The Abbey Craig, a crag with tail near The
University of Stirling.
The University of Stirling founded in 1967 in Stirling, Scotland. The
Wallace Monument stands on the crag at the right, and the long tail slopes down leftward
Salisbury Crags to the left and
Arthur's Seat to the right, with their tails sloping east to the right.
The National Wallace Monument (generally known as the Wallace Monument) is a tower standing on the summit of Abbey Craig, a hilltop near Stirling in Holyrood Park (also called Queen's Park, and formerly King's Park) is a royal park in central Edinburgh, Scotland. Arthur's Seat is the main peak of the group of hills which form most of Holyrood Park, a remarkably wild piece of highland landscape in the centre of the city of
A crag (sometimes spelled cragg, or in Scotland craig) is a rocky hill or mountain, generally isolated from other high ground. Scotland ( Gaelic: Alba) is a Country in northwest Europethat occupies the northern third of the island of Great Britain. Crags are formed when a glacier or ice-sheet passes over an area that contains a particularly resilient chunk of rock (often a granite plug or some volcanic structure). "Glacial" and "Glaciation" redirect here For the geological periods see Glacial period. Granite (ˈɡrænɪt is a common and widely occurring type of intrusive, Felsic, igneous rock. A volcanic plug, also called a volcanic neck or lava neck, is a volcanic landform created when Lava hardens within a Vent on Plate tectonics and hotspots Divergent plate boundaries At the The force of the glacier erodes the surrounding softer material, leaving the rocky block protruding from the surrounding terrain. Frequently the crag serves as a partial shelter to softer material in the wake of the glacier, which remains as a gradual fan or ridge forming a tapered ramp (called the tail) up the leeward side of the crag.
In older examples, or those which are latterly surrounded by the sea, the tail is often missing, having been removed by post-glacial erosion.
Examples of such crag and tail formations include:
- The Castle Rock in Edinburgh, Scotland, the rock on which Edinburgh Castle stands. Edinburgh ( ˈɛdɪnb(ərə Dùn Èideann) is the Capital of Scotland and is its second largest city after Glasgow. Scotland ( Gaelic: Alba) is a Country in northwest Europethat occupies the northern third of the island of Great Britain. Edinburgh Castle is an ancient Stronghold which dominates the sky-line of the
- Salisbury Crags and Arthur's Seat, Edinburgh
- Three in or near Stirling, Scotland, including the rock on which Stirling Castle stands. Holyrood Park (also called Queen's Park, and formerly King's Park) is a royal park in central Edinburgh, Scotland. Arthur's Seat is the main peak of the group of hills which form most of Holyrood Park, a remarkably wild piece of highland landscape in the centre of the city of Stirling ( Gaelic: Sruighlea, Scots: Stirlin) is a city and former ancient Burgh in Scotland, and is at Scotland ( Gaelic: Alba) is a Country in northwest Europethat occupies the northern third of the island of Great Britain. For ships named after the castle see Stirling Castle (disambiguation Stirling Castle, located in Stirling, is one of the largest
Similar formations to the Crag and Tail are:
A drumlin (Irish droimnín, a little hill ridge is an elongated whale-shaped Hill formed by glacial action In Glaciology, a roche moutonnée (or sheepback) is a Rock formation created by the passing of a Glacier.
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