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 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.
Green Gable stands to the north east of its mightier sibling.

Green and Great Gable rise at the head of Ennerdale, the infant River Liza tumbling down from their connecting col, Windy Gap.
To their backs they have the walkers' pass of Sty Head, connecting Borrowdale to Wasdale.
Green Gable has a footing in Borrowdale only, standing to the north of the pass.
It is from Ennerdale that the fell achieves a peaked "gabled" outline, although only the lower slopes could be considered green- the summit area being a desert of stones.

Taking Great Gable as the pivot of the Western Fells, the northward arm begins over Green Gable, before swinging round over Brandreth and Haystacks to begin the long northern wall of Ennerdale.
Green Gable also has a secondary ridge to the north east, culminating in the separate fell of Base Brown.

Windy Gap (2,460 ft) stands a little way to the south west of the summit, at the bottom of a stony slope.
On the Ennerdale side is Stone Cove- not named by chance, they are yards deep- while the south eastern descent leads down Aaron Slack. "
Slack" is the dialect word for scree, and this too is a rough chute leading down to Sty Head Pass.
Sty Head Tarn lies at the bottom of the Slack, a large pool in a scooped out hollow, the outlet blocked by boulders.
It is 30 ft deep and reputed to contain trout.

Green Gable's eastern face contains the slight hollow of Mitchell Cove, its stream joining Styhead Gill on the way to Borrowdale.
At the northern corner is the ridge to Base Brown, the flat topped depression of Blackmoor Pots.
The dale between the Base Brown and Brandreth ridges is Gillercomb, a classic hanging valley.
Its stream, Sourmilk Gill, exits around the nose of Base Brown via a series of cascades to Seathwaite.
This ensures that all of Green Gable's waters, bar those from the western face, reach the River Derwent.
Brandreth connects via the narrow ridge of Gillercomb Head, site of a few small pools after wet weather.
The Ennerdale side provides the gentlest slopes, at least at lower levels, with the long grassy spur of Tongue gradually rising up the fell.
The topmost section however is guarded by Greengable Crags, stretching around from Stone Cove.
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 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. Green Gable stands to the north east of its mightier sibling.
Green and Great Gable rise at the head of Ennerdale, the infant River Liza tumbling down from their connecting col, Windy Gap. To their backs they have the walkers' pass of Sty Head, connecting Borrowdale to Wasdale. Green Gable has a footing in Borrowdale only, standing to the north of the pass. It is from Ennerdale that the fell achieves a peaked "gabled" outline, although only the lower slopes could be considered green- the summit area being a desert of stones.
Taking Great Gable as the pivot of the Western Fells, the northward arm begins over Green Gable, before swinging round over Brandreth and Haystacks to begin the long northern wall of Ennerdale. Green Gable also has a secondary ridge to the north east, culminating in the separate fell of Base Brown.
Windy Gap (2,460 ft) stands a little way to the south west of the summit, at the bottom of a stony slope. On the Ennerdale side is Stone Cove- not named by chance, they are yards deep- while the south eastern descent leads down Aaron Slack. "Slack" is the dialect word for scree, and this too is a rough chute leading down to Sty Head Pass. Sty Head Tarn lies at the bottom of the Slack, a large pool in a scooped out hollow, the outlet blocked by boulders. It is 30 ft deep and reputed to contain trout.
Green Gable's eastern face contains the slight hollow of Mitchell Cove, its stream joining Styhead Gill on the way to Borrowdale. At the northern corner is the ridge to Base Brown, the flat topped depression of Blackmoor Pots. The dale between the Base Brown and Brandreth ridges is Gillercomb, a classic hanging valley. Its stream, Sourmilk Gill, exits around the nose of Base Brown via a series of cascades to Seathwaite. This ensures that all of Green Gable's waters, bar those from the western face, reach the River Derwent. Brandreth connects via the narrow ridge of Gillercomb Head, site of a few small pools after wet weather. The Ennerdale side provides the gentlest slopes, at least at lower levels, with the long grassy spur of Tongue gradually rising up the fell. The topmost section however is guarded by Greengable Crags, stretching around from Stone Cove.
Green Gable