Firths Of Scotland
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Firths Of Scotland
Firth is a word in the English language, English and Scots language, Scots languages used to denote various coastal waters in the United Kingdom, predominantly within Scotland. In the Northern Isles, it more often refers to a smaller inlet. It is linguistically cognate to Scandinavian ''fjord'' and ''fjard'' (all from Proto-Germanic *''ferþuz''), with the original meaning of "sailable waterway". The word 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 Scottish Highlands, 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 loch, sea lochs. Before about 1850, the spelling "Frith" was more common. A firth is generally the result of Quaternary glaciation, ice age glacier, glaciation and is very oft ...
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English Language
English is a West Germanic language that developed in early medieval England and has since become a English as a lingua franca, global lingua franca. The namesake of the language is the Angles (tribe), Angles, one of the Germanic peoples that Anglo-Saxon settlement of Britain, migrated to Britain after its End of Roman rule in Britain, Roman occupiers left. English is the list of languages by total number of speakers, most spoken language in the world, primarily due to the global influences of the former British Empire (succeeded by the Commonwealth of Nations) and the United States. English is the list of languages by number of native speakers, third-most spoken native language, after Mandarin Chinese and Spanish language, Spanish; it is also the most widely learned second language in the world, with more second-language speakers than native speakers. English is either the official language or one of the official languages in list of countries and territories where English ...
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Estuary
An estuary is a partially enclosed coastal body of brackish water with one or more rivers or streams flowing into it, and with a free connection to the open sea. Estuaries form a transition zone between river environments and maritime environments and are an example of an ecotone. Estuaries are subject both to marine influences such as tides, waves, and the influx of saline water, and to fluvial influences such as flows of freshwater and sediment. The mixing of seawater and freshwater provides high levels of nutrients both in the water column and in sediment, making estuaries among the most productive natural habitats in the world. Most existing estuaries formed during the Holocene epoch with the flooding of river-eroded or glacially scoured valleys when the sea level began to rise about 10,000–12,000 years ago. Estuaries are typically classified according to their geomorphological features or to water-circulation patterns. They can have many different names, such as ba ...
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Strait
A strait is a water body connecting two seas or water basins. The surface water is, for the most part, at the same elevation on both sides and flows through the strait in both directions, even though the topography generally constricts the flow somewhat. In some straits there is a dominant directional current. Most commonly, the strait is a narrowing channel that lies between two land masses. Straits are loci for sediment accumulation, with sand-size deposits usually occurring on the two strait exits, forming subaqueous fans or deltas. Some straits are not navigable because, for example, they are too narrow or too shallow, or because of an unnavigable reef or archipelago. 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 impor ...
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Pentland Firth
The Pentland Firth (, 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 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 in the east, while on the Orkney (norther ...
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Moray Firth
The Moray Firth (; , or ) is a roughly triangular inlet (or firth) of the North Sea, north and east of Inverness, which is in the Highland council area of the 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 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, whilst ''Murav'' and ''Morav'' are believed to be rooted in Celtic words (sea) and (side), co ...
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Solway Firth
The Solway Firth is an inlet on the west coast of Great Britain, forming part of the border between England and Scotland. The firth (a Scottish term for an inlet of the sea) divides Cumbria (including the Solway Plain) from 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 marsh, salt marshes and mud flats that can be dangerous, due to their frequently shifting patches of quicksa ...
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Cromarty Firth
The Cromarty Firth (; ; literally "kyles [straits] of 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 shoemaking, shoemakers (in Scots language, 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 between Nigg Bay and Cromarty Bay where it is about wide, and Alness Bay where it is wide, it has an average width of . The southern shore of the Firth is formed by a peninsula known as the Black Isle. Good views of the Cromarty Firth are to be had from the Sutors or Cnoc Fyrish. At its head the Firth receives its principal river, the River Conon, other rivers include the Allt Graad, Peffery, River Sgitheach, Sgitheach, Averon and Balnagown. The Dingwall C ...
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Gourock
Gourock ( ; ) is a town in the Inverclyde council areas of Scotland, council area and formerly a burgh of the County of Renfrew in the west of Scotland. It was a resort town, 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 of Scotland, James IV sailed from the shore at Gourock to quell the rebellious Highland clans. Two hundred years later William III of England, 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 ...
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Gare Loch
The Gare Loch or Gareloch () is an open sea loch in Argyll and Bute in the west of Scotland, and it bears a similar name to the village of Gairloch in the north west Highlands. The loch is well used for sailing, recreational boating, list of water sports, water sports and sea fishing, fishing. Harbor seal, Harbour and grey seals are often seen in the Gare Loch along with pods of porpoise. Bottle Nose whales were photographed in September 2020. The loch also has been used since the early 20th century for naval training and as a base for the United Kingdom's submarine based nuclear weapons system. Geography A sea loch aligned north–south, Gare Loch is long with an average width of . At its southern end it opens into the Firth of Clyde through the Rhu narrows. The village of Rosneath lies on the western shore just north of Rosneath Point and gives the name Rosneath Peninsula to the whole body of land separating the Gare Loch from Loch Long to the west. The town of Helensburg ...
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Greenock
Greenock (; ; , ) is a town in Inverclyde, Scotland, located in the west central Lowlands of Scotland. The town is the administrative centre of Inverclyde Council. It is a former burgh within the historic county of Renfrewshire, and forms part of a contiguous urban area with Gourock to the west and Port Glasgow to the east. The 2011 UK Census showed that Greenock had a population of 44,248, a decrease from the 46,861 recorded in the 2001 UK Census. It lies on the south bank of the Clyde at the " Tail of the Bank" where the River Clyde deepens into the Firth of Clyde. History Name Place-name scholar William J. Watson wrote that "Greenock is well known in Gaelic as , dative of , 'a sunny knoll. The Scottish Gaelic place-name is relatively common, with another Greenock near Callander in Menteith (formerly in Perthshire) and yet another at Muirkirk in Kyle, now in East Ayrshire. R. M. Smith in (1921) described the alternative derivation from Common Brittonic *, ...
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Sandbar
In oceanography, geomorphology, and geoscience, a shoal is a natural submerged ridge, bank, or bar that consists of, or is covered by, sand or other unconsolidated material, and rises from the bed of a body of water close to the surface or above it, which poses a danger to navigation. Shoals are also known as sandbanks, sandbars, or gravelbars. Two or more shoals that are either separated by shared troughs or interconnected by past or present sedimentary and hydrographic processes are referred to as a shoal complex.Neuendorf, K.K.E., J.P. Mehl Jr., and J.A. Jackson, eds. (2005) ''Glossary of Geology'' (5th ed.). Alexandria, Virginia, American Geological Institute. 779 pp. The term ''shoal'' is also used in a number of ways that can be either similar to, or quite different from, how it is used in geologic, geomorphic, and oceanographic literature. Sometimes, the term refers to either any relatively shallow place in a stream, lake, sea, or other body of water; a rocky area ...
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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 Greenock Ocean ...
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