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<h1 id="firstHeading" class="firstHeading mw-first-heading"><span class="mw-page-title-main">Garlock-Verwerfung</span></h1>
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<div id="mw-content-text" class="mw-body-content mw-content-ltr" lang="de" dir="ltr"><div class="mw-content-ltr mw-parser-output" lang="de" dir="ltr"><p>Die <b>Garlock-Verwerfung</b> (<span style="font-style:normal;font-weight:normal"><a href="Englische_Sprache" title="Englische Sprache">englisch</a></span> <span lang="en-Latn" style="font-style:italic">Garlock Fault</span>) ist eine <a href="Blattverschiebung" title="Blattverschiebung">Blattverschiebungen</a> (sinistraler Versatz) von etwa 250 km Länge im Westen der <a href="Mojave-W%C3%BCste" title="Mojave-Wüste">Mojave-Wüste</a>.<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> Sie ist die zweitgrößte Verwerfung in Kalifornien.<sup id="cite_ref-2" class="reference"><a href="#cite_note-2"><span class="cite-bracket">[</span>2<span class="cite-bracket">]</span></a></sup>
</p><p>Sie beginnt an der <a href="San-Andreas-Verwerfung" title="San-Andreas-Verwerfung">San-Andreas-Verwerfung</a> ca. 5 km WNW von <a href="Gorman" class="mw-disambig" title="Gorman">Gorman</a> und verläuft nach Osten entlang Frazier Park und <a href="Mojave_(Kalifornien)" title="Mojave (Kalifornien)">Mojave</a> und endet bei Salt Springs.<sup id="cite_ref-3" class="reference"><a href="#cite_note-3"><span class="cite-bracket">[</span>3<span class="cite-bracket">]</span></a></sup><sup id="cite_ref-4" class="reference"><a href="#cite_note-4"><span class="cite-bracket">[</span>4<span class="cite-bracket">]</span></a></sup> Die gesamte Verschiebung beträgt 30 km.<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> Die Verwerfung markiert die nördliche Grenze des als Mojave-Block bekannten Gebiets sowie die südlichen Enden der <a href="Sierra_Nevada_(Vereinigte_Staaten)" title="Sierra Nevada (Vereinigte Staaten)">Sierra Nevada</a> und der westlichsten <a href="Basin_and_Range_Province" title="Basin and Range Province">Basin and Range-Provinz</a>.<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><sup id="cite_ref-7" class="reference"><a href="#cite_note-7"><span class="cite-bracket">[</span>7<span class="cite-bracket">]</span></a></sup>
</p><p>In einem Zeitraum von vor 2000 bis vor 500 Jahren ereigneten sich vier große Erdbeben.<sup id="cite_ref-8" class="reference"><a href="#cite_note-8"><span class="cite-bracket">[</span>8<span class="cite-bracket">]</span></a></sup>
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<div class="mw-heading mw-heading2"><h2 id="Einzelnachweise">Einzelnachweise</h2></div>
<ol class="references">
<li id="cite_note-1"><span class="mw-cite-backlink"><a href="#cite_ref-1">↑</a></span> <span class="reference-text"><a rel="nofollow" class="external text" href="https://www.latimes.com/local/lanow/la-me-ln-earthquake-fault-cluster-20150422-story.html"><i>The Big One could trigger series of large earthquakes, study finds.</i></a></span>
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<li id="cite_note-2"><span class="mw-cite-backlink"><a href="#cite_ref-2">↑</a></span> <span class="reference-text">Hongrui Qiu, Benxin Chi, Yehuda Ben‐Zion: <cite style="font-style:italic">Internal Structure of the Central Garlock Fault Zone From Ridgecrest Aftershocks Recorded by Dense Linear Seismic Arrays</cite>. In: <cite style="font-style:italic">Geophysical Research Letters</cite>. <span style="white-space:nowrap">Band<span style="display:inline-block;width:.2em"> </span>50</span>, <span style="white-space:nowrap">Nr.<span style="display:inline-block;width:.2em"> </span>2</span>, 28. Januar 2023, <a href="Internationale_Standardnummer_f%C3%BCr_fortlaufende_Sammelwerke" title="Internationale Standardnummer für fortlaufende Sammelwerke">ISSN</a> <span style="white-space:nowrap"><a rel="nofollow" class="external text" href="https://zdb-katalog.de/list.xhtml?t=iss%3D%220094-8276%22&key=cql">0094-8276</a></span>, <a href="Digital_Object_Identifier" title="Digital Object Identifier">doi</a>:<span class="uri-handle" style="white-space:nowrap"><a rel="nofollow" class="external text" href="https://doi.org/10.1029/2022GL101761">10.1029/2022GL101761</a></span> (<a rel="nofollow" class="external text" href="https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2022GL101761">wiley.com</a> [abgerufen am 27. Oktober 2024]).<span class="Z3988" title="ctx_ver=Z39.88-2004&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Ajournal&rfr_id=info:sid/de.wikipedia.org:Garlock-Verwerfung&rft.atitle=Internal+Structure+of+the+Central+Garlock+Fault+Zone+From+Ridgecrest+Aftershocks+Recorded+by+Dense+Linear+Seismic+Arrays&rft.au=Hongrui+Qiu%2C+Benxin+Chi%2C+Yehuda+Ben%E2%80%90Zion&rft.date=2023-01-28&rft.doi=10.1029%2F2022GL101761&rft.genre=journal&rft.issn=0094-8276&rft.issue=2&rft.jtitle=Geophysical+Research+Letters&rft.volume=50" style="display:none"> </span></span>
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<li id="cite_note-3"><span class="mw-cite-backlink"><a href="#cite_ref-3">↑</a></span> <span class="reference-text"><a rel="nofollow" class="external text" href="https://digital-desert.com/garlock-fault/"><i>Garlock Fault.</i></a></span>
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<li id="cite_note-4"><span class="mw-cite-backlink"><a href="#cite_ref-4">↑</a></span> <span class="reference-text"><a rel="nofollow" class="external text" href="https://marcel-oehler.marcellosendos.ch/sav/kapitel2.html"><i>San Andreas Verwerfung.</i></a></span>
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<li id="cite_note-5"><span class="mw-cite-backlink"><a href="#cite_ref-5">↑</a></span> <span class="reference-text"><a rel="nofollow" class="external text" href="https://www.livescience.com/53165-san-andreas-zipper-fault.html"><i>San Andreas May Be a 'Zipper' Fault.</i></a></span>
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<li id="cite_note-6"><span class="mw-cite-backlink"><a href="#cite_ref-6">↑</a></span> <span class="reference-text"><span class="cite"><a rel="nofollow" class="external text" href="https://scedc.caltech.edu/earthquake/garlock.html"><i>Southern California Earthquake Data Center at Caltech.</i></a><span class="Abrufdatum"> Abgerufen am 27. Oktober 2024</span>.</span><span style="display: none;" class="Z3988" title="ctx_ver=Z39.88-2004&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Adc&rfr_id=info%3Asid%2Fde.wikipedia.org%3AGarlock-Verwerfung&rft.title=Southern+California+Earthquake+Data+Center+at+Caltech&rft.description=Southern+California+Earthquake+Data+Center+at+Caltech&rft.identifier=https%3A%2F%2Fscedc.caltech.edu%2Fearthquake%2Fgarlock.html"> </span></span>
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<li id="cite_note-7"><span class="mw-cite-backlink"><a href="#cite_ref-7">↑</a></span> <span class="reference-text">Gregory A. Davis, B. C. Burchfiel: <cite style="font-style:italic">Garlock Fault: An Intracontinental Transform Structure, Southern California</cite>. In: <cite style="font-style:italic">Geological Society of America Bulletin</cite>. <span style="white-space:nowrap">Band<span style="display:inline-block;width:.2em"> </span>84</span>, <span style="white-space:nowrap">Nr.<span style="display:inline-block;width:.2em"> </span>4</span>, 1973, <a href="Internationale_Standardnummer_f%C3%BCr_fortlaufende_Sammelwerke" title="Internationale Standardnummer für fortlaufende Sammelwerke">ISSN</a> <span style="white-space:nowrap"><a rel="nofollow" class="external text" href="https://zdb-katalog.de/list.xhtml?t=iss%3D%220016-7606%22&key=cql">0016-7606</a></span>, <span style="white-space:nowrap">S.<span style="display:inline-block;width:.2em"> </span>1407</span>, <a href="Digital_Object_Identifier" title="Digital Object Identifier">doi</a>:<span class="uri-handle" style="white-space:nowrap"><a rel="nofollow" class="external text" href="https://doi.org/10.1130/0016-7606%281973%2984%3C1407%3AGFAITS%3E2.0.CO%3B2">10.1130/0016-7606(1973)84<1407:GFAITS>2.0.CO;2</a></span> (<a rel="nofollow" class="external text" href="https://pubs.geoscienceworld.org/gsabulletin/article/84/4/1407-1422/201387">geoscienceworld.org</a> [abgerufen am 27. Oktober 2024]).<span class="Z3988" title="ctx_ver=Z39.88-2004&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Ajournal&rfr_id=info:sid/de.wikipedia.org:Garlock-Verwerfung&rft.atitle=Garlock+Fault%3A+An+Intracontinental+Transform+Structure%2C+Southern+California&rft.au=Gregory+A.+Davis%2C+B.+C.+Burchfiel&rft.date=1973&rft.doi=10.1130%2F0016-7606%281973%2984%3C1407%3AGFAITS%3E2.0.CO%3B2&rft.genre=journal&rft.issn=0016-7606&rft.issue=4&rft.jtitle=Geological+Society+of+America+Bulletin&rft.pages=1407&rft.volume=84" style="display:none"> </span></span>
</li>
<li id="cite_note-8"><span class="mw-cite-backlink"><a href="#cite_ref-8">↑</a></span> <span class="reference-text"><a rel="nofollow" class="external text" href="https://phys.org/news/2015-04-earthquake-super-cycle-patterns-garlock-fault.html"><i>Earthquake 'super-cycle' patterns on the Garlock fault.</i></a></span>
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