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High Seat (Lake District)
High Seat is a fell in the centre of the English Lake District. Despite being below 2,000 ft it is the highest point for about 5 miles in any direction; a consequence of the curious fact that the centre of the district is lower than the surrounding parts.
==Topography==
The main watershed of the Central Fells runs north-south, with Bleaberry Fell forming the northern end of the ridge. High Seat is the next fell to the south, before the land falls to High Tove.
High Seat sends out the spur of Dodd to the north west, separated from the body of the fell by Ashness Gill — a feeder of Watendlath Beck. Oddly, by the time the Gill reaches the famed viewpoint of Ashness Bridge, it has actually become Barrow Beck. The western flank here is clad in broadleaved woodland, but further south along Watendlath Beck this gives way to rock. Reecastle Crag being the principal face.
The southern boundary of the fell is formed by Raise Gill on the western side of the ridge and Shoulthwaite Gill in the east. To say that they drain The Peewits — the hideous bog on the ridge to High Tove — would be untrue, but they are fed by it. Shoulthwaite Gill does not head due east for Thirlmere as might be expected, but turns due north to form the eastern boundary. It is cut off from the reservoir by the lower parallel ridge of Raven Crag and High Rigg and instead makes a beeline for the River Greta. Mere Gill, one of its many tributaries forms the north eastern edge of High Seat. This flows from a point on the ridge to Bleaberry Fell which bears the name of Threefooted Brandreth: (a brandreth being the word for a three-legged stand in an oven on which a griddle was placed when cakes etc. were baked.)
抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』
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