data-file-width="410" data-file-height="430" /></span></span> </span>This article incorporates text from a publication now in the <a href="/wiki/Public_domain" title="Public domain">public domain</a>: <link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1238218222" /><cite id="CITEREFFlett1911" class="citation encyclopaedia cs1"><a href="/wiki/John_Smith_Flett" class="mw-redirect" title="John Smith Flett">Flett, John Smith</a> (1911). "<a href="https://en.wikisource.org/wiki/1911_Encyclop%C3%A6dia_Britannica/Hornfels" class="extiw" title="s:1911 Encyclopædia Britannica/Hornfels">Hornfels</a>". In <a href="/wiki/Hugh_Chisholm" title="Hugh Chisholm">Chisholm, Hugh</a> (ed.). <i><a href="/wiki/Encyclop%C3%A6dia_Britannica_Eleventh_Edition" title="Encyclopædia Britannica Eleventh Edition">Encyclopædia Britannica</a></i>. Vol. 13 (11th ed.). Cambridge University Press. pp. <span class="nowrap">710–</span>711.</cite><span title="ctx_ver=Z39.88-2004&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Abook&rft.genre=bookitem&rft.atitle=Hornfels&rft.btitle=Encyclop%C3%A6dia+Britannica&rft.pages=%3Cspan+class%3D%22nowrap%22%3E710-%3C%2Fspan%3E711&rft.edition=11th&rft.pub=Cambridge+University+Press&rft.date=1911&rft.aulast=Flett&rft.aufirst=John+Smith&rfr_id=info%3Asid%2Fen.wikipedia.org%3AHornfels" class="Z3988"></span></li></ul> <div class="mw-heading mw-heading2"><h2 id="External_links">External links</h2><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Hornfels&action=edit&section=10" title="Edit section: External links"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <p><span class="noviewer" typeof="mw:File"><a href="/wiki/File:Commons-logo.svg" class="mw-file-description"><img alt="" src="//upload.wikimedia.org/wikipedia/en/thumb/4/4a/Commons-logo.svg/20px-Commons-logo.svg.png" decoding="async" width="12" height="16" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/en/thumb/4/4a/Commons-logo.svg/40px-Commons-logo.svg.png 2x" data-file-width="1024" data-file-height="1376" /></a></span> Media related to <a href="https://commons.wikimedia.org/wiki/Category:Hornfels" class="extiw" title="commons:Category:Hornfels">Hornfels</a> at Wikimedia Commons </p> <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 dl,.mw-parser-output .hlist dl ol,.mw-parser-output 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href="/wiki/Special:EditPage/Template:Rock_type" title="Special:EditPage/Template:Rock type"><abbr title="Edit this template">e</abbr></a></li></ul></div><div id="Types_of_rocks88" style="font-size:114%;margin:0 4em">Types of rocks</div></th></tr><tr><th scope="row" class="navbox-group" style="width:1%"><a href="/wiki/Igneous_rock" title="Igneous rock">Igneous rock</a></th><td class="navbox-list-with-group navbox-list navbox-odd hlist" style="width:100%;padding:0"><div style="padding:0 0.25em"> <ul><li><a href="/wiki/Adakite" title="Adakite">Adakite</a></li> <li><a href="/wiki/Alkali_feldspar_granite" title="Alkali feldspar granite">Alkali feldspar granite</a></li> <li><a href="/wiki/Andesite" title="Andesite">Andesite</a></li> <li><a href="/wiki/Anorthosite" title="Anorthosite">Anorthosite</a></li> <li><a href="/wiki/Aplite" title="Aplite">Aplite</a></li> <li><a href="/wiki/Basalt" title="Basalt">Basalt</a> <ul><li><a href="/wiki/Alkali_basalt" title="Alkali basalt">Alkali basalt</a></li> <li><a href="/wiki/Picrite_basalt" title="Picrite basalt">Picrite basalt</a></li></ul></li> <li><a href="/wiki/Basaltic_trachyandesite" class="mw-redirect" title="Basaltic trachyandesite">Basaltic trachyandesite</a> <ul><li><a href="/wiki/Mugearite" title="Mugearite">Mugearite</a></li> <li><a href="/wiki/Shoshonite" title="Shoshonite">Shoshonite</a></li></ul></li> <li><a href="/wiki/Basanite" title="Basanite">Basanite</a></li> <li><a href="/wiki/Blairmorite" title="Blairmorite">Blairmorite</a></li> <li><a href="/wiki/Boninite" title="Boninite">Boninite</a></li> <li><a href="/wiki/Carbonatite" title="Carbonatite">Carbonatite</a></li> <li><a href="/wiki/Charnockite" title="Charnockite">Charnockite</a> <ul><li><a href="/wiki/Enderbite" title="Enderbite">Enderbite</a></li></ul></li> <li><a href="/wiki/Dacite" title="Dacite">Dacite</a></li> <li><a href="/wiki/Diabase" title="Diabase">Diabase</a></li> <li><a href="/wiki/Diorite" title="Diorite">Diorite</a> <ul><li><a href="/wiki/Napoleonite" title="Napoleonite">Napoleonite</a></li></ul></li> <li><a href="/wiki/Dunite" title="Dunite">Dunite</a></li> <li><a href="/wiki/Essexite" title="Essexite">Essexite</a></li> <li><a href="/wiki/Foidolite" title="Foidolite">Foidolite</a></li> <li><a href="/wiki/Gabbro" title="Gabbro">Gabbro</a></li> <li><a href="/wiki/Granite" title="Granite">Granite</a></li> <li><a href="/wiki/Granodiorite" title="Granodiorite">Granodiorite</a></li> <li><a href="/wiki/Granophyre" title="Granophyre">Granophyre</a></li> <li><a href="/wiki/Harzburgite" title="Harzburgite">Harzburgite</a></li> <li><a href="/wiki/Hornblendite" title="Hornblendite">Hornblendite</a></li> <li><a href="/wiki/Hyaloclastite" title="Hyaloclastite">Hyaloclastite</a></li> <li><a href="/wiki/Icelandite" title="Icelandite">Icelandite</a></li> <li><a href="/wiki/Ignimbrite" title="Ignimbrite">Ignimbrite</a></li> <li><a href="/wiki/Ijolite" title="Ijolite">Ijolite</a></li> <li><a href="/wiki/Kimberlite" title="Kimberlite">Kimberlite</a></li> <li><a href="/wiki/Komatiite" title="Komatiite">Komatiite</a></li> <li><a href="/wiki/Lamproite" title="Lamproite">Lamproite</a></li> <li><a href="/wiki/Lamprophyre" title="Lamprophyre">Lamprophyre</a></li> <li><a href="/wiki/Latite" title="Latite">Latite</a></li> <li><a href="/wiki/Lherzolite" title="Lherzolite">Lherzolite</a></li> <li><a href="/wiki/Monzogranite" title="Monzogranite">Monzogranite</a></li> <li><a href="/wiki/Monzonite" title="Monzonite">Monzonite</a></li> <li><a href="/wiki/Nepheline_syenite" title="Nepheline syenite">Nepheline syenite</a></li> <li><a href="/wiki/Nephelinite" title="Nephelinite">Nephelinite</a></li> <li><a href="/wiki/Norite" title="Norite">Norite</a></li> <li><a href="/wiki/Obsidian" title="Obsidian">Obsidian</a></li> <li><a href="/wiki/Pegmatite" title="Pegmatite">Pegmatite</a></li> <li><a href="/wiki/Peridotite" title="Peridotite">Peridotite</a></li> <li><a href="/wiki/Phonolite" title="Phonolite">Phonolite</a></li> <li><a href="/wiki/Phonotephrite" title="Phonotephrite">Phonotephrite</a></li> <li><a href="/wiki/Porphyry_(geology)" title="Porphyry (geology)">Porphyry</a></li> <li><a href="/wiki/Pumice" title="Pumice">Pumice</a></li> <li><a href="/wiki/Pyroxenite" title="Pyroxenite">Pyroxenite</a></li> <li><a href="/wiki/Quartz_diorite" title="Quartz diorite">Quartz diorite</a></li> <li><a href="/wiki/Quartz_monzonite" title="Quartz monzonite">Quartz monzonite</a></li> <li><a href="/wiki/Quartzolite" title="Quartzolite">Quartzolite</a></li> <li><a href="/wiki/Rhyodacite" title="Rhyodacite">Rhyodacite</a></li> <li><a href="/wiki/Rhyolite" title="Rhyolite">Rhyolite</a> <ul><li><a href="/wiki/Comendite" title="Comendite">Comendite</a></li> <li><a href="/wiki/Pantellerite" title="Pantellerite">Pantellerite</a></li></ul></li> <li><a href="/wiki/Scoria" title="Scoria">Scoria</a></li> <li><a href="/wiki/Shonkinite" title="Shonkinite">Shonkinite</a></li> <li><a href="/wiki/Sovite" title="Sovite">Sovite</a></li> <li><a href="/wiki/Syenite" title="Syenite">Syenite</a></li> <li><a href="/wiki/Tachylyte" class="mw-redirect" title="Tachylyte">Tachylyte</a></li> <li><a href="/wiki/Tephriphonolite" title="Tephriphonolite">Tephriphonolite</a></li> <li><a href="/wiki/Tephrite" title="Tephrite">Tephrite</a></li> <li><a href="/wiki/Tonalite" title="Tonalite">Tonalite</a></li> <li><a href="/wiki/Trachyandesite" title="Trachyandesite">Trachyandesite</a> <ul><li><a href="/wiki/Benmoreite" title="Benmoreite">Benmoreite</a></li></ul></li> <li><a href="/wiki/Trachybasalt" title="Trachybasalt">Trachybasalt</a> <ul><li><a href="/wiki/Hawaiite" title="Hawaiite">Hawaiite</a></li></ul></li> <li><a href="/wiki/Trachyte" title="Trachyte">Trachyte</a></li> <li><a href="/wiki/Troctolite" title="Troctolite">Troctolite</a></li> <li><a href="/wiki/Trondhjemite" title="Trondhjemite">Trondhjemite</a></li> <li><a href="/wiki/Tuff" title="Tuff">Tuff</a></li> <li><a href="/wiki/Websterite" title="Websterite">Websterite</a></li> <li><a href="/wiki/Wehrlite" title="Wehrlite">Wehrlite</a></li></ul> </div></td></tr><tr><th scope="row" class="navbox-group" style="width:1%"><a href="/wiki/Sedimentary_rock" title="Sedimentary rock">Sedimentary rock</a></th><td class="navbox-list-with-group navbox-list navbox-even hlist" style="width:100%;padding:0"><div style="padding:0 0.25em"> <ul><li><a href="/wiki/Argillite" title="Argillite">Argillite</a></li> <li><a href="/wiki/Arkose" title="Arkose">Arkose</a></li> <li><a href="/wiki/Banded_iron_formation" title="Banded iron formation">Banded iron formation</a></li> <li><a href="/wiki/Breccia" title="Breccia">Breccia</a></li> <li><a href="/wiki/Calcarenite" title="Calcarenite">Calcarenite</a></li> <li><a href="/wiki/Chalk" title="Chalk">Chalk</a></li> <li><a href="/wiki/Chert" title="Chert">Chert</a></li> <li><a href="/wiki/Claystone" class="mw-redirect" title="Claystone">Claystone</a></li> <li><a href="/wiki/Coal" title="Coal">Coal</a></li> <li><a href="/wiki/Conglomerate_(geology)" title="Conglomerate (geology)">Conglomerate</a></li> <li><a href="/wiki/Coquina" title="Coquina">Coquina</a></li> <li><a href="/wiki/Diamictite" title="Diamictite">Diamictite</a></li> <li><a href="/wiki/Diatomite" class="mw-redirect" title="Diatomite">Diatomite</a></li> <li><a href="/wiki/Dolomite_(rock)" title="Dolomite (rock)">Dolomite</a></li> <li><a href="/wiki/Evaporite" title="Evaporite">Evaporite</a></li> <li><a href="/wiki/Flint" title="Flint">Flint</a></li> <li><a href="/wiki/Geyserite" title="Geyserite">Geyserite</a></li> <li><a href="/wiki/Greywacke" title="Greywacke">Greywacke</a></li> <li><a href="/wiki/Gritstone" title="Gritstone">Gritstone</a></li> <li><a href="/wiki/Itacolumite" title="Itacolumite">Itacolumite</a></li> <li><a href="/wiki/Jaspillite" title="Jaspillite">Jaspillite</a></li> <li><a href="/wiki/Laterite" title="Laterite">Laterite</a></li> <li><a href="/wiki/Lignite" title="Lignite">Lignite</a></li> <li><a href="/wiki/Limestone" title="Limestone">Limestone</a></li> <li><a href="/wiki/Lumachelle" title="Lumachelle">Lumachelle</a></li> <li><a href="/wiki/Marl" title="Marl">Marl</a></li> <li><a href="/wiki/Mudstone" title="Mudstone">Mudstone</a></li> <li><a href="/wiki/Oil_shale" title="Oil shale">Oil shale</a></li> <li><a href="/wiki/Oolite" title="Oolite">Oolite</a></li> <li><a href="/wiki/Phosphorite" title="Phosphorite">Phosphorite</a></li> <li><a href="/wiki/Sandstone" title="Sandstone">Sandstone</a></li> <li><a href="/wiki/Shale" title="Shale">Shale</a></li> <li><a href="/wiki/Siltstone" title="Siltstone">Siltstone</a></li> <li><a href="/wiki/Sylvinite" title="Sylvinite">Sylvinite</a></li> <li><a href="/wiki/Tillite" class="mw-redirect" title="Tillite">Tillite</a></li> <li><a href="/wiki/Travertine" title="Travertine">Travertine</a></li> <li><a href="/wiki/Tufa" title="Tufa">Tufa</a></li> <li><a href="/wiki/Turbidite" title="Turbidite">Turbidite</a></li> <li><a href="/wiki/Varve" title="Varve">Varve</a></li> <li><a href="/wiki/Wackestone" title="Wackestone">Wackestone</a></li></ul> </div></td></tr><tr><th scope="row" class="navbox-group" style="width:1%"><a href="/wiki/Metamorphic_rock" title="Metamorphic rock">Metamorphic rock</a></th><td class="navbox-list-with-group navbox-list navbox-odd hlist" style="width:100%;padding:0"><div style="padding:0 0.25em"> <ul><li><a href="/wiki/Anthracite" title="Anthracite">Anthracite</a></li> <li><a href="/wiki/Amphibolite" title="Amphibolite">Amphibolite</a></li> <li><a href="/wiki/Blueschist" title="Blueschist">Blueschist</a></li> <li><a href="/wiki/Cataclasite" title="Cataclasite">Cataclasite</a></li> <li><a href="/wiki/Eclogite" title="Eclogite">Eclogite</a></li> <li><a href="/wiki/Gneiss" title="Gneiss">Gneiss</a></li> <li><a href="/wiki/Granulite" title="Granulite">Granulite</a></li> <li><a href="/wiki/Greenschist" title="Greenschist">Greenschist</a></li> <li><a class="mw-selflink selflink">Hornfels</a> <ul><li><a href="/wiki/Calcflinta" title="Calcflinta">Calcflinta</a></li></ul></li> <li><a href="/wiki/Itabirite" title="Itabirite">Itabirite</a></li> <li><a href="/wiki/Litchfieldite" title="Litchfieldite">Litchfieldite</a></li> <li><a href="/wiki/Marble" title="Marble">Marble</a></li> <li><a href="/wiki/Migmatite" title="Migmatite">Migmatite</a></li> <li><a href="/wiki/Mylonite" title="Mylonite">Mylonite</a></li> <li><a href="/wiki/Metapelite" class="mw-redirect" title="Metapelite">Metapelite</a></li> <li><a href="/w/index.php?title=Metapsammite&action=edit&redlink=1" class="new" title="Metapsammite (page does not exist)">Metapsammite</a></li> <li><a href="/wiki/Phyllite" title="Phyllite">Phyllite</a></li> <li><a href="/wiki/Pseudotachylite" class="mw-redirect" title="Pseudotachylite">Pseudotachylite</a></li> <li><a href="/wiki/Quartzite" title="Quartzite">Quartzite</a></li> <li><a href="/wiki/Schist" title="Schist">Schist</a></li> <li><a href="/wiki/Serpentinite" title="Serpentinite">Serpentinite</a></li> <li><a href="/wiki/Skarn" title="Skarn">Skarn</a></li> <li><a href="/wiki/Slate" title="Slate">Slate</a></li> <li><a href="/wiki/Suevite" title="Suevite">Suevite</a></li> <li><a href="/wiki/Talc_carbonate" title="Talc carbonate">Talc carbonate</a> <ul><li><a href="/wiki/Soapstone" title="Soapstone">Soapstone</a></li></ul></li> <li><a href="/wiki/Tectonite" title="Tectonite">Tectonite</a></li> <li><a href="/wiki/Whiteschist" title="Whiteschist">Whiteschist</a></li></ul> </div></td></tr><tr><th scope="row" class="navbox-group" style="width:1%">Specific varieties</th><td class="navbox-list-with-group navbox-list navbox-even hlist" style="width:100%;padding:0"><div style="padding:0 0.25em"> <ul><li><a href="/wiki/Adamellite" class="mw-redirect" title="Adamellite">Adamellite</a></li> <li><a href="/wiki/Appinite" title="Appinite">Appinite</a></li> <li><a href="/wiki/Aphanite" title="Aphanite">Aphanite</a></li> <li><a href="/wiki/Borolanite" title="Borolanite">Borolanite</a></li> <li><a href="/wiki/Larvikite" title="Larvikite">Blue Granite</a></li> <li><a href="/wiki/Epidosite" title="Epidosite">Epidosite</a></li> <li><a href="/wiki/Felsite" title="Felsite">Felsite</a></li> <li><a href="/wiki/Flint" title="Flint">Flint</a></li> <li><a href="/wiki/Ganister" title="Ganister">Ganister</a></li> <li><a href="/wiki/Gossan" title="Gossan">Gossan</a></li> <li><a href="/wiki/Hyaloclastite" title="Hyaloclastite">Hyaloclastite</a></li> <li><a href="/wiki/Ijolite" title="Ijolite">Ijolite</a></li> <li><a href="/wiki/Jadeitite" title="Jadeitite">Jadeitite</a></li> <li><a href="/wiki/Jasperoid" title="Jasperoid">Jasperoid</a></li> <li><a href="/wiki/Kenyte" title="Kenyte">Kenyte</a></li> <li><a href="/wiki/Lapis_lazuli" title="Lapis lazuli">Lapis lazuli</a></li> <li><a href="/wiki/Larvikite" title="Larvikite">Larvikite</a></li> <li><a href="/wiki/Litchfieldite" title="Litchfieldite">Litchfieldite</a></li> <li><a href="/wiki/Llanite" title="Llanite">Llanite</a></li> <li><a href="/wiki/Luxullianite" title="Luxullianite">Luxullianite</a></li> <li><a href="/wiki/Mangerite" title="Mangerite">Mangerite</a></li> <li><a href="/wiki/Novaculite" title="Novaculite">Novaculite</a></li> <li><a href="/wiki/Pietersite" title="Pietersite">Pietersite</a></li> <li><a href="/wiki/Pyrolite" title="Pyrolite">Pyrolite</a></li> <li><a href="/wiki/Rapakivi_granite" title="Rapakivi granite">Rapakivi granite</a></li> <li><a href="/wiki/Rhomb_porphyry" class="mw-redirect" title="Rhomb porphyry">Rhomb porphyry</a></li> <li><a href="/wiki/Rodingite" title="Rodingite">Rodingite</a></li> <li><a href="/wiki/Shonkinite" title="Shonkinite">Shonkinite</a></li> <li><a href="/wiki/Taconite" title="Taconite">Taconite</a></li> <li><a href="/wiki/Tachylite" title="Tachylite">Tachylite</a></li> <li><a href="/wiki/Teschenite" title="Teschenite">Teschenite</a></li> <li><a href="/wiki/Theralite" title="Theralite">Theralite</a></li> <li><a href="/wiki/Unakite" title="Unakite">Unakite</a></li> <li><a href="/wiki/Variolite" title="Variolite">Variolite</a></li> <li><a href="/wiki/Wad_(mineral)" title="Wad (mineral)">Wad</a></li></ul> </div></td></tr></tbody></table></div> <!-- NewPP limit report Parsed by mw‐web.eqiad.main‐6d78b94fdf‐sp6lm Cached time: 20250320215848 Cache expiry: 2592000 Reduced expiry: false Complications: [vary‐revision‐sha1, show‐toc] CPU time usage: 0.596 seconds Real time usage: 0.748 seconds Preprocessor visited node count: 3172/1000000 Post‐expand include size: 60041/2097152 bytes Template argument size: 2580/2097152 bytes Highest expansion depth: 12/100 Expensive parser function count: 1/500 Unstrip recursion depth: 1/20 Unstrip post‐expand size: 56523/5000000 bytes Lua time usage: 0.380/10.000 seconds Lua memory usage: 15789854/52428800 bytes Number of Wikibase entities loaded: 1/400 --> <!-- Transclusion expansion time report (%,ms,calls,template) 100.00% 625.137 1 -total 31.75% 198.462 1 Template:Reflist 24.50% 153.166 1 Template:Annotated_link 20.90% 130.644 2 Template:EB1911 14.68% 91.797 1 Template:Rock_type 13.96% 87.274 1 Template:Navbox 13.24% 82.778 1 Template:Short_description 7.24% 45.243 2 Template:Pagetype 5.61% 35.045 1 Template:Commons_category_inline 5.16% 32.275 1 Template:Metamorphic_facies_to_click --> <!-- Saved in parser cache with key enwiki:pcache:1231792:|#|:idhash:canonical and timestamp 20250320215848 and revision id 1240799520. Rendering was triggered because: page-view --> </div><!--esi <esi:include src="/esitest-fa8a495983347898/content" /> --><noscript><img src="https://login.wikimedia.org/wiki/Special:CentralAutoLogin/start?useformat=desktop&type=1x1&usesul3=0" alt="" width="1" height="1" style="border: none; position: absolute;"></noscript> <div class="printfooter" data-nosnippet="">Retrieved from "<a dir="ltr" href="https://en.wikipedia.org/w/index.php?title=Hornfels&oldid=1240799520">https://en.wikipedia.org/w/index.php?title=Hornfels&oldid=1240799520</a>"</div></div> <div id="catlinks" class="catlinks" data-mw="interface"><div id="mw-normal-catlinks" class="mw-normal-catlinks"><a href="/wiki/Help:Category" title="Help:Category">Category</a>: <ul><li><a href="/wiki/Category:Metamorphic_rocks" title="Category:Metamorphic rocks">Metamorphic rocks</a></li></ul></div><div id="mw-hidden-catlinks" class="mw-hidden-catlinks mw-hidden-cats-hidden">Hidden categories: <ul><li><a href="/wiki/Category:Wikipedia_articles_incorporating_a_citation_from_the_1911_Encyclopaedia_Britannica_with_Wikisource_reference" title="Category:Wikipedia articles incorporating a citation from the 1911 Encyclopaedia Britannica with Wikisource reference">Wikipedia articles incorporating a citation from the 1911 Encyclopaedia Britannica with Wikisource reference</a></li><li><a href="/wiki/Category:Wikipedia_articles_incorporating_text_from_the_1911_Encyclop%C3%A6dia_Britannica" title="Category:Wikipedia articles incorporating text from the 1911 Encyclopædia Britannica">Wikipedia articles incorporating text from the 1911 Encyclopædia Britannica</a></li><li><a href="/wiki/Category:Articles_with_short_description" title="Category:Articles with short description">Articles with short description</a></li><li><a href="/wiki/Category:Short_description_is_different_from_Wikidata" title="Category:Short description is different from Wikidata">Short description is different from Wikidata</a></li><li><a href="/wiki/Category:Commons_category_link_is_on_Wikidata" title="Category:Commons category link is on Wikidata">Commons category link is on Wikidata</a></li></ul></div></div> </div> </main> </div> <div class="mw-footer-container"> <footer id="footer" class="mw-footer" > <ul id="footer-info"> <li id="footer-info-lastmod"> This page was last edited on 17 August 2024, at 14:08<span class="anonymous-show"> (UTC)</span>.</li> <li id="footer-info-copyright">Text is available under the <a href="/wiki/Wikipedia:Text_of_the_Creative_Commons_Attribution-ShareAlike_4.0_International_License" title="Wikipedia:Text of the Creative Commons Attribution-ShareAlike 4.0 International License">Creative Commons Attribution-ShareAlike 4.0 License</a>; additional terms may apply. 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