Rod's Pot
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Rod's Pot is a
limestone Limestone is a type of carbonate rock, carbonate sedimentary rock which is the main source of the material Lime (material), lime. It is composed mostly of the minerals calcite and aragonite, which are different Polymorphism (materials science) ...
cave above
Burrington Combe Burrington Combe is a Carboniferous Limestone Canyon, gorge near the village of Burrington, Somerset, Burrington, on the north side of the Mendip Hills Area of Outstanding Natural Beauty, in North Somerset, England. "Combe" or "coombe" is a wo ...
in the
Mendip Hills The Mendip Hills (commonly called the Mendips) is a range of limestone hills to the south of Bristol and Bath, Somerset, Bath in Somerset, England. Running from Weston-super-Mare and the Bristol Channel in the west to the River Frome, Somerset ...
, in
Somerset Somerset ( , ), Archaism, archaically Somersetshire ( , , ) is a Ceremonial counties of England, ceremonial county in South West England. It is bordered by the Bristol Channel, Gloucestershire, and Bristol to the north, Wiltshire to the east ...
,
England England is a Countries of the United Kingdom, country that is part of the United Kingdom. It is located on the island of Great Britain, of which it covers about 62%, and List of islands of England, more than 100 smaller adjacent islands. It ...
. The cave was first excavated in 1944 by the
University of Bristol Spelæological Society The University of Bristol Spelæological Society (UBSS) was founded in 1919 by cavers in the University of Bristol. Among its earliest activities was the archaeological excavation of Aveline's Hole. The club owns a hut, which was formerly a ladi ...
. It is one of a line of swallets marking the junction of the Limestone shales with the Carboniferous Limestones where water running off the
Old Red Sandstone Old Red Sandstone, abbreviated ORS, is an assemblage of rocks in the North Atlantic region largely of Devonian age. It extends in the east across Great Britain, Ireland and Norway, and in the west along the eastern seaboard of North America. It ...
of Blackdown finds its way underground. Further excavation has now linked Rod's Pot to nearby Bath Swallet. The cave was originally known as Pearce's Pot after Rodney Pearce.


Main features

Rod's Pot is formed mainly of vertical rift passages, probably in the original joints in the limestone which have been enlarged by water action. The north wall of the main chamber is a continuation of the main chamber in Read's Cave, a quarter mile to the west. The entry chamber divides into two passages about high and long. They merge again at the top of a deep vertical pothole which is a dead end. From the top of the pothole a long passage leads to the roof of the main chamber. The main chamber is about long, high and slopes down some . It contains a
stalagmite A stalagmite (, ; ; ) 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 composed of calcium carbonate, but may consist ...
pillar formation and several
stalactite A stalactite (, ; , ) 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 soluble and that can be deposited as a colloid, or is in suspension (chemistry ...
curtains. A small hole leads to a smaller chamber about high in which is a stalactite curtain about long and which is
translucent In the field of optics, transparency (also called pellucidity or diaphaneity) is the physical property of allowing light to pass through the material without appreciable light scattering by particles, scattering of light. On a macroscopic scale ...
and coloured with stripes of reddish-brown deposits. A further passageway leads to the terminal pothole. At the base of the Bear Pit, a 3 metre deep chamber reached through a small hole halfway through the cave, a pool containing a small community of '' Niphargus fontanus'' been found.


See also

*
Caves of the Mendip Hills The caves of the Mendip Hills are formed by the particular geology of the Mendip Hills: large areas of limestone worn away by water makes it a national centre for caving. The hills conceal the largest underground river system in Britain. Geolog ...


References

{{Mendip Hills Caves of the Mendip Hills Limestone caves Wild caves