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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, 
  
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