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. [1]
In geology, a fault is a planar fracture or discontinuity in a volume of rock, across which there has been significant displacement as a result of rock-mass movement. Large faults within the Earth's crust result from the action of plate tectonic forces, with the largest forming the boundaries between the plates, such as subduction zones or transform faults. Energy release associated with rapid movement on active faults is the cause of most earthquakes.
County Armagh is one of the traditional counties of Ireland and one of six counties that form Northern Ireland. Adjoined to the southern shore of Lough Neagh, the county covers an area of 1,326 km² and has a population of about 174,792. County Armagh is known as the "Orchard County" because of its many apple orchards. The county is part of the historic province of Ulster.
Northern Ireland is a part of the United Kingdom in the north-east of the island of Ireland, variously described as a country, province or region. Northern Ireland shares a border to the south and west with the Republic of Ireland. In 2011, its population was 1,810,863, constituting about 30% of the island's total population and about 3% of the UK's population. Established by the Northern Ireland Act 1998 as part of the Good Friday Agreement, the Northern Ireland Assembly holds responsibility for a range of devolved policy matters, while other areas are reserved for the British government. Northern Ireland co-operates with the Republic of Ireland in some areas, and the Agreement granted the Republic the ability to "put forward views and proposals" with "determined efforts to resolve disagreements between the two governments".
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.
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.
Pettigoe Fault is a geological fault in County Tyrone, Northern Ireland.
Coordinates: 54°38′13″N5°40′39″W / 54.63686°N 5.67759°W
A geographic coordinate system is a coordinate system that enables every location on Earth to be specified by a set of numbers, letters or symbols. The coordinates are often chosen such that one of the numbers represents a vertical position and two or three of the numbers represent a horizontal position; alternatively, a geographic position may be expressed in a combined three-dimensional Cartesian vector. A common choice of coordinates is latitude, longitude and elevation. To specify a location on a plane requires a map projection.
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