Blake Fell
Encyclopedia
Blake Fell is a hill
in the Western part of the English
Lake District
. It is the highest point of the Loweswater Fells, an area of low grassy hills with steep sides overlooking the lake of Loweswater
. The fell also overlooks the village of Loweswater
, from which it can be climbed. An alternative route is from the Cogra Moss reservoir on its western slopes. Because the Loweswater Fells are a separate geographical unit, Blake Fell is a Marilyn
. It is located in the Parish of Lamplugh
.
occupy a triangular sector of the Lake District, bordered by the River Cocker to the north east and Wasdale
to the south east. Westwards the hills diminish toward the coastal plain of Cumberland. At the central hub of the high country are Great Gable
and its satellites, while two principal ridges fan out on either flank of Ennerdale
, the western fells in effect being a great horseshoe around this long wild valley. Blake Fell and the other Loweswater Fells form the extremity of the northern arm.
The Loweswater Fells have been compared to the digits of a hand, radiating out south westward from the "palm" centred on Loweswater village. From the west these are Burnbank Fell
, Blake Fell, Gavel Fell
, Hen Comb
and Mellbreak
, the "thumb".
Blake Fell is the highest hill in this group, the summit area being a long ridge running southwest along the "finger". This begins above the shore of Loweswater, rising steeply through the mixed forestry of Holme Wood to the craggy height of Loweswater End. Atop the rise is Carling Knott (1,784 ft), the north eastern summit. The ridge then dips slightly, the landscape changing from rock outcrop to grass, before the final ascent to Blake Fell. A transverse ridge now connects northwards to Burnbank Fell, in truth an outlier of Blake Fell, but given separate status by Alfred Wainwright
in his influential Pictorial Guide to the Lakeland Fells
. Southward is the narrow grassy col
of Fothergill Head, providing a much more tenuous link to Gavel Fell. The western slopes are heavily wooded with conifers and contoured by forest roads.
In addition to Carling Knott, Blake Fell has a number of other subsidiary tops. Descending south west from the summit are High Pen (1,558 ft), Low Pen (1,427 ft), Godworth (1,197 ft) and Kelton Fell (1,020 ft). Beyond lie the Croasdale road and the West Cumberland plain. Standing aloof from these tops, but still within Blake Fell's orbit, is Knock Murton (1,467 ft). This is a steep sided fell, forested on the western flank and with sufficient prominence that it is only barely excluded from the list of Marilyns
in its own right. Blake Fell also extends a western ridge over the prominent top of Sharp Knott (1,581 ft) and the wooded High Howes (1,027 ft), falling gently to the village of Lamplugh. These tops are recognised in some guidebooks.
Drainage from the western slopes flows via Sharp Knott Gill and Fother Gill to Cogra Moss
. This is a reservoir sitting in the deep valley between Blake Fell and Knock Murton, a reed rimmed waterbody held back by a substantial dam at the western end. Also known as Arlecdon Reservoir, it has a depth of around 30 feet. The waters from this flank of the fell join the River Marron and ultimately the Derwent. The eastern face of Blake Fell flows either to Loweswater or to its outfall, ensuring that all of the drainage eventually runs to the River Derwent.
and siltstone
typical of the Skiddaw
fells. The rougher terrain of Carling Knott is an outcropping of the underlying Loweswater Formation, composed of greywacke
sandstone
turbidities.
Knock Murton and Kelton Fell bear the scars of mining activity, having been the site of extensive haematite workings. Between 1853 and their closure in 1914 these mines produced anything up to 60,000 tons of ore per year. A railway, the Rowrah and Kelton Fell Line, was built up the valley between the two hills, the line of which can still be traced. A further working, the Croasdale Iron Mine, operated to the south of Kelton Fell.
, the meeting point of paths from the various ridges. Westwards there is no higher ground to interrupt the sea view. To the east is a fine array of hills stretching from Binsey
in the north to Grike
in the south. The North Western Fells
across Crummock Water
are particularly fine, although much better seen from Loweswater End.
Hill
A hill is a landform that extends above the surrounding terrain. Hills often have a distinct summit, although in areas with scarp/dip topography a hill may refer to a particular section of flat terrain without a massive summit A hill is a landform that extends above the surrounding terrain. Hills...
in the Western part of the English
England
England is a country that is part of the United Kingdom. It shares land borders with Scotland to the north and Wales to the west; the Irish Sea is to the north west, the Celtic Sea to the south west, with the North Sea to the east and the English Channel to the south separating it from continental...
Lake District
Lake District
The Lake District, also commonly known as The Lakes or Lakeland, is a mountainous region in North West England. A popular holiday destination, it is famous not only for its lakes and its mountains but also for its associations with the early 19th century poetry and writings of William Wordsworth...
. It is the highest point of the Loweswater Fells, an area of low grassy hills with steep sides overlooking the lake of Loweswater
Loweswater
Loweswater is one of the smaller lakes in the English Lake District. The village of Loweswater is situated at the foot of the lake.The lake is not far from Cockermouth and is also easily reached from elsewhere in West Cumbria. The group of fells to the south of Loweswater is known as the Loweswater...
. The fell also overlooks the village of Loweswater
Loweswater, Cumbria
Loweswater is a village and civil parish in the county of Cumbria, England.-Village:The village lies between the Lake District lakes of Loweswater and Crummock Water, about south of Cockermouth and within the Lake District National Park...
, from which it can be climbed. An alternative route is from the Cogra Moss reservoir on its western slopes. Because the Loweswater Fells are a separate geographical unit, Blake Fell is a Marilyn
Marilyn (hill)
A Marilyn is a mountain or hill in the United Kingdom, Republic of Ireland or Isle of Man with a relative height of at least 150 metres , regardless of absolute height or other merit...
. It is located in the Parish of Lamplugh
Lamplugh
Lamplugh is a scattered community and civil parish located in west Cumbria on the edge of the English Lake District. It is the starting point for a number of walks, and is on the Sea to Sea / C2C / Coast to Coast Cycle Route....
.
Topography
The Western FellsWestern Fells
The Western Fells are a group of hills in the English Lake District. Centred on Great Gable they occupy a triangular area between Buttermere and Wasdale...
occupy a triangular sector of the Lake District, bordered by the River Cocker to the north east and Wasdale
Wasdale
Wasdale is a valley and civil parish in the western part of the Lake District National Park in Cumbria, England. The River Irt flows through the valley to its estuary at Ravenglass. A large part of the main valley floor is occupied by Wastwater, the deepest lake in England...
to the south east. Westwards the hills diminish toward the coastal plain of Cumberland. At the central hub of the high country are Great Gable
Great Gable
Great Gable is a mountain lying at the very heart of the English Lake District, appearing as a pyramid from Wasdale , but as a dome from most other directions. It is one of the most popular of the Lakeland fells, and there are many different routes to the summit...
and its satellites, while two principal ridges fan out on either flank of Ennerdale
Ennerdale
Ennerdale may refer to:* Ennerdale, Gauteng, a suburb of Johannesburg, South Africa* Ennerdale Water, a lake in the Lake District in England**Ennerdale Bridge, a nearby settlement...
, the western fells in effect being a great horseshoe around this long wild valley. Blake Fell and the other Loweswater Fells form the extremity of the northern arm.
The Loweswater Fells have been compared to the digits of a hand, radiating out south westward from the "palm" centred on Loweswater village. From the west these are Burnbank Fell
Burnbank Fell
Burnbank Fell is a small hill in the west of the English Lake District. It is the most westerly of the Loweswater Fells, a group of low grassy hills lying just south of Loweswater. The hill is predominantly grassy with sprawling flanks and a broad ridge connecting it to Blake Fell...
, Blake Fell, Gavel Fell
Gavel Fell
Gavel Fell is a hill in the English Lake District. Centremost of the five Loweswater Fells in the western part of the District, it stands between Hen Comb and Blake Fell...
, Hen Comb
Hen Comb
Hen Comb is a fell in the west of the English Lake District. One of the Loweswater Fells it lies to the south of Loweswater lake and Loweswater village...
and Mellbreak
Mellbreak
Mellbreak is a hill in the Western part of the English Lake District. Despite being surrounded on all sides by higher fells , it stands in isolation. It is surrounded on three sides by a 'moat' of deep marshy land, and on the east side by the lake of Crummock Water...
, the "thumb".
Blake Fell is the highest hill in this group, the summit area being a long ridge running southwest along the "finger". This begins above the shore of Loweswater, rising steeply through the mixed forestry of Holme Wood to the craggy height of Loweswater End. Atop the rise is Carling Knott (1,784 ft), the north eastern summit. The ridge then dips slightly, the landscape changing from rock outcrop to grass, before the final ascent to Blake Fell. A transverse ridge now connects northwards to Burnbank Fell, in truth an outlier of Blake Fell, but given separate status by Alfred Wainwright
Alfred Wainwright
Alfred Wainwright MBE was a British fellwalker, guidebook author and illustrator. His seven-volume Pictorial Guide to the Lakeland Fells, published between 1955 and 1966 and consisting entirely of reproductions of his manuscript, has become the standard reference work to 214 of the fells of the...
in his influential Pictorial Guide to the Lakeland Fells
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 of the Lake District in northwest England...
. Southward is the narrow grassy col
Mountain pass
A mountain pass is a route through a mountain range or over a ridge. If following the lowest possible route, a pass is locally the highest point on that route...
of Fothergill Head, providing a much more tenuous link to Gavel Fell. The western slopes are heavily wooded with conifers and contoured by forest roads.
In addition to Carling Knott, Blake Fell has a number of other subsidiary tops. Descending south west from the summit are High Pen (1,558 ft), Low Pen (1,427 ft), Godworth (1,197 ft) and Kelton Fell (1,020 ft). Beyond lie the Croasdale road and the West Cumberland plain. Standing aloof from these tops, but still within Blake Fell's orbit, is Knock Murton (1,467 ft). This is a steep sided fell, forested on the western flank and with sufficient prominence that it is only barely excluded from the list of Marilyns
Marilyn (hill)
A Marilyn is a mountain or hill in the United Kingdom, Republic of Ireland or Isle of Man with a relative height of at least 150 metres , regardless of absolute height or other merit...
in its own right. Blake Fell also extends a western ridge over the prominent top of Sharp Knott (1,581 ft) and the wooded High Howes (1,027 ft), falling gently to the village of Lamplugh. These tops are recognised in some guidebooks.
Drainage from the western slopes flows via Sharp Knott Gill and Fother Gill to Cogra Moss
Cogra Moss
Cogra Moss is a shallow reservoir to the east of the village of Lamplugh on the western edge of the English Lake District. It was created by the damming of Rakegill Beck in about 1880 though its function as a water supply ceased in 1975. The reservoir which is surrounded by forestry plantations on...
. This is a reservoir sitting in the deep valley between Blake Fell and Knock Murton, a reed rimmed waterbody held back by a substantial dam at the western end. Also known as Arlecdon Reservoir, it has a depth of around 30 feet. The waters from this flank of the fell join the River Marron and ultimately the Derwent. The eastern face of Blake Fell flows either to Loweswater or to its outfall, ensuring that all of the drainage eventually runs to the River Derwent.
Geology and Mining
The summit of Blake Fell is representative of the Kirkstile Formation, laminated mudstoneMudstone
Mudstone is a fine grained sedimentary rock whose original constituents were clays or muds. Grain size is up to 0.0625 mm with individual grains too small to be distinguished without a microscope. With increased pressure over time the platey clay minerals may become aligned, with the...
and siltstone
Siltstone
Siltstone is a sedimentary rock which has a grain size in the silt range, finer than sandstone and coarser than claystones.- Description :As its name implies, it is primarily composed of silt sized particles, defined as grains 1/16 - 1/256 mm or 4 to 8 on the Krumbein phi scale...
typical of the Skiddaw
Skiddaw
Skiddaw is a mountain in the Lake District National Park in England. With a summit at 931 m above sea level it is the fourth highest mountain in England. It lies just north of the town of Keswick, Cumbria, and dominates the skyline in this part of the northern lakes...
fells. The rougher terrain of Carling Knott is an outcropping of the underlying Loweswater Formation, composed of greywacke
Greywacke
Greywacke or Graywacke is a variety of sandstone generally characterized by its hardness, dark color, and poorly sorted angular grains of quartz, feldspar, and small rock fragments or lithic fragments set in a compact, clay-fine matrix. It is a texturally immature sedimentary rock generally found...
sandstone
Sandstone
Sandstone is a sedimentary rock composed mainly of sand-sized minerals or rock grains.Most sandstone is composed of quartz and/or feldspar because these are the most common minerals in the Earth's crust. Like sand, sandstone may be any colour, but the most common colours are tan, brown, yellow,...
turbidities.
Knock Murton and Kelton Fell bear the scars of mining activity, having been the site of extensive haematite workings. Between 1853 and their closure in 1914 these mines produced anything up to 60,000 tons of ore per year. A railway, the Rowrah and Kelton Fell Line, was built up the valley between the two hills, the line of which can still be traced. A further working, the Croasdale Iron Mine, operated to the south of Kelton Fell.
Summit and View
The summit is a grassy dome decorated with a large cairnCairn
Cairn is a term used mainly in the English-speaking world for a man-made pile of stones. It comes from the or . Cairns are found all over the world in uplands, on moorland, on mountaintops, near waterways and on sea cliffs, and also in barren desert and tundra areas...
, the meeting point of paths from the various ridges. Westwards there is no higher ground to interrupt the sea view. To the east is a fine array of hills stretching from Binsey
Binsey
Binsey is a hill on the northern edge of the Lake District in Cumbria, England. It is detached from the rest of the Lakeland hills, and thus provides a good spot to look out at the Northern and North Western Fells of the Lake District, as well as the coastal plain and, across the Solway Firth,...
in the north to Grike
Grike (Lake District)
Grike is a hill in the west of the English Lake District, near Ennerdale Water. It is part of the Lank Rigg group, the most westerly Wainwright as the fells diminish toward the coastal plain...
in the south. The North Western Fells
North Western Fells
The North Western Fells are a group of hills in the English Lake District. Including such favourites as Catbells and Grisedale Pike, they occupy an oval area beneath the Buttermere and Borrowdale valley systems...
across Crummock Water
Crummock Water
Crummock Water is a lake in the Lake District in Cumbria, North West England situated between Buttermere to the south and Loweswater to the north. Crummock Water is two and a half miles long, three quarters of a mile wide and 140ft deep. The River Cocker is considered to start at the north of the...
are particularly fine, although much better seen from Loweswater End.