Kitley Show Cave
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Kitley Show Cave is a
solution cave A solutional cave, solution cave, or karst cave is a cave usually formed in the soluble rock limestone. It is the most frequently occurring type of cave. It can also form in other rocks, including chalk, dolomite, marble, salt beds, and gypsum. ...
in
Yealmpton Yealmpton () is a village and civil parish in the English county of Devon. It is located in the South Hams on the A379 Plymouth to Kingsbridge road and is about from Plymouth. Its name derives from the River Yealm that flows through the villag ...
,
Devon Devon ( , historically known as Devonshire , ) is a ceremonial and non-metropolitan county in South West England. The most populous settlement in Devon is the city of Plymouth, followed by Devon's county town, the city of Exeter. Devon is ...
, England. Originally discovered by quarrying, it used to be open to the public as a show cave, but is now closed.


Description

The cave is a fragment of a system associated with the
River Yealm The Yealm is a river in Devon in England that rises above sea level on the Stall Moor mires of south Dartmoor and travels to the sea, passing through Cornwood, Lee Mill and Yealmpton, a mid-sized village with a population of c.2,000 which is ...
, which was exposed by quarrying. The main show cave has two entrances apart, both of which lead to the same extensive bedding plane chamber. Originally low, the passages were enlarged by archaeological excavation, and the two entrance passages were originally separated until connected by excavation between 1820 and 1835. The show cave is very short. The ''Lower Entrance'' to the north, which is only a little above river level, enters a short passage which after passes a flooded passage on the right the water level of which fluctuates with that of the River Yealm. This sumps after . The main route goes off to the left along a winding passage for some to where some steps on the left lead down into ''The Bedding Plane Chamber''. Straight on the passage enlarges, with a large passage to the right leading to a boulder choke. This was passed to reach a chamber some high, but the route has since collapsed. To the left, the main path also enters ''The Bedding Plane Chamber'', a low chamber with an area of over . At the far end some steps enter a passage leading to the ''Upper Entrance''. The caves are bat roosts and the Greater Horseshoe, Lesser Horseshoe, and Natterer's bats have all been recorded.


Geology

Kitley Show Cave is a solutional formed in
Devonian The Devonian ( ) is a geologic period and system of the Paleozoic era, spanning 60.3 million years from the end of the Silurian, million years ago (Mya), to the beginning of the Carboniferous, Mya. It is named after Devon, England, whe ...
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 ...
, laid down some 350-400 Ma ago. The cave is
phreatic ''Phreatic'' is a term used in hydrology to refer to aquifers, in speleology to refer to cave passages, and in volcanology to refer to a type of volcanic eruption. Hydrology The term phreatic (the word originates from the Greek , meaning "well" ...
, formed by a river below the
water table The water table is the upper surface of the zone of saturation. The zone of saturation is where the pores and fractures of the ground are saturated with water. It can also be simply explained as the depth below which the ground is saturated. T ...
, but was left dry when sea levels fell which allowed the deposition of
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 ...
s. Animal remains found in the cave date to the last interglacial, about 120,000 years ago, and were found in fluvial deposits covered by speleothems, so the caves must have been active then. The path dug through in 1834 has since been covered by several centimetres of stalagmitic deposit.


History

The Kitley Cave Guide indicates that the main cave was entered about 1800 when quarry blasting exposed the entrance, although a more contemporaneous account claims that it was first entered in 1834 in similar circumstances. When it was opened it was reported as being "beautifully decorated with stalactites and stalagmites", and that the owner ordered a path be dug through the stalagmitic floor, which exposed the bones of a large animal. By 1905 it had been gated. In 1971 it was opened up as a self-guided show cave, with informational boards, within a nature reserve area. Over the next thirty years the show cave was closed and reopened twice, before being finally closed in 2000. During this time exploration work was undertaken by the Plymouth Caving Group and others, who extended Yealmpton Passage to the west to open up a high sloping chamber.


Archaeology

Much of the archaeology of Kitley Show Cave was destroyed when the path was dug in 1835, although remains of mammoth, rhino, horse, bison, hyena and bear bones have been identified. They were found in fluvial deposits and date from the last interglacial. Finds in neignbouring fragments of the same cave system include human remains and artefacts from the Late
Magdalenian The Magdalenian cultures (also Madelenian; French: ''Magdalénien'') are later cultures of the Upper Paleolithic and Mesolithic in western Europe. They date from around 17,000 to 12,000 years ago. It is named after the type site of La Madele ...
period of the
Upper Paleolithic The Upper Paleolithic (or Upper Palaeolithic) is the third and last subdivision of the Paleolithic or Old Stone Age. Very broadly, it dates to between 50,000 and 12,000 years ago (the beginning of the Holocene), according to some theories coin ...
, as well as from the
Bronze Age The Bronze Age is a historic period, lasting approximately from 3300 BC to 1200 BC, characterized by the use of bronze, the presence of writing in some areas, and other early features of urban civilization. The Bronze Age is the second pri ...
, but it is thought that at the time Kitley Show Cave was too wet to be used for habitation by animals or humans.


References

{{reflist Wild caves Limestone caves Karst caves Closed show caves in the United Kingdom Caves of Devon