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Bannerdale Crags is a fell in the English Lake District. It stands between Blencathra and Bowscale Fell in the Northern Fells. ==Topography== Bannerdale Crags is a ridge running north west to south east. The name was originally applied purely to the steep north eastern flank, but is now generally given to the fell as a whole.〔Wainwright, Alfred: ''A Pictorial Guide to the Lakeland Fells,Book 5 The Northern Fells'': ISBN 0-7112-2458-7〕 A broad convex slope descends northward from Blencathra's Atkinson Pike top, gradually resolving into two ridges. The western arm continues to Mungrisdale Common while the north eastern limb, flecked with outcropping rock, falls to a steep sided col at . From the depression Blackhazel Beck descends north west to join the River Caldew while the source of the Glenderamackin lies on the opposite slope. Across the col smooth slopes rise once more up the south western flank of the Bannerdale Crags ridge. There is little clue here to the wall of crags on the other side. The north eastern side of the ridge looks down upon the valley of Bannerdale Beck, a tributary of the Glenderamackin. The crags on this side are almost continuous for a mile in length, the highest sections falling to the valley. The major breach is a spur protruding from the face almost below the summit, providing a fine route of ascent.(see below) To the north the summit ridge continues across a broad grassy saddle to Bowscale Fell, the crags continuing a little way into the territory of the neighbouring fell. By contrast to the south east the fell ends in White Horse Bent, the abrupt ridge-end descent to the Glenderamackin. This river has one of the most convoluted passages in the district, passing around the south and east of Bannerdale Crags, before turning back on itself to surround Souther Fell on almost all sides and finally head west for Keswick and the River Derwent. 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「Bannerdale Crags」の詳細全文を読む スポンサード リンク
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