Boho Caves
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The Boho Caves (pronounced , ) are a collection of caves centred on the village of
Boho, County Fermanagh Boho (pronounced , ) is a hamlet and a civil parish covering approximately southwest of Enniskillen in County Fermanagh, Northern Ireland. It is situated within Fermanagh and Omagh district. This area contains a high density of historically ...
, Northern Ireland, on the northern slopes of
Belmore Mountain Belmore Mountain () is a hill in the townland of Gortgall, western County Fermanagh, Northern Ireland. With a summit roughly above sea level, it is the second highest point in Fermanagh, the highest being at Cuilcagh on the Northern Ireland& ...
. They encompass the main Boho Cave and the smaller Waterfall Cave and Upper and Lower Ravine Caves. The Boho Cave system is the sixth-longest cave system in Northern Ireland, is designated an
Area of Special Scientific Interest A Site of Special Scientific Interest (SSSI) in Great Britain, or an Area of Special Scientific Interest (ASSI) in the Isle of Man and Northern Ireland, is a conservation designation denoting a protected area in the United Kingdom and Isle ...
(ASSI #144) and is the only example of joint-controlled caves in Northern Ireland.


Geology and hydrology

The rock strata at Boho Caves date from the Asbian substage of the
Carboniferous The Carboniferous ( ) is a Geologic time scale, geologic period and System (stratigraphy), system of the Paleozoic era (geology), era that spans 60 million years, from the end of the Devonian Period Ma (million years ago) to the beginning of the ...
period, estimated to be around 325 million years old. The rock sequence exposed at Boho consists of the
Glencar Limestone Formation The Glencar Limestone is a geologic formation in Ireland. It preserves fossils dating back to the Carboniferous period. See also * List of fossiliferous stratigraphic units in Ireland See also * Lists of fossiliferous stratigraphic units ...
which is overlain by the Dartry Limestone Formation, composed of
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 prec ...
y limestones and limestones and
shale Shale is a fine-grained, clastic sedimentary rock formed from mud that is a mix of flakes of Clay mineral, clay minerals (hydrous aluminium phyllosilicates, e.g., Kaolinite, kaolin, aluminium, Al2Silicon, Si2Oxygen, O5(hydroxide, OH)4) and tiny f ...
s of the Carn Limestone Member. The Dartry Limestone is, in turn, overlain by the Meenymore Formation and the Glenade
Sandstone Sandstone is a Clastic rock#Sedimentary clastic rocks, clastic sedimentary rock composed mainly of grain size, sand-sized (0.0625 to 2 mm) silicate mineral, silicate grains, Cementation (geology), cemented together by another mineral. Sand ...
. The caves are formed within the Dartry Limestone. The main cave contains typical
karst Karst () is a topography formed from the dissolution of soluble carbonate rocks such as limestone and Dolomite (rock), dolomite. It is characterized by features like poljes above and drainage systems with sinkholes and caves underground. Ther ...
features such as
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 ...
s,
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 ...
s, cave curtains and
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 ...
. The water flowing through the Boho Caves originates from Aghanaglack River. After dry weather, the river sinks in the streambed well upstream of the caves and does not emerge until far downstream past the ravine. In wetter conditions, water flows into the cave system via several routes including the Main Sink entrance, which can sump and overflow into the nearby field shakeholes. It then exits the cave at the usual downstream resurgences, as well as the Upper and Lower Ravine caves (via bedding planes from the northern end of Boho Cave) and in particularly high floods, the Quarry entrance (see picture).


History of exploration

The caves at Boho have been known locally for hundreds of years, and are mentioned on
Ordnance Survey Ireland Ordnance Survey Ireland (OSI; ) was the national mapping agency of the Republic of Ireland. It was established on 4 March 2002 as a body corporate. It was the successor to the former Ordnance Survey of Ireland. It and the Ordnance Survey of ...
's 6-inch survey of Ireland, conducted between 1829 and 1841. By 1870 it was quite the norm for tourists to arrange a guided tour with a local resident, as William Wakeman described in his guide book of that year. Although
Édouard-Alfred Martel Édouard-Alfred Martel (1 July 1859, Pontoise, Val-d'Oise – 3 June 1938, Montbrison (Loire), Montbrison), the 'father of modern speleology', was a world pioneer of cave exploration, study, and documentation. Martel explored thousands of caves ...
and
Lyster Jameson Henry Paul William Lyster Jameson (1875 – 26 February 1922) was an Irish zoologist who studied pearl-formation. He also made contributions to speleology and encouraged the study of psychology in adult education. Life H. Lyster Jameson was bor ...
definitely visited Boho parish in 1895 and investigated some of the caves, Martel's description makes it unclear as to whether he visited Boho Caves or nearby Pollnagollum Coolarkan. It is however clear that Jameson visited both caves himself, before Martel's arrival in the area and with the assistance of Rev. A. Knight, and reported on the fauna he discovered in the caves. Boho quarry, in which there are a number of entrances to the cave, was active until the mid-1950s and many local people would have explored short sections of the cave during and before this time. The Yorkshire Ramblers explored Boho Caves in 1907 but it was not until the mid-1960s that a survey of this complicated system was attempted by Dublin cavers. The system was extensively resurveyed by the Reyfad Group in the 1980s.


Access

Boho is a cave much used by guided educational parties studying the local environment and by casual visitors, but exploration should never be undertaken lightly. In wet weather the narrow passages flood quickly and at these times the cave is extremely dangerous and should be avoided. Heavy flood pulses have been known to inundate the cave up to 24 hours after heavy rain has ceased, and the entire system is known to flood to the roof in under an hour. It is also recommended that the Upper Ravine area downstream of Boho quarry should not be visited under any circumstances because of roosting bats.


Fauna

The main biospeleological interest in the Boho area is the population of approximately 50 Daubenton's or Water Bats () which roost in the Upper Ravine Cave. These were recorded as early as 1895 by Lyster Jameson (as ) and specimens were sent to the then Science and Art Museum in Dublin. On this visit, Jameson and his guide, Rev. A. Knight, also identified two large spiders, and , and three additional invertebrates that were likely washed in by floods: the water bug and two flies belonging to the
genera Genus (; : genera ) is a taxonomic rank above species and below family as used in the biological classification of living and fossil organisms as well as viruses. In binomial nomenclature, the genus name forms the first part of the binomial s ...
and . Lass of the
University of Nottingham The University of Nottingham is a public research university in Nottingham, England. It was founded as University College Nottingham in 1881, and was granted a royal charter in 1948. Nottingham's main campus (University Park Campus, Nottingh ...
(in Hazelton, 1974) made extensive faunal collections in Boho Caves which included the identification of the
troglobitic A troglobite (or, formally, troglobiont) is an animal species, or population of a species, strictly bound to underground habitats, such as caves. These are separate from species that mainly live in above-ground habitats but are also able to live u ...
Springtail Springtails (class Collembola) form the largest of the three lineages of modern Hexapoda, hexapods that are no longer considered insects. Although the three lineages are sometimes grouped together in a class called Entognatha because they have in ...
(). Phil Chapman cites the collection of a
stickleback The sticklebacks are a family of ray-finned fishes, the Gasterosteidae which have a Holarctic distribution in fresh, brackish and marine waters. They were thought to be related to the pipefish and seahorses but are now thought to be more close ...
() from Boho and the Field Shake Holes and Southern Series have been observed to support a large spider population (). The strong draughts may bring
trogloxene Trogloxenes or subtroglophiles, also called cave guests, are animal species which periodically live in underground habitats such as caves or at the very entrance, but cannot live exclusively in such habitats. Among many scientists, trogloxenes and ...
s into the cave on which this population thrives. The record of the water beetle, , was of some interest at the time of the caves' declaration as an ASSI in 1985, as there had been no other modern Irish records of this cave-dwelling species up to this point.


See also

*
Caves of the Tullybrack and Belmore hills The Caves of the Tullybrack and Belmore hills are a collection of caves in southwest County Fermanagh, Northern Ireland. The region is also described as the West Fermanagh Scarplands by environmental agencies and shares many similar karst feature ...
*
List of caves in the United Kingdom This is an incomplete list of caves in the United Kingdom, including information on the largest and deepest caves in the UK. Longest, deepest and largest The longest cave system in the UK is the Three Counties System in the Yorkshire Dales, with ...
*
List of caves This is a list of caves of the world that have articles or that are properly cited. They are sorted by continent and then country. Caves which are in overseas territories on a different continent than the home country are sorted by the territory' ...


References


Further reading

* {{County Fermanagh Bat roosts Landforms of County Fermanagh Caves of Northern Ireland Limestone caves