Shannon Cave
| Shannon Cave | |
|---|---|
The Vegetable Patch Formations
|
|
| Location |
Cuilcagh mountains, Ulster |
| Coordinates | 54°14′26″N 7°50′53″W / 54.24056°N 7.84806°WCoordinates: 54°14′26″N 7°50′53″W / 54.24056°N 7.84806°W |
| Depth | 130 m (430 ft) |
| Length | 5.4 km (3.4 mi) |
| Discovery | 1980 |
| Geology | Limestone |
| Entrances | 1 |
| List of entrances |
Polltullyard Pollahune (collapsed) |
| Difficulty | High |
| Hazards | Vertical pitch; rock falls; boulder |
| Access | With experienced guide only |
| Associated caves | Polltullyard, Pigeon Pot, Shannon Pot |
Shannon Cave is an active stream passage cave in southern Ulster.
At 130-metre (430 ft) vertical depth, it stands joint sixth with Poulnagree in Munster in the deepest caves of Ireland. The cave is recorded at 5.4 kilometres (3.4 mi) in length (making it the sixth-longest on the island Ireland), but exploration is ongoing and further passage is expected to be found.
The cave consists in the main of a large mainstream passage running to a terminal sump. The water flowing in the cave has been dye traced to Shannon Pot, two kilometres to the west of the terminal sump, which is the traditional source of the River Shannon. Inlets to the main passage are numerous. Some, such as the large "Mistake Passage" have been pushed only a short distance. Since the cave is undergoing active exploration, there remain many issues to be sorted out and the sinks for many of these inlets remains unclear. The stream passage itself is of considerable proportions in parts, but also contains many higher level fossil passages which have been deserted by the stream. The cave contains numerous calcite formations, with large amounts of helictites in places. Boulder chokes are frequent with several parts of the cave being quite unstable, especially the JCP passage.
While the location of the entrance to the cave is in County Fermanagh, the majority of the cave lies under County Cavan. The original entrance to the cave was in Cavan; however, this is now inaccessible. The current entrance of Polltullyard is located north of the Marlbank area of Fermanagh, high in the moors.
The cave was discovered in August 1980 by members of the Reyfad Group, the cavers' collective responsible for exploring the Reyfad system. The entrance was made in a shakehole adjacent to the sink point of the Hune (pronounced "honey") stream, and close the border in County Cavan. The initial route was dug through a highly unstable area of glacial fill, making it extremely treacherous. Once in the cave the cavers encountered a "main" streamway into which the Hune flowed, with the upstream section leading to "JCP Passage" and the downstream section passing another significant inlet, "Mistake Passage". By the end of August, the team had progressed past several boulder and explored cave passages some 1.6 kilometres (1 mi) in length.
...
Wikipedia