|
Berwickshire
Berwickshire (; ) is a historic county, registration county and lieutenancy area in south-eastern Scotland, on the English border. 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. 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 low-lying part of Berwickshire between the Tweed and the Lammermuirs is known as "the Merse", from an old Scots word for a floodplain, and this ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Shires Of Scotland
The counties or shires of Scotland () were historic subdivisions of Scotland. The shires were originally established in the Middle Ages for judicial purposes, being territories over which a Sheriff principal, sheriff had jurisdiction. They were distinct from the various older mormaerdoms, earldoms and other territories into which Scotland was also divided, which are collectively termed the provinces of Scotland by modern historians. The provinces gradually lost their functions, whereas the shires gradually gained functions. From the 16th century, the shires served as county constituency, constituencies, electing shire commissioners to the Parliament of Scotland. From 1667 each shire had Commissioners of Supply, commissioners of supply responsible for collecting local taxes; the commissioners of supply were subsequently given various local government functions as well. From 1797, the shires also served as areas for organising the militia, which was the responsibility of a lord-li ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Midlothian
Midlothian (; ) is registration county, lieutenancy areas of Scotland, lieutenancy area and one of 32 council areas of Scotland used for local government. Midlothian lies in the east-central Lowlands, bordering the City of Edinburgh council area, East Lothian and the Scottish Borders. The modern council area was formed in 1975 when the Midlothian (historic), historic county of Midlothian, also known as Edinburghshire, was altered substantially as part of local government reforms; its southern part formed a new Midlothian Districts of Scotland, District within the Local government areas of Scotland 1973 to 1996, Region of Lothian, whilst areas on the peripheries were assigned to other districts and the city of Edinburgh, which had always been autonomous to an extent, was formally separated as the Edinburgh (district), City of Edinburgh District. In 1996 Midlothian became a unitary authority area, using the same name and territory as in 1975. History Midlothian County Council w ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eden Water
Eden Water is a tributary of the River Tweed in the Scottish Borders of Scotland. "Water" is the Lowland Scots term for a small river. The Eden Burn rises to the east of Lauder at Corsbie Moor on Boon Farm. The Eden Water passes Bassendean village and Bassendean House and the hamlets of Fawside and Mack's Mill. Next is the county town of Gordon, and the Water flows through Gordon East Mains, under the A6105, then through the Mellerstain House estate, and the river now turns east towards Old Nenthorn, Nenthorn House, and Nenthorn where the A6089, the B6404 and the B6364 pass over it. After passing by Ednam Cliftonhill and Ednam East Mill, the Eden Water joins the River Tweed where the A698 bridges it. Etymology ''Eden'' is a fairly common outcome in English of a Brittonic river name that can be reconstructed as *''ituna'' 'to gush forth'.Bethany Fox, 'The P-Celtic Place-Names of North-East England and South-East Scotland', The Heroic Age, 10 (2007), http://www.heroicage.org/ ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Watch Water
The Watch Water is a river in the Scottish Borders area of Scotland. It rises in the Lammermuir Hills, around west of Longformacus, and flows generally eastward to its confluence with the Dye Water, around west of Longformacus. The Dye Water flows into the Whiteadder Water, which in turn is a tributary of the River Tweed. Watch Water Reservoir Watch Water Reservoir is a man-made reservoir, located approximately halfway along the river's course, around from Longformacus and from Duns, Scottish Borders, Duns. It extends to , and is formed by an earthen dam. The Southern Upland Way, a Long Distance Route which runs across southern Scotland, skirts the northern edge of the reservoir, and the Sir Walter Scott Way from Moffat to Cockburnspath also passes by it. The partial ruins of a peel tower survive as part of Old Scarlaw Cottage, also on the northern edge of the reservoir. John Dippie's Well Close to where the Southern Upland Way crosses the Watch Water is John Dippie's Well. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dye Water
The Dye Water () is a river in the Lammermuir Hills in the Scottish Borders area of Scotland. It rises in the Hope Hills, continues along the East Lothian boundary, a mile north east of Seenes Law, then east to Longformacus. The Dye Water joins the Whiteadder Water and completes its 12.5 mile journey. The Sir Walter Scott Way and the Southern Upland Way long distance footpaths also pass through Longformacus. See also *List of places in the Scottish Borders *List of places in Scotland External links CANMORE/RCAHMS record of Dye Water- (RCAHMS - the Royal Commission on the Ancient and Historical Monuments of Scotland The Royal Commission on the Ancient and Historical Monuments of Scotland (RCAHMS) was an executive non-departmental public body of the Scottish Government that was "sponsored" inanced and with oversightthrough Historic Scotland, an executive ... Rivers of the Scottish Borders 2Dye {{Scotland-river-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Whiteadder Water
Whiteadder Water is a river in East Lothian and Berwickshire, Scotland. It also flows for a very short distance through Northumberland before joining the River Tweed. In common with the headwaters of the Biel Water it rises on the low hillside of Clints Dod () in the Lammermuir Hills, just ESE of Whitecastle Hillfort and south-east of the village of Garvald. Etymology ''Adder'' may be derived from Brittonic ''*ador, *edir'' or Old English ''edre'', possible ancient hydronymic terms derived from an Indo-European formation meaning "a watercourse, a channel" (compare River Etherow). The possibility of the name deriving from Old English ''ǣdre'', "a vein" ( Anglian ''ēdre''), or ''*ǣdre'', meaning "quickly" is objected on the grounds that these would have maintained the long initial vowel in English and Scots. Also suggested is derivation from Gaelic ''fad dûr'', meaning "long water". though the Gaelic was never spoken in the Scottish southeast. Course The stream wend ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eye Water
Eye Water is a river in the Scottish Borders, it flows in a general southeasterly direction from its source in the Lammermuir Hills to its estuary at Eyemouth on the east coast of Scotland, having a length of approximately .''"Ordnance Survey Explorer Map"'' Sheet 346, Used to give estimated length and general course description of Eye Water. River course The Eye Water rises on the eastern slopes of Wester Dod at height of 375 metres, it flows SE for 10 km before swinging NE for three km to reach the village of Grantshouse. The Eye Water flows on the southern outskirts of Grantshouse as it again turns SE and runs in a valley between Horseley Hill and Dalks Law alongside the A1 road (Great Britain), A1 road and the East Coast Main Line railway. The river keeps to the SW side of the A1 passing through the villages of Reston, Scottish Borders, Reston and Ayton, Scottish Borders, Ayton where it flows through a pleasant wooded valley on the Ayton Castle, Scottish Borders, Ayton Ca ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Anglo-Scottish Border
The Anglo-Scottish border runs for between Marshall Meadows Bay on the east coast and the Solway Firth in the west, separating Scotland and England. The Firth of Forth was the border between the Picto- Gaelic Kingdom of Alba and the Anglian Kingdom of Northumbria in the early 10th century. It became the first Anglo-Scottish border with the annexation of Northumbria by Anglo-Saxon England in the mid-10th century. In 973, the Scottish king Kenneth II attended the English king Edgar the Peaceful at Edgar's council in Chester. After Kenneth had reportedly done homage, Edgar rewarded Kenneth by granting him Lothian. Despite this transaction, the control of Lothian was not finally settled and the region was taken by the Scots at the Battle of Carham in 1018 and the River Tweed became the '' de facto'' Anglo-Scottish border. The Solway–Tweed line was legally established in 1237 by the Treaty of York between England and Scotland. It remains the border today, with the exc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Meikle Says Law
The Lammermuirs are a range of hills in southern Scotland, forming a natural boundary between East Lothian and the Scottish Borders, Borders. The name ''Lammermuir'' comes from the Old English , 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 (geology), Gala Group. Unconformity (geology), Unconformably overlying these highly fault (geology), faulted and fold (geology), 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 conglomerate (geology), 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lammermuir Hills
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 , 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 lithologies ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Northumberland
Northumberland ( ) is a ceremonial counties of England, ceremonial county in North East England, on the Anglo-Scottish border, border with Scotland. It is bordered by the North Sea to the east, Tyne and Wear and County Durham to the south, Cumbria to the west, and the Scottish Borders council area to the north. The town of Blyth, Northumberland, Blyth is the largest settlement. Northumberland is the northernmost county in England. The county has an area of and a population of 320,274, making it the least-densely populated county in England. The south-east contains the largest towns: Blyth, Northumberland, Blyth, Cramlington, Ashington, Bedlington, and Morpeth, Northumberland, Morpeth, the last of which is the administrative centre. The remainder of the county is rural, the largest towns being Berwick-upon-Tweed in the far north and Hexham in the south-west. For local government purposes Northumberland is a Unitary authorities of England, unitary authority area. The county Histo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
