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{{Short description|Maar in New Mexico, United States}}
[[File:Kilbourne and Hunts Holes and White Sands.jpg|thumb|Kilbourne Hole (center) and Hunt's Hole (lower right), with [[White Sands National Park]] lit by the sun in the distance beyond the [[Organ Mountains]].]]
[[File:Kilbourne Hole basalt.jpg|thumb|upright|[[Basalt]] cliffs of Kilbourne Hole, looking northwest from near the southwest corner. The cliffs come from the earlier [[Cenozoic]] Afton basalt flow; the magma that caused the maar explosion was also basalt.<ref name="wood" />]]
'''Kilbourne Hole''' is a [[maar]] [[volcanic crater]], located {{convert|30|mi|km}} west of the [[Franklin Mountains (Texas)|Franklin Mountains]] of [[El Paso, Texas]], in the [[Potrillo volcanic field]] of [[Doña Ana County, New Mexico]]. Another maar, Hunt's Hole, lies just two miles south of Kilbourne Hole. These holes are rare examples of volcanic action without a mountainous rim.
 
'''Kilbourne Hole''' is a [[maar]] [[volcanic crater]], located {{convert|30|mi|km}} west of the [[Franklin Mountains (Texas)|Franklin Mountains]] of [[El Paso, Texas]], in the [[Potrillo volcanic field]] of [[Doña Ana County, New Mexico]]. Another maar, Hunt's Hole, lies just two miles{{Convert|2|mi|km|spell=in}} south of. Kilbourne Hole. is Thesenotable holesfor arethe rarelarge examplesnumber of volcanic[[Earth's mantle|mantle]] [[xenolith]]s (solid fragments of mantle rock) that were carried to actionthe withoutsurface aby mountainousthe rimeruption.
The theory of maar formation is that rising [[magma]] super-heats water-saturated earth, far enough below the surface that a high pressure can be contained. At some point, the pressure is too much, and a steam explosion occurs, throwing the earth out in a catastrophic event.<ref>{{cite web|url=http://museum2.utep.edu/archive/geology/DDkilbourne.htm |title=Fossils/Kilbourne Hole |work=Desert Diary |publisher=UTEP Geology Dept. |accessdate=4 Aug 2012 |url-status=dead |archiveurl=https://web.archive.org/web/20100614235452/http://museum2.utep.edu/archive/geology/DDkilbourne.htm |archivedate=2010-06-14 }}</ref> [[Country rock (geology)|Country rocks]] are fragmented and expelled in the atmosphere (together with fragments of the [[magma]]), eventually creating a deep crater, the bottom of which sits below the pre-eruptive ground surface.
 
Estimates of the age of the crater vary from about 24,000 to about 80,000 years.<ref name="Cordell">{{cite journal|first=L. |last=Cordell |year=1975 |title=Combined Geophysical Studies at Kilbourne Hole Maar |publisher=[[University of New Mexico]] Press |workjournal=New Mexico Geological Society Guidebook: 26th Field Conference |pages=273–281}}</ref><ref name="wood">{{cite book |editor-last1=Wood |editor-first1=Charles A. |editor-last2=Kienle |editor-first2=Jürgen (eds.) |year=1990 |url=https://books.google.com/books?id=eyDRib-FJh4C&pg=PA310&lpg=PA310 |title=Volcanoes of North America: United States and Canada |publisher=[[Cambridge University]] Press |isbn=0-521-36469-8 |pages=310–311}}</ref><ref>
{{cite journal
| journal = Soil Science Society of America Journal
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| doi=10.2136/sssaj1987.03615995005100030033x
}}</ref>
 
The volcanic features around El Paso and vicinity are part of the [[Potrillo volcanic field]], in the [[Rio Grande rift]], which extends northward into [[Colorado]].
 
In 1975, Kilbourne Hole was designated as a National Natural Landmark by the National Park Service.<ref>{{Cite web
|url=https://www.nps.gov/subjects/nnlandmarks/site.htm?Site=KIHO-NM|title=National Natural Landmarks - National Natural Landmarks (U.S. National Park Service)|website=www.nps.gov|language=en|quote="Year designated: 1975"|access-date=2019-03-25}}</ref> It is now part of [[Organ Mountains–Desert Peaks National Monument]].
 
==Geologic setting and formation==
==Description of the crater==
Kilbourne Hole and Hunt's Hole are found in the central part of the [[Potrillo volcanic field]], which also contains the Afton-Aden [[basalt]] flows. The area is part of the [[Rio Grande rift]], where the [[Earth's crust]] is being stretched and thinned. The rift is characterized by deep [[sedimentary basin]]s, recent faulting and volcanic activity, and unusually high heat flow upwards from the [[Earth's mantle]]. Kilbourne Hole and Hunt's Hole are located on the same north-trending fault of the Fitzgerald-Robledo fault system.<ref name="padovani-reid-1989">{{cite journal |last1=Padovani |first1=Elaine R. |last2=Reid |first2=Mary R. |title=Field guide to Kilbourne Hole maar, Dona Ana County, New Mexico |journal=New Mexico Bureau of Mines and Mineral Resources Memoir |date=1989 |volume=46 |pages=174–185 |url=https://geoinfo.nmt.edu/publications/monographs/memoirs/46/ |access-date=22 March 2022}}</ref>
 
A [[maar]] forms when rising [[magma]] encounters sediment beds saturated with [[groundwater]]. The magma heats the groundwater to the point where the [[vapor pressure]] overcomes the weight of the overlying beds (the [[overburden pressure]]) and the beds are catastrophically blown out. [[Country rock (geology)|Country rock]] is fragmented and expelled into the atmosphere together with fragments of the [[magma]], creating a deep crater, the bottom of which sits below the pre-eruptive ground surface.<ref name="schmincke-2203-209-228">{{cite book |last1=Schmincke |first1=Hans-Ulrich |title=Volcanism |date=2003 |publisher=Springer |location=Berlin |isbn=9783540436508 |pages=209–228}}</ref> The eruption that is attributed with the formation of the maar depression was dated to around 20,000 years.<ref>{{Cite journal |last=Perkins |first=Dexter |last2=Anthony |first2=Elizabeth Y. |date=2011-12-01 |title=The evolution of spinel lherzolite xenoliths and the nature of the mantle at Kilbourne Hole, New Mexico |url=https://link.springer.com/article/10.1007/s00410-011-0644-1 |journal=Contributions to Mineralogy and Petrology |language=en |volume=162 |issue=6 |pages=1139–1157 |doi=10.1007/s00410-011-0644-1 |issn=1432-0967}}</ref> As a result of the eruption, the maar also experienced a collapse similar to that of a [[caldera]].<ref>{{Cite web |title=New Mexico Geology: Abstract |url=https://geoinfo.nmt.edu/publications/periodicals/nmg/details.cfml?id=28291 |access-date=2024-10-25 |website=New Mexico Bureau of Geology & Mineral Resources |language=en |doi=10.58799/nmg-v9n4.69}}</ref>
 
Kilbourne Hole erupted through [[alluvium]] (unconsolidated water-deposited sediments), the [[Camp Rice Formation]] and through the pre-existing Afton basalt flow. Like most maars, it has a shallow rim, composed of erupted material that was deposited as thin [[pyroclastic surge]] deposits.<ref name="padovani-reid-1989"/>
 
==Characteristics==
[[File:Kilbourne Hole path in.jpg|thumb|left|A view of the Kilbourne Hole from the trail at the southwest corner. Everything visible in this photo is the maar, bottom lands and rim with basalt cliffs.]]
The crater is at an elevation of {{convert|4239|ft|abbr=on}}. It has a diameter of {{convert|1.5|mi|abbr=on}} by {{convert|2.1|mi||abbr=on}} and a depth of {{convert|443|ft|abbr=on}}.<ref name = nlcd2016 >[https://viewer.nationalmap.gov/advanced-viewer/viewer/index.html?marker=-106.964722,31.971944,4326,from%20Kilbourne_Hole,,Kilbourne%20Hole&scale=10000 2016 National Land Cover (NLCD) dataset] Kilbourne Hole</ref>
 
The hole is over a mile wide, and over {{convert|300|ft|m}} deep, with crumbling [[basalt]] cliffs all around except at the southwest corner. The basaltrim cliffs, resemblemeasuring theabout cliffs{{convert|40|ft|m}} in height, are composed of the[[basalt]] and exhibit clear [[columnar jointing]] (a feature common to many basalt cliffs, including those of [[Devils Postpile National Monument]] near [[Yosemite National Park]], withand [[Moses Coulee]] in the [[Channeled Scablands]] of [[Washington (state)|Washington]]), with characteristic reddish -purple, polygonal (mostly [[Hexagonal_prism|hexagonal]]) columns,. except The base of the cliffs is obscured by [[scree]] composed of blocks of basalt that theyhave arebeen notdislodged asfrom tall.the columns Theabove cliffsby arethe aboutwork {{convertof [[erosion]] and [[Weathering#Physical_weathering|40|ft|m}}mechanical highweathering]]. The basalt [[Lava flow|flow]] chunksthat existcomprises inthese abundancecolumns [[Pinch-out|pinches out]] (thins) and eventually disappears as it approaches the southwestern rim of the maar.<ref name="padovani-reid-1989"/>
 
[[File:Dropstone at Kilbourne Hole.jpg|thumb|[[Dropstone#Volcanoes|Dropstone]] in pyroclastic surge beds at Kilbourne Hole]]
Hunt's Hole is a little smaller, with basalt cliffs only at the northeast and southeast sides of the crater. Layers of ashfall and crumbling [[sediment]] also rise about {{convert|40|ft|m}} high, on the south rim of the crater. Sand dunes have collected on the east sides of the both craters, rising about {{convert|100|ft|m}} above the desert floor. A dry lakebed lies on the floor of each crater.
The eastern and northern rim of the hole have low rim deposits of ejecta from the maar eruptions. These rest on the basalt flow where it is present or on older sediments. The ejecta at Kilbourne Hole contains [[dropstones]] launched as [[Volcanic bomb|bombs]], usually greater than 2.5 inches across<ref>{{Cite web |title=Tour: Kilbourne Hole |url=https://geoinfo.nmt.edu/tour/landmarks/kilbourne_hole/ |access-date=2024-10-26 |website=New Mexico Bureau of Geology & Mineral Resources |language=en}}</ref> and a large number of [[xenolith]]s derived from the lower crust and mantle. These have been closely studied by geologists to learn more about geologic processes deep underground.<ref name="padovani-reid-1989"/>
 
Hunt's Hole is a little smaller, with basalt cliffs only at the northeast and southeast sides of the crater. Layers of ashfall and crumbling [[sediment]] also rise about {{convert|40|ft|m}} high, on the south rim of the crater. Sand dunes have collected on the east sides of the both craters, rising about {{convert|100|ft|m}} above the desert floor. A dry lakebed lies on the floor of each crater.
 
==Xenoliths==
Kilbourne Hole is notable for the abundance of xenoliths in the crater ejecta. These are fragments of country rock carried intact to the surface by the eruption. Xenoliths at Kilbourne Hole include both upper mantle rocks and lower crustal rocks and are most abundant in the northern and eastern rim. Because these are samples of portions of the Earth that are inaccessible by mining or drilling, they are of great scientific interest.<ref name="padovani-reid-1989"/>
 
Most of the mantle xenoliths at Kilbourne Hole are composed of [[lherzolite]], a rock composed mostly of [[olivine]] and [[pyroxene]]. The olivine has a distinctive pale green color in which the pyroxene forms black flecks. [[Wehrlite]] is occasionally found here as well.<ref name="padovani-reid-1989"/>
 
Deep crustal rocks include a variety of [[granulite]]s of both high-silica ([[felsic]]) and low-silica ([[mafic]]) compositions, mostly [[charnockite]] and [[anorthosite]].<ref>{{Cite web |title=Tour: Kilbourne Hole |url=https://geoinfo.nmt.edu/tour/landmarks/kilbourne_hole/ |access-date=2024-10-26 |website=New Mexico Bureau of Geology & Mineral Resources |language=en}}</ref> These likely took less than three days to reach the surface from their place of origin, and show pristine composition and texture. Their characteristics show that they were little altered from their formation 1.6 to 1.8 billion years ago, other than some reheating during the opening of the Rio Grande rift.<ref name="padovani-reid-1989"/>
 
Xenoliths are almost entirely absent in the ejecta from Hunt's Hole, but xenoliths are found in Potrillo maar to the south.<ref name="padovani-reid-1989"/>
<gallery>
File:Kilbourne Hole embedded xenolith.jpg|Mantle xenolith embedded in basalt
File:Kilbourne Hole lxenoliths.jpg|Mantle xenoliths
File:Kilbourne Hole lower crust xenolith.jpg|Lower crust xenolith
</gallery>
 
==NASA training==
[[NASA]] geologically trained the [[Apollo Astronauts]] in April and Nov.November 1969, June 1970, and Jan.January and Dec.December 1971. Astronauts who would use this training on the Moon included [[Apollo 12]]'s [[Pete Conrad]] and [[Alan Bean]], [[Apollo 14]]'s [[Alan Shepard]] and [[Edgar Mitchell]], [[Apollo 15]]'s [[David Scott]] and [[James Irwin]], [[Apollo 16]]'s [[John Young (astronaut)|John Young]] and [[Charlie Duke]], and [[Apollo 17]]'s [[Gene Cernan]] and [[Jack Schmitt]].<ref>{{cite book |last1=Phinney |first1=William |title=Science Training History of the Apollo Astronauts |date=2015 |publisher=NASA SP -2015-626 |pages=233, 235, 237, 241, 245, 251}}</ref>
 
In 2017, a NASA field team visited the hole to test various instruments that are planned to be used in future space missions. Jack Schmitt attended the tests, as well as astronaut [[Barry E. Wilmore|Barry Wilmore]] who was there to assist in simulated moonwalks at the hole.<ref>{{Cite web |last=Bleacher |first=David Ladd, Rob Andreoli, and Jacob |date=2017-12-11 |title=NASA Scientific Visualization Studio {{!}} Exploring A Crater |url=https://svs.gsfc.nasa.gov/12788/ |access-date=2024-09-15 |website=NASA Scientific Visualization Studio |language=english}}</ref>
 
[[Image:Donaana-countymap.jpg|thumb|General location of Kilbourne Hole, Doña Ana County, New Mexico]]
 
==Access==
Kilbourne Hole is located within [[Organ Mountains–Desert Peaks National Monument]] and administered by the [[Bureau of Land Management]].<ref name=BLM>{{cite web | url = https://www.blm.gov/visit/kilbourne-hole-volcanic-crater | title = Kilbourne Hole Volcanic Crater | accessdate = 10 September 2020 |publisher=Bureau of Land Management}}</ref> It is accessed via Doña Ana County Road A-011, driving {{Convert|8 miles|mi|km}} west from the railroad. The hole is "on the right, past the big tan dirt bank."<ref name=BLM/> Much of the land inside the hole is private property., and collecting rocks from the location is illegal. Hunt's Hole is about {{Convert|2 miles|mi|km}} south on A-013.
 
== See also ==
 
* [[List of National Natural Landmarks in New Mexico]]
 
[[File:BLM Sign on the Road to Kilbourne Hole.jpg|thumb|right|BLM sign on the road to Kilbourne Hole.]]
 
==References==
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[[Category:Landforms of Doña Ana County, New Mexico]]
[[Category:National Natural Landmarks in New Mexico]]
[[Category:Volcanoes of New Mexico]]