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Strontian
Strontian (; gd, Sròn an t-Sìthein) is the main village in Sunart, an area in western Lochaber, Highland, Scotland, on the A861 road. Prior to 1975 it was part of Argyllshire. It lies on the north shore of Loch Sunart, close to the head of the loch. In the hills to the north of Strontian lead was mined in the 18th century and in these mines the mineral strontianite was discovered, from which the element strontium was first isolated. The village name in Gaelic, '' Sròn an t-Sìthein'', translates as the ''nose'' .e. 'point'''of the fairy hill'', meaning a knoll or low round hill inhabited by the mythological '' sídhe''. The nearby hamlets of Anaheilt, Bellsgrove, and Upper and Lower Scotstown are now generally considered part of Strontian, with Polloch several miles away on the terminus of the road to Loch Shiel. Strontian is the location of Ardnamurchan High School, the local fire station, police station and other facilities. Geology and mining history It was obse ...
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Strontian 01
Strontian (; gd, Sròn an t-Sìthein) is the main village in Sunart, an area in western Lochaber, Highland, Scotland, on the A861 road. Prior to 1975 it was part of Argyllshire. It lies on the north shore of Loch Sunart, close to the head of the loch. In the hills to the north of Strontian lead was mined in the 18th century and in these mines the mineral strontianite was discovered, from which the element strontium was first isolated. The village name in Gaelic, ''Sròn an t-Sìthein'', translates as the ''nose'' .e. 'point'''of the fairy hill'', meaning a knoll or low round hill inhabited by the mythological '' sídhe''. The nearby hamlets of Anaheilt, Bellsgrove, and Upper and Lower Scotstown are now generally considered part of Strontian, with Polloch several miles away on the terminus of the road to Loch Shiel. Strontian is the location of Ardnamurchan High School, the local fire station, police station and other facilities. Geology and mining history It was obser ...
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Strontianite
Strontianite ( Sr C O3) is an important raw material for the extraction of strontium. It is a rare carbonate mineral and one of only a few strontium minerals. It is a member of the aragonite group. Aragonite group members: aragonite (CaCO3), witherite (BaCO3), strontianite (SrCO3), cerussite (PbCO3) The ideal formula of strontianite is SrCO3, with molar mass 147.63 g, but calcium (Ca) can substitute for up to 27% of the strontium (Sr) cations, and barium (Ba) up to 3.3%. The mineral was named in 1791 for the locality, Strontian, Argyllshire, Scotland, where the element strontium had been discovered the previous year. Although good mineral specimens of strontianite are rare, strontium is a fairly common element, with abundance in the Earth's crust of 370 parts per million by weight, 87 parts per million by moles, much more common than copper with only 60 parts per million by weight, 19 by moles. Strontium is never found free in nature. The principal strontium ores are ce ...
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Strontium
Strontium is the chemical element with the symbol Sr and atomic number 38. An alkaline earth metal, strontium is a soft silver-white yellowish metallic element that is highly chemically reactive. The metal forms a dark oxide layer when it is exposed to air. Strontium has physical and chemical properties similar to those of its two vertical neighbors in the periodic table, calcium and barium. It occurs naturally mainly in the minerals celestine and strontianite, and is mostly mined from these. Both strontium and strontianite are named after Strontian, a village in Scotland near which the mineral was discovered in 1790 by Adair Crawford and William Cruickshank; it was identified as a new element the next year from its crimson-red flame test color. Strontium was first isolated as a metal in 1808 by Humphry Davy using the then newly discovered process of electrolysis. During the 19th century, strontium was mostly used in the production of sugar from sugar beets (see strontian ...
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Strontium
Strontium is the chemical element with the symbol Sr and atomic number 38. An alkaline earth metal, strontium is a soft silver-white yellowish metallic element that is highly chemically reactive. The metal forms a dark oxide layer when it is exposed to air. Strontium has physical and chemical properties similar to those of its two vertical neighbors in the periodic table, calcium and barium. It occurs naturally mainly in the minerals celestine and strontianite, and is mostly mined from these. Both strontium and strontianite are named after Strontian, a village in Scotland near which the mineral was discovered in 1790 by Adair Crawford and William Cruickshank; it was identified as a new element the next year from its crimson-red flame test color. Strontium was first isolated as a metal in 1808 by Humphry Davy using the then newly discovered process of electrolysis. During the 19th century, strontium was mostly used in the production of sugar from sugar beets (see strontian ...
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Thomas Charles Hope
Thomas Charles Hope (21 July 1766 – 13 June 1844) was a British physician, chemist and lecturer. He proved the existence of the element strontium, and gave his name to Hope's Experiment, which shows that water reaches its maximum density at . In 1815 Hope was elected as president of the Royal College of Physicians of Edinburgh (1815–19), and as vice-president of Royal Society of Edinburgh (1823–33) during the presidencies of Walter Scott and Thomas Makdougall Brisbane. He founded a chemistry prize at the University of Edinburgh. Charles Darwin was one of Hope's students, and Darwin viewed his chemistry lectures as highlights in his otherwise largely dull education at the University. Early life Born in Edinburgh, the third son of Juliana Stevenson and surgeon and botanist John Hope, he lived at High School Yards on the south side of the old town. He was educated next door to his house at the High School, the University of Edinburgh (MD 1787) and the University of ...
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Sunart
Sunart ( , Scottish Gaelic: ''Suaineart'') is a rural district and community in the south west of Lochaber in Highland, Scotland, on the shores of Loch Sunart, and part of the civil parish of Ardnamurchan. The main village is Strontian, at the head of the loch, which is the location of Ardnamurchan High School, the local fire station, police station and other facilities. The district is bounded to the south by the eastern half of Loch Sunart and by part of Morvern, to the west by the Ardnamurchan peninsula (beyond Salen), to the north by Loch Shiel, and to the east and north east by the district of Ardgour, from which it is divided by a range of high hills. Main access to the area today is via Glen Tarbert, from the Corran Ferry, although there is also a road coming in from Lochailort, via Moidart, to the north. Although the area may seem isolated now, in the past the main mode of transport in the West Highlands was boat, and the district was well-integrated into the west co ...
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A861 Road
The A861 road is a circuitous, primarily coastal, road in Lochaber, within the Highland council area of Scotland. The A861 serves the communities of the remote Ardgour, Sunart, Moidart and Ardnamurchan areas Although the ends of this road are only apart (the direct link being by way of the A830 road) its total length is . The last stretch to be built was the part from Kinlochmoidart to Lochailort. It was opened on 29 July 1966 by the Minister of State for Scotland, George Willis M.P. Mr Willis described it as the longest completely new road to be built in Scotland since the days of Thomas Telford, 150 years earlier. Route (clockwise) The A861 is a long-way-round route in the Lochaber area of western Scotland, connecting the A830 Fort William to Mallaig road with itself via the shores of Loch Sunart. *junction with the A830 road west of Kinlocheil *under the West Highland Line *through Drimsallie *eastwards along the south shore of Loch Eil, through Garvan, Duisky a ...
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Highland (council Area)
Highland ( gd, A' Ghàidhealtachd, ; sco, Hieland) is a council area in the Scottish Highlands and is the largest local government area in the United Kingdom. It was the 7th most populous council area in Scotland at the 2011 census. It shares borders with the council areas of Aberdeenshire, Argyll and Bute, Moray and Perth and Kinross. Their councils, and those of Angus and Stirling, also have areas of the Scottish Highlands within their administrative boundaries. The Highland area covers most of the mainland and inner-Hebridean parts of the historic counties of Inverness-shire and Ross and Cromarty, all of Caithness, Nairnshire and Sutherland and small parts of Argyll and Moray. Despite its name, the area does not cover the entire Scottish Highlands. Name Unlike the other council areas of Scotland, the name ''Highland'' is often not used as a proper noun. The council's website only sometimes refers to the area as being ''Highland'', and other times as being '' ...
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Loch Sunart
Loch Sunart (Scottish Gaelic ) is a sea loch on the west coast of Scotland. Loch Sunart is bounded to the north by the Sunart district of Ardnamurchan and to the south by the Morvern district. At long, it is the longest sea loch in the Highland local government area. The maximum depth of the loch is 124 metres, east of Càrna and near the entrance to Loch Teacuis. Other islands in the loch include Oronsay, seaward of Càrna, Risga, which lies between the two larger islands, and Eilean Mòr, which lies towards the landward end of the loch in line with Beinn Resipol. A considerable part of the loch is leased for aquaculture, with fish farming, originally only of salmon but now somewhat diversified, being established in the 1980s. A local legend holds that the absence of resident swans in Loch Sunart is the result of a doomed love affair between a Celtic chieftain and a local girl. When his mother, who opposed a marriage, turned her into a swan to thwart their love, th ...
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Sròn
Sròn is the Scottish Gaelic word for nose and is the name of some hills in the Scottish Highlands. Before the abolition of the acute accent in Scottish Gaelic, it was sometimes spelt as ''srón''. The name "sròn" is often applied to pointed hills or promontories that form the edge of a mountain massive, giving the appearance of a nose-like ridge. As such, they are often not the highest hilltops; in fact only one of the 282 Munros is called Sròn: Sròn a' Choire Ghairbh ("the nose of the rough corrie"), located west of Loch Lochy. Sròn also appears in names of towns (often anglicized as ''Stron''), such as Strontian (''Sròn an t-Sìtheinn''), the ''nose of the fairies'' ('' Sìth''), and Stranraer Stranraer ( , in Scotland also ; gd, An t-Sròn Reamhar ), also known as The Toon, is a town in Dumfries and Galloway, Scotland. It is located in the historical parish of Inch in the historic county of Wigtownshire. It lies on the shores of ..., (''An t-Sròn Reamhar'' ...
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Argyllshire
Argyll (; archaically Argyle, in modern Gaelic, ), sometimes called Argyllshire, is a historic county and registration county of western Scotland. Argyll is of ancient origin, and corresponds to most of the part of the ancient kingdom of on Great Britain. Argyll was also a medieval bishopric with its cathedral at Lismore, as well as an early modern earldom and dukedom, the Dukedom of Argyll. It borders Inverness-shire to the north, Perthshire and Dunbartonshire to the east, and—separated by the Firth of Clyde—neighbours Renfrewshire and Ayrshire to the south-east, and Buteshire to the south. Between 1890 and 1975, Argyll was an administrative county with a county council. Its area corresponds with most of the modern council area of Argyll and Bute, excluding the Isle of Bute and the Helensburgh area, but including the Morvern and Ardnamurchan areas of the Highland council area. There was an Argyllshire constituency of the Parliament of Great Britain then Parlia ...
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Moine Supergroup
The Moine Supergroup is a sequence of Neoproterozoic metamorphic rocks that form the dominant outcrop of the Scottish Highlands between the Moine Thrust Belt to the northwest and the Great Glen Fault to the southeast. The sequence is metasedimentary in nature and was metamorphosed and deformed in a series of tectonic events during the Late Proterozoic and Early Paleozoic. It takes its name from ''A' Mhòine'', a peat bog in northern Sutherland. Distribution The main outcrop of the Moine series lies northwest of the Great Glen Fault, structurally above the Moine Thrust to the west forming what is known as the Northern Highlands Terrane. A smaller area of similar rocks that are correlated with these, outcrop within the 'Grampian Terrane' to the southeast of the Great Glen. Moinian rocks are also recognised on Mull, Orkney and Shetland. Stratigraphy The Moine Supergroup has been subdivided into different groups or divisions. The relationship between individual groups in terms of ...
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