We are now crossing the deepest part of the northern basin of the
lake, where Dr. Mill found over 150 feet of water. The bottom
rises, when we pass Hoathwaite boathouse on the right, to little
more than 125 feet, and off Fir Island deepens again, attaining
184 feet half a mile farther down--making this the deepest of
the lakes after Wastwater, Windermere, and Ullswater, as its
5-1/2 miles of length makes it the longest except Windermere and
Ullswater. Its normal level is 143 feet above the sea, though it
rises and falls in drought and damp weather as much as six feet.
Of the form of its bed Dr. Mill says:--"If the water were reduced
to sea level, there would remain two small lakes, the southern
measuring one mile and a half in length, and a quarter of a mile
in breadth, and having a maximum depth of 42 feet; the northern
one, separated by a quarter of a mile, being only 9 feet deep,
three-quarters of a mile long, and perhaps 200 yards wide at the
most. Quite possibly the two might be connected by a channel, and
give a long shallow lake of two and a half miles" (_Bathymetrical
Survey of the English Lakes_, p. 39). This bank or dam between the
two deeps is not caused by filling up from any stream like that at
the steamer pier; it points to the fact, more strikingly seen in
Windermere, that these long lakes, like most of the long valleys,
are not mere troughs or grooves ploughed in the rock, but a series
of basins, partly filled up with glacial débris, and partly joined
together by glacial erosion, which broke and planed away the
dividing barriers.
Fir Island (formerly from its owner called Knott Island, now
the property of Arthur Severn, Esq., R.I., J.P.) is low and
close to the water's edge, hardly distinguishable except by its
grove of Scotch firs from the rest of the coast. In very dry
weather it becomes a peninsula, but usually a boat can make the
circumnavigation, though there is risk of shipwreck on the sharp
rocks to the landward side. Near it, beyond the road which winds
prettily along the uneven and craggy shore, are the ruins of
Copland's Barn; and above it the great larch woods of the Heald,
on a noble slope of nearly 700 feet from the brow of the fell to
the lake. The western shore is formed by the long and varied slope
of Torver Common, down which runs the Moor Gill. At its foot,
exactly opposite Copland's Barn, is the most extensive of the
bloomeries, with the ruins of an old hearth still to be found.
At last the continuous skylines are broken. On the left, a steep
dingle runs up among rocks and woods to Parkamoor, a lonely farm
on a bleak brow top; and on the right, the valley of Torver begins
to open out, with glimpses of Dow Crags and the Old Man in a new
aspect, showing their precipices boldly against the sky, and
beneath them Sunny Bank and Oxness at the mouth of Torver Beck.
Public-domain text, read in full here on John Shaqi.
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