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Lammermuir
The Lammermuirs are a range of hills in southern Scotland, forming a natural boundary between East Lothian and the Borders. The name "Lammermuir" comes from the Old English ''lambra mōr'', meaning "moorland of the lambs". Geology The Lammermuir Hills are formed from a succession of Silurian and Ordovician age marine sediments known as greywackes together with siltstones, shales and mudstones. They are assigned to the Gala Group. Unconformably overlying these highly faulted and folded strata are outcrops of the early Devonian age Great Conglomerate Formation which forms a part of the Reston Group of Old Red Sandstone rocks. These coarse red-purple conglomerates underlie a band of country in the east between Longformacus and Oldhamstocks and also occur in an isolated outcrop east of Soutra Hill and beneath the Dun Law Wind Farm on the western margin of the hills. The same strata extend down Lauderdale on the western margin of the hills. Numerous dykes of different l ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lammermuirs
The Lammermuirs are a range of hills in southern Scotland, forming a natural boundary between East Lothian and the Borders. The name "Lammermuir" comes from the Old English ''lambra mōr'', meaning "moorland of the lambs". Geology The Lammermuir Hills are formed from a succession of Silurian and Ordovician age marine sediments known as greywackes together with siltstones, shales and mudstones. They are assigned to the Gala Group. Unconformably overlying these highly faulted and folded strata are outcrops of the early Devonian age Great Conglomerate Formation which forms a part of the Reston Group of Old Red Sandstone rocks. These coarse red-purple conglomerates underlie a band of country in the east between Longformacus and Oldhamstocks and also occur in an isolated outcrop east of Soutra Hill and beneath the Dun Law Wind Farm on the western margin of the hills. The same strata extend down Lauderdale on the western margin of the hills. Numerous dykes of different ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lammermuir Hills2
The Lammermuirs are a range of hills in southern Scotland, forming a natural boundary between East Lothian and the Borders. The name "Lammermuir" comes from the Old English ''lambra mōr'', meaning "moorland of the lambs". Geology The Lammermuir Hills are formed from a succession of Silurian and Ordovician age marine sediments known as greywackes together with siltstones, shales and mudstones. They are assigned to the Gala Group. Unconformably overlying these highly faulted and folded strata are outcrops of the early Devonian age Great Conglomerate Formation which forms a part of the Reston Group of Old Red Sandstone rocks. These coarse red-purple conglomerates underlie a band of country in the east between Longformacus and Oldhamstocks and also occur in an isolated outcrop east of Soutra Hill and beneath the Dun Law Wind Farm on the western margin of the hills. The same strata extend down Lauderdale on the western margin of the hills. Numerous dykes of different ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Longformacus
Longformacus ( gd, Longphort Mhacais) is a small village in Berwickshire in the Scottish Borders area of Scotland. It is around north-west of Duns, in the Lammermuir Hills. The Dye Water runs through the village, flowing east towards its confluence with the Whiteadder Water nearby. In the vicinity are traces of an ancient fortification at Runklie or Wrinklaw and the Mutiny Stones cairn. The opera ''Lucia di Lammermoor'', written by Gaetano Donizetti and based on Sir Walter Scott's ''The Bride of Lammermoor'', was set in the Lammermuirs and an old form of the village's name, Lockermachus, is mentioned in Scott's novel. The Southern Upland Way, a Long Distance Route which crosses southern Scotland, passes through the village, and the Sir Walter Scott Way from Moffat to Cockburnspath passes through Longformacus. Etymology Longformacus derives its name from the Gaelic ''Longphort Mhacais'', meaning 'Macas's camp'. Derivation from ''Lann Fothir Maccus'', meaning 'church on the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Berwickshire
Berwickshire ( gd, Siorrachd Bhearaig) is a historic county, registration county and lieutenancy area in south-eastern Scotland, on the English border. Berwickshire County Council existed from 1890 until 1975, when the area became part of the Borders region, with most of the historic county becoming part of the lower-tier Berwickshire district. Berwickshire district was abolished in 1996, when all the districts in the Borders region merged to become the Scottish Borders council area. The county takes its name from Berwick-upon-Tweed, its original county town, which was part of Scotland at the time of the county's formation in the twelfth century, but became part of England in 1482 after several centuries of swapping back and forth between the two kingdoms. After the loss of Berwick, Duns and Greenlaw both served as county town at different periods. The low-lying part of Berwickshire between the Tweed and the Lammermuirs is known as "the Merse", from an old Scots wor ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
East Lothian
East Lothian (; sco, East Lowden; gd, Lodainn an Ear) is one of the 32 council areas of Scotland, as well as a historic county, registration county and lieutenancy area. The county was called Haddingtonshire until 1921. In 1975, the historic county was incorporated for local government purposes into Lothian Region as East Lothian District, with some slight alterations of its boundaries. The Local Government etc. (Scotland) Act 1994 later created East Lothian as one of 32 modern council areas. East Lothian lies south of the Firth of Forth in the eastern central Lowlands of Scotland. It borders Edinburgh to the west, Midlothian to the south-west and the Scottish Borders to the south. Its administrative centre and former county town is Haddington while the largest town is Musselburgh. Haddingtonshire has ancient origins and is named in a charter of 1139 as ''Hadintunschira'' and in another of 1141 as ''Hadintunshire''. Three of the county's towns were designated as roya ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Scottish Borders
The Scottish Borders ( sco, the Mairches, 'the Marches'; gd, Crìochan na h-Alba) is one of 32 council areas of Scotland. It borders the City of Edinburgh, Dumfries and Galloway, East Lothian, Midlothian, South Lanarkshire, West Lothian and, to the south-west, south and east, the English counties of Cumbria and Northumberland. The administrative centre of the area is Newtown St Boswells. The term Scottish Borders, or normally just "the Borders", is also used to designate the areas of southern Scotland and northern England that bound the Anglo-Scottish border. Geography The Scottish Borders are in the eastern part of the Southern Uplands. The region is hilly and largely rural, with the River Tweed flowing west to east through it. The highest hill in the region is Broad Law in the Manor Hills. In the east of the region, the area that borders the River Tweed is flat and is known as 'The Merse'. The Tweed and its tributaries drain the entire region with the river fl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
St Abb's Head
St Abb's Head is a rocky promontory by the village of St Abbs in Scottish Borders, Scotland, and a national nature reserve administered by the National Trust for Scotland. St Abb's Head Lighthouse was designed and built by the brothers David Stevenson and Thomas Stevenson and began service on 24 February 1862. Geology The layered sedimentary rocks of greywacke and siltstone which lie to the north and south of the Head were laid down at the bottom of the sea between 460 and 410 million years ago. The Head itself is made from hard volcanic rock which formed as lava flowed from volcanoes around 400 million years ago. The different type of rocks accounts for the contrast in colour between the rocks of the Head and those of mainland cliffs. The softer sedimentary rocks have eroded over time, leaving behind the high headland made from the harder rock. However even this tough volcanic rock has been affected by the actions of the sea, leaving steep gullies and sea stacks which are ide ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gala Water
The Gala Water ( Lowland Scots: Gala Watter; Scottish Gaelic An Geal Ath) is a river in the Scottish Borders area of Scotland and a tributary of the River Tweed. It is sometimes known as the "Gala", which nickname is also shared with Galashiels, which it flows through. The "Braw Lads O Gala Watter" is a song about people from Galashiels. Etymology The name ''Gala'' may be from the Old English ''galga'' meaning "gallows" ( Scots ''galwe''), perhaps by back-formation from Galashiels. Or else, ''Gala'' may originally be from Brittonic, and derived from ''*gāl'' meaning "enmity, hatred" ( Welsh ''gâl''), or cognate to the Welsh verb ''galw'', "call" ( Cornish ''galow'', "a call"). The river may share an etymology with Gala Lane in Ayrshire, which flows into Loch Doon. Levels At Galashiels the depth of the water is between and , although was as deep at on one occasion in 2002. See also *List of places in the Scottish Borders *Leader Water The River Leader, or Leader Water, is ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Selkirkshire
Selkirkshire or the County of Selkirk ( gd, Siorrachd Shalcraig) is a historic county and registration county of Scotland. It borders Peeblesshire to the west, Midlothian to the north, Roxburghshire to the east, and Dumfriesshire to the south. It derives its name from its county town, the royal burgh of Selkirk. The county was historically also known as Ettrick Forest. Unlike many historic counties, Selkirkshire does not have its own lieutenancy area, but forms part of the Roxburgh, Ettrick and Lauderdale lieutenancy area. History In the 1st Century AD Selkirk formed part of the lands of the native people who hunted it rather than settled there. Neither the Romans, Angles, or the Saxons cleared much of the forestry there and for centuries Selkirk was known for its forest coverage. Indeed, an alternative name for the county was Ettrick Forest. Under the Scottish kings the forest was regarded as Royal. Despite this it was not until the reign of James V that sheriffs were a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Old Red Sandstone
The Old Red Sandstone is an assemblage of rocks in the North Atlantic region largely of Devonian age. It extends in the east across Great Britain, Ireland and Norway, and in the west along the northeastern seaboard of North America. It also extends northwards into Greenland and Svalbard. These areas were a part of the ancient continent of Euramerica/Laurussia. In Britain it is a lithostratigraphic unit (a sequence of rock strata) to which stratigraphers accord supergroup status and which is of considerable importance to early paleontology. For convenience the short version of the term, ORS is often used in literature on the subject. The term was coined to distinguish the sequence from the younger New Red Sandstone which also occurs widely throughout Britain. Sedimentology The Old Red Sandstone describes a suite of sedimentary rocks deposited in a variety of environments during the Devonian but extending back into the late Silurian and on into the earliest part of the Car ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Granite
Granite () is a coarse-grained ( phaneritic) intrusive igneous rock composed mostly of quartz, alkali feldspar, and plagioclase. It forms from magma with a high content of silica and alkali metal oxides that slowly cools and solidifies underground. It is common in the continental crust of Earth, where it is found in igneous intrusions. These range in size from dikes only a few centimeters across to batholiths exposed over hundreds of square kilometers. Granite is typical of a larger family of ''granitic rocks'', or '' granitoids'', that are composed mostly of coarse-grained quartz and feldspars in varying proportions. These rocks are classified by the relative percentages of quartz, alkali feldspar, and plagioclase (the QAPF classification), with true granite representing granitic rocks rich in quartz and alkali feldspar. Most granitic rocks also contain mica or amphibole minerals, though a few (known as leucogranites) contain almost no dark minerals. Granite is near ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Carboniferous
The Carboniferous ( ) is a geologic period and system of the Paleozoic that spans 60 million years from the end of the Devonian Period million years ago ( Mya), to the beginning of the Permian Period, million years ago. The name ''Carboniferous'' means "coal-bearing", from the Latin '' carbō'' ("coal") and '' ferō'' ("bear, carry"), and refers to the many coal beds formed globally during that time. The first of the modern 'system' names, it was coined by geologists William Conybeare and William Phillips in 1822, based on a study of the British rock succession. The Carboniferous is often treated in North America as two geological periods, the earlier Mississippian and the later Pennsylvanian. Terrestrial animal life was well established by the Carboniferous Period. Tetrapods (four limbed vertebrates), which had originated from lobe-finned fish during the preceding Devonian, became pentadactylous in and diversified during the Carboniferous, including early amphibian lin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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