Indian Caverns
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Indian Caverns was a
show cave A show cave—also called tourist cave, public cave, and, in the United States, commercial cave—is a cave which has been made accessible to the public for guided visits. Definition A show cave is a cave that has been made accessible to ...
in Spruce Creek,
Pennsylvania Pennsylvania (; ( Pennsylvania Dutch: )), officially the Commonwealth of Pennsylvania, is a state spanning the Mid-Atlantic, Northeastern, Appalachian, and Great Lakes regions of the United States. It borders Delaware to its southeast, ...
,
United States The United States of America (U.S.A. or USA), commonly known as the United States (U.S. or US) or America, is a country primarily located in North America. It consists of 50 states, a federal district, five major unincorporated territorie ...
from 1929-2017. It is a horizontal karst cave of
Ordovician The Ordovician ( ) is a geologic period and System (geology), system, the second of six periods of the Paleozoic Era (geology), Era. The Ordovician spans 41.6 million years from the end of the Cambrian Period million years ago (Mya) to the start ...
Nealmont/Benner
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 ...
, estimated to be about 500,000 years old. It is the second-largest cave in Pennsylvania and the largest limestone cave. Indian Caverns consists of two sections, originally separated by a 14-foot wall: the "Historic Cave" and the "Giant's Hall". The "historic" part of the cave is generally low-ceilinged and closer to the surface (as shallow as 15 ft) with a couple of wide rooms and extensive
speleothem 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 ...
formation. The Giant's Hall area consists of several large passageways, up to 60 feet high, but with fewer speleothems - though it does include the largest sheet of
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 speleothe ...
in the northeast and a substantial rimstone pool. The lowest point of the cave is approximately 140 feet beneath the surface and the cave temperature is a constant 56 degrees Fahrenheit (13 degrees Celsius).


Background

Artifacts found in the cave indicate that it was inhabited as long ago as 8000 BC. The earliest tribe known to have used the cave were the
Susquehannock The Susquehannock people, also called the Conestoga by some English settlers or Andastes were Iroquoian Native Americans who lived in areas adjacent to the Susquehanna River and its tributaries, ranging from its upper reaches in the southern p ...
s, circa 1600 AD. It was later used by Algonkian (including
Lenni Lenape The Lenape (, , or Lenape , del, Lënapeyok) also called the Leni Lenape, Lenni Lenape and Delaware people, are an indigenous peoples of the Northeastern Woodlands, who live in the United States and Canada. Their historical territory inclu ...
) and
Iroquois The Iroquois ( or ), officially the Haudenosaunee ( meaning "people of the longhouse"), are an Iroquoian-speaking confederacy of First Nations peoples in northeast North America/ Turtle Island. They were known during the colonial years to ...
(probably
Mohawk Mohawk may refer to: Related to Native Americans *Mohawk people, an indigenous people of North America (Canada and New York) *Mohawk language, the language spoken by the Mohawk people *Mohawk hairstyle, from a hairstyle once thought to have been t ...
) tribes through the early eighteenth century. Examples of the artifacts are on display in the cave and include arrow and spearheads, tobacco pipes, tomahawks, punches, banner stones, a bone flute, and pottery shards. They also include a rare effigy of the Algonkian guardian spirit, Mesingw. One room, the "Grotto of the Wah-Wah-Taysee", features a
phosphorescent Phosphorescence is a type of photoluminescence related to fluorescence. When exposed to light (radiation) of a shorter wavelength, a phosphorescent substance will glow, absorbing the light and reemitting it at a longer wavelength. Unlike fluor ...
mineral deposit in the ceiling and walls. It was originally thought to be
radium Radium is a chemical element with the symbol Ra and atomic number 88. It is the sixth element in group 2 of the periodic table, also known as the alkaline earth metals. Pure radium is silvery-white, but it readily reacts with nitrogen (rather t ...
, but has since been identified as
zinc sulfide Zinc sulfide (or zinc sulphide) is an inorganic compound with the chemical formula of ZnS. This is the main form of zinc found in nature, where it mainly occurs as the mineral sphalerite. Although this mineral is usually black because of various i ...
reacting with
calcite Calcite is a Carbonate minerals, carbonate mineral and the most stable Polymorphism (materials science), polymorph of calcium carbonate (CaCO3). It is a very common mineral, particularly as a component of limestone. Calcite defines hardness 3 on ...
in the limestone. The cave also contains a "musical rock", which resounds with a bell-like tone when struck. Indian Caverns was known about by European settlers from the late eighteenth century. From about 1816, it was one of several caves used as a hideout by the outlaw David Lewis until his death in 1820. The entrance and grounds were bought in 1928 by Harold Wertz, Sr., a local entrepreneur, and the cave was opened to the public on June 14, 1929. Wertz opened the cave after two years of excavation and about half a million dollars worth of investments. Wertz, along with his family, moved to Florida during the great depression, but returned each summer to run and upkeep the caves. Before the Indian relics were found inside the first few chambers in the caverns, the cave was planned to be called "Franklin Cave", but it seemed more appropriate to be called "Historic Indian Cave". Then in the late 1930s - early 1940s the name was changed to "Indian Caverns". It was a popular destination during the Early Auto Era due to the Edwardian fascination with the "wonders" of nature and remained in continuous operation until 2017. In 2017, the Western Pennsylvania Convervancy purchased the property and is currently in the works of naturalizing the cave (returning it to its original state). The Conservancy plans to use the caverns as a bat sanctuary in the coming years and conduct research on the local bat species.


External links


Show Caves of the United States website
{{coord, 40.6455, -78.0904, region:US-PA_type:landmark, display=title Caves of Pennsylvania Show caves in the United States Limestone caves Landforms of Huntingdon County, Pennsylvania Tourist attractions in Huntingdon County, Pennsylvania