The largest
caves in the Cheddar catchment occur along the southern side of Blackdown,
around Charterhouse. These caves, GB Cave, Charterhouse Cave, Longwood
Swallet, Manor Farm Swallet and the recently extended Upper Flood
Swallet are classic examples of swallet caves. Relative to their
size, this group of caves, especially GB Cave, are some of the
most intensively studied in the world. All five major caves are similar
with streamways, often well decorated with stalagmites, descending
down to a sump or a choke, with up to four tiers of relict high-level
phreatic passages.
The caves drain to Cheddar Risings. Above these large springs at
the mouth of Cheddar Gorge there is a complex series of abandoned
caves. The largest is Gough’s Cave, 2.1 km long, which intercepts
the underground River Yeo, which has been followed upstream through
several deep sumps.

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Discovered in 1898, this show cave is also one
of Europe’s most important Upper Palaeolithic archaeological
sites and the home of ‘Cheddar Man’, one of several skeletons
found in the cave. Mitochondrial DNA from this skeleton was found
to match that of a school teacher living nearby today. Several other
smaller caves, Great Oones Hole, Long Hole and Gough’s Old
Cave occur higher in the cliffs. Further up the gorge is Reservoir
Hole, a relict cave system which once drained to Cheddar.
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