Wyandotte Caves
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The Wyandotte Caves is a pair of
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 whe ...
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 ...
located on the Ohio River in Harrison-Crawford State Forest in
Crawford County Crawford County is the name of eleven counties in the United States: * Crawford County, Arkansas * Crawford County, Georgia * Crawford County, Illinois * Crawford County, Indiana * Crawford County, Iowa * Crawford County, Kansas * Crawford Count ...
, north-east of Leavenworth and from Corydon in southern
Indiana Indiana () is a U.S. state in the Midwestern United States. It is the 38th-largest by area and the 17th-most populous of the 50 States. Its capital and largest city is Indianapolis. Indiana was admitted to the United States as the 19th s ...
which are a popular tourist attraction. Wyandotte Caves were designated a
National Natural Landmark The National Natural Landmarks (NNL) Program recognizes and encourages the conservation of outstanding examples of the natural history of the United States. It is the only national natural areas program that identifies and recognizes the best ...
in 1972. They are now part of O'Bannon Woods State Park. The cave system is the 5th largest in the state of Indiana. The term "Wyandotte Caves" is used to refer to Wyandotte Cave (sometimes called the "Historic Cave") and Little Wyandotte Cave (also called Siberts Cave and sometimes called the "New Cave"), but the two caves are completely different. They are located very close to each other, and are owned and managed by the same entity. There the resemblance ends.


Geological history and formations

Wyandotte Caves began to form in the
Pliocene The Pliocene ( ; also Pleiocene) is the epoch in the geologic time scale that extends from 5.333 million to 2.58
dissolved limestone, causing hollow caves to form. The limestone which forms much of Southern Indiana's bedrock, and from which Wyandotte and other local caves are formed, was first deposited in the Mississippian epoch (360  Ma to 325 Ma), when Indiana was covered by a shallow inland sea. Although the glaciers of the Pliocene and
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 in ...
periods did not quite reach as far south as the area now known as
Crawford County Crawford County is the name of eleven counties in the United States: * Crawford County, Arkansas * Crawford County, Georgia * Crawford County, Illinois * Crawford County, Indiana * Crawford County, Iowa * Crawford County, Kansas * Crawford Count ...
, where Wyandotte and Marengo Caves are located, they dramatically influenced the development of those caves. The Ohio River was formed at this time, and today flows only minutes from Wyandotte Caves. The advancing and retreating glaciers destroyed the pre-existing
Teays River The Teays River (pronounced taze) was a major preglacial river that drained much of the present Ohio River watershed, but took a more northerly downstream course. Traces of the Teays across northern Ohio and Indiana are represented by a network ...
, and the Ohio River was formed, draining the land that the Teays once drained. As the glaciers melted, the icy cold water flowing towards the Ohio River (which was then much higher than it is now) dissolved the limestone which is the bedrock for much of Southern Indiana, hollowing out caves such as Wyandotte. The main entrance to Wyandotte Cave is above the level of the Blue River. Wyandotte Cave is known for its long open passageways and large rooms. With of passageways on five levels it is the fifth longest cave in Indiana. Included in its formations is Monument Mountain. At tall, Monument Mountain is considered to be the world's largest underground mountain. Wyandotte Cave is also home to a great many
helictite A helictite is a speleothem (cave-formed mineral) found in a limestone cave that changes its axis from the vertical at one or more stages during its growth. Helictites have a curving or angular form that looks as if they were grown in zero gra ...
s, which are considered rare. The cave is also home to the tallest stalagmite in the world, known as the Pillar of the Constitution, but this is only visible on crawling tours. Long
speleothems 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 on ...
, formed by rainwater dissolving calcium carbonate, abound in Siberts Cave. The cave exhibits a wide variety of speleothems including; stalactites, stalagmites, columns,
flowstone Flowstones are sheetlike deposits of calcite or other carbonate minerals, formed where water flows down the walls or along the floors of a cave. They are typically found in "solution caves", in limestone, where they are the most common speleoth ...
, flowstone colored with iron oxide known as cave bacon, flowstone known as cave draperies,
soda straw A soda straw (or simply straw) is a speleothem in the form of a hollow mineral cylinder (geometry), cylindrical tube. They are also known as tubular stalactites. Soda straws grow in places where water leaches slowly through cracks in rock, such a ...
s, popcorn, and rimstone dams. The temperature inside both caves maintains a constant .


History of human use

Wyandotte Cave was used by Native Americans for nearly 4000 years before Europeans arrived in the area; carbon dating of artifacts provided evidence of human activity potentially as far back as 8000 BC. The Native Americans used torches made of hickory bark and grape vines to light the cave where they mined for
aragonite Aragonite is a carbonate mineral, one of the three most common naturally occurring crystal forms of calcium carbonate, (the other forms being the minerals calcite and vaterite). It is formed by biological and physical processes, including pre ...
, which they used for pipes and necklaces, and
chert Chert () is a hard, fine-grained sedimentary rock composed of microcrystalline or cryptocrystalline quartz, the mineral form of silicon dioxide (SiO2). Chert is characteristically of biological origin, but may also occur inorganically as a ...
, which they used to make stone tools. The remains of their mining explorations can be seen on tours to this day. The discovery of Wyandotte Cave by European settlers is believed to have occurred around 1798. Shortly thereafter Wyandotte Cave became known as an excellent source of
saltpeter Potassium nitrate is a chemical compound with the chemical formula . This alkali metal nitrate Salt (chemistry), salt is also known as Indian saltpetre (large deposits of which were historically mined in India). It is an ionic salt of potassium ...
, an integral component of
gunpowder Gunpowder, also commonly known as black powder to distinguish it from modern smokeless powder, is the earliest known chemical explosive. It consists of a mixture of sulfur, carbon (in the form of charcoal) and potassium nitrate (saltpeter). Th ...
, and of
Epsom salts Magnesium sulfate or magnesium sulphate (in English-speaking countries other than the US) is a chemical compound, a salt with the formula , consisting of magnesium cations (20.19% by mass) and sulfate anions . It is a white crystalline solid, s ...
, which have medical uses. Saltpeter mining in the cave reached a peak under a man by the name of Dr. Benjamin Adams during the
War of 1812 The War of 1812 (18 June 1812 – 17 February 1815) was fought by the United States, United States of America and its Indigenous peoples of the Americas, indigenous allies against the United Kingdom of Great Britain and Ireland, United Kingdom ...
. Modern tours feature Dr. Adams' vats and hoppers, and point out where
magnesium sulfate Magnesium sulfate or magnesium sulphate (in English-speaking countries other than the US) is a chemical compound, a salt with the formula , consisting of magnesium cations (20.19% by mass) and sulfate anions . It is a white crystalline solid, ...
(the chemical name of Epsom salt) is visible as a glittery substance lining the cave walls. The cave was also used to store supplies for the army of
William Henry Harrison William Henry Harrison (February 9, 1773April 4, 1841) was an American military officer and politician who served as the ninth president of the United States. Harrison died just 31 days after his inauguration in 1841, and had the shortest pres ...
. Wyandotte Cave was named by Governor David Wallace after the river which was then known as the Wyandotte, but which is currently known as the Blue River. Before receiving its current name it was variously called the Mammoth Cave of Indiana, the Epsom Salts Cave, and the Indiana Saltpetre Cave. The land beneath which the caves are located was bought by Henry Peter Rothrock in 1819. The Rothrocks seemed to have had little to do with the cave until 1850, when they offered the first commercial tours of the cave after the discovery of a large new section of cavern. This date of 1850 makes Wyandotte cave the fourth oldest commercial cave in the United States. Siberts Cave was discovered in 1851 and named after the person who discovered it. The caves were sold to the
Department of Natural Resources This article lists subnational environmental agencies in the United States, by state. Agencies with a variety of titles and responsibilities are included, e.g. Department of Environment, Department of Environmental Conservation, Department of E ...
, Division of Forestry in 1966, along with of woodland. The caves were closed to visitation from 2009 to 2016 in order to slow the spread of
White Nose Syndrome White-nose syndrome (WNS) is a fungal disease in North American bats which has resulted in the dramatic decrease of the bat population in the United States and Canada, reportedly killing millions as of 2018. The condition is named for a distincti ...
affecting the bat population. After eight years, the agencies studying the bats gave the "okay" to open up the caves, as long as "decontamination stations" were walked through at the end of each tour. The eight-year closure of the caves drastically affected the buildings on site, and many were taken down due to structural damage. State Representative Lloyd Arnold (R-74) and Lieutenant Governor
Eric Holcomb Eric Joseph Holcomb (born May 2, 1968) is an American politician who is the 51st and current governor of Indiana, serving since 2017. A member of the Republican Party, he served as the 51st lieutenant governor of Indiana from 2016 to 2017 under ...
showcased the $1.7 million project to replace the main building on-site and re-wire the interior of the cave. As of 2018, the lights in the cave have been repaired and replaced and a temporary gatehouse has been built.


Cave Tours (2018)


Little Wyandotte Cave

Little Wyandotte Cave is entirely separate from Big Wyandotte Cave and contains many
flowstone Flowstones are sheetlike deposits of calcite or other carbonate minerals, formed where water flows down the walls or along the floors of a cave. They are typically found in "solution caves", in limestone, where they are the most common speleoth ...
and dripstone formations. The park tour of this cave, open to all ages and 30-45 minutes long, involves no long stairways and is considered the least difficult of tours offered at Wyandotte Caves.


Big Wyandotte Cave

A demanding 2 hour/ tour deep into Big Wyandotte Cave allows visitors to see the rare formations called helictites,
gypsum Gypsum is a soft sulfate mineral composed of calcium sulfate dihydrate, with the chemical formula . It is widely mined and is used as a fertilizer and as the main constituent in many forms of plaster, blackboard or sidewalk chalk, and drywal ...
,
epsomite Epsomite, Epsom salt, or magnesium sulfate heptahydrate, is a hydrous magnesium sulfate mineral with formula MgSO4·7H2O. Epsomite crystallizes in the orthorhombic system as rarely found acicular or fibrous crystals, the normal form is as massiv ...
, prehistoric
flint Flint, occasionally flintstone, is a sedimentary cryptocrystalline form of the mineral quartz, categorized as the variety of chert that occurs in chalk or marly limestone. Flint was widely used historically to make stone tools and sta ...
quarries, and a formation called "Monument Mountain".


Cave life

Both Wyandotte Caves are believed to home more than 20 known animal species, including bats, cave salamanders, crayfish, and crickets. Bones of larger wildlife have also been found in both caves.


Bats

Indiana is home to 12 native species of
bat Bats are mammals of the order Chiroptera.''cheir'', "hand" and πτερόν''pteron'', "wing". With their forelimbs adapted as wings, they are the only mammals capable of true and sustained flight. Bats are more agile in flight than most ...
s. Wyandotte Cave is occupied by members of nine of those 12 species; the total bat population is over 30,000. The most common bat in the cave is the
endangered An endangered species is a species that is very likely to become extinct in the near future, either worldwide or in a particular political jurisdiction. Endangered species may be at risk due to factors such as habitat loss, poaching and in ...
Myotis sodalis The Indiana bat (''Myotis sodalis'') is a medium-sized mouse-eared bat native to North America. It lives primarily in Southern and Midwestern U.S. states and is listed as an endangered species. The Indiana bat is grey, black, or chestnut in colo ...
, (commonly known as the Indiana Bat), followed by the Myotis lucifugus (commonly known as the little brown bat). Little Wyandotte cave rarely gets bats, as the only entrance to that cave is less than 200 years old, and humans have been present in that cave on a regular basis since it first opened. However, the occasional adventurous bat will venture in. The presence of hibernating bats in the winter is the main reason that the caves are closed to the public from the first of November until February 28. Bats can occasionally be seen by the lucky visitor during the rest of the year, but they are far less numerous and less likely to be disturbed in the warmer months.


Salamanders

Cave
salamanders Salamanders are a group of amphibians typically characterized by their lizard-like appearance, with slender bodies, blunt snouts, short limbs projecting at right angles to the body, and the presence of a tail in both larvae and adults. All ten ...
can often be seen in the entrance area of Wyandotte cave and inside of Little Wyandotte Cave.


Fish

Blind
cavefish Cavefish or cave fish is a generic term for fresh and brackish water fish adapted to life in caves and other underground habitats. Related terms are subterranean fish, troglomorphic fish, troglobitic fish, stygobitic fish, phreatic fish and ...
are rarely seen in the larger of Wyandotte Caves, as it is very dry in modern times. Little Wyandotte Cave, however, is much wetter than the historic cave, but still contains no fish. The only living aquatic life found is bacteria.


Crickets

Cave cricket The orthopteran family Rhaphidophoridae of the suborder Ensifera has a worldwide distribution. Common names for these insects include cave wētā, cave crickets, camelback crickets, camel crickets, Hogan bugs, spider crickets (sometimes shorte ...
s abound in the smaller cave, and some occasionally enter the larger cave. They are often eaten by snakes, however.


Gallery

Image:Wyandotte cave17.jpg, alt=A red sign with yellow letters that read "Historic Wyandotte Caves Indiana Department of Natural Resources Division of Forestry Now Open". The sign also has a drawing of Monument Mountain., Park Entrance Image:Wyandotte cave8.jpg, alt=refer to caption, Rare
helictite A helictite is a speleothem (cave-formed mineral) found in a limestone cave that changes its axis from the vertical at one or more stages during its growth. Helictites have a curving or angular form that looks as if they were grown in zero gra ...
formations Image:Wyandotte cave9.jpg, alt=refer to caption, Column formation Image:Wyandotte cave12.jpg, alt=refer to caption, Narrow passageway in the cave Image:Wyandotte cave16.jpg, alt=A large room in the cave containing approximately 11 dusty benches., An Oddfellows meeting hall, used in the mid-1800s Image:Wyandotte Cave stalagmite.jpg, alt=refer to caption, Wyandotte Cave stalagmite


References


External links


Wyandotte Caves Official Facebook Page
*
Indiana Caves Subterranean Club website
*
Postcard
depicting "Monument Mountain" {{authority control Caves of Indiana Show caves in the United States Limestone caves Protected areas of Crawford County, Indiana State parks of Indiana National Natural Landmarks in Indiana Archaeological sites in Indiana Indiana in the War of 1812 Landforms of Crawford County, Indiana