Montrose Basin

The Montrose Basin is part of the estuary of the South Esk forming a tidal basin near to the town of Montrose, Angus, on the east coast of Scotland.

The nature reserve in this embayment is internationally important for pink-footed geese, red knot and common redshank and is nationally important for common shelduck, wigeon and common eider ducks. It is also popular with mute swans, oystercatchers and northern lapwings as well as smaller birds. Breeding birds are preyed on by peregrine falcons and sparrowhawks. The visitor centre, run by the Scottish Wildlife Trust, is accessible from the A92 road.

The swans give the Basin its old, more poetic name, the "Sea of Swans".

The Montrose Basin Heritage Society was formed in 1999 to bring together information about the basin, including its history and archaeology.

The Basin has been exploited for its seafood. At one time Montrose was Scotland's second largest exporter of salmon; and mussel cultivation gave it the largest mussel beds in the country during the 19th and early 20th centuries. Eels have also been an important catch.

The Montrose Basin was hit by a tsunami in 6100 BC, generated by the massive underwater Storegga Slide, in Norway. It was 70 feet (21 m) high when it hit the basin, with the waters travelling inland as far as Forfar.

Designations
Official nameMontrose Basin
Designated3 February 1995
Reference no.716[1]
Montrose Basin
Montrose Basin

See also

References

  1. ^ "Montrose Basin". Ramsar Sites Information Service. Retrieved 25 April 2018.

External links

Coordinates: 56°42′29″N 2°30′11″W / 56.70818°N 2.50305°W

Angus, Scotland

Angus (Scottish Gaelic: Aonghas) is one of the 32 local government council areas of Scotland, a registration county and a lieutenancy area. The council area borders Aberdeenshire, Dundee City and Perth and Kinross. Main industries include agriculture and fishing. Global pharmaceuticals company GSK has a significant presence in Montrose in the north of the county.

Angus was historically a county, known officially as Forfarshire from the 18th century until 1928, bordering Kincardineshire to the north-east, Aberdeenshire to the north and Perthshire to the west; southwards it faced Fife across the Firth of Tay (essentially the same border as today minus Dundee). It remains a registration county and a lieutenancy area. In 1975 some of its administrative functions were transferred to the council district of the Tayside Region, and in 1995 further reform resulted in the establishment of the unitary Angus Council.

Brechin Castle

Brechin Castle is a castle in Brechin, Angus, Scotland. The castle is the seat of the Earl of Dalhousie, who is the clan chieftain of Clan Maule of Panmure in Angus, and Clan Ramsay of Dalhousie in Midlothian. The castle was constructed in stone during the 13th century. Most of the current building dates to the early 18th century, when extensive reconstruction was carried out by architect Alexander Edward for James Maule, 4th Earl of Panmure, between approximately 1696 and 1709. The castle is a Category A listed building and the grounds are included in the Inventory of Gardens and Designed Landscapes in Scotland.The grounds have been in the Maule-Ramsay family since the 12th century. The castle has been the seat of the Clan Maule since medieval times. The Maule and Ramsay clans were joined under a single chieftain in the 18th century. The seat of the Ramsay clan was moved from Dalhousie Castle to Brechin Castle in the early 20th century.

Marie Stewart, Countess of Mar entertained John Taylor the Water Poet at Brechin Castle and King James on his return to Scotland in 1617. She had inventories made of the contents and furnishings of Brechin Castle in 1611 and 1622.The estate consisted of approximately 150,000 acres (61,000 ha) at its height and is now 55,000 acres (22,000 ha). The formal gardens date to the early 18th century. Agriculture and forestry largely dominate the estate grounds, but tourists can stay at several guest lodges on the property.

A 1990s addition to the grounds is Brechin Castle Centre, a retail shopping complex.

Fauna of Scotland

The fauna of Scotland is generally typical of the northwest European part of the Palearctic ecozone, although several of the country's larger mammals were hunted to extinction in historic times and human activity has also led to various species of wildlife being introduced. Scotland's diverse temperate environments support 62 species of wild mammals, including a population of wild cats, important numbers of grey and harbour seals and the most northerly colony of bottlenose dolphins in the world.Many populations of moorland birds, including the black and red grouse live here, and the country has internationally significant nesting grounds for seabirds such as the northern gannet. The golden eagle has become a national icon, and white-tailed eagles and ospreys have recently re-colonised the land. The Scottish crossbill is the only endemic vertebrate species in the UK.Scotland's seas are among the most biologically productive in the world; it is estimated that the total number of Scottish marine species exceeds 40,000. The Darwin Mounds are an important area of deep sea cold water coral reefs discovered in 1998. Inland, nearly 400 genetically distinct populations of Atlantic salmon live in Scottish rivers. Of the 42 species of fish found in the country's fresh waters, half have arrived by natural colonisation and half by human introduction.

Only six amphibians and four land reptiles are native to Scotland, but many species of invertebrates live there that are otherwise rare in the United Kingdom (UK). An estimated 14,000 species of insect, including rare bees and butterflies protected by conservation action plans, inhabit Scotland. Conservation agencies in the UK are concerned that climate change, especially its potential effects on mountain plateaus and marine life, threaten much of the fauna of Scotland.

Firth

Firth is a word in the Scots and English languages used to denote various coastal waters in Scotland and even a strait. 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 east coast, or in the southwest of the country, although the Firth of Lorn 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 can be rather vague. The Firth of Clyde is sometimes thought to include the estuary as far upriver as Dumbarton, but the Ordnance Survey map shows the change from river to firth occurring off Port Glasgow, while locally the change is held to be at the Tail of the Bank where the river crosses a sandbar off Greenock at the junction to the Gare Loch, or even further west at Gourock point.

However, some firths are exceptions. The Cromarty Firth on the east coast of Scotland, for example, resembles a large loch with only a relatively small outlet to the sea and the Solway Firth and the Moray Firth are more like extremely large bays. The Pentland Firth is a strait rather than a bay or an inlet.

House of Dun

The House of Dun is a National Trust for Scotland property in the parish of Dun, west of Montrose in Angus, Scotland. The Dun Estate was home to the Erskine (later Kennedy-Erskine) family from 1375 until 1980. John Erskine of Dun was a key figure in the Scottish Reformation. The current house was designed by William Adam and was finished in 1743. (Work had commenced in 1732.) There is elaborate plaster-work by Joseph Enzer, principally and most elaborately in the saloon. The house replaced the original 14th Century Tower House to the west when David Erskine, the 13th Laird of Dun, an Edinburgh lawyer appointed Lord of Justiciary in 1710, wanted a more comfortable and prestigious home. It continued as the home to the Erskines for a further 250 years, undergoing some internal re-modeling when Lady Augusta Fitzclarence, natural daughter to William lV (previously the Duke of Clarence) and his long term mistress, Dora Jordan, married the Honourable John Kennedy Erskine, heir to the property through his mother Margaret Erskine of Dun. When they married they moved to the property and Augusta set about making a number of alterations, modernizing the property. The writer and poet Violet Jacob (1863 - 1946), author of "Flemington" and "Tales of Angus", was a member of the Kennedy-Erskine family and was born in the house. The last Laird of Dun was Mrs. Millicent Lovett. She moved out of the house to an estate house "temporarily" in 1948, moving all the furnishings and artifacts up into the attic. The rest of the house was leased to a local farming family who ran it as a bed and breakfast establishment for many years. Millicent never returned to the house and on her death in 1980 it was bequeathed by her to the National Trust for Scotland. The Trust discovered all the original furnishings in the attic and spent 9 years returning the house to the state it had been in at the time of Augusta. In 1989 the house opened to the public, the Queen Mother presiding to mark the tercentenary of William Adam's death.

The adjacent Montrose Basin nature reserve, part of the estuary of the South Esk, is also a National Trust for Scotland property.

Lagoon

A lagoon is a shallow body of water separated from a larger body of water by barrier islands or reefs. Lagoons are commonly divided into coastal lagoons and atoll lagoons. They have also been identified as occurring on mixed-sand and gravel coastlines. There is an overlap between bodies of water classified as coastal lagoons and bodies of water classified as estuaries. Lagoons are common coastal features around many parts of the world.

List of National Trust for Scotland properties

National Trust for Scotland properties is a link page listing the cultural, built and natural heritage properties and sites owned or managed by the National Trust for Scotland.

List of Ramsar sites in Scotland

This list includes all Ramsar sites in Scotland. Ramsar sites are internationally recognised wetland sites, protected under the terms of the Ramsar Convention on Wetlands, which was developed and adopted by participating nations at a meeting in Ramsar, Iran, on 2 February 1971. At the end of 2010, 160 states were contracting parties to the Convention, and the worldwide total of sites was 1,920. The United Kingdom was one of 18 original signatories to the Convention, and has since designated 168 Ramsar sites. 51 of these sites are within Scotland, including one site, the Upper Solway Flats and Marshes, which covers parts of both Scotland and England in the Solway Firth. The total area of all Ramsar sites in Scotland is approximately 313,500 hectares (775,000 acres). All of Scotland's Ramsar sites form part of the European Natura 2000 network as either Special Protection Areas or Special Areas of Conservation, and many sites are further protected as Sites of Special Scientific Interest under UK legislation.

List of Sites of Special Scientific Interest in Angus and Dundee

The following is a list of Sites of Special Scientific Interest in the Angus and Dundee Area of Search. For other areas, see List of SSSIs by Area of Search.

Auchterhouse Hill

Balloch Moss

Balshando Bog

Barry Links

Blacklaw Hill Mire

Caenlochan

Carrot Hill Meadow

Craigs of Lundie and Ardgarth Loch

Crossbog Pinewood

Den of Airlie

Den of Fowlis

Den of Ogil

Dilty Moss

Dryleys Brick Pit

Dun's Dish

Easthaven

Elliot Links

Fafernie

Forest Muir

Gagie Marsh

Gannochy Gorge

Garbh Choire

Glen Callater

Inner Tay Estuary

Lairds Loch

Little Ballo

Loch Brandy

Loch of Kinnordy

Loch of Lintrathen

Lochindores

Long Loch of Lundie

Monifieth Bay

Montrose Basin

North Esk and West Water Palaeochannels

Red Craig

Redmyre

Rescobie and Balgavies Lochs

Restenneth Moss

Rickle Craig - Scurdie Ness

Rossie Moor

Round Loch of Lundie

St Cyrus and Kinnaber Links

Turin Hill

Whitehouse Den

Whiting Ness - Ethie Haven Coast

List of local nature reserves in Scotland

This is a list of local nature reserves in Scotland.

Aberlady Bay

Arnhall Moss

Balquhidderock Wood

Birnie and Gaddon Lochs

Bishop Loch

Bonnyfield Nature Park

Broughty Ferry

Burdiehouse Burn Valley Park

Cardowan Moss

Castle and Hightae Lochs

Catrine Voes and Woodlands

Commonhead Moss

Corstorphine Hill

Coul Den

Coves Community Park

Cullaloe

Dalbeath Marsh

Dawsholm Park

Den of Maidencraig

Donmouth

Duchess Wood

Dumbreck Marsh

Durrockstock Park

Easter Craiglockhart Hill

Easter Inch Moss and Seafield Law

Eden Estuary

Findhorn Bay

Garscadden Wood

Gartcosh

Gartmorn Dam

Gillingshill Reservoir

Hermitage of Braid / Blackford Hill

Hogganfield Park

Inner Tay Estuary

Jenny's Well

Kincorth Hill

Langlands Moss

Loch Stiapabhat

Malls Mire

Meadows Yard

Merkinch

Merklands

Montrose Basin

Mull Head

Paisley Moss

Perchy Pond

Ravelston Woods

Robroyston Park

Scotstown Moor

Stevenston Beach

Straiton Pond

The Saltings

Torry Bay

Trottick Mill Ponds

Waters of Philorth

Wigtown Bay

List of places in Angus

Map of places in Angus compiled from this listThis List of places in Angus is a list of links for any town, village, hamlet, castle, golf course, historic house, nature reserve, reservoir, river, and other place of interest in the Angus council area of Scotland.

Loch of the Lowes

Loch of the Lowes is a loch near Dunkeld in Perth and Kinross, Scotland. The loch and the surrounding area are designated as a wildlife reserve, run by the Scottish Wildlife Trust. The loch is also a designated Site of Special Scientific Interest (SSSI), as well as forming part of a Special Area of Conservation.The loch hosts a variety of wildlife, including a pair of breeding ospreys, red squirrels, otters and beavers.Wildfowl numbers peak in early winter with migrant greylag geese roosting on the loch. In addition, goldeneyes, mallards, goosanders, wigeons, teals, tufted ducks and great crested grebes can also be seen.

Montrose, Angus

Montrose ( mon-TROHZ, Scottish Gaelic: Monadh Rois) is a town and former royal burgh in Angus, Scotland. It is situated 38 miles (61 kilometres) north of Dundee between the mouths of the North and South Esk rivers. It is the northernmost coastal town in Angus and developed at a natural harbour that traded in skins, hides and cured salmon in medieval times.

With a population of approximately 12,000, the town functions as a port, but the major employer is GlaxoSmithKline, which was saved from closure in 2006. The skyline of Montrose is dominated by the 220-foot (67 m) steeple of Old and St Andrew's Church, designed by James Gillespie Graham and built between 1832 and 1834.

Montrose is a town with a wealth of architecture, and is a centre for international trade. It is an important commercial port for the thriving oil and gas industry. It is known for its wide thoroughfare and high street which

leads to picturesque closes containing secluded gardens. The town has a view of a 2 mi (3 km) square tidal lagoon, Montrose Basin, which is considered a nature reserve of international importance. It is the largest inland salt water basin in the UK, and an important habitat for the mute swan. Just outside Montrose is the 18th-century House of Dun, designed by the Scottish architect William Adam and built in 1730 for David Erskine, 13th Laird of Dun.

Montrose railway station

Montrose railway station serves the town of Montrose in Angus, Scotland. The station overlooks the Montrose Basin and is situated on the Edinburgh to Aberdeen Line, 90 miles (144 km) north of Edinburgh Waverley.

North British, Arbroath and Montrose Railway

The North British, Arbroath and Montrose Railway was a company established by Act of Parliament in 1871 to construct and operate a railway line from north of Arbroath via Montrose to Kinnaber Junction, 38 miles (61 km) south of Aberdeen. The company was originally a subsidiary of the North British Railway but it was absorbed into its parent in 1880. Construction of the line was delayed and a viaduct had to be dismantled and rebuilt following the Tay Bridge disaster. Rivalry between the companies on the east and west coast routes from London to Aberdeen, the "Race to the North", culminated in 1895 – the crucial point was at Kinnaber Junction where the two routes converged into a single railway.

River South Esk

Note: the southern headwater of the River Esk in Lothian is also known as the South Esk.The South Esk (Scottish Gaelic: Easg Dheas) is a river in Angus, Scotland. It rises in the Grampian Mountains at Loch Esk in Glen Doll and flows through Glen Clova to Strathmore at Cortachy, 5 km north of Kirriemuir. Its course takes it past Brechin and enters the North Sea at Montrose.The river gives its name to the title of Earl of Southesk, held by the Carnegie family.

Scottish Wildlife Trust

The Scottish Wildlife Trust is a registered charity dedicated to conserving the wildlife and natural environment of Scotland.

Scurdie Ness

Scurdie Ness is a headland located on the South side of the River South Esk estuary, Montrose, Angus, Scotland. The River leads from the North Sea into Montrose Harbour and then into Montrose Basin. The headland has also been referred to as Scurdy Ness, Montrose point or Montroseness. The word Scurdie is a local word for the volcanic rock found there and Ness means a promontory, cape or headland. The coastline from Scurdie Ness to Rickle Craig has been designated a Site of Special Scientific Interest (SSSI code 1351).

Storegga Slide

The three Storegga Slides are considered to be amongst the largest known landslides. They occurred under water, at the edge of Norway's continental shelf in the Norwegian Sea, approximately 6225–6170 BCE. The collapse involved an estimated 290 km (180 mi) length of coastal shelf, with a total volume of 3,500 km3 (840 cu mi) of debris, which caused a very large tsunami in the North Atlantic Ocean.

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