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Sperrins
The Sperrins or Sperrin Mountains () are a mountain range in Northern Ireland. The range stretches from Strabane and Mullaghcarn in the west, to Slieve Gallion and the Glenshane Pass in the east, in the counties of Tyrone and Londonderry. The landscape is mostly moorland and blanket bog. The region has a population of some 150,000 and is a designated Area of Outstanding Natural Beauty. Features It has a distinctive glaciated landscape. The mountains mostly have rounded summits and the landscape is mainly moorland and blanket bog. The Glenshane Pass, part of the A6 Belfast to Derry road, is in the mountains and has notoriously bad weather in winter. Sawel Mountain is the highest peak in the Sperrins, and the seventh highest in Northern Ireland. Its summit rises to . Another of the Sperrins, Carntogher (464 m), towers over the Glenshane Pass. Geologically, the Sperrins are formed mostly from Precambrian metamorphic rocks, with some younger Ordovician igneous rocks in t ...
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Sawel Mountain
Sawel Mountain () is the highest peak in the Sperrin Mountains, and the 8th highest in Northern Ireland. It is also the highest mountain in Northern Ireland outside of the Mourne Mountain range located in County Down. Geography To the north of Sawel is County Londonderry and to the south, County Tyrone. The summit is high and is composed of crystalline limestone. Around the peak, there is "montane heathland", with plant life including heather, bilberries and cowberries, although this is being damaged by hillwalking and grazing. Sawel is the source of the River Faughan, a long tributary of the River Foyle. Naming The Irish name of the mountain is a reference to a glen or hollow on the side of Sawel. It was also historically called Slieve Sawel, from the Irish word ''sliabh'' ("mountain"). Plane crash On 5 January 1944 a Royal Navy Stinson Reliant (FK914) of 878 Naval Air Squadron was on a flight from RNAS Eglinton (HMS Gannet) to RNAS Machrihanish (HMS Landrail) when it cr ...
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Mullaghcarn
Mullaghcarn () is a mountain in the southwest Sperrins, County Tyrone, Northern Ireland. The peak reaches a height of 542 m (1778 ft), and is the 370th highest in Ireland. Mullaghcarn is in the Fermanagh and Omagh District Council area, on the edge of Gortin Glen Forest Park, and is the most southerly peak in the Sperrins. It is northeast of Omagh, and is south of Gortin. Nature Mullaghcarn is steep, and has a rocky summit. The west of the mountain is home to conifers. "Acid" grassland is the most common on Mullaghcarn, and peat is not especially common, due to the draining of the eastern mountain. Heather is most common on the northern slopes. The red grouse can be found on heathland around Mullaghcarn. History Mullaghcarn was home to firing ranges during World War II. These were used by the police and US Army soldiers stationed in the area. Gallery File:Mullaghcarn Summit - geograph.org.uk - 556865.jpg, The summit of Mullaghcarn from above File:Mullaghcarn Summ ...
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Slieve Gallion
Slieve Gallion () is a mountain in County Londonderry, Northern Ireland. It is the easternmost of the Sperrin Mountains. It reaches a height of and dominates the western shore of Lough Neagh. Its prominent northeastern summit has a transmitter station with a small road leading to it, and stands at a height of . By road, Slieve Gallion is from Moneymore, from Cookstown, and from Magherafelt. The mountain is part of the parishes of Desertmartin, Lissan and Ballinascreen. Landscape Slieve Gallion is a volcanic plug. The mountain is formed from volcanic-derived igneous rock, and also granite on the southern slopes. It is steep, and has a flat top. There is a telecommunications mast on the northeastern summit. To the west, the landscape consists of blanket bog and coniferous forest; most of the trees in the Slieve Gallion area are Sitka spruce. There are also lodgepole pine trees, as well as oak towards the south of the area. Animal species living in the area ...
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Area Of Outstanding Natural Beauty
An Area of Outstanding Natural Beauty (AONB; , AHNE) is one of 46 areas of countryside in England, Wales, or Northern Ireland that has been designated for conservation due to its significant landscape value. Since 2023, the areas in England and Wales have also adopted the name National Landscape (). Areas are designated in recognition of their national importance by the relevant public body: Natural England, Natural Resources Wales, and the Northern Ireland Environment Agency respectively. On 22 November 2023, following a review, the AONBs in England and Wales adopted the National Landscapes name, and are in the process of rebranding. AONBs in Northern Ireland did not rename. The name "area of outstanding natural beauty" is still the designated legal term. In place of the term AONB, Scotland uses the similar national scenic area (NSA) designation. Areas of Outstanding Natural Beauty enjoy levels of protection from development similar to those of UK national parks, but unli ...
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Strabane
Strabane (; ) is a town in County Tyrone, Northern Ireland. Strabane had a population of 13,507 at the 2021 United Kingdom census, 2021 census. This article contains quotations from this source, which is available under th Open Government Licence v3.0 © Crown copyright. It lies on the east bank of the River Foyle. It is roughly midway from Omagh, Derry and Letterkenny. The River Foyle marks Irish border, the border between Northern Ireland and the Republic of Ireland. On the other side of the river (across Lifford Bridge) is the smaller town of Lifford, which is the county town of County Donegal, Donegal. The River Mourne flows through the centre of the town and meets the River Finn (County Donegal), Finn to form the Foyle River. A large hill named Knockavoe, which marks the beginning of the Sperrins, Sperrin Mountains, forms the backdrop to the town. History Early history The locale was home to a group of northern Celts known as the Orighella as far back as the fourth cen ...
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Glenshane Pass
The Glenshane Pass () is a major mountain pass cutting through the Sperrin Mountains in County Londonderry, Northern Ireland. It is in the townland of Glenshane Pass on the main Derry to Belfast route, the A6. A large wildfire broke out in Glenshane Pass in late June 2018, burning more than 600 acres of dry gorse in the pass by 27 June. Features It is a Special Area of Conservation. Carn/Glenshane Pass is a large area of intact blanket bog, characterised by undulating topography and including a large, well-developed hummock and pool system within a thick mantle of blanket peat. It is also classed as an Area of Special Scientific Interest. The Ponderosa is the second highest public house on the island of Ireland, situated above sea level. History The Glenshane Pass derives its name from the townland of Glenshane. It is named after Shane Crossagh O'Mullan a notorious rapparee, or highwayman, who roamed the highways of County Londonderry and County Tyrone in the late seventee ...
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Mullaghmore, County Londonderry
Mullaghmore () is a mountain in County Londonderry, Northern Ireland. It is part of the Sperrins and the 359th highest point on the island of Ireland Ireland (, ; ; Ulster Scots dialect, Ulster-Scots: ) is an island in the North Atlantic Ocean, in Northwestern Europe. Geopolitically, the island is divided between the Republic of Ireland (officially Names of the Irish state, named Irelan ... The summit is dominated by a large telecommunication tower. The peak is located 5 miles north of the village of Draperstown, and 6 miles south of Dungiven. It is also locally known as, "The Birren" hence the road name passing over it is "Birren Road" References Mountains and hills of County Londonderry Marilyns of Northern Ireland {{Londonderry-geo-stub ...
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County Tyrone
County Tyrone (; ) is one of the six counties of Northern Ireland, one of the nine counties of Ulster and one of the thirty-two traditional counties of Ireland. Its county town is Omagh. Adjoined to the south-west shore of Lough Neagh, the county covers an area of , making it the largest of Northern Ireland's six counties by size, and the second largest county in Ulster after Donegal. With a population of 188,383 as of the 2021 census, Tyrone is the 5th most populous county in both Northern Ireland and Ulster, and the 11th most populous county on the island of Ireland. The county derives its name and general geographic location from Tír Eoghain, a Gaelic kingdom under the O'Neill dynasty which existed until the 17th century. Name The name ''Tyrone'' is derived from the Irish , meaning 'land of Eoghan', the name given to the conquests made by the from the provinces of and Ulaid. Historically, it was anglicised as ''Tirowen'' or ''Tyrowen'', which are closer to the Irish ...
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Topographic Prominence
In topography, prominence or relative height (also referred to as autonomous height, and shoulder drop in US English, and drop in British English) measures the height of a mountain or hill's summit relative to the lowest contour line encircling it but containing no higher summit within it. It is a measure of the independence of a summit. The key col ("saddle") around the peak is a unique point on this contour line and the ''parent peak'' (if any) is some higher mountain, selected according to various criteria. Definitions The prominence of a peak is the least drop in height necessary in order to get from the summit to any higher terrain. This can be calculated for a given peak in the following manner: for every path connecting the peak to higher terrain, find the lowest point on the path; the ''key col'' (or ''highest saddle (landform), saddle'', or ''linking col'', or ''link'') is defined as the highest of these points, along all connecting paths; the prominence is the differ ...
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Ordovician
The Ordovician ( ) is a geologic period and System (geology), system, the second of six periods of the Paleozoic Era (geology), Era, and the second of twelve periods of the Phanerozoic Eon (geology), Eon. The Ordovician spans 41.6 million years from the end of the Cambrian Period Megaannum, Ma (million years ago) to the start of the Silurian Period Ma. The Ordovician, named after the Celtic Britons, Welsh tribe of the Ordovices, was defined by Charles Lapworth in 1879 to resolve a dispute between followers of Adam Sedgwick and Roderick Murchison, who were placing the same Rock (geology), rock beds in North Wales in the Cambrian and Silurian systems, respectively. Lapworth recognized that the fossil fauna in the disputed Stratum, strata were different from those of either the Cambrian or the Silurian systems, and placed them in a system of their own. The Ordovician received international approval in 1960 (forty years after Lapworth's death), when it was adopted as an official per ...
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Metamorphic Rock
Metamorphic rocks arise from the transformation of existing rock to new types of rock in a process called metamorphism. The original rock ( protolith) is subjected to temperatures greater than and, often, elevated pressure of or more, causing profound physical or chemical changes. During this process, the rock remains mostly in the solid state, but gradually recrystallizes to a new texture or mineral composition. The protolith may be an igneous, sedimentary, or existing metamorphic rock. Metamorphic rocks make up a large part of the Earth's crust and form 12% of the Earth's land surface. They are classified by their protolith, their chemical and mineral makeup, and their texture. They may be formed simply by being deeply buried beneath the Earth's surface, where they are subject to high temperatures and the great pressure of the rock layers above. They can also form from tectonic processes such as continental collisions, which cause horizontal pressure, friction, and dist ...
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Blanket Bog
Blanket bog or blanket mire, also known as featherbed bog, is an area of peatland, forming where there is a climate of high rainfall and a low level of evapotranspiration, allowing peat to develop not only in wet hollows but over large expanses of undulating ground. The blanketing of the ground with a variable depth of peat gives the habitat type its name. Blanket bogs are found extensively throughout the northern hemisphere - well-studied examples are found in Ireland and Scotland, but vast areas of North American tundra also qualify as blanket bogs. In Europe, the southernmost edge of range of this habitat has been recently mapped in the Cantabrian Mountains, northern Spain, but the current distribution of blanket bogs globally remains unknown. In the southern hemisphere they are less well-developed due to the relatively low latitudes of the main land areas, though similar environments are reported in Patagonia, the Falkland Islands and New Zealand. The blanket bogs known as ...
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