ex 



PROCEEDINGS OP THE GEOLOGICAL SOCIETY. [May I906, 



a line continuous with that of the Oxen dale shatter-belt ; and north 

 of the main valley along this part of its course is the hanging valley 

 containing Stickle Tarn on the Langdale Pikes, which mouths at a 

 height of about 1200 feet above the Great Langdale Beck. Still 

 lower down the main valley, the Little Langdale stream enters 

 from the south-west. It forms another hanging valley, which 

 mouths above Colwith Force. 



We may now pass on to consider the Duddon Valley, with which 



is associated that of the Upper Esk. 



To illustrate the changes 



Fig. 6. — Map of the upper Duddon Valley and part of EsJcdale, 

 on the scale of 2 miles to the inch. 



a Scawf ell 



Altitudes in feet 

 A= Present drainage 

 B= Supposed former 



drainage. 

 ) - M outhing-points 



of hanging valleys. 



, ..Seathivaite 



XLong House 

 55° 



XLong House 



(position of) 



'Seathwaite Church 

 340 



[For 'Lincove ' read 'Lingcove ' ; and f or ' Troatal ' read ' Troutal.'] 



which appear to have taken place here, two diagrams are given, of 

 which the second (B) indicates the original drainage as inferred 

 from the structure of the ground, while the first (A) shows the 

 present drainage. ( See fig. 6, above.) 



