|
Gentleman's Magazine 1900 part 1 p.436
rocks, picturesqueness in the beetling crags, and lively
interest in the many charms of the ghylls of the fells.
A ghyll, it may be explained, is the hacked-out course of a
fell beck or stream, and may be divided into three scenic
sections: first, the approach - generally by a wide moorland
glen, narrowing into a defile at its head and choked with
boulders of all sizs and shapes. The succeeding portion is
the gully proper. The deepest waterfalls are here, as is
also the hardest climbing. The lofty cliffs surrounding the
fosse are split into irregular chimneys and negotiable
angles, aiguilles abound, yards wide rise spray-washed slabs
without the slightest irregularity on their polished
surfaces. The head of the ghyll is a return to the natural
scenery of the fell; in some places this is reached by an
easy grass ascent, in others after a rough scramble over
piled fragments of rock. A steep cornice may, however, bar
the way, or the ghyll bebouch into the hollow of a scree
basin. Then comes a struggle upwards, the grit slides away
at every step. The wide scree gully in which the stream of
debris originates is reached, and progress becomes not a
little dangerous. The rotten "mountain delights" which your
feet have set in motion slip away from loose rocks on the
higher slopes, and down they bound at fearful rates. Keep in
the shelter if you can, and wait for the solid rain to
cease. You cannot dodge the flying pieces, for however quick
your eye may be in marking, the treacherous foothold does
not permit rapid movement. And the speed some of these
dislodged stones attain is wonderful. The writer remembers,
when climbing a scree under Fairfield, seeing a portion of
cliff topple over, some hundred feet in front. It simply
bounced through the air, struck a spur from the parent rock
some dozen yards from him, and burst into dust and
splinters. The crash was louder than the explosion of a
fair-sized cannon, and the very mountain seemed to quiver at
the shock. Had not a crevice afforded shelter from the mass
of shingle which for some ten minutes whistled down the
side, these lines would never have been written.
Some ghylls are mere fissures in the mountain sides, with
lofty cliffs rising sheer from their beck beds. In these the
imprisoned water races down without a break on its surface,
a yard wide, perhaps four deep. You scramble along the wall
of rock and look down upon the scene, or laboriously work a
way along the ledges, at every turn leaping the stream,
leaving insecure foot- and hand-hold on one side for points
equally insecure on the other. Then you come to a cataract,
the brook tumbles over an abrupt scar into the deep and
narrow basin, hollowed by and for itself. The gorge is
closed,
|