Holme Fell
| Holme Fell | |
|---|---|
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| Highest point | |
| Elevation | 317 m (1,040 ft) |
| Prominence | 165 m (541 ft) |
| Parent peak | Old Man of Coniston |
| Listing | Marilyn, Wainwright |
| Coordinates | 54°23′46″N 3°03′22″W / 54.396°N 3.056°WCoordinates: 54°23′46″N 3°03′22″W / 54.396°N 3.056°W |
| Geography | |
 Holme Fell
Lake District
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| Location | Cumbria, England |
| Parent range | Lake District, Southern Fells |
| OS grid | NY315006 |
| Topo map | OS Landranger 90, Explorer OL7 |
Holme Fell or Holm Fell is a fell in the Lake District in Cumbria, England. It is located between Coniston Water and Little Langdale, almost isolated from the neighbouring Coniston Fells by Yewdale Beck.
Holme Fell is an eastern outlier of Wetherlam, although the topographical connection via Great Intake and Low Tilberthwaite is rather tortuous. Further east, beyond Oxen Fell High Cross, the high ground continues to Black Fell.
The fell itself is a ridge running broadly north-south and about a mile and a half long. The summit is at the southern extremity, a flank guarded by Calf and Raven Crags. Immediately to the north is Ivy Crag, a second top sporting a large cairn, followed by the depression of Uskdale Gap. Continuing northward are a succession of lower tops, gradually descending toward the final knoll of Great How (692 ft). A swift descent to the floor of Little Langdale then follows.
The boundaries of the fell are all formed by roads and tracks, giving opportunities for circular walks. The main Ambleside-Coniston road lies to the east and the minor road along Little Langdale to the north. Yewdale Beck runs around the southern perimeter, with the narrow access lane to Hodge Close hugging its bank. From Hodge Close a bridleway runs north to Little Langdale. The southern half of the fell has much natural woodland, mostly deciduous species. There are also some larger artificial plantings to the north.
Hodge Close bears the remains of quarrying (see below), as does Uskdale Gap. To the west of the Gap are two small tarns. These were built as reservoirs for the quarry, with the water used to operate a funicular to raise slate to ground level.
A further artificial water body is Yew Tree Tarn beside the Ambleside-Coniston road. This was dammed to a depth of 10 ft (3 metres) in the 1930s by James Marshall, the landowner. The original intent was to provide fishing, and trout are still plentiful today.
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Wikipedia