The Western Fells 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 Cumbria.
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 forming a horseshoe around this valley.

Great Gable and its lesser companion Green Gable stand at the head of Ennerdale, with the walkers' pass of Sty Head to their backs.
This connects Borrowdale to Wasdale, giving Gable a footing in both valleys.
The Borrowdale connection is quite tenuous, but Great Gable is prominent in almost any view up the lake.

The upper section of Great Gable has a roughly square plan, about half a mile on each side, with the faces running in line with the four points of the compass.
The fells connecting and subsidiary ridges occupy the corners of the square.

The northern face is formed by Gable Crag, prominent in views from Haystacks and the surrounding fells.
This is the longest continuous wall of crag on the fell and reaches up almost to the summit.
Scree slopes fall away below to the headwaters of the River Liza, which flows down Ennerdale.
There are few crags on the eastern slopes, although these fall steeply to Styhead Tarn, a feeder of the Borrowdale system.
About 30 feet (9.1 m) deep, this tarn occupies a scooped hollow, dammed by boulders fallen from the slopes above.
It is reputed to contain trout and is a popular location for wild camping.
The southern flank of Great Gable falls 2,300 feet (700 m) direct to Lingmell Beck, one of the main feeders of Wastwater.
Right below the summit are the Westmorland Crags, and then a second tier breaks out lower down.
These are Kern Knotts, Raven Crag and Great Napes, all footed by great tongues of scree.
Finally on the west rough slopes fall below the rocks of White Napes to the narrow valley of Gable Beck, a tributary of Lingmell Beck.

From the north-western corner of the pyramid the connecting ridge to Kirk Fell runs out across the col of Beck Head (2,050 feet (620 m)).
There is a small tarn in the depression, and sometimes a second after heavy rain.
Both are blind, having no apparent inlet or outflow.
Gable Beck runs south from Beck Head, while an unnamed tributary of the Liza flows northward.
The main spine of the Western Fells continues along the north east ridge to Green Gable, dropping to Windy Gap (2,460 feet (750 m)) as it rounds the end of Gable Crag.
This ridge is rough and rocky, further worn by the boots of countless walkers.
Stone Cove lies on the Ennerdale side while the rough gully of Aaron Slack runs down toward Styhead Tarn.
The south-eastern ridge provides the connection to the Southern Fells, across the pass of Sty Head.
This is a major crossroads for walkers and climbers, the summit being at around 1,560 feet (480 m).
On the opposite slope is Great End in the Scafells.
Kern Knotts lies on this south-east ridge, as does the small pool of Dry Tarn.
The south-western ridge gives to high level connection, dropping down Gavel Neese in the angle between Lingmell Beck and Gable Beck.
The Western Fells 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 Cumbria. 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 forming a horseshoe around this valley.
Great Gable and its lesser companion Green Gable stand at the head of Ennerdale, with the walkers' pass of Sty Head to their backs. This connects Borrowdale to Wasdale, giving Gable a footing in both valleys. The Borrowdale connection is quite tenuous, but Great Gable is prominent in almost any view up the lake.
The upper section of Great Gable has a roughly square plan, about half a mile on each side, with the faces running in line with the four points of the compass. The fells connecting and subsidiary ridges occupy the corners of the square.
The northern face is formed by Gable Crag, prominent in views from Haystacks and the surrounding fells. This is the longest continuous wall of crag on the fell and reaches up almost to the summit. Scree slopes fall away below to the headwaters of the River Liza, which flows down Ennerdale. There are few crags on the eastern slopes, although these fall steeply to Styhead Tarn, a feeder of the Borrowdale system. About 30 feet (9.1 m) deep, this tarn occupies a scooped hollow, dammed by boulders fallen from the slopes above. It is reputed to contain trout and is a popular location for wild camping. The southern flank of Great Gable falls 2,300 feet (700 m) direct to Lingmell Beck, one of the main feeders of Wastwater. Right below the summit are the Westmorland Crags, and then a second tier breaks out lower down. These are Kern Knotts, Raven Crag and Great Napes, all footed by great tongues of scree. Finally on the west rough slopes fall below the rocks of White Napes to the narrow valley of Gable Beck, a tributary of Lingmell Beck.
From the north-western corner of the pyramid the connecting ridge to Kirk Fell runs out across the col of Beck Head (2,050 feet (620 m)). There is a small tarn in the depression, and sometimes a second after heavy rain. Both are blind, having no apparent inlet or outflow. Gable Beck runs south from Beck Head, while an unnamed tributary of the Liza flows northward. The main spine of the Western Fells continues along the north east ridge to Green Gable, dropping to Windy Gap (2,460 feet (750 m)) as it rounds the end of Gable Crag. This ridge is rough and rocky, further worn by the boots of countless walkers. Stone Cove lies on the Ennerdale side while the rough gully of Aaron Slack runs down toward Styhead Tarn. The south-eastern ridge provides the connection to the Southern Fells, across the pass of Sty Head. This is a major crossroads for walkers and climbers, the summit being at around 1,560 feet (480 m). On the opposite slope is Great End in the Scafells. Kern Knotts lies on this south-east ridge, as does the small pool of Dry Tarn. The south-western ridge gives to high level connection, dropping down Gavel Neese in the angle between Lingmell Beck and Gable Beck.
Great Gable