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GPX Download Of Route... https://drive.google.com/file/d/1F0Vb... Little Mell Fell is a small U-shaped area of high ground, about 1 square mile in area, north of Ullswater and east of Great Mell Fell. Its summit is a symmetrical rounded grassy dome in the south-east corner of the fell which reaches a height of 505 m, 32 m lower than Great Mell Fell. Two short grassy spurs extend from this dome: one to the north and one to the west. The western spur then turns northwards so that a deep valley is enclosed between the two spurs, drained by the upper reaches of Thackthwaite Gill. The fell has one visible connection to other fells. Due south from the summit a narrow col called The Hause connects it to Watermillock Fell and a ridge of high ground running south west, parallel to the shore of Ullswater, until it culminates at Gowbarrow Fell. Intermediate tops along this ridge include Watermillock Fell (424 m, unnamed on Ordnance Survey maps), Little Meldrum (404 m) and Great Meldrum (437 m). The south-east corner of the fell is drained by a small beck which flows directly into Ullswater. All other parts of the fell are drained by various tributaries of Dacre Beck, which joins the River Eamont below its outfall from Ullswater. Thus the whole fell drains ultimately into the Eamont and to the Solway Firth. The fell has a few small areas of broadleaved plantation, but otherwise is bare, the lower slopes being parcelled up into fields for agriculture. Notices indicate the presence of adders on the fell. Great Mell Fell is an isolated hill which rises abruptly from a wide expanse of marshy lowland to a height of 537 m. The fell has smooth, rounded outlines with no crags. Rock is represented only by a number of large erratic boulders, mainly on the north slopes, but also by the Cloven Stone near a barn to the south of the fell. The hill is triangular in plan (indeed, it is almost the shape of a broad arrow-head) with the apex pointing west, down the steep "nose" of the fell, and with the gentler, broader eastern slopes divided by two shallow valleys which drain into the Wham Sike and Routing Gill Beck. Great Mell Fell lies on the watershed between the Derwent river system to the west and the Eden system to the east. This watershed is formed by a low ridge, barely perceptible in places, which connects the Northern and Eastern Fells. From Bowscale Fell it runs across Eycott Hill to Great Mell Fell, then over Cockley Moor to High Brow and up the north-east ridge of Great Dodd, to join the main ridge on the Helvellyn range. Thus the eastern sides of the fell drain eventually into the River Eden via Dacre Beck and the River Eamont, while the western parts drain through Keswick via Trout Beck, the River Glenderamackin and the River Greta to the Derwent. Great Mell Fell is a quiet place of refuge within the surrounding agricultural land, for wildlife as well as for walkers. The sheltered lower eastern slopes are well covered by mixed woods of oak, rowan, birch, holly and Scots pine. Within the trees badgers and roe deer live, and green woodpeckers nest. It is said that the last wild cat in Cumberland was snared here in the nineteenth century. Higher up the fell an old planting of Scots pine straddles the eastern ridge, and contorted wind-blown larches grow higher still, some blown almost horizontal. The trees give a glimpse of what other fells may have looked like in better-wooded times. A nineteenth-century guidebook claims that larch was planted all over the fell. However the fell’s name suggests that it was treeless in first millennium Celtic-speaking times. Clumps of tough grass and occasional clumps of heather cover the highest parts, where occasional red grouse may nest. #littlmellfell #greatmellfell #cinematic #dji #drone #djimini2se #mountains #mountain #rivers #hills #hillwalking #fellwalking #waterfall #lakedistrict #cumbria #lakedistrictnationalpark #nature #hiking #getoutside #wainwrights #birketts #hewitts #marilyns #wellbeing #alfredwainwright #billbirkett #liveyourbestlife #mentalhealthmatters