Cold Pike is a
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 moor-covered hill. The term is most often employed in Fennoscandia, Iceland, the Isle of Man, pa ...
in the English
Lake District. It is a satellite of
Crinkle Crags
Crinkle Crags is a fell in the English Lake District in the county of Cumbria. It forms part of two major rings of mountains, surrounding the valleys of Great Langdale and Upper Eskdale. The name reflects the fell's physical appearance ...
and stands above the Upper
Duddon Valley
The Duddon Valley is a valley in the southern Lake District National Park in Cumbria, England. The River Duddon flows through the valley, rising in the mountains between Eskdale and Langdale, before flowing into the Irish Sea near Broughton i ...
.
Topography
When travelling clockwise,
Crinkle Crags
Crinkle Crags is a fell in the English Lake District in the county of Cumbria. It forms part of two major rings of mountains, surrounding the valleys of Great Langdale and Upper Eskdale. The name reflects the fell's physical appearance ...
is the last of the high cirque of fells forming the head of upper Eskdale. It sends out a trio of ridges to the south, running parallel like the prongs of a trident. Working from the west these ridges culminate in
Hard Knott
Hard Knott is a fell in the English Lake District, at the head of Eskdale.
Geology
Rhyolitic lava-like tuff of the Bad Step Tuff forms the summit rocks with the dacitic lapilli-tuffs of the Lincomb Tarns Formation to the north west. Bord ...
, Little Stand and Cold Pike. The Cold Pike ridge begins indistinctly in an area of rocky knolls and small
tarns beneath the Fifth Crinkle. Gradually gaining definition it descends to a broad grassy saddle before rising again to the summit plateau of Cold Pike. To the north of the saddle is Great Knott (2,283 ft). This top is considered by most guidebooks to be a subsidiary of Crinkle Crags rather than the nearer Cold Pike.
Alfred Wainwright
Alfred Wainwright MBE (17 January 1907 – 20 January 1991), who preferred to be known as A. Wainwright or A.W., was a British fellwalker, guidebook author and illustrator. His seven-volume ''Pictorial Guide to the Lakeland Fells'', published ...
: ''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 4: [Richards, Mark: ''Mid-Western Fells'': Collins (2004): ] Beyond the summit the ridge continues for another half mile south eastward before falling steeply over the many tiered crags of Wrynose Breast.
Wrynose Breast stands above the nascent Duddon and the
Wrynose Pass
The Wrynose Pass is a mountain pass in the Lake District National Park in Cumbria, England between the Duddon Valley and Little Langdale.
Etymology
The unusual name of the pass is taken from that of the adjacent Wrynose hill, also called Wryn ...
road, which provides the only vehicular link between central Lakeland and the Duddon Valley. Together with
Hardknott Pass
Hardknott Pass is a hill pass between Eskdale and the Duddon Valley in the Lake District National Park, Cumbria, England. The tarmac-surfaced road, which is the most direct route from the central Lake District to West Cumbria, shares the ti ...
to the west, Wrynose is the latest incarnation of the
Roman
Roman or Romans most often refers to:
*Rome, the capital city of Italy
*Ancient Rome, Roman civilization from 8th century BC to 5th century AD
* Roman people, the people of ancient Rome
*'' Epistle to the Romans'', shortened to ''Romans'', a lett ...
road from
Ambleside
Ambleside is a town and former civil parish, now in the parish of Lakes, in Cumbria, in North West England.
Historically in Westmorland, it marks the head (and sits on the east side of the northern headwater) of Windermere, England's largest n ...
to the port of
Ravenglass
Ravenglass is a coastal village in the Copeland District in Cumbria, England. It is between Barrow-in-Furness and Whitehaven. Historically in Cumberland, it is the only coastal village in the Lake District National Park. It is located at the e ...
.
To the west of Cold Pike is the Gaitscale Beck, the watercourse separating it from Little Stand. To the east across a wide low
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 ...
is
Pike of Blisco
Pike of Blisco, or Pike o' Blisco, is a mountain in the Lake District in Cumbria, England. Located between the valleys of Great Langdale and Little Langdale, its relative isolation from neighbouring fells together with slopes falling away imme ...
, a conical fell with its footing firmly in
Langdale. The source of the River Duddon flows south from this col, curving westward around the foot of Wrynose Breast. To the north is Red Tarn, a feeder via Oxendale of
Great Langdale
Great Langdale is a valley in the Lake District National Park in North West England, the epithet Great distinguishing it from the neighbouring valley of Little Langdale. Langdale is also the name of a valley in the Howgill Fells, elsewhere i ...
Beck. Red Tarn is an elongated pool whose stony bed can be seen through clear shallow waters, reputed to hold trout.
[Blair, Don: ''Exploring Lakeland Tarns'': Lakeland Manor Press (2003): ] It forms a focal point for walkers as the wide path from the summit of Wrynose Pass down to Stool End runs beside it, a further path branching off across the outflow to Crinkle Crags.
Geology
The fell top is composed of
dacite
Dacite () is a volcanic rock formed by rapid solidification of lava that is high in silica and low in alkali metal oxides. It has a fine-grained ( aphanitic) to porphyritic texture and is intermediate in composition between andesite and rhy ...
lava
Lava is molten or partially molten rock ( magma) that has been expelled from the interior of a terrestrial planet (such as Earth) or a moon onto its surface. Lava may be erupted at a volcano or through a fracture in the crust, on land or ...
flows with the
volcaniclastic
Volcaniclastics are geologic materials composed of broken fragments (clasts) of volcanic rock. These encompass all clastic volcanic materials, regardless of what process fragmented the rock, how it was subsequently transported, what environment it ...
sandstone
Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks.
Most sandstone is composed of quartz or feldspar (both silicates ...
s and
tuff
Tuff is a type of rock made of volcanic ash ejected from a vent during a volcanic eruption. Following ejection and deposition, the ash is lithified into a solid rock. Rock that contains greater than 75% ash is considered tuff, while rock ...
s of the Blisco Member outcropping to the south.
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 he ...
: 1:50,000 series maps, ''England & Wales Sheet 38'': BGS (1998)
The main Red Tarn path was originally made to serve Red Crag Mine. This consists of a series of pits and trial borings for
iron
Iron () is a chemical element with symbol Fe (from la, ferrum) and atomic number 26. It is a metal that belongs to the first transition series and group 8 of the periodic table. It is, by mass, the most common element on Earth, right in ...
, concentrated about 300 yards north of the tarn. It was worked from 1860 to 1875 but never achieved commercial success.
[Adams, John: ''Mines of the Lake District Fells'': Dalesman (1995) ]
Summit
The summit plateau of Cold Pike has three widely separated summits, all of which are listed as
nuttalls Nuttall may refer to:
People
* Nuttall (name)
* Nuttall baronets
Nature
* Nuttall's oak, a fast-growing large deciduous oak tree native to North America
* Nuttall's woodpecker, a species of woodpecker found in oak woodlands of California
* Nu ...
. The lower two are unnamed on
Ordnance Survey
Ordnance Survey (OS) is the national mapping agency for Great Britain. The agency's name indicates its original military purpose (see ordnance and surveying), which was to map Scotland in the wake of the Jacobite rising of 1745. There was ...
maps, but are generally referred to as Cold Pike West Top and Cold Pike Far West Top.
[Nuttall, John & Anne: ''The Mountains of England & Wales - Volume 2: England'' (2nd edition): Cicerone (1990): ] The true summit is itself one of a series of three outcrops in a mild echoing of Crinkle Crags. Each has a
cairn, the highest being a fine example. The top is an excellent place from which to survey Crinkle Crags, the
Langdale Pikes, and the northern end of the Coniston Fells across Wrynose Bottom; there is a fine distant prospect of the
Pennines
The Pennines (), also known as the Pennine Chain or Pennine Hills, are a range of uplands running between three regions of Northern England: North West England on the west, North East England and Yorkshire and the Humber on the east. Commonly ...
above
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 ...
, and
Morecambe Bay
Morecambe Bay is a large estuary in northwest England, just to the south of the Lake District National Park. It is the largest expanse of intertidal mudflats and sand in the United Kingdom, covering a total area of . In 1974, the second large ...
above the
Duddon Valley
The Duddon Valley is a valley in the southern Lake District National Park in Cumbria, England. The River Duddon flows through the valley, rising in the mountains between Eskdale and Langdale, before flowing into the Irish Sea near Broughton i ...
.
Panorama
Ascents
Cold Pike can be reached easily via Red Tarn from the carpark at the summit of Wrynose Pass. It can also be climbed (less easily) from Great Langdale. More ‘honest’ walkers beginning in the south may wish to start from
Little Langdale or Wrynose Bottom, first ascending Wrynose Pass. A direct route from Wrynose Bottom is also possible although pathless, skirting around the left of the crags. A consideration here is that the Duddon will need to be forded when starting out.
Cold Pike is often seen as a worthwhile detour ''en route'' to Crinkle Crags.
References
{{Southern Fells
Hewitts of England
Fells of the Lake District
Nuttalls
Borough of Copeland
South Lakeland District