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Mellbreak is a hill in the Western part of the English
Lake District The Lake District, also known as the Lakes or Lakeland, is a mountainous region in North West England. A popular holiday destination, it is famous for its lakes, forests, and mountains (or ''fells''), and its associations with William Wordswor ...
. Despite being surrounded on all sides by higher fells (the
Loweswater Fells Loweswater is a village and civil parish in the county of Cumbria, England. Village Historically part of Cumberland, the village lies between the Lake District lakes of Loweswater and Crummock Water, about south of Cockermouth and within the La ...
, the High Stile Ridge and the
Grasmoor Grasmoor is a mountain in the north-western part of the Lake District, northern England. It is the highest peak in a group of hills between the villages of Lorton, Braithwaite and Buttermere, and overlooks Crummock Water. Grasmoor is distingui ...
Group), it stands in isolation. It is surrounded on three sides by a "
moat A moat is a deep, broad ditch, either dry or filled with water, that is dug and surrounds a castle, fortification, building or town, historically to provide it with a preliminary line of defence. In some places moats evolved into more extensive ...
" of deep marshy land, and on the east side by the lake of Crummock Water. The fell forms a partnership with the lake, running parallel to it, falling sheer into it, and regularly providing the backdrop for pictures of it.


Name

Mellbreak's name is derived from differing sources: the
Celtic Celtic, Celtics or Keltic may refer to: Language and ethnicity *pertaining to Celts, a collection of Indo-European peoples in Europe and Anatolia **Celts (modern) *Celtic languages **Proto-Celtic language * Celtic music *Celtic nations Sports Fo ...
"moel", meaning "bare hill", and the later Old Norse of the Vikings, "brekka", which means a hill slope.


Topography

The
Western 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. The Western Fells are characterised by high ridges and an abundance of naked rock. Partitio ...
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. Alfred Wainwright: ''A Pictorial Guide to the Lakeland Fells, Volume 7 The Western Fells'': Westmorland Gazette (1966): Mellbreak 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 Loweswater is one of the smaller lakes in the English Lake District. The village of Loweswater is situated to the east of the lake. Geography The lake is not far from Cockermouth and is also easily reached from elsewhere in West Cumbria. ...
village. From the west these are
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 just south of Loweswater. It is predominantly grassy, with sprawling flanks and a broad ridge co ...
, Blake 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. Of moderate altitude it can be climbed from Loweswater village, or from Cr ...
,
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. Although of only moderate height, its ascent can be difficult as it is largely surrounded by ...
and Mellbreak, the "thumb". To continue the hand metaphor, the opposing thumb of Mellbreak is the tenuous northern extremity of
Starling Dodd Starling Dodd is a fell in the western part of the English Lake District, located between the valleys of Ennerdale and Buttermere, on the ridge between Great Borne to its west and Red Pike to its east. Not visible from Buttermere and rounded in ...
, whilst the other Loweswater Fells are satellites of
Great Borne Great Borne is a fell in the English Lake District with a height of . It is a rather secluded hill situated at the western end of the long ridge which divides the Ennerdale and Buttermere valleys. Name The name Great Borne only really applies t ...
. The fell has been likened (by Alfred Wainwright and others) to the shape of an upturned boat, having north and south tops of roughly equal height and a wide flat depression in between. On the eastern side the steep slopes run down directly to the shore of Crummock Water. Low Ling Crag, a rocky projection into the lake, is a continuation of outcrops higher up. Other crags rim the depression between the two tops. The southern boundary is formed by Scale Beck and its tributary Black Beck. Mellbreak has a third much lower top overlooking this steep sided valley, Scale Kott (1,109 ft). At the head of Black Beck is the connection to Starling Dodd, running south west from Scale Knott. This could hardly be considered a ridge in walking terms, since it begins at the foot of an 800 ft scree slope on the northern flank of Starling Dodd. To the west of Mellbreak is the marshy valley of Mosedale, its beck flowing north to Loweswater village. On the other side is the parallel ridge of Hen Comb. The northern end of Mellbreak rises direct from the valley behind the village, precipitous like a sand castle on a flat beach. From this vantage point its steep gabled profile is an arresting sight. The successive rock tiers of White, Dropping and Raven Crags complete the picture.


Geology

Mellbreak is formed primarily from the 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 (parallel layering).Blatt, H., and R.J. Tracy, 1996, ''Petrology. ...
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.Blatt ''et al.'' 1980, p ...
of the Kirkstile Formation. There is an intrusion of basalt on the Crummock face and the southern end around Scale Knott exhibit the Buttermere Formation. This is an olistostrome of disrupted, sheared and folded mudstone, siltstone and sandstone. The rocks of Hen Comb are of the Kirkstile Formation, 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 (parallel layering).Blatt, H., and R.J. Tracy, 1996, ''Petrology. ...
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.Blatt ''et al.'' 1980, p ...
, often associated with the
Skiddaw Skiddaw is a mountain in the Lake District National Park in England. Its summit is the sixth-highest in England. It lies just north of the town of Keswick, Cumbria, and dominates the skyline in this part of the northern lakes. It is the ...
group.
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 h ...
: 1:50,000 series maps, ''England & Wales Sheet 29'': BGS (1999)
There are two small trials for iron, one on each side of the fell. Neither penetrates for more than a few feet.Adams, John: ''Mines of the Lake District Fells'': Dalesman (1995)


Summit

Although the south top is slightly higher, at 512 m (1,680 ft) it is the north top (509 m, 1,670 ft) that is the better summit, being rocky and situated on the top of the crags that make up the north face of the fell. Both carry substantial
cairn A cairn is a man-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 gd, càrn (plural ). Cairns have been and are used for a broad variety of purposes. In prehis ...
s, that of the true summit being on grass. The views are good from both summits, a consequence of Mellbreak's isolation and great relative height. The north top brings the Solway Firth into view, but otherwise the differences are mainly confined to the foreground.
Grasmoor Grasmoor is a mountain in the north-western part of the Lake District, northern England. It is the highest peak in a group of hills between the villages of Lorton, Braithwaite and Buttermere, and overlooks Crummock Water. Grasmoor is distingui ...
and Rannerdale Knotts look impressive across the lake, an unexpected glimpse of the Helvellyn range seen behind.


Ascents

A popular route up the fell is a path from the village of Loweswater, that threads its way between the crags and rocky outcrops on the north side. The north top is then traversed to reach the summit. A variation misses out the north top, following a slanting path southwards along the Mosedale face to the depression. From the shore of Crummock Water an ascent can be made following Pillar Rake, a diagonal breach in the central rim of crag. A direct climb of the south top direct is best achieved from Buttermere village, starting along the Scale Force path before making for Scale Knott.Bill Birkett: Complete Lakeland Fells: Collins Willow (1994):


References

{{Marilyns N Eng Marilyns of England Fells of the Lake District Loweswater (village)