Omagh Thrust
The Omagh Thrust Fault is a
geological fault in County Tyrone. It is of one of the most important structural discontinuities in Northern Ireland[1] and an extension of the Highland Boundary Fault which runs through Scotland.[2]
The fault occurred in the
strata were moved over younger Ordovician
ones with the fault as their boundary.
There is access to a view of the fault at Mountfield Quarry, County Tyrone. This has been designated an
Area of Special Scientific Interest.[1]
See also
- List of geological faults in Northern Ireland
- Geology of Northern Ireland
References
General 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
Footnotes
54°36′08″N 8°51′06″W / 54.60224°N 8.85178°W
| Volcanism |  | |
|---|---|---|
| Volcanic plugs | ||
| Dykes and sills |
| |
| Metamorphic | ||
| Sedimentary | ||
| Lists | ||
 | This article related to the geography of County Tyrone, Northern Ireland is a stub. You can help Wikipedia by expanding it. |
 | This article about a specific United Kingdom geological feature is a stub. You can help Wikipedia by expanding it. |