Робинсон тауы: Англия көлдерінің сипаттамасы мен геологиялық ерекшеліктері

Robinson is a fell in the English Lake District, its southern slopes descending to Buttermere, while its northern side is set in the Newlands Valley. Paths lead to the summit from the village of Buttermere, from the nearby summit Dale Head and from various locations in the valleys to the north.

According to influential guidebook author Alfred Wainwright, the name Robinson comes from a Richard Robinson who purchased estates in the Buttermere area many centuries ago. These included this unnamed hill which was then called "Robinson's Fell", later shortened to Robinson.

The North Western Fells occupy the area between the rivers Derwent and Cocker, a broadly oval swathe of hilly country, elongated on a north–south axis. Two roads cross from east to west, dividing the fells into three convenient groups. Robinson stands in the southern sector. The principal ridge in this group of fells runs east from Buttermere, climbing over Robinson, Hindscarth and Dale Head. It then turns north, descending gradually toward Derwentwater, the main tops being High Spy, Maiden Moor and Catbells. Robinson appears bland from Buttermere, smooth rounded slopes curving up from the valley floor. Viewed from Keswick or Newlands to the north, its character is altogether different. From here the wall of Robinson Crags drops from the summit of the fell, a great chunk of the hillside seemingly missing. The western flanks of the fell fall to Buttermere, the village itself standing on Robinson's territory. The top and bottom sections are quite steep but the slope levels out at 1500 feet (457 m) to accommodate Buttermere Moss, in Wainwright's words “ a wide marshy depression from which water cannot escape except by being carried away in the boots of pedestrians.”

There has been considerable mining activity in the vicinity, particularly at the Goldscope Mine, but this has all taken place beneath the slopes of neighbouring Hindscarth. The remains of a small reservoir can still be seen in Little Dale. Robinson itself has a pair of short levels driven for lead, near to the south east corner of Buttermere lake. They appear not to have progressed beyond trials. The mysterious Hackney Holes are now interpreted as the source of the largest 'rock slope failure' in the Lake District (1.3 sq. km. ), where most of the Buttermere Gatesgarthdale trough wall has deformed and bulged downslope, leaving open trenches (the Holes) or, across the Little Dale col, a chevron pattern of short steep scarps; midslope, there are bold antiscarps (uphill facing scarplets), a classic indicator. Littledale Edge marks the beheading of the original dale by the more vigorous Buttermere valley, fed by ice escaping through Honister Pass from Borrowdale. This geologically recent deep incision has destabilised the slope.

The top is rounded and mainly of grass, but there are two low outcrops of rock with loose stones between. The more westerly of these is the summit and bears a cairn. There is another prominent cairn at the top of the north east ridge. From below this appears to be the summit, but disappointment awaits anyone so deceived by the convex slope. Fair paths run to Buttermere, Littledale Edge and the north east ridge, once the grass is reached.