The Mitchell Caverns, within the Mitchell Caverns Natural Preserve, are three solution
limestone
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms wh ...
caves
A cave or cavern is a natural void in the ground, specifically a space large enough for a human to enter. Caves often form by the weathering of rock and often extend deep underground. The word ''cave'' can refer to smaller openings such as sea ...
, only two of which are open to the public, located on the east side of the
Providence Mountains
The Providence Mountains are found in the eastern Mojave Desert of San Bernardino County, California, U.S. The range reaches an elevation of at Edgar Peak and is home to the Mitchell Caverns Natural Preserve in the Providence Mountains State ...
at an elevation of , within the
Providence Mountains State Recreation Area. The caverns are located in the
Mojave Desert
The Mojave Desert ( ; mov, Hayikwiir Mat'aar; es, Desierto de Mojave) is a desert in the rain shadow of the Sierra Nevada mountains in the Southwestern United States. It is named for the indigenous Mojave people. It is located primarily i ...
, in
San Bernardino County, California
San Bernardino County (), officially the County of San Bernardino, is a county located in the southern portion of the U.S. state of California, and is located within the Inland Empire area. As of the 2020 U.S. Census, the population was 2,18 ...
.
Geology
The caves lie within a thick sequence of marine
Permian
The Permian ( ) is a geologic period and stratigraphic system which spans 47 million years from the end of the Carboniferous Period million years ago (Mya), to the beginning of the Triassic Period 251.9 Mya. It is the last period of the Pale ...
limestone
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms wh ...
. They were formed before the
Pleistocene
The Pleistocene ( , often referred to as the '' Ice age'') is the geological epoch that lasted from about 2,580,000 to 11,700 years ago, spanning the Earth's most recent period of repeated glaciations. Before a change was finally confirmed ...
epoch
In chronology and periodization, an epoch or reference epoch is an instant in time chosen as the origin of a particular calendar era. The "epoch" serves as a reference point from which time is measured.
The moment of epoch is usually decided by ...
, when ground water with a high
carbonic acid content ate into the surrounding
sedimentary
Sedimentary rocks are types of rock that are formed by the accumulation or deposition of mineral or organic particles at Earth's surface, followed by cementation. Sedimentation is the collective name for processes that cause these particles ...
limestone.
Stalactites
A stalactite (, ; from the Greek 'stalaktos' ('dripping') via
''stalassein'' ('to drip') is a mineral formation that hangs from the ceiling of caves, hot springs, or man-made structures such as bridges and mines. Any material that is solubl ...
,
stalagmite
A stalagmite (, ; from the Greek , from , "dropping, trickling")
is a type of rock formation that rises from the floor of a cave due to the accumulation of material deposited on the floor from ceiling drippings. Stalagmites are typically ...
s, and other
cave formations
A speleothem (; ) is a geological formation by mineral deposits that accumulate over time in natural caves. Speleothems most commonly form in calcareous caves due to carbonate dissolution reactions. They can take a variety of forms, depending o ...
were formed from
calcium carbonate left by dripping mineral water.
History
Numerous paleontological and archaeological finds have been made in and around the caverns. Scientists have found the remains of several prehistoric animals, including a
Shasta ground sloth. The caverns were a special place for the
Chemehuevi
The Chemehuevi are an indigenous people of the Great Basin. They are the southernmost branch of Southern Paiute.[tourist
Tourism is travel for pleasure or business; also the theory and practice of touring, the business of attracting, accommodating, and entertaining tourists, and the business of operating tours. The World Tourism Organization defines tourism ...]
attraction and rest stop for travelers on nearby
U.S. Route 66. The Mitchells also held mining rights to the area and dug several prospect holes and tunnels, some of which are still visible.
The area became a state park in 1956. The surrounding lands became a part of the
National Park Service
The National Park Service (NPS) is an List of federal agencies in the United States, agency of the Federal government of the United States, United States federal government within the United States Department of the Interior, U.S. Department of ...
Mojave National Preserve
Mojave National Preserve is a United States National Preserve located in the Mojave Desert of San Bernardino County, California, USA, between Interstate 15 and Interstate 40. The preserve was established October 31, 1994, with the passage of ...
in 1994, but the caves are still owned and operated by the state of California.
Cavern tours
The "Tecopa" and "El Pakiva" caves are connected by a man-made tunnel and are open to guided tours led by
California State Park
The California Department of Parks and Recreation, more commonly known as California State Parks, manages the California state parks system. The system administers 279 separate park units on 1.4 million acres (570,000 hectares), with over 280 ...
rangers. These caves are the only limestone caves in the California State Park system.
According to a California tourism guide, “You enter the limestone caverns at an altitude of about above the desert floor. The higher view of the desert from the Visitor Center is magnificent…Not too spacious, these chambers contain strangely beautiful cave coral, stalactites, and stalagmites.”
[
]
;2011-2017 closure
In January 2011, due to California's budget crisis, all tours were suspended and the Providence Mountains State Recreation Area closed. Vandalism plagued the caverns' visitor center and installations after their closure.
Over a long period, major infrastructure upgrades took place. Mitchell Caverns and Providence Mountains SRA reopened, and the caverns resumed tours, on November 3, 2017, after being closed for nearly seven years.
["Reopening" http://www.parks.ca.gov/?page_id=615]
See also
*
Providence Mountains State Recreation Area
*
Mojave National Preserve
Mojave National Preserve is a United States National Preserve located in the Mojave Desert of San Bernardino County, California, USA, between Interstate 15 and Interstate 40. The preserve was established October 31, 1994, with the passage of ...
References
* http://Desertusa.com - Mitchell Caverns article.
* Robert P. Sharp and Allen F. Glazner, ''Geology Underfoot in Southern California'', Missoula Mont: Mountain Press, 1993.
External links
Official Providence Mountains State Recreation Area websiteCommittee to Reopen Mitchell Caverns non-profit website
{{authority control
Caves of California
Limestone caves
Mojave Desert
Mojave National Preserve
Protected areas of the Mojave Desert
Protected areas of San Bernardino County, California
Archaeological sites in California
National Natural Landmarks in California
Landforms of San Bernardino County, California
Landmarks in California
Chemehuevi