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The Craven Fault System is the name applied by geologists to the group of crustal faults in the Pennines that form the southern edge of the Askrigg Block and which partly bounds the Craven Basin. Sections of the system's component faults which include the North, Middle and South Craven faults and the Feizor Fault are evident at the surface in the form of degraded faults scarps where Carboniferous Limestone abuts millstone grit. The fault system is approximately coincident with the southwestern edge of the Yorkshire Dales National Park and the northeastern edge of the Bowland Fells.
The Marble Arch Caves Global Geopark straddles the border between Northern Ireland and the Republic of Ireland. It is centred on the Marble Arch Caves and in 2001 it became one of the first geoparks to be designated in Europe.
Ballytober Fault is a geological fault in County Antrim, Northern Ireland.
Carnlough Fault is a geological fault in County Antrim, Northern Ireland.
Sixmilewater Fault is a geological fault in County Antrim, Northern Ireland.
Camlough Fault is a geological fault in County Armagh, Northern Ireland.
Kinnegoe Fault is a geological fault in County Armagh, Northern Ireland.
Newry Fault is a geological fault in County Armagh, Northern Ireland.
Orlock Bridge Fault is a major geological fault which extends through County Armagh, Northern Ireland and across the North Channel into Galloway in southern Scotland.
Tow Valley Fault is a geological fault in County Antrim, Northern Ireland.
Clogher Valley Fault is a geological fault in County Fermanagh, Northern Ireland.
The Killadeas – Seskinore Fault is a geological fault in County Fermanagh, Northern Ireland.
Tempo – Sixmilecross Fault is a geological fault in County Fermanagh, Northern Ireland.
Belcoo Fault is a geological fault in County Fermanagh, Northern Ireland.
Elagh Fault is a geological fault in County Tyrone, Northern Ireland.
Laghy Fault is a geological fault in County Tyrone, Northern Ireland.
The Omagh Thrust Fault is a geological fault in County Tyrone. It is of one of the most important structural discontinuities in Northern Ireland and an extension of the Highland Boundary Fault which runs through Scotland.
The Aire Valley Fault is an inactive strike slip fault in Yorkshire, England. It is considered a northwestern continuation of the Morley-Campsall Fault Belt and extends northwards from the Huddersfield and Wakefield area into the South Craven fault. It is connected to the Denholme Clough Fault.
References
- Map sheet 44 (and accompanying memoir) of the series of 1:50,000 scale geological maps of Northern Ireland published by Geological Survey of Northern Ireland.
- Lyle, P. 2003 Classic geology in Europe 5 The north of Ireland Terra Publishing, Harpenden
Coordinates: 54°40′04″N7°41′27″W / 54.66772°N 7.69079°W
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