Seat Sandal

Infobox Mountain
Name = Seat Sandal
Photo = Seat_Sandal_from_Helm_Crag.jpg
Caption = Seat Sandal (left) and Fairfield (right) seen from Helm Crag two km to the SW.
Location = Cumbria, ENG
Range = Lake District, Eastern Fells
Elevation = 736 m (2,415 ft)
Grid_ref_UK = NY343115
Topographic
OS "Landranger" 90 OS "Explorer" 5
Prominence = c 150 m
Parent peak = Fairfield
Listing = Hewitt, Marilyn, Nuttall, Wainwright

Seat Sandal is a fell in the English Lake District, it is situated four kilometres north of the village of Grasmere from where it is very well seen. Nevertheless, it tends to be overshadowed by its more illustrious neighbours in the Eastern Fells, Helvellyn and Fairfield.

Topography

The fells western flanks above Dunmail Raise are grassy and smooth while its eastern slopes are steep and craggy as they fall away towards Grisedale Hause which at 537 m (1,761 ft) contains Lakeland's highest substantial tarn, Grisedale Tarn. The fell reaches a height of 736 m (2,415 ft) and just scrapes into the list of Marilyns by being given prominence of "around" 150 metres from the higher fell of Fairfield, however this must be a borderline case as there is no Ordnance Survey surveyed height for the top of Grisedale Hause. Alfred Wainwright gives it a height of 1929 feet (588 metres) giving Seat Sandal a topographic prominence of only 148 metres (two metres short of Marilyn qualification). The hills unusual name comes from the Norse language, meaning “Sandulf’s Hill Pasture”, Sandulf being being a Nordic personal name.

Seat Sandal is distinctive in that its drainage reaches the sea at more widely spread points than any other Lakeland Fell. with Raise Beck going through Thirlmere and Derwent Water to reach the Irish Sea at Workington, Tongue Beck going through Grasmere and Windermere to reach Morecambe Bay and Grisedale Beck draining into Ullswater and then to the sea at the Solway Firth. The fell's main topographic attraction is Gavel Crag on its eastern side, which is connected to the main body of the fell by a fine rock arete.

Dunmail Raise provides the topographical connection between the Eastern and Central Fells, Steel Fell rising on the other side of the pass.

Geology

A ill of andesite lava forms the summit, the rocks beneath being the dacitic lapilli-tuffs of the Lincomb Tarns Formation.British Geological Survey: 1:50,000 series maps, "England & Wales Sheet 29": BGS (1999)]

Ascents

The fell can be ascended from Grasmere or Dunmail Raise although a start from Patterdale is quite feasible. The Grasmere or Patterdale starts use the old packhorse route that links the two places; this is now part of Wainwright’s Coast to Coast Walk. When Grisedale Hause is reached it is a steep climb to the summit following a broken wall. The ascent from Dunmail Raise follows the bed of Raise Beck until it peters out at a height of 580 m (1,900 ft), it is then a walk south up easy slopes to reach the summit.

View

The view from the top is limited by the nearby Helvellyn and Fairfield ranges although there is a good view of Lakeland to the west, the Solway Firth and Criffel are viewed on a good day as is Morecambe Bay to the south.

References

* A Pictorial Guide to the Lakeland Fells, Eastern Fells, Alfred Wainwright, ISBN 0-7112-2454-4
* Complete Lakeland Fells, Bill Birkett, ISBN 0-00-713629-3
* The Mountains of England and Wales, John and Anne Nuttall ISBN 1-85284-037-4