FREE BOOKS

Author's List




PREV.   NEXT  
|<   90   91   92   93   94   95   96   97   98   99   100   101   102   103   104   105   106   107   108   109   110   111   112   113   114  
115   116   117   118   119   120   121   122   123   124   125   126   127   128   129   130   131   132   133   134   135   136   137   138   139   >>   >|  
about Lake Tahoe and Lake Mono ran out far into the water and formed icebergs I think is quite certain, and that parallel moraines open below are characteristic signs of such conditions I also think nearly certain. _f. Glacial Erosion_. My observations on glacial pathways in the High Sierra, and especially about Lake Tahoe, have greatly modified my views as to the nature of glacial erosion. Writers on this subject seem to regard glacial erosion as mostly, if not wholly, a _grinding_ and _scoring_; the debris of this erosion as rock-meal; the great bowlders, which are found in such immense quantities in the terminal deposit, as derived wholly from the crumbling cliffs above the glacial surface; the _rounded_ bowlders, which are often the most numerous, as derived in precisely the same way, only they have been engulfed by crevasses, or between the sides of the glacier and the bounding wall, and thus carried between the moving ice and its rocky bed, as between the upper and nether millstone. In a word, all bowlders, whether angular or rounded, are supposed to owe their _origin_ or _separation_ and _shaping_ to glacial agency. Now, if such be the true view of glacial erosion, evidently its effect in mountain sculpture must be small indeed. _Roches moutonnees_ are recognized by all as the most universal and characteristic sign of a glacial bed. Sometimes these beds are only imperfect _moutonnees_, i.e., they are composed of _broken angular surface with only the points and edges planed off_. Now, _moutonnees_ surfaces always, and especially angular surfaces with only points and edges beveled, show that the erosion by grinding has been only very superficial. They show that if the usual view of glacial erosion be correct, the great canyons, so far from being _formed_, were only very _slightly modified_ by glacial agency. But I am quite satisfied from my own observations, that this is not the only _nor the principal_ mode of glacial erosion. I am convinced that a glacier, by its enormous pressure and resistless onward movement, is _constantly breaking off large blocks_ from its bed and bounding walls. Its erosion is not only a grinding and scoring, but also a _crushing and breaking_. It makes by its erosion not only rock-meal, but also large _rock-chips_.
PREV.   NEXT  
|<   90   91   92   93   94   95   96   97   98   99   100   101   102   103   104   105   106   107   108   109   110   111   112   113   114  
115   116   117   118   119   120   121   122   123   124   125   126   127   128   129   130   131   132   133   134   135   136   137   138   139   >>   >|  



Top keywords:

glacial

 

erosion

 

bowlders

 

angular

 

grinding

 

moutonnees

 

derived

 

wholly

 
scoring
 

glacier


bounding

 

agency

 

points

 

rounded

 

surfaces

 

surface

 

characteristic

 
breaking
 

observations

 

modified


formed
 

blocks

 

imperfect

 

evidently

 

broken

 

composed

 

Roches

 

sculpture

 

mountain

 

effect


Sometimes

 

universal

 

recognized

 
onward
 

crushing

 
correct
 

superficial

 

satisfied

 

canyons

 

slightly


pressure

 
enormous
 
resistless
 
movement
 

planed

 

convinced

 
beveled
 

principal

 

constantly

 

crevasses