Great Borne

Great Borne is a fell in the English Lake District with a height of 616 m (2,021 ft). It is a rather secluded hill situated at the western end of the long ridge which divides the Ennerdale and Buttermere valleys.

Great Borne
Great Borne seen from near the western end of Ennerdale Water.
Highest point
Elevation616 m (2,021 ft)
Prominence113 m (371 ft)
Parent peakHigh Stile
ListingHewitt, Nuttall, Wainwright
Coordinates54°32′04″N 3°21′25″W 
Geography
Great Borne
Great Borne
Location in Allerdale, Cumbria
Great Borne
Location in Copeland, Cumbria
LocationCumbria, England
Parent rangeLake District, Western Fells
OS gridNY124163
Topo mapOS Landranger 89, OS Explorer 4

Name

The name Great Borne only really applies to the fell's summit area with most West Cumbrians actually referring to the fell as Herdus. However Bill Birkett in his Complete Lakeland Fells gives Great Borne and Herdus the status of separate fells, with Herdus’ summit standing half a kilometre west of Great Borne with an altitude 562 m (1,844 ft). The meaning of Great Borne translates from the French language meaning "Great Boundary" as in the 13th century the fell denoted the edge of the Loweswater forest, an alternative meaning has been put forward as "Great Stream" from the southern Old English language with bourne meaning a stream flowing from a spring.

Topography and geology
The subsidiary top of Bowness Knott, seen from Crag Fell

Great Borne's southern slopes are of some interest, they fall away precipitously towards Ennerdale Water with steep crags and scree which are composed of pink granophyre rock which give these slopes a reddish tinge (see picture). Approximately halfway between Great Borne and the part of the fell labelled Herdus on the 1:50,000 O.S. map is the boundary between the Skiddaw Group and the Ennerdale Granophyre intrusion.[1]

The outlying low summit of Bowness Knott (333 m (1,093 ft)) also lies to the south. It is a geological Site of Special Scientific Interest (SSSI), showing the granophyre in contact with Skiddaw Slate.[2] Bowness Knott gives good views of Ennerdale Water and is an easy climb from the car park which lies at its foot. Historians have also found evidence of an old (possibly Middle Ages) field system on the lower southern slopes of Great Borne below the crags and scree. The northern flanks of the fell descend to the Floutern Pass, a pedestrian route between Ennerdale and Buttermere. To the east Great Borne is connected to the neighbouring fell of Starling Dodd by a ridge, while the western slopes descend quickly to the low ground of the west Cumbrian plain.

Ascents

Great Borne is customarily climbed from the Ennerdale side of the fell, with the car park beneath Bowness Knott being the usual starting point. The route follows Rake Beck for a short distance and skirts the Herdus crags on the eastern side to gain the summit. An ascent using the Floutern Pass is not recommended as the top of the pass is very boggy and the route rather circuitous. The route described in the Wainwright series of guidebooks is currently challenged by a nearby farmer Mr Ireland who has a strong antipathy to walkers and the National Park.

Summit

The summit of the fell has two separate tops divided by a shallow valley, the south top is slightly higher and is marked by an Ordnance Survey trig point and a considerable wind shelter while the northern top has a large cairn which is visible for miles around and gives extensive views of the Loweswater Fells. This large cairn is thought to be the boundary marker from which the fell takes its name.

  • Great Borne seen from Ennerdale Water
  • South face of Great Borne
  • Great Borne from Crag Fell
  • Rake Beck on Great Borne

References
  1. The Geology of the Whitehaven and Workington district. T. Eastwood et al. pub. HMSO. 1931. page 49.
  2. "Bowness Knott SSSI".
This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.