Topography
Little Hart Crag is composed of grassy slopes on its eastern slopes above the Scandale pass, with the tiny Scandale Tarn tucked in a hollow in the hill. To the east it drops steeply into Caiston Glen. On its west side it is connected to Dove Crag by the boggy hollow of Bakestone Moss and to the north east a ridge falls away towards Patterdale going over High Hartsop Dodd before dropping steeply to the valley. The fell is craggy on its northern side as the crags of Black Brow fall into Dovedale.
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“That the mere matter of a poem, for instance—its subject, its given incidents or situation; that the mere matter of a picture—the actual circumstances of an event, the actual topography of a landscape—should be nothing without the form, the spirit of the handling, that this form, this mode of handling, should become an end in itself, should penetrate every part of the matter;Mthis is what all art constantly strives after, and achieves in different degrees.”
—Walter Pater (1839–1894)