Columnar jointing

<h2 id="physics">Physics</h2>
<p>When magma or lava cools into solid igneous rock, for example basalt, much heat still remains. As it cools down further, the basalt contracts, and it forms cracks to release the tensile energy. It then is cooled down further by <a href="/facts/Groundwater/JYM2IDS2">groundwater</a> boiling and reflux.
</p><p>When the cracks first form at the surface, the cracks are dominated by T-junctions, like <a href="/facts/Mudcrack/ux4RS6fu">mudcracks</a>, because they were formed individually. One crack would form and move across the surface, until it hits upon a previous crack, forming a T-junction.
</p><p>Then, these cracks extend downwards in a moving front that is roughly planar and parallel to the surface. As it moves, the crack pattern <a href="/facts/Annealing_(materials_science)/2AfoCE4X">anneals</a> to become lower in energy. The speed <i>v</i> at which the front moves is determined by the groundwater flow rate. After the front moves a few meters deep, it would evolve into a hexagonal grid with roughly equal width <i>L</i>. The width <i>L</i> is determined by the basalt's <a href="/facts/List_of_materials_properties/Cg2LVoQe">material properties</a>, and the speed <i>v</i> at which the front moves.<a class="footnote-ref" id="fnref:7" href="#fn:7"><sup>7</sup></a>
</p>
<h3>Scaling</h3>
<p>Define <a href="/facts/P%25C3%25A9clet_number/lIGehNcg">Péclet number</a> 
  
    
      
        P
        e
        =
        
          
            
              L
              v
            
            D
          
        
      
    
    {\displaystyle Pe={\frac {Lv}{D}}}
  
 where 
  
    
      
        D
      
    
    {\displaystyle D}
  
 is the <a href="/facts/Thermal_diffusivity/dRa1aeHY">thermal diffusivity</a> of the material. For all columnar jointing, the value of <i>Pe</i> is around 0.2, and thus the shape and speed of all columnar joints are similar after scaling. A <a href="/facts/Scale_model/YgCtlwqb">scaled model</a> can be made by drying <a href="/facts/Corn_starch/ASblJB4P">cornstarch</a> a centimeter thick, which creates columns about 1 mm wide.
</p><p>For basalt, 
  
    
      
        P
        e
        ≈
        0.35
      
    
    {\displaystyle Pe\approx 0.35}
  
. For cornstarch, 
  
    
      
        P
        e
        ≈
        0.1
      
    
    {\displaystyle Pe\approx 0.1}
  
.<a class="footnote-ref" id="fnref:8" href="#fn:8"><sup>8</sup></a>
</p>
<h2 id="places">Places</h2>
<p class="note">Main article: <a href="/facts/List_of_places_with_columnar_jointed_volcanics/YeN5HNWJ">List of places with columnar jointed volcanics</a></p>
<p>Some famous locations in the United States where columnar jointing can be found are <a href="/facts/Devils_Tower/J3aJQoo2">Devils Tower</a> in Wyoming, <a href="/facts/Devils_Postpile/JwL3vaxp">Devils Postpile</a> in California and the <a href="/facts/Columbia_River/XTEInQB8">Columbia River</a> <a href="/facts/Flood_basalt/omlPkoyM">flood basalts</a> in <a href="/facts/Oregon/4Uq446Ko">Oregon</a>, <a href="/facts/Washington_(state)/7tCrTFnN">Washington</a> and <a href="/facts/Idaho/68ELs9Um">Idaho</a>. Other famous places include the <a href="/facts/Giant%2527s_Causeway/QqwrI4lF">Giant's Causeway</a> in <a href="/facts/Northern_Ireland/Jmr0NRyl">Northern Ireland</a>, <a href="/facts/Fingal%2527s_Cave/DNvT4aqc">Fingal's Cave</a> on the island of <a href="/facts/Staffa/GxzygAEz">Staffa</a>, <a href="/facts/Scotland/VGwbbxB2">Scotland</a> and the <a href="/facts/Stu%25C3%25B0lagil/T4xdNwqu">Stuðlagil</a> Canyon, <a href="/facts/Iceland/E4KGYs2j">Iceland</a>.<a class="footnote-ref" id="fnref:9" href="#fn:9"><sup>9</sup></a>
</p>
<h3>Devils Tower</h3>
<p class="note">Main article: <a href="/facts/Devils_Tower/J3aJQoo2">Devils Tower</a></p>

<p>Devils Tower in Wyoming in the United States is about 40 million years old and 382 meters (1,253 feet) high.<a class="footnote-ref" id="fnref:10" href="#fn:10"><sup>10</sup></a> Geologists agree that the rock forming Devils Tower solidified from an intrusion, but it has not been established whether the <a href="/facts/Magma/hRotHju9">magma</a> from this intrusion ever reached the surface. Most columns are 6-sided, but 4, 5, and 7-sided ones can also be found.<a class="footnote-ref" id="fnref:11" href="#fn:11"><sup>11</sup></a>
</p>
<h3>Giant's Causeway</h3>
<p class="note">Main article: <a href="/facts/Giant%2527s_Causeway/QqwrI4lF">Giant's Causeway</a></p>
<p>The Giant's Causeway (<a href="/facts/Irish_language/Kw97s2l4">Irish</a>: <i>Clochán An Aifir</i>) on the <a href="/facts/County_Antrim/e1orqgLY">north Antrim coast</a> of Northern Ireland was created by volcanic activity 60 million years ago, and consists of over 40,000 columns.<a class="footnote-ref" id="fnref:12" href="#fn:12"><sup>12</sup></a><a class="footnote-ref" id="fnref:13" href="#fn:13"><sup>13</sup></a> According to a legend, the giant <a href="/facts/Finn_McCool/pgpKJy9y">Finn McCool</a> created the Giant's Causeway, as a <a href="/facts/Causeway/rxdAVmNz">causeway</a> to Scotland.<a class="footnote-ref" id="fnref:14" href="#fn:14"><sup>14</sup></a>
</p>
<h3>Sōunkyō Gorge</h3>
<p class="note">Main article: <a href="/facts/S%25C5%258Dunky%25C5%258D/lQblHRk2">Sōunkyō</a></p>
<p>Sōunkyō Gorge, a part of the town of <a href="/facts/Kamikawa%2c_Hokkaido/4m4gHN7k">Kamikawa, Hokkaido</a>, Japan, features a 24-kilometre (15 mi) stretch of columnar jointing, which is the result of an eruption of the <a href="/facts/Daisetsuzan_Volcanic_Group/KTTPJCpR">Daisetsuzan Volcanic Group</a> 30,000 years ago.
</p>
<h3>Deccan Traps</h3>
<p class="note">Main article: <a href="/facts/Deccan_Traps/HdvPLMuQ">Deccan Traps</a></p>
<p>The late Cretaceous <a href="/facts/Deccan_Traps/HdvPLMuQ">Deccan Traps</a> of India constitute one of the largest volcanic provinces of Earth, and examples of columnar jointing can be found in <a href="/facts/St._Mary%2527s_Islands/eLG9ArBY">St. Mary's Island</a> in the state of Karnataka.<a class="footnote-ref" id="fnref:15" href="#fn:15"><sup>15</sup></a>
</p>
<h3>High Island Reservoir</h3>
<p>Formed in Cretaceous, the columnar rocks are found around the reservoir and the islands nearby in <a href="/facts/Sai_Kung_Peninsula/mCrfEtC8">Sai Kung</a>, <a href="/facts/Hong_Kong/4nAf3mqQ">Hong Kong</a>. It is special that the rocks are not mafic, but felsic <a href="/facts/Tuff/PhhRoLdJ">tuff</a> instead.
</p>

<h3>Makhtesh Ramon</h3>
<p>The columnar jointed sandstone of the <i>HaMinsara</i> (Carpentry Shop) in the <a href="/facts/Makhtesh/FI42GxY2">makhtesh</a> (erosion <a href="/facts/Cirque/AP63fr64">cirque</a>) of <a href="/facts/Makhtesh_Ramon/yNR0vjHl">Makhtesh Ramon</a>, <a href="/facts/Negev_desert/LFYIQtkY">Negev desert</a>, <a href="/facts/Israel/dEe3IcaY">Israel</a>.
</p>

<h3>Cerro Kõi</h3>
<p>There are several examples of columnar jointed sandstones in the greater <a href="/facts/Asunci%25C3%25B3n/SS4v1g4f">Asunción</a> region of <a href="/facts/Paraguay/sbzfv4Rl">Paraguay</a>. The best known is Cerro Kõi in <a href="/facts/Aregu%25C3%25A1/Smztwr0S">Areguá</a>, but there are also several quarries in <a href="/facts/Luque/NHmX2rXR">Luque</a>. 
</p>
<h3>Mars</h3>
<p class="note">Main article: <a href="/facts/Marte_Vallis/SqBfybeN">Marte Vallis</a></p>
<p>Several exposures of columnar jointing have been discovered on the planet Mars by the High Resolution Imaging Science Experiment (<a href="/facts/HiRISE/yePqnn3F">HiRISE</a>) camera, which is carried by the <a href="/facts/Mars_Reconnaissance_Orbiter/7odg7YfX">Mars Reconnaissance Orbiter</a> (MRO).<a class="footnote-ref" id="fnref:16" href="#fn:16"><sup>16</sup></a><a class="footnote-ref" id="fnref:17" href="#fn:17"><sup>17</sup></a>
</p>

<h3>Sawn Rocks</h3>

<p>Sawn Rocks, in <a href="/facts/Mount_Kaputar_National_Park/KtJxfqNY">Mount Kaputar National Park</a> close to <a href="/facts/Narrabri/SI5Kpq9V">Narrabri</a>, <a href="/facts/New_South_Wales%2c_Australia/aW7eJXSS">New South Wales, Australia</a>, features 40 meters of columnar jointing above the creek and 30 meters below the surface.<a class="footnote-ref" id="fnref:18" href="#fn:18"><sup>18</sup></a>
</p>
<h3>Basaltic Prisms of Santa María Regla</h3>
<p class="note">Main article: <a href="/facts/Basaltic_Prisms_of_Santa_Mar%25C3%25ADa_Regla/ongMK9Jv">Basaltic Prisms of Santa María Regla</a></p>
<p><a href="/facts/Alexander_von_Humboldt/5AuxyDbh">Alexander von Humboldt</a> documented the prisms located in <a href="/facts/Huasca_de_Ocampo/RmjjQvfr">Huasca de Ocampo</a>, in the Mexican state of <a href="/facts/Hidalgo_(state)/0FDNVVs4">Hidalgo</a>.
</p>
<h3>Columnar basalt of Tawau (Batu Bersusun)</h3>
<p>At Kampung Balung Cocos, <a href="/facts/Tawau/ItxxyBa9">Tawau</a>, <a href="/facts/Malaysia/8zbUMzCP">Malaysia</a>, the river flows through the area of columnar basalt. One section is seen vertically high on river bank. The rest lies on river bank. The water flows from the lowest area forming waterfall.
</p>

<h3>Gorge of Garni, Armenia</h3>
<p>The <a href="/facts/Garni_Gorge/kfJo5hz1">Garni Gorge</a> is situated 23 km east of Yerevan, Armenia, just below the village of the same name. This portion of the Garni Gorge is typically referred to as the "Symphony of the Stones." On a promontory above the gorge the first-century AD Temple of Garni may be seen.
</p>
<h3>Stuðlagil Canyon, Iceland</h3>
<p class="note">Main article: <a href="/facts/Stu%25C3%25B0lagil/T4xdNwqu">Stuðlagil</a></p>
<p>The Stuðlagil Canyon, situated 45 miles west of Egilsstaðir, showing a view of columnar joint basalts rock formations and the blue-green water that runs through it.
</p>
<h3>Black Point, Australia</h3>
<p>Black Point, situated in the D'Entrecasteaux National Park, in Western Australia is an example of black columnar basalt.
</p>
<h3>Jusangjeolli, South Korea</h3>
<p>The columnar jointing (<i><a href="/facts/Daepo_Jusangjeolli_Cliff/VV3tnVn7">Jusangjeolli</a></i> in Korean) on the southern coast near <a href="/facts/Seogwipo/0K9JhtVT">Seogwipo</a> on the island of <a href="/facts/Jeju_Province/MTjgpExX">Jeju</a> is a popular tourist destination.
</p>
<h2 id="see-also">See also</h2>
<ul><li><a href="/facts/Basalt_fan_structure/olhaTc6K">Basalt fan structure</a></li>
<li><a href="/facts/Honeycomb_conjecture/g45j09Io">Honeycomb conjecture</a></li>
<li><a href="/facts/Mudcrack/ux4RS6fu">Mudcrack</a></li>
<li><a href="/facts/Prism_(geology)/IW8HPnQB">Prism (geology)</a></li>
<li><a href="/facts/Syneresis_crack/LFpCdcrl">Syneresis crack</a></li></ul>

Wikimedia Commons has media related to Columnar igneous rocks.

<h2 id="external-links">External links</h2>
<ul><li>Aydin, A., and J. Zhong  (nda) <a href="https://web.archive.org/web/20140713211646/http://rockfracture.com/html2/ColumnarJoint.html">Columnar Joints</a>, <a href="https://web.archive.org/web/20140713211202/http://rockfracture.com/html2/MultipleJointSet.html">Multiple Joint Sets</a>,  <a href="https://web.archive.org/web/20140713211128/http://rockfracture.com/html2/Index.html">Rock Fracture Knolwedgebase</a>, Stanford University, Stanford, California.</li></ul>

<h2 id="references">References</h2>

<ol>
<li id="fn:1"><p>Oregon State University > Volcano World > ... > Columnar Jointing. Accessed 29 December 2013. <a href="http://volcano.oregonstate.edu/columnar-jointing" target="_blank">http://volcano.oregonstate.edu/columnar-jointing</a> <a href="#fnref:1" class="footnote-back-ref">↩</a></p></li>
<li id="fn:2"><p>Velázquez, Victor F.; Giannini, Paolo C. F.; Riccomini, Claudio; Ernandes, Alethéa; Sallun, Martins; Hachiro, Jorge; de Barros Gomes, Celso (1 September 2008). "Columnar joints in the Patiño Formation sandstones, Eastern Paraguay: a dynamic interaction between dyke intrusion, quartz dissolution and cooling-induced fractures". Episodes. 31 (3). International Union of Geological Sciences: 302–308. doi:10.18814/epiiugs/2008/v31i3/003. ISSN 2586-1298. <a href="https://doi.org/10.18814%2Fepiiugs%2F2008%2Fv31i3%2F003" target="_blank">https://doi.org/10.18814%2Fepiiugs%2F2008%2Fv31i3%2F003</a> <a href="#fnref:2" class="footnote-back-ref">↩</a></p></li>
<li id="fn:3"><p>Oregon State University > Volcano World > ... > Columnar Jointing. Accessed 29 December 2013. <a href="http://volcano.oregonstate.edu/columnar-jointing" target="_blank">http://volcano.oregonstate.edu/columnar-jointing</a> <a href="#fnref:3" class="footnote-back-ref">↩</a></p></li>
<li id="fn:4"><p>Oregon State University > Volcano World > ... > Columnar Jointing. Accessed 29 December 2013. <a href="http://volcano.oregonstate.edu/columnar-jointing" target="_blank">http://volcano.oregonstate.edu/columnar-jointing</a> <a href="#fnref:4" class="footnote-back-ref">↩</a></p></li>
<li id="fn:5"><p>Long, Philip E.; Wood, Bernard J. (1 September 1986). "Structures, textures, and cooling histories of Columbia River basalt flows". Geological Society of America Bulletin. 97 (9): 1144–1155. Bibcode:1986GSAB...97.1144L. doi:10.1130/0016-7606(1986)97<1144:STACHO>2.0.CO;2. <a href="https://www.researchgate.net/publication/249525837" target="_blank">https://www.researchgate.net/publication/249525837</a> <a href="#fnref:5" class="footnote-back-ref">↩</a></p></li>
<li id="fn:6"><p>Oregon State University > Volcano World > ... > Columnar Jointing. Accessed 29 December 2013. <a href="http://volcano.oregonstate.edu/columnar-jointing" target="_blank">http://volcano.oregonstate.edu/columnar-jointing</a> <a href="#fnref:6" class="footnote-back-ref">↩</a></p></li>
<li id="fn:7"><p>Goehring, Lucas; Morris, Stephen W. (1 November 2014). "Cracking mud, freezing dirt, and breaking rocks". Physics Today. 67 (11): 39–44. doi:10.1063/PT.3.2584. ISSN 0031-9228. <a href="https://pubs.aip.org/physicstoday/article/67/11/39/414529/Cracking-mud-freezing-dirt-and-breaking-rocksThe" target="_blank">https://pubs.aip.org/physicstoday/article/67/11/39/414529/Cracking-mud-freezing-dirt-and-breaking-rocksThe</a> <a href="#fnref:7" class="footnote-back-ref">↩</a></p></li>
<li id="fn:8"><p>Goehring, Lucas; Morris, Stephen W. (1 November 2014). "Cracking mud, freezing dirt, and breaking rocks". Physics Today. 67 (11): 39–44. doi:10.1063/PT.3.2584. ISSN 0031-9228. <a href="https://pubs.aip.org/physicstoday/article/67/11/39/414529/Cracking-mud-freezing-dirt-and-breaking-rocksThe" target="_blank">https://pubs.aip.org/physicstoday/article/67/11/39/414529/Cracking-mud-freezing-dirt-and-breaking-rocksThe</a> <a href="#fnref:8" class="footnote-back-ref">↩</a></p></li>
<li id="fn:9"><p>southernhebrides.com > Staffa - A Geological Marvel. Accessed 29 December 2013. <a href="http://www.southernhebrides.com/staffa.html" target="_blank">http://www.southernhebrides.com/staffa.html</a> <a href="#fnref:9" class="footnote-back-ref">↩</a></p></li>
<li id="fn:10"><p>Oregon State University > Volcano World > ... > Columnar Jointing. Accessed 29 December 2013. <a href="http://volcano.oregonstate.edu/columnar-jointing" target="_blank">http://volcano.oregonstate.edu/columnar-jointing</a> <a href="#fnref:10" class="footnote-back-ref">↩</a></p></li>
<li id="fn:11"><p>U.S. National Park Service > Devils Tower > Geologic Formations. Accessed 29 December 2013. <a href="http://www.nps.gov/deto/naturescience/geologicformations.htm" target="_blank">http://www.nps.gov/deto/naturescience/geologicformations.htm</a> <a href="#fnref:11" class="footnote-back-ref">↩</a></p></li>
<li id="fn:12"><p>Oregon State University > Volcano World > ... > Columnar Jointing. Accessed 29 December 2013. <a href="http://volcano.oregonstate.edu/columnar-jointing" target="_blank">http://volcano.oregonstate.edu/columnar-jointing</a> <a href="#fnref:12" class="footnote-back-ref">↩</a></p></li>
<li id="fn:13"><p>National Trust > Giant's Causeway. Accessed 29 December 2013. <a href="http://www.nationaltrust.org.uk/giants-causeway/history/" target="_blank">http://www.nationaltrust.org.uk/giants-causeway/history/</a> <a href="#fnref:13" class="footnote-back-ref">↩</a></p></li>
<li id="fn:14"><p>Northern Ireland Tourist Board > Causeway Coast & Glens > The Giant's Causeway > Folklore and Legend Archived 2015-05-02 at the Wayback Machine. Accessed 29 December 2013. <a href="http://www.causewaycoastandglens.com/Myths-and-Legends.T1090.aspx" target="_blank">http://www.causewaycoastandglens.com/Myths-and-Legends.T1090.aspx</a> <a href="#fnref:14" class="footnote-back-ref">↩</a></p></li>
<li id="fn:15"><p>Geological Survey of India > Columnar Basalt Retrieved 17 April 2020. <a href="https://www.gsi.gov.in/webcenter/portal/OCBIS/page17/pageGEOTOURISM/page1155" target="_blank">https://www.gsi.gov.in/webcenter/portal/OCBIS/page17/pageGEOTOURISM/page1155</a> <a href="#fnref:15" class="footnote-back-ref">↩</a></p></li>
<li id="fn:16"><p>"HiRISE | Columnar Jointing on Mars and Earth (ESP_029286_1885)". <a href="https://www.uahirise.org/ESP_029286_1885" target="_blank">https://www.uahirise.org/ESP_029286_1885</a> <a href="#fnref:16" class="footnote-back-ref">↩</a></p></li>
<li id="fn:17"><p>Milazzo, Moses (2009). "Discovery of columnar jointing on Mars". Geology. 37 (2): 171–174. doi:10.1130/G25187A.1. <a href="https://pubs.geoscienceworld.org/gsa/geology/article-abstract/37/2/171/519456/Discovery-of-columnar-jointing-on-Mars" target="_blank">https://pubs.geoscienceworld.org/gsa/geology/article-abstract/37/2/171/519456/Discovery-of-columnar-jointing-on-Mars</a> <a href="#fnref:17" class="footnote-back-ref">↩</a></p></li>
<li id="fn:18"><p>Sawn Rocks walking track, Mount Kaputar National Park  NSW National Parks and Wildlife Service. Retrieved 3 January 2019. <a href="https://www.nationalparks.nsw.gov.au/things-to-do/walking-tracks/sawn-rocks-walking-track" target="_blank">https://www.nationalparks.nsw.gov.au/things-to-do/walking-tracks/sawn-rocks-walking-track</a> <a href="#fnref:18" class="footnote-back-ref">↩</a></p></li>
</ol>

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Columnar jointing