Wilson Butte Cave is located on the
Snake River
The Snake River is a major river in the interior Pacific Northwest region of the United States. About long, it is the largest tributary of the Columbia River, which is the largest North American river that empties into the Pacific Ocean. Begin ...
plain in
Jerome County, northeast of
Twin Falls and southeast of
Shoshone
The Shoshone or Shoshoni ( or ), also known by the endonym Newe, are an Native Americans in the United States, Indigenous people of the United States with four large cultural/linguistic divisions:
* Eastern Shoshone: Wyoming
* Northern Shoshon ...
, Idaho. It is an archeological site listed on the
National Register of Historic Places
The National Register of Historic Places (NRHP) is the Federal government of the United States, United States federal government's official United States National Register of Historic Places listings, list of sites, buildings, structures, Hist ...
and maintained by the
Bureau of Land Management
The Bureau of Land Management (BLM) is an agency within the United States Department of the Interior responsible for administering federal lands, U.S. federal lands. Headquartered in Washington, D.C., the BLM oversees more than of land, or one ...
(BLM).
A round bubble in appearance, it pops up from a flat, wide bed of ancient
basalt
Basalt (; ) is an aphanite, aphanitic (fine-grained) extrusive igneous rock formed from the rapid cooling of low-viscosity lava rich in magnesium and iron (mafic lava) exposed at or very near the planetary surface, surface of a terrestrial ...
lava. An
inflationary or uplift cave is inside the bubble. While archeologists are uncertain of the exact dates prior to 10,000 years ago, evidence has been found that native peoples lived at Wilson Butte Cave at least 10,000 years ago. Artifacts found here provide the oldest evidence of human presence on the
Snake River Plain and are among the oldest evidence in North America.
Archeologists are fairly certain that the cave was settled so early because it was used as a base to hunt
bison
A bison (: bison) is a large bovine in the genus ''Bison'' (from Greek, meaning 'wild ox') within the tribe Bovini. Two extant taxon, extant and numerous extinction, extinct species are recognised.
Of the two surviving species, the American ...
.
[ Strong connections have been found between the Fremont culture and the ]Shoshone people
The Shoshone or Shoshoni ( or ), also known by the endonym Newe, are an Native Americans in the United States, Indigenous people of the United States with four large cultural/linguistic divisions:
* Eastern Shoshone: Wyoming
* Northern Shoshon ...
, who lived there after the Fremont peoples. Vegetation in the region was very similar to modern times. Camel
A camel (from and () from Ancient Semitic: ''gāmāl'') is an even-toed ungulate in the genus ''Camelus'' that bears distinctive fatty deposits known as "humps" on its back. Camels have long been domesticated and, as livestock, they provid ...
s and giant ground sloth
Ground sloths are a diverse group of extinct sloths in the mammalian superorder Xenarthra. They varied widely in size with the largest, belonging to genera '' Lestodon'', ''Eremotherium'' and ''Megatherium'', being around the size of elephants. ...
s once roamed this region. Deposits here are believed to have been undisturbed until amateurs discovered them in 1958. Two of the major excavations of the cave were conducted by teams led by Ruth Gruhn: one in 1959–1960 and one in 1988–1989. Gruhn dates the site's earliest occupation to 14,000–15,000 years ago.
The lava
Lava is molten or partially molten rock (magma) that has been expelled from the interior of a terrestrial planet (such as Earth) or a Natural satellite, moon onto its surface. Lava may be erupted at a volcano or through a Fissure vent, fractu ...
of the area is a dark gray to black fine-grained basalt
Basalt (; ) is an aphanite, aphanitic (fine-grained) extrusive igneous rock formed from the rapid cooling of low-viscosity lava rich in magnesium and iron (mafic lava) exposed at or very near the planetary surface, surface of a terrestrial ...
. The cave is a lava tube developed in a pressure ridge in the flowing lava. The source of the lava is Wilson's Butte, which is about one half mile southeast of the cave. The lava is more than 15,000 years old, as determined by radiocarbon dating
Radiocarbon dating (also referred to as carbon dating or carbon-14 dating) is a method for Chronological dating, determining the age of an object containing organic material by using the properties of carbon-14, radiocarbon, a radioactive Isotop ...
of a camel bone from within a lava tube cave. The bone had tool markings indicating working by humans.
See also
* National Register of Historic Places listings in Jerome County, Idaho
References
Further reading
* Ruth Gruhn. ''The Archaeology of Wilson Butte Cave, South-central Idaho''. Occasional papers 6. Pocatello: Idaho State College Museum, 1961.
* Ruth Gruhn. ''New excavations at Wilson Butte Cave, South-central Idaho''. Idaho Museum of Natural History occasional paper 38. Pocatello: Idaho State Museum of Natural History, 2006.
External links
Visit Idaho - Wilson Butte Cave
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Archaeological sites on the National Register of Historic Places in Idaho
Bureau of Land Management areas in Idaho
Caves of Idaho
Landforms of Jerome County, Idaho
Lava tubes
Protected areas of Jerome County, Idaho
National Register of Historic Places in Jerome County, Idaho