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List Of Geological Faults Of Northern Ireland
This is a list of the named geological faults affecting the rocks of Northern Ireland. Terminology See the main article on faults for a fuller treatment of fault types and nomenclature but in brief, the main types are normal faults, reverse faults, thrusts or thrust faults and strike-slip faults. Key to table *Column 1 indicates the name of the fault. Note that different authors may deploy different names for one and the same feature, or a part of a feature. Conversely the same name may be applied to two different features, particularly in the case of smaller faults with a wide geographic separation. *Column 2 indicates the county in which the fault occurs. Some traverse two or more counties of course. *Column 3 indicates the Irish grid reference for the approximate midpoint of the fault (as mapped). Note that the mapped extent of a fault may not correspond to its actual extent. *Column 4 indicates on which sheet of the Geological Survey of Northern Ireland's 1:50,000 scale geol ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Northern Ireland
Northern Ireland ( ga, Tuaisceart Éireann ; sco, label= Ulster-Scots, Norlin Airlann) is a part of the United Kingdom, situated in the north-east of the island of Ireland, that is variously described as a country, province or region. Northern Ireland shares an open border to the south and west with the Republic of Ireland. In 2021, its population was 1,903,100, making up about 27% of Ireland's population and about 3% of the UK's population. The Northern Ireland Assembly (colloquially referred to as Stormont after its location), established by the Northern Ireland Act 1998, holds responsibility for a range of devolved policy matters, while other areas are reserved for the UK Government. Northern Ireland cooperates with the Republic of Ireland in several areas. Northern Ireland was created in May 1921, when Ireland was partitioned by the Government of Ireland Act 1920, creating a devolved government for the six northeastern counties. As was intended, Northern Ireland ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Killadeas - Seskinore Fault
Killadeas () is a small village in County Fermanagh, Northern Ireland. It is about 7 miles north of Enniskillen near the shores of Lower Lough Erne, and is within Fermanagh and Omagh district. In the 2001 Census it had a population of 90 people. The Royal National Lifeboat Institution (RNLI) operates a lifeboat station on Lower Lough Erne at Killadeas. It works in conjunction with another lifeboat station on Upper Lough Erne at Carrybridge. History In the cemetery of the Church of Ireland Parish "Priory" Church of Killadeas are several stones, the most noted of which is known as the Bishops Stone. The figure carved stone and cross-slab are Scheduled Historic Monuments and are in Rockfield townland at grid ref: H206540. There is a large slab to the west, possibly being some bullaun stones. Near to this is a hole stone and a pillar. Near Killadeas, on Lower Lough Erne, is Gublusk Bay, a Royal Air Force base for Short Sunderland and PBY Catalina flying boats during World War ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Geological Faults Of England
This is a list of the named geological faults affecting the rocks of England. See the main article on faults for a fuller treatment of fault types and nomenclature but in brief, the main types are normal faults, reverse faults, thrusts or thrust faults and strike-slip faults. Many faults may have acted as both normal faults at one time and as reverse or thrust faults at another and may or may not have also incorporated some degree of strike-slip movement too. There are also a few 'disturbances'. These linear features are a combination of faults and folds - the relative importance of faulting and folding varying along the length of each disturbance. Key to tables *Column 1 indicates the name of the fault. Note that different authors may use different names for the same fault or a section of it. Conversely the same name may be applied to more than one fault, particularly in the case of smaller faults which are geographically distant from each another. Some composite names e.g. ' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
County Londonderry
County Londonderry ( Ulster-Scots: ''Coontie Lunnonderrie''), also known as County Derry ( ga, Contae Dhoire), is one of the six counties of Northern Ireland, one of the thirty two counties of Ireland and one of the nine counties of Ulster. Before the partition of Ireland, it was one of the counties of the Kingdom of Ireland from 1613 onward and then of the United Kingdom after the Acts of Union 1800. Adjoining the north-west shore of Lough Neagh, the county covers an area of and today has a population of about 247,132. Since 1972, the counties in Northern Ireland, including Londonderry, have no longer been used by the state as part of the local administration. Following further reforms in 2015, the area is now governed under three different districts; Derry and Strabane, Causeway Coast and Glens and Mid-Ulster. Despite no longer being used for local government and administrative purposes, it is sometimes used in a cultural context in All-Ireland sporting and cultural even ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tow Valley Fault
Tow Valley Fault is a geological fault in County Antrim, Northern Ireland. See also *List of geological faults in Northern Ireland This is a list of the named geological faults affecting the rocks of Northern Ireland. Terminology See the main article on faults for a fuller treatment of fault types and nomenclature but in brief, the main types are normal faults, reverse faul ... 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 Geography of County Antrim Seismic faults of Northern Ireland {{UK-geology-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tempo - Sixmilecross Fault
In musical terminology, tempo (Italian, 'time'; plural ''tempos'', or ''tempi'' from the Italian plural) is the speed or pace of a given piece. In classical music, tempo is typically indicated with an instruction at the start of a piece (often using conventional Italian terms) and is usually measured in beats per minute (or bpm). In modern classical compositions, a "metronome mark" in beats per minute may supplement or replace the normal tempo marking, while in modern genres like electronic dance music, tempo will typically simply be stated in BPM. Tempo may be separated from articulation and meter, or these aspects may be indicated along with tempo, all contributing to the overall texture. While the ability to hold a steady tempo is a vital skill for a musical performer, tempo is changeable. Depending on the genre of a piece of music and the performers' interpretation, a piece may be played with slight tempo rubato or drastic variances. In ensembles, the tempo is often ind ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sixmilewater Fault
Sixmilewater Fault is a geological fault in County Antrim, Northern Ireland. See also *List of geological faults in Northern Ireland This is a list of the named geological faults affecting the rocks of Northern Ireland. Terminology See the main article on faults for a fuller treatment of fault types and nomenclature but in brief, the main types are normal faults, reverse faul ... 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 Geography of County Antrim Seismic faults of Northern Ireland {{UK-geology-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pettigoe Fault
Pettigoe Fault is a geological fault in County Tyrone, Northern Ireland. See also *List of geological faults in Northern Ireland This is a list of the named geological faults affecting the rocks of Northern Ireland. Terminology See the main article on faults for a fuller treatment of fault types and nomenclature but in brief, the main types are normal faults, reverse faul ... 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 Geography of County Tyrone Seismic faults of Northern Ireland {{UK-geology-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Orlock Bridge Fault
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.Sheets 1 & 3 with pts of 7 and 4W (Scotland series) ''The Rhins of Galloway'' 1:50,000 scale geological map. British Geological Survey. See also * List of geological faults in Northern Ireland This is a list of the named geological faults affecting the rocks of Northern Ireland. Terminology See the main article on faults for a fuller treatment of fault types and nomenclature but in brief, the main types are normal faults, reverse faul ... 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 Geography of County Armagh Seismic faults of Northern Ireland Geology of Scotland {{UK-geology-s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 and an extension of the Highland Boundary Fault which runs through Scotland. The fault occurred in the Caledonian orogeny, during a late stage of this period of mountain building. Older sequences of Dalriadan metamorphic 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. See also *List of geological faults in Northern Ireland *Geology of Northern Ireland The geology of Ireland consists of the study of the rock formations on the island of Ireland. It includes rocks from every age from Proterozoic to Holocene and a large variety of different rock types is represented. The basalt columns of the Gian ... References General references * Map sheet 44 (and accompany ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Omagh Fault
Omagh Fault is a geological fault in County Tyrone, Northern Ireland. See also *List of geological faults in Northern Ireland This is a list of the named geological faults affecting the rocks of Northern Ireland. Terminology See the main article on faults for a fuller treatment of fault types and nomenclature but in brief, the main types are normal faults, reverse faul ... 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 Geography of County Tyrone Seismic faults of Northern Ireland {{UK-geology-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
County Down
County Down () is one of the six counties of Northern Ireland, one of the nine counties of Ulster and one of the traditional thirty-two counties of Ireland. It covers an area of and has a population of 531,665. It borders County Antrim to the north, the Irish Sea to the east, County Armagh to the west, and County Louth across Carlingford Lough to the southwest. In the east of the county is Strangford Lough and the Ards Peninsula. The largest town is Bangor, on the northeast coast. Three other large towns and cities are on its border: Newry lies on the western border with County Armagh, while Lisburn and Belfast lie on the northern border with County Antrim. Down contains both the southernmost point of Northern Ireland (Cranfield Point) and the easternmost point of Ireland (Burr Point). It was one of two counties of Northern Ireland to have a Protestant majority at the 2001 census. The other Protestant majority County is County Antrim to the north. In March 2018, ''The Sunda ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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