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Whin Sill information


The Whin Sill at Crag Lough, showing Hadrian's Wall running along the top.

The Whin Sill or Great Whin Sill is a tabular layer of the igneous rock dolerite in County Durham, Northumberland and Cumbria in the northeast of England. It lies partly in the North Pennines Area of Outstanding Natural Beauty and partly in Northumberland National Park and stretches from Teesdale northwards towards Berwick.

It is one of the key natural features of the North Pennines. A major outcrop is at the High Force waterfall in Teesdale. Bamburgh Castle, Dunstanburgh Castle, Lindisfarne Castle and stretches of Hadrian's Wall all strategically take advantage of high, rocky cliff lines formed by the sill.

The Whin Sill complex is usually divided into three components: Holy Island Sill, Alnwick Sill and the Hadrian's Wall-Pennines Sill, which were created by separate magma flows, but at about the same time.[1]

The Little Whin Sill is an associated formation to the south, in Weardale.

  1. ^ D. Liss, W.H. Owens and D.H.W. Hutton, New palaeomagnetic results from the Whin Sill complex: evidence for a multiple intrusion event and revised virtual geomagnetic poles for the late Carboniferous for the British Isles, Journal of the Geological Society; December 2004; v. 161; no. 6; p. 927–938; doi:10.1144/0016-764903-156, 2004 Geological Society of London, England

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Whin Sill

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The Whin Sill or Great Whin Sill is a tabular layer of the igneous rock dolerite in County Durham, Northumberland and Cumbria in the northeast of England...

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Sycamore Gap tree

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This section of the wall follows the edge of a cliff – an outcrop of the Whin Sill – and several sharp dips in it caused by melting glacial waters. The tree...

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Crag Lough

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England. At this point Hadrian's Wall is at the top of a line of crags, the Whin Sill, with Crag Lough at the foot of the crags. The etymology of Crag Lough...

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Northumberland

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granite and andesite lava. A second area of igneous rock underlies the Whin Sill (on which Hadrian's Wall runs), an intrusion of Carboniferous dolerite...

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Geology of Northumberland National Park

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Carboniferous age. These are intruded by Permian dykes and sills, of which the Whin Sill makes a significant impact in the south of the park. Further...

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Craster

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are a significant feature of the local landscape, and are part of the Whin Sill. The walk along the rocky shore to the north along leads to the ruins...

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Bamburgh Castle

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public. Built on top of a black crag of volcanic dolerite, and part of the Whin Sill, the location was previously home to a fort of the indigenous Celtic Britons...

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High Force

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Nature Reserve. High Force was formed where the River Tees crosses the Whin Sill – a hard layer of igneous rock (also seen at Hadrian's Wall and other...

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Housesteads Roman Fort

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It is dramatically positioned on the end of the mile-long crag of the Whin Sill over which the Wall runs, overlooking sparsely populated hills. It was...

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Cauldron Snout

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falls are caused by the upper Tees passing over dolerite steps of the Whin Sill. An engraving of a painting of the cataract by Thomas Allom was published...

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Once Brewed

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Brewed lies just south of Hadrian's Wall, which runs along the top of the Whin Sill ridge above the village to the north. The Roman fort of Vindolanda is...

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Teesdale

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Fell into June. Unusually for the Pennines, rock of igneous origin (the Whin Sill) contributes to the surface geology and scenery of Upper Teesdale. Around...

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Bamburgh Coast and Hills

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and displays the interaction of a fluid magma rock, now known as the Whin Sill, interacting with older sedimentary rock. Coastal erosion at the site...

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Bavington Crags

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(SSSI) in north Northumberland, England. The site is an outcropping of the Whin Sill which gives rise to distinctive flora particular to the thin soil conditions...

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North Pennines

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sedimentary rocks laid down during the Palaeozoic era, later intruded by the Whin Sill and affected by glaciation during the Quaternary period. Mud and volcanic...

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Allolee to Walltown

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unusually wide range of grassland types growing on thin soil above the Whin Sill, a rock formation peculiar to the Northern Pennines. Allolee to Walltown...

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Haltwhistle

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striding eastwards from the lake at Crag Lough along the spine of the Whin Sill. The remains of Haltwhistle Castle and the series of Bastles, and Haltwhistle...

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Yorkshire

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with County Durham, the River Tees plunges 22 metres (72 ft) over the Whin Sill (an intrusion of igneous rock). High Force is not, as is sometimes claimed...

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High Cup Gill

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England. High Cup Scar is formed by a near-horizontal outcrop of the Whin Sill, a dolerite intrusion of late Carboniferous age which underlies much of...

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Budle Bay

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along parts of its southeastern shore. The quartz-microgabbro of the Whin Sill occupies the higher ground on this southeastern side of the bay. There...

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Geography of England

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Jurassic Coast – a UNESCO World Heritage Site Salisbury Plain Tees–Exe line Whin Sill London Basin Hampshire Basin London-Brabant Massif Dartmoor – one of a...

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Pennines

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Conversely, the Border Moors and Cheviot Hills, separated by the Tyne Gap and Whin Sill, along which run the A69 and Hadrian's Wall, are not part of the Pennines...

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Alnmouth

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of glacial till in the form of boulder clay lying on often outcropping Whin Sill, a carboniferous limestone, with peat deposits, and, at the coast, wind-blown...

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The Laidly Worm of Spindleston Heugh

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verses. Spindlestone Heugh (or Heughs) is a dolerite crag on the Great Whin Sill escarpment in the parish of Easington, Northumberland. The Spindlestone...

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Longhoughton Quarry

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yielded whinstone, a hard dark rock associated in Northumberland with the Whin Sill. Longhoughton Quarry is situated 0.9 miles (1.4 km) west of Longhoughton...

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Dunstanburgh Castle

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coast. The castle is situated on a prominent headland, part of the Great Whin Sill geological formation. On the south side of the castle there is a gentle...

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Geology of Great Britain

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the Giant's Causeway in Northern Ireland) Salisbury Plain Tees–Exe line Whin Sill Siccar Point in Berwickshire provided early proof of the immense age of...

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