
Lonscale Fell is a hill 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 ...
. Its pointed second top is instantly recognisable, standing at the eastern end 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 ...
massif. The fell is easily climbed from Keswick or from Skiddaw House to the north. Although now primarily a sheep pasture, it once saw considerable mining activity beneath the long eastern wall of crag.
Topography
The long south east ridge of Skiddaw descends over
Little Man and Jenkin Hill to the depression of Flag Pots. Beyond this is the final upthrust of Lonscale Fell before the craggy descent to the Glenderaterra Beck,
The southern flanks fall gently over acres of sheep pasture in the manner of the Skiddaw range. At the base of the slope is the wooded valley of Whit Beck, separating Lonscale Fell from the east ridge of
Latrigg
Latrigg is one of the lowest fells in the Lake District in North West England, but is a popular climb due to its convenient location overlooking the town of Keswick and the beautiful views down the valley of Borrowdale from the summit. It is th ...
. Here also is Lonscale, the farm which has given its name to the
fell
A fell (from Old Norse ''fell'', ''fjall'', "mountain"Falk and Torp (2006:161).) is a high and barren landscape feature, such as a mountain or Moorland, moor-covered hill. The term is most often employed in Fennoscandia, Iceland, the Isle of M ...
. Whit Beck is a tributary of the Glenderaterra, a stream which forms the eastern boundary of Lonscale Fell. This flows due south from Skiddaw Forest between the Skiddaw massif and
Blencathra, before joining the River Greta and running on through
Keswick. The eastern face of the fell above the Glenderaterra is a scarp of crags, a singular feature in the Skiddaw range.
To the north of the fell is Skiddaw Forest. Confusingly this forest contains no trees (other than the windbreak of Skiddaw House) but is a marshy upland area at around surrounded on all sides by higher fells. Three streams flow from Skiddaw Forest, dividing the Northern Fells into three sectors. Dash Beck runs north west, the River Caldew north east and the River Glenderaterra south. The single building in Skiddaw Forest is Skiddaw House, which has variously seen service as a shepherds' bothy and a
Youth Hostel
A hostel is a form of low-cost, short-term shared sociable lodging where guests can rent a bed, usually a bunk bed in a dormitory sleeping 4–20 people, with shared use of a lounge and usually a kitchen. Rooms can be private or shared - mixe ...
.
The northern boundary of Lonscale Fell is Salehow Beck, a tributary of the River Caldew, its waters bound for 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 ...
by way of
Carlisle
Carlisle ( , ; from ) is a city in the Cumberland district of Cumbria, England.
Carlisle's early history is marked by the establishment of a settlement called Luguvalium to serve forts along Hadrian's Wall in Roman Britain. Due to its pro ...
. Beyond the river is
Great Calva
Great Calva is a fell in the Lake District, England. It is in the Northern Fells, lying roughly at the centre of this region of high ground. As a result, it is distant from roads and quite remote by Lakeland standards. Great Calva stands at ...
, the first of the Back o'Skiddaw fells. The feeders of Salehow Beck and Whit Beck flow from the
col of Flag Pots, completing the western boundary.
Geology
In common with much of the
Northern Fells the Kirk Stile Formation of the Skiddaw Group predominates. This is composed of 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 ...
with
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 and is 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 ...
age.
[British Geological Survey: 1:50,000 series maps, ''England & Wales Sheet 29'': BGS (1999)]
The Glenderaterra valley was the scene of some mining activity in the nineteenth century. The northern workings were first named Glenderaterra Mine and later Brundholme Mine. These were driven primarily for
lead
Lead () is a chemical element; it has Chemical symbol, symbol Pb (from Latin ) and atomic number 82. It is a Heavy metal (elements), heavy metal that is density, denser than most common materials. Lead is Mohs scale, soft and Ductility, malleabl ...
, but also
copper
Copper is a chemical element; it has symbol Cu (from Latin ) and atomic number 29. It is a soft, malleable, and ductile metal with very high thermal and electrical conductivity. A freshly exposed surface of pure copper has a pinkish-orang ...
ore and
baryte
Baryte, barite or barytes ( or ) is a mineral consisting of barium sulfate (Ba S O4). Baryte is generally white or colorless, and is the main source of the element barium. The ''baryte group'' consists of baryte, celestine (strontium sulfate), ...
. The returns were never economic, the mine being abandoned in 1920. A little to the south was Blencathra Mine, worked unsuccessfully until about 1880.
[Adams, John: ''Mines of the Lake District Fells'': Dalesman (1995) ] There are also some abandoned quarries below the eastern crags.
Summit
The highest point lies on a gentle dome on the western side of the fell. The prominent peaked top visible from below lies to the east at a height of . This is referred to as Lonscale Pike by some guidebooks.
[Birkett, Bill: ''Complete Lakeland Fells'': Collins Willow (1994): ] The watershed between the Greta to the south and the Caldew to the north actually bypasses both of these tops, following the north eastern ridge of Burnt Horse over a top at and then onward to
Mungrisdale Common
Mungrisdale Common, pronounced ''mun-grize-dl'', with emphasis on ''grize'', is a fell in the English Lake District. Although Alfred Wainwright listed it as one of the 214 featured hills in his influential ''Pictorial Guide to the Lakeland Fel ...
, an outlier of Blencathra.
The highest point bears 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 ...
from which a fine Lakeland panorama is displayed southward.
Thirlmere
Thirlmere is a reservoir in the Cumberland (unitary authority), Cumberland district in Cumbria and the English Lake District National Park, Lake District. The Helvellyn ridge lies to the east of Thirlmere. To the west of Thirlmere are a numbe ...
and
Derwentwater
Derwentwater, or Derwent Water, is a lake in the Lake District in North West England, immediately south of Keswick, Cumbria, Keswick. It is in the unitary authority of Cumberland (unitary authority), Cumberland within the ceremonial county of ...
are seen along with all of the major fell groupings. To the other points of the compass the northern fells intervene, close up but less inspiring.
[ Wainwright, Alfred: '']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 5 The Northern Fells'':
Ascents
From Keswick, or as a labour saving alternative from the Gale Road car park behind Latrigg, a number of routes present themselves. Flag Pots can be reached from the tourist route to Skiddaw, or a direct line can be taken up the southern slopes. Another possibility is to follow the southern edge of Lonscale Crags, and the final (and longest) option is to contour right around the fell up the Glenderaterra and outflank it from behind.
From the Glenderaterra, or from Skiddaw House, the climber can make use of either the Burnt Horse Ridge, or a direct scramble up the buttress to reach Lonscale Pike.
References
{{Northern Fells
Fells of the Lake District
Nuttalls
Hewitts of England