Esk Pike
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Esk Pike is a fell in the English
Lake District The Lake District, also known as the Lakes or Lakeland, is a mountainous region in North West England. A popular holiday destination, it is famous for its lakes, forests, and mountains (or '' fells''), and its associations with William Wordswor ...
, one of the cirque of hills forming the head of Eskdale.


Topography

The Southern Fells include the highest ground in England, a horseshoe which begins with Scafell and Scafell Pike in the west and then curves around the north of Upper Eskdale to take in Great End, Esk Pike,
Bow Fell Bowfell (named ''Bow Fell'' on Ordnance Survey maps) is a pyramid-shaped mountain lying at the heart of the English Lake District, in the Southern Fells area. It is the sixth-highest mountain in the Lake District and one of the most popular ...
and Crinkle Crags. As the name suggests, Esk Pike stands at the head of the valley, although it is not the highest of these fells. To the north-west of Esk Pike is the depression of Esk Hause, a broad saddle carrying a number of important paths. The ‘true’ Esk Hause—so named by Alfred Wainwright in his influential '' Pictorial Guide to the Lakeland Fells''—is the north–south route from
Borrowdale Borrowdale is a valley and civil parish in the English Lake District in the Borough of Allerdale in Cumbria, England. It lies within the historic county boundaries of Cumberland. It is sometimes referred to as ''Cumberland Borrowdale'' ...
to Eskdale. A lower path—the ‘false’ Hause—runs east–west from Langdale to Wasdale, passing a stone windshelter. There are also paths climbing to the summits of Esk Pike and Allen Crags, together with the popular Calf Cove route to Scafell Pike, all contributing to make Esk Hause a confusing place in mist. The source of the main branch of the Esk flows south from the Hause, while to the north the topography is more complex. Allen Crags stands adrift from the main ridge, with the valleys of Langstrath and Grains Gill falling on either side. These combine some miles downstream to form the River Derwent, flowing through Borrowdale to Derwentwater and Keswick. South-east of the summit of Esk Pike is Ore Gap, the
col In geomorphology, a col is the lowest point on a mountain ridge between two peaks.Whittow, John (1984). ''Dictionary of Physical Geography''. London: Penguin, 1984, p. 103. . It may also be called a gap. Particularly rugged and forbidding co ...
separating it from Bow Fell. The soil here is red due to
haematite Hematite (), also spelled as haematite, is a common iron oxide compound with the formula, Fe2O3 and is widely found in rocks and soils. Hematite crystals belong to the rhombohedral lattice system which is designated the alpha polymorph of . I ...
, and climbing lore suggests that magnetic compasses cannot be trusted in this locality. Alfred Wainwright: '' A Pictorial Guide to the Lakeland Fells'', Book 4: North of the gap is Angle Tarn, a feeder of the Langstrath. This round tarn occupies a corrie beneath Hanging Knotts, small trout lurking in its 50-foot depths.Blair, Don: ''Exploring Lakeland Tarns'': Lakeland Manor Press (2003): Southward from the summit, Esk Pike throws out a long descending ridge into the uninhabited fastness of Upper Eskdale. This divides the Esk from its major upper tributary, Lingcove Beck, which has its beginnings at Ore Gap. Two miles in length, this ridge falls over a series of craggy steps to the confluence of the two streams at Lingcove Bridge. An old Packhorse Bridge, this is a focal point for those approaching from the south, particularly when the Esk is in spate. The south ridge has a number of subsidiary tops which are recognised by some guidebooks,Birkett, Bill: ''Complete Lakeland Fells'': Collins Willow (1994): the principal summits being Pike de Bield (2,657 ft / 810 m.), Scar Lathing (1,440 ft / 439 m.) and Throstlehow Crag (1,325 ft / 404 m.). Scar Lathing is particularly impressive, presenting sheer cliffs above a bend in the Esk. Although of minor significance Pianet Knott on the eastern side of the ridge also has a very striking appearance from lower down the valley.


Geology

Laminated volcaniclastic
claystone Mudrocks are a class of fine-grained siliciclastic sedimentary rocks. The varying types of mudrocks include siltstone, claystone, mudstone, slate, and shale. Most of the particles of which the stone is composed are less than and are too ...
s and siltstones of the Esk Pike Formation form the upper reaches, crossed by an intrusion of
andesite Andesite () is a volcanic rock of intermediate composition. In a general sense, it is the intermediate type between silica-poor basalt and silica-rich rhyolite. It is fine-grained (aphanitic) to porphyritic in texture, and is composed predo ...
and hybridized andesite porphyry.
British Geological Survey The British Geological Survey (BGS) is a partly publicly funded body which aims to advance geoscientific knowledge of the United Kingdom landmass and its continental shelf by means of systematic surveying, monitoring and research. The BGS hea ...
: 1:50,000 series maps, ''England & Wales Sheet 38'': BGS (1998)


Summit

The summit area is extremely stony, striking pale rocks being much in evidence.Richards, Mark: ''Mid-Western Fells'': Collins (2004): A series of steps rise up from Ore Gap whilst the approach from Esk Hause is rough and eroded. A small
cairn A cairn is a man-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 gd, càrn (plural ). Cairns have been and are used for a broad variety of purposes. In prehi ...
on the highest craggy outcrop marks the highest point. Esk Pike's central position above Eskdale gives it glorious views of the Scafells, with the Eastern and Northern Fells also forming a fine panorama. Derwentwater and a section of
Windermere Windermere (sometimes tautologically called Windermere Lake to distinguish it from the nearby town of Windermere) is the largest natural lake in England. More than 11 miles (18 km) in length, and almost 1 mile (1.5 km) at its wides ...
complete the scene. A little to the south, Pike de Bield provides an intimate view of the upper Esk.


Ascents

Being far from any roads, all ascents of Esk Pike involve considerable distance by Cumbrian standards. From Brotherilkeld on the Eskdale road the climber can choose between Ore Gap, Esk Hause and the south ridge, all of these options being around five and a half miles. Borrowdale gives a choice of starting points, either making for Esk Hause from Seathwaite, or Ore Gap from Stonethwaite. Access is also possible from Great Langdale, ascending Rossett Gill from the Old Hotel. Many walkers will reach the summit indirectly having climbed Bow Fell first via the Band, or perhaps climbed from Borrowdale over
Glaramara Glaramara is a fell in the English Lake District in Cumbria. It is a substantial fell that is part of a long ridge that stretches for over six kilometres from Stonethwaite in Borrowdale up to the important mountain pass of Esk Hause. T ...
and Allen Crags.


References

{{Southern Fells Hewitts of England Fells of the Lake District Nuttalls Allerdale Borough of Copeland