FREE BOOKS

Author's List




PREV.   NEXT  
|<   12   13   14   15   16   17   18   19   20   21   22   23   24   25   26   27   28   29   30   31   32   33   34   35   36  
37   38   39   40   41   42   43   44   45   46   47   48   49   50   51   52   53   54   55   56   57   58   59   60   61   >>   >|  
t a certain height, while lower that snow becomes rain." "Well, then, this valley we are looking at ought to be snow, not ice." "Snow is ice in the form of light flocculent crystals, is it not? Why, at home, if you take up moist snow and press it hard in your hands, you can almost turn it into ice. If you placed it in a press, and applied much force, it would become perfectly clear ice. Well, there's pressure enough here to turn it into ice; and besides, the snow is always melting in the hot sun, and then freezing again at night." "Yes, I see!" cried Saxe; "but it does seem queer. Why, we've got summer here, with flowers and bees and butterflies, and if we go down to that glacier, I suppose we can step on to winter." "Yes, my lad; and if we like to climb a little higher up the ice, we can place ourselves in such severe winter that we should be frozen to death." "Then we will not go," said Saxe, laughing. "You told me one day--No, you didn't, it was in a story I read, `man is best as he is.' But I say, Mr Dale, how about the river? doesn't it come from the glacier?" "Yes, of course. These vast glaciers are the sources of the great Swiss and Italian rivers. The Rhine and the Rhone both begin up in the mountains here, and the Aar and the Reuss start pretty close to them. When we get down here you will see how this stream runs from a little ice-cave." "But what makes it so dirty?" "My good fellow, we have come to climb, and my name is not Barlow. You must read and search out these things. You know how that stone or mass fell with a roar lower down?" "Not likely to forget it, sir," replied Saxe, with a laugh. "Well, the stones are always falling from the bare sides of the gorge; they drop on to the glacier, and in course of time are washed by the melting ice into the crevasses and down to the bare rock beneath the glacier. There they glide down, with its weight upon them, right over the rock, and the surface is worn off from the fallen stone and the bed rock in a thin paste, which is washed away by the glacier. Then, as it descends, it of course discolours the water." "Shall we go down to the toe of the glacier!" said the guide. "Yes; come along." "Can we trust the young herr to descend?" Dale leaned forward to gaze down the rugged slope, which was excessively steep, but broken up into rift and gully, offering plenty of foot and hand-hold. "What do you think, Saxe?" he said. "Can
PREV.   NEXT  
|<   12   13   14   15   16   17   18   19   20   21   22   23   24   25   26   27   28   29   30   31   32   33   34   35   36  
37   38   39   40   41   42   43   44   45   46   47   48   49   50   51   52   53   54   55   56   57   58   59   60   61   >>   >|  



Top keywords:
glacier
 
melting
 

winter

 

washed

 

stones

 

falling

 

stream

 

replied

 

Barlow

 
search

fellow
 

things

 

forget

 

crevasses

 

descend

 
leaned
 

forward

 

plenty

 
offering
 

broken


rugged

 

excessively

 

discolours

 

descends

 
weight
 

beneath

 

fallen

 

pretty

 

surface

 

pressure


perfectly
 
freezing
 
applied
 

valley

 

height

 
flocculent
 

crystals

 

summer

 

flowers

 
glaciers

sources

 
mountains
 

Italian

 

rivers

 

higher

 
butterflies
 
suppose
 
severe
 

frozen

 
laughing