High Raise (Langdale)

Coordinates: 54°28′34″N 3°06′47″W / 54.476°N 3.113°W / 54.476; -3.113
Source: Wikipedia, the free encyclopedia.

High Raise
Nuttall
Coordinates54°28′34″N 3°06′47″W / 54.476°N 3.113°W / 54.476; -3.113
Geography
LocationCumbria, England
Parent rangeLake District, Central Fells
OS gridNY280095
Topo mapOS Explorer OL6
Listed summits
of High Raise (Langdale)
Name Grid ref Height Status
Codale Head NY288090 730 m Nuttall

High Raise is a fell in the Central Fells of the English Lake District, not to be confused with another High Raise situated in the Far Eastern Fells. High Raise is one of the most spectacular mountains in the district; with a height of 762 metres (2,500 ft) it is the highest point in the central fells of Lakeland.

High Raise is in fact commonly regarded as the most central mountain in the district and this position gives a fine viewpoint to admire the surrounding mountains and beyond. All of England's 3,000-foot (910-metre) mountains (

Three Peaks in the Yorkshire Dales at 37 miles (60 km) and Morecambe Bay
at 25 miles (40 km).

Summit

The summit itself, which is also known as High White Stones due to a smattering of grey boulders in the vicinity of the highest point, has an

column and a large cairn which also doubles as a wind shelter; a ruined fence also crosses the summit plateau.[1][2]

The view is extensive as befits the central location with all major fell groups visible. The only disappointment being the

Langdale Pikes, which seen from behind lack most of their distinctiveness. No lakes are seen other than short sections of Bassenthwaite Lake and Derwentwater.[1]

Ascents

Ascents of High Raise are usually done from Stonethwaite in Borrowdale or the New Dungeon Ghyll Hotel in Great Langdale, although routes are also viable from Grasmere and Thirlmere. The Stonethwaite approach gives the walker a chance to climb the neighbouring fell of Ullscarf, while the route from Great Langdale allows visits to the splendid Langdale Pikes either before or after climbing High Raise.[1][2]

Topography

The fell is the meeting-point of many

High Seat towards the low fells above Keswick. South-eastward the spine continues over Blea Rigg and Silver How, terminating at Loughrigg Fell above Grasmere and Rydal Water
.

To the east there are a number of subsidiary ridges, diverging from

Langdale Pikes
. These picturesque craggy heights form the parapet of High Raise's southern plateau, standing atop the valley wall and the centrepiece of many views.

Geology

High White Stones is an outcrop of the Lincomb Tarns Formation. This consists of

volcaniclastic sandstone. These rocks are overlain by till over the rest of the summit area.[3]

References

  1. ^ a b c d Wainwright, A (1958). A Pictorial Guide to the Lakeland Fells, Book 3 The Central Fells. Westmorland Gazette.
  2. ^
  3. ^ British Geological Survey 1:50,000 series maps: Sheet 38: BGS (1998)