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Sale Fell is a small hill near
Cockermouth Cockermouth is a market town and civil parish in the Cumberland unitary authority area of Cumbria, England. The name refers to the town's position by the confluence of the River Cocker into the River Derwent. At the 2021 census, the built u ...
in the English
Lake District The Lake District, also known as ''the Lakes'' or ''Lakeland'', is a mountainous region and National parks of the United Kingdom, national park in Cumbria, North West England. It is famous for its landscape, including its lakes, coast, and mou ...
. It is popular with locals, as it offers gentle walking and lovely views across
Bassenthwaite Lake Bassenthwaite Lake is a body of water in the Lake District in North West England, near the town of Keswick. It has an area of , making the fourth largest of the lakes in the region. The lake has a length of approximately long and maximum wid ...
to
Skiddaw Skiddaw is a mountain in the Lake District National Park in England. Its summit is traditionally considered to be the List of Wainwrights, fourth-highest peak but depending on what topographic prominence is thought to be significant is also ...
.


Topography

The
North Western Fells The North Western Fells are a part of the Cumbrian Mountains in the Lake District of England. Including such favourites as Catbells and Grisedale Pike, they occupy an oval area beneath the Buttermere and Borrowdale valley systems. The North We ...
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. The most northerly sector, rising between
Whinlatter Pass The Whinlatter Pass is a mountain pass in the Lake District in Cumbria, England. It is located on the B5292 road linking Braithwaite, to the west of Keswick, with High Lorton to the south of Cockermouth. To the north the pass is flanked ...
and the Vale of Embleton includes Sale Fell. Sale Fell and its twin companion to the west, Ling Fell, are the final hills with any lakeland character in the northwest of the district. Further north across the Vale of Embleton is a final group of very low tops on either side of the Derwent Valley but these are ignored by most guidebooks and hill lists.
Alfred Wainwright Alfred Wainwright Order of the British Empire, MBE (17 January 1907 – 20 January 1991), who preferred to be known as A. Wainwright or A.W., was a British fellwalking, fellwalker, guidebook author and illustrator. His seven-volume ''Pictorial ...
: ''
A Pictorial Guide to the Lakeland Fells ''A Pictorial Guide to the Lakeland Fells'' is a series of seven books by A. Wainwright, detailing the fells (the local word for hills and mountains) of the Lake District in northwest England. Written over a period of 13 years from 1952, they ...
, Book 6, The North Western Fells'': Westmorland Gazette (1964):
Bill Birkett: ''Complete Lakeland Fells'': Collins Willow (1994): (apart from the all-inclusive
Marilyns This is a list of Marilyn hills and mountains in the United Kingdom, Ireland and surrounding islands and sea stacks. Marilyns are defined as peaks with a prominence of or more, regardless of height or any other merit (e.g. topographic isolation ...
.) The natural boundaries of the fell are Bassenthwaite Lake to the east, Wythop Valley to the south and west, and the Vale of Embleton to the north. Sale Fell is a satellite of
Lord's Seat Lord's Seat is a fell in the English Lake District The Lake District, also known as ''the Lakes'' or ''Lakeland'', is a mountainous region and National parks of the United Kingdom, national park in Cumbria, North West England. It is fam ...
, the highest of the hills north of Whinlatter. The connecting high ground runs southeastward above the shore of Bassenthwaite before turning inland to the summit of the parent fell. The connection is extremely tenuous, passing along a very narrow strip of land between Wythop Beck and Beck Wythop. These two streams run side by side down the slopes of Lord's Seat before diverging to surround Sale Fell on all sides. Wythop Beck is the main stream of the Wythop Valley, running west around Sale Fell and then out down the narrow wooded defile which stands between it and Ling Fell. Joining the Dubwath Beck it then flows eastward along the Vale of Embleton and into the northern end of Bassenthwaite. Beck Wythop by contrast cuts through the ridge of high ground running alongside Bassenthwaite and drops directly into the lake. Sale Fell itself is an east-west ridge about a mile long, clad primarily in fell grass and bracken The eastern end is heavily forested as part of Wythop Wood. These are mostly conifers, although the mix of trees is gradually changing. There are Forestry Commission offices hidden in the trees at the base of the fell. The summit of the fell is toward the west of the ridge and there are two other tops to the east. Rivings (1,099 ft) and Lothwaite (1,132 ft) are included in some guidebooks


Geology

The fell is predominantly composed of
Ordovician The Ordovician ( ) is a geologic period and System (geology), system, the second of six periods of the Paleozoic Era (geology), Era, and the second of twelve periods of the Phanerozoic Eon (geology), Eon. The Ordovician spans 41.6 million years f ...
rocks of the Loweswater Formation. This consists of
greywacke Greywacke or graywacke ( ) is a variety of sandstone generally characterized by its hardness (6–7 on Mohs scale), dark color, and Sorting (sediment), poorly sorted angular grains of quartz, feldspar, and small rock fragments or sand-size Lith ...
sandstone Sandstone is a Clastic rock#Sedimentary clastic rocks, clastic sedimentary rock composed mainly of grain size, sand-sized (0.0625 to 2 mm) silicate mineral, silicate grains, Cementation (geology), cemented together by another mineral. Sand ...
turbidities. The southern flanks are of the laminated
mudstone Mudstone, a type of mudrock, is a fine-grained sedimentary rock whose original constituents were clays or muds. Mudstone is distinguished from ''shale'' by its lack of fissility.Blatt, H., and R.J. Tracy, 1996, ''Petrology.'' New York, New York, ...
and
siltstone Siltstone, also known as aleurolite, is a clastic sedimentary rock that is composed mostly of silt. It is a form of mudrock with a low clay mineral content, which can be distinguished from shale by its lack of fissility. Although its permeabil ...
of the Kirk Stile Formation.British Geological Survey: 1:50,000 series maps, ''England & Wales Sheet 29'': BGS (1999)


Summit

A small
cairn A cairn is a human-made pile (or stack) of stones raised for a purpose, usually as a marker or as a burial mound. The word ''cairn'' comes from the (plural ). Cairns have been and are used for a broad variety of purposes. In prehistory, t ...
sits on an expanse of grass. The view of the
Skiddaw Skiddaw is a mountain in the Lake District National Park in England. Its summit is traditionally considered to be the List of Wainwrights, fourth-highest peak but depending on what topographic prominence is thought to be significant is also ...
group is excellent and the
Helvellyn range The Helvellyn range is the name given to a part of the Eastern Fells in the English Lake District, "fell" being the local word for "hill". The name comes from Helvellyn, the highest summit of the group. The Helvellyn range forms a ridge exte ...
is also laid out end to end. Most of the District is unfortunately obscured by the Lord's Seat ridge. Bassenthwaite Lake completes the eastern foreground, the hills of Galloway are visible across the
Solway Firth The Solway Firth is an inlet on the west coast of Great Britain, forming part of the border between England and Scotland. The firth (a Scottish term for an inlet of the sea) divides Cumbria (including the Solway Plain) from Dumfries and Gallow ...
, whilst the Isle of Man can be seen to the west.


Ascents

From the Pheasant Inn at the northern end of the lake, a side road runs west towards Routenbeck and Wythop Mill. A footpath branches off left before St Margaret's Church and makes up the fellside, joining a terrace path higher up. There is now a choice, either making for the western end of the summit ridge or joining it to the east near the forest fence. From the village of Wythop Mill, the road between Ling Fell and Sale Fell provides a starting point, branching off up the fellside at the gate of Kelswick Farm. There is no ridge connection to Ling Fell although the two can be easily climbed from Wythop Mill.


References

{{North Western Fells Fells of the Lake District