Firth
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Firth
Firth is a word in the English and Scots languages used to denote various coastal waters in the United Kingdom, predominantly within Scotland. In the Northern Isles, it more usually refers to a smaller inlet. It is linguistically cognate to ''fjord'' (both from Proto-Germanic *''ferþuz''), which has a more constrained sense in English. Bodies of water named "firths" tend to be more common on the Scottish east coast, or in the southwest of the country, although the Firth of Clyde is an exception to this. The Highland coast contains numerous estuaries, straits, and inlets of a similar kind, but not called "firth" (e.g. the Minch and Loch Torridon); instead, these are often called sea lochs. Before about 1850, the spelling "Frith" was more common. A firth is generally the result of ice age glaciation and is very often associated with a large river, where erosion caused by the tidal effects of incoming sea water passing upriver has widened the riverbed into an estuary. Demarcation c ...
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Firth Of Clyde
The Firth of Clyde is the mouth of the River Clyde. It is located on the west coast of Scotland and constitutes the deepest coastal waters in the British Isles (it is 164 metres deep at its deepest). The firth is sheltered from the Atlantic Ocean by the Kintyre peninsula, which encloses the outer firth in Argyll and Ayrshire. The Kilbrannan Sound is a large arm of the Firth of Clyde, separating the Kintyre Peninsula from the Isle of Arran. Within the Firth of Clyde is another major island – the Isle of Bute. Given its strategic location at the entrance to the middle and upper Clyde, Bute played a vital naval military role during World War II. Geography At its entrance, the firth is about wide. At one area in its upper reaches, it is joined by Loch Long and the Gare Loch. This area includes the large anchorage off of Greenock that is known as the Tail of the Bank. (The “Bank” is a reference to the sandbank and shoal that separates the firth from the estuary of the Ri ...
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Pentland Firth
The Pentland Firth ( gd, An Caol Arcach, meaning the Orcadian Strait) is a strait which separates the Orkney Islands from Caithness in the north of Scotland. Despite the name, it is not a firth. Etymology The name is presumed to be a corruption of the Old Norse "Petlandsfjörð", meaning "the fjord of Pictland", and is completely unrelated to the Pentland Hills near Edinburgh. Prior to the Norse occupation of Orkney the strait was known as the "Sea of Orcs" – a reference to the Picts, Pictish tribe who inhabited Orkney. Such was their marine prowess that there are also instances of this name referring to the sea lanes of the entire west coast of Scotland down to Kintyre. One version of the 9th-century ''Historia Brittonum'' states that "the Britons originally filled the whole island with their peoples from the English Channel to the Sea of Orcs". Geography On the Caithness (southern) side the Firth extends from Dunnet Head in the west to Duncansby Head point, Duncansby Head i ...
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Solway Firth
The Solway Firth ( gd, Tràchd Romhra) is a firth that forms part of the border between England and Scotland, between Cumbria (including the Solway Plain) and Dumfries and Galloway. It stretches from St Bees Head, just south of Whitehaven in Cumbria, to the Mull of Galloway, on the western end of Dumfries and Galloway. The Isle of Man is also very near to the firth. The firth comprises part of the Irish Sea. The firth’s coastline is characterised by lowland hills and small mountains. It is a mainly rural area, with mostly small villages and settlements (such as Powfoot). Fishing, hill farming, and some arable farming play a large part in the local economy, although tourism is increasing. The northern part of the English coast of the Solway Firth was designated as an Area of Outstanding Natural Beauty, known as the Solway Coast, in 1964. Construction of the Robin Rigg Wind Farm in the firth began in 2007. Within the firth, there are some salt flats and mud flats that can b ...
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Moray Firth
The Moray Firth (; Scottish Gaelic: ''An Cuan Moireach'', ''Linne Mhoireibh'' or ''Caolas Mhoireibh'') is a roughly triangular inlet (or firth) of the North Sea, north and east of Inverness, which is in the Highland council area of north of Scotland. It is the largest firth in Scotland, stretching from Duncansby Head (near John o' Groats) in the north, in the Highland council area, and Fraserburgh in the east, in the Aberdeenshire council area, to Inverness and the Beauly Firth in the west. Therefore, three council areas have Moray Firth coastline: Highland to the west and north of the Moray Firth and Highland, Moray and Aberdeenshire to the south. The firth has more than 800 kilometres (about 500 miles) of coastline, much of which is cliff. Etymology The firth is named after the 10th-century Province of Moray, whose name in turn is believed to derive from the sea of the firth itself. The local names ''Murar'' or ''Morar'' are suggested to derive from , the Gaelic for sea, whi ...
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Cromarty Firth
The Cromarty Firth (; gd, Caolas Chrombaidh ; literally "kyles /nowiki>straits.html"_;"title="strait.html"_;"title="/nowiki>strait">/nowiki>straits">strait.html"_;"title="/nowiki>strait">/nowiki>straitsof_Cromarty.html" ;"title="strait">/nowiki>straits.html" ;"title="strait.html" ;"title="/nowiki>strait">/nowiki>straits">strait.html" ;"title="/nowiki>strait">/nowiki>straitsof Cromarty">strait">/nowiki>straits.html" ;"title="strait.html" ;"title="/nowiki>strait">/nowiki>straits">strait.html" ;"title="/nowiki>strait">/nowiki>straitsof Cromarty") is an arm of the Moray Firth in Scotland. Geography The entrance to the Cromarty Firth is guarded by two precipitous headlands; the one on the north high and the one on the south high — called " The Sutors" from a fancied resemblance to a couple of shoemakers (in Scots, ''souters'') bent over their lasts. From the Sutors the Firth extends inland in a westerly and then south-westerly direction for a distance of . Excepting be ...
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Fjord
In physical geography, a fjord or fiord () is a long, narrow inlet with steep sides or cliffs, created by a glacier. Fjords exist on the coasts of Alaska, Antarctica, British Columbia, Chile, Denmark, Germany, Greenland, the Faroe Islands, Iceland, Ireland, Kamchatka, the Kerguelen Islands, Labrador, Newfoundland, New Zealand, Norway, Novaya Zemlya, Nunavut, Quebec, the Patagonia region of Argentina and Chile, Russia, South Georgia Island, Tasmania, United Kingdom, and Washington state. Norway's coastline is estimated to be long with its nearly 1,200 fjords, but only long excluding the fjords. Formation A true fjord is formed when a glacier cuts a U-shaped valley by ice segregation and abrasion of the surrounding bedrock. According to the standard model, glaciers formed in pre-glacial valleys with a gently sloping valley floor. The work of the glacier then left an overdeepened U-shaped valley that ends abruptly at a valley or trough end. Such valleys are fjords wh ...
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Tail Of The Bank
The Tail of the Bank is the name given to the anchorage in the upper Firth of Clyde immediately North of Greenock, between Inverclyde and Argyll and Bute. This area of the Firth gets its name from the deep water immediately to the west of the sandbank which marks the entrance to the navigable channel up the Estuary of the River Clyde. Location From the Glasgow Green Tidal Weir westwards, the River Clyde is tidal, mixing fresh and salt water. At Milton Island the river was still shallow, then past Dumbarton and the confluence with the River Leven a shoal and sandbank increasingly takes up most of the width of the estuary and extends along the north shore for about to Ardmore. Areas of sandbank dry out at low tide, including the Pillar Bank off Dumbarton and Cardross. By Port Glasgow the main flow of the river is close to the south shore, with the Cockle Bank to its north, then the Greenock Bank which extends past the waterfront harbours to a point off Ocean Terminal where ...
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Strait
A strait is an oceanic landform connecting two seas or two other large areas of water. The surface water generally flows at the same elevation on both sides and through the strait in either direction. Most commonly, it is a narrow ocean channel that lies between two land masses. Some straits are not navigable, for example because they are either too narrow or too shallow, or because of an unnavigable reef or archipelago. Straits are also known to be loci for sediment accumulation. Usually, sand-size deposits occur on both the two opposite strait exits, forming subaqueous fans or deltas. Terminology The terms ''channel'', ''pass'', or ''passage'' can be synonymous and used interchangeably with ''strait'', although each is sometimes differentiated with varying senses. In Scotland, ''firth'' or ''Kyle'' are also sometimes used as synonyms for strait. Many straits are economically important. Straits can be important shipping routes and wars have been fought for control of them. ...
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Gourock
Gourock ( ; gd, Guireag ) is a town in the Inverclyde council area and formerly a burgh of the County of Renfrew in the west of Scotland. It was a seaside resort on the East shore of the upper Firth of Clyde. Its main function today is as a residential area, extending contiguously from Greenock, with a railway terminus and ferry services across the Clyde. History The name Gourock comes from a Gaelic word for "pimple", in reference to the hill above the town. As far back as 1494 it is recorded that James IV sailed from the shore at Gourock to quell the rebellious Highland clans. Two hundred years later William and Mary granted a Charter in favour of Stewart of Castlemilk which raised Gourock to a Burgh of Barony. In 1784 the lands of Gourock were purchased by Duncan Darroch, a former merchant in Jamaica. He built Gourock House near the site of the castle in what the family eventually gifted to the town as Darroch Park, later renamed by the council as Gourock Park. From a sma ...
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The Minch
The Minch ( gd, An Cuan Sgitheanach, ', ', '), also called North Minch, is a strait in north-west Scotland, separating the north-west Scottish Highlands, Highlands and the northern Inner Hebrides from Lewis and Harris in the Outer Hebrides. It was known as ("Scotland's fjord/firth") in Old Norse. The Lower Minch (), also known as the Little Minch, is the Minch's southern extension, separating Skye from the lower Outer Hebrides: North Uist, Benbecula, South Uist, Barra etc. It opens into the Sea of the Hebrides. The Little Minch is the northern limit of the Sea of the Hebrides. Geography The Minch and Lower Minch form part of the Inner Seas off the West Coast of Scotland, as defined by the International Hydrographic Organization. The Minch ranges from wide and is approximately long. It is believed to be the site of the Ullapool bolide impact, biggest meteorite ever to hit the British Isles. The Lower Minch is about wide. In June 2010 Eilidh Macdonald became the first person ...
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Loch
''Loch'' () is the Scottish Gaelic, Scots language, Scots and Irish language, Irish word for a lake or sea inlet. It is Cognate, cognate with the Manx language, Manx lough, Cornish language, Cornish logh, and one of the Welsh language, Welsh words for lake, llwch. In English English and Hiberno-English, the Anglicisation, anglicised spelling lough is commonly found in place names; in Lowland Scots and Scottish English, the spelling "loch" is always used. Many loughs are connected to stories of lake-bursts, signifying their mythical origin. Sea-inlet lochs are often called sea lochs or sea loughs. Some such bodies of water could also be called firths, fjords, estuary, estuaries, straits or bays. Background This name for a body of water is Insular Celtic languages, Insular CelticThe current form has currency in the following languages: Scottish Gaelic, Irish language, Irish, Manx language, Manx, and has been borrowed into Scots language, Lowland Scots, Scottish English, Iri ...
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Port Glasgow
Port Glasgow ( gd, Port Ghlaschu, ) is the second-largest town in the Inverclyde council area of Scotland. The population according to the 1991 census for Port Glasgow was 19,426 persons and in the 2001 census was 16,617 persons. The most recent census in 2011 states that the population has declined to 15,414. It is located immediately to the east of Greenock and was previously a burgh in the county of Renfrewshire. Originally a fishing hamlet named Newark, Port Glasgow came about as a result of large ships being unable to navigate the shallow and meandering River Clyde to the centre of the city of Glasgow. As a result, it was formed as a remote port for Glasgow in 1668, and became known as 'New Port Glasgow', which was shortened to 'Port Glasgow' in 1775. Port Glasgow was home to dry docks and shipbuilding beginning in 1780. The town grew from the central area of the present town and thus many of the town's historic buildings and people are found here. Port Glasgow expanded up ...
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