FREE BOOKS

Author's List




PREV.   NEXT  
|<   542   543   544   545   546   547   548   549   550   551   552   553   554   555   556   557   558   559   560   561   562   563   564   565   566  
567   568   569   570   571   572   573   574   575   576   577   578   579   580   581   582   583   584   585   586   587   588   589   590   591   >>   >|  
contrary, is deep, and about eighteen kilometres from its mouth flows through another lake, from the eastern shore of which rugged and shattered mountains rise to a height which I estimate at 800 to 1000 metres; but it is quite possible that their height is twice as great, for in making such estimates one is liable to fall into error. South of the river and the harbour the land rises abruptly from the river bank, which is from ten to twenty metres high. On the north side, on the other hand, the bank is for the most part low, but farther into the interior the ground rises rapidly to rounded hills from 300 to 400 metres high. Only in the valleys and at other places where very large masses of snow had collected during the winter, were snow-drifts still to be seen. On the other hand, we saw no glaciers, though we might have expected to find them on the sides of the high mountains which bound the inner lake on the east. It was also clear that during the recent ages no widely extended ice-sheet was to be found here, for in the many excursions we made in different directions, among others up the river to the lake just mentioned, we saw nowhere any moraines, erratic blocks, striated rock-surfaces, or other traces of a past ice-age. Many signs, on the other hand, indicate that during a not very remote geological period glaciers covered considerable areas of the opposite Asiatic shore, and contributed to excavate the fjords there--Kolyutschin Bay, St. Lawrence Bay, Metschigme Bay, Konyam Bay, &c. When we approached the American side we could see that the shore cliffs were formed of stratified rocks. I therefore hoped to be able, at last, to make a rich collection of fossils, something that I had no opportunity of doing during the preceding part of the voyage. But I found, on reaching them, that the stratified rocks only consisted of crystalline schists without any traces of animal or vegetable remains. Nor did we find on the shore any whale-bones or any of the remarkable mammoth-bearing ice-strata which were discovered in the bay situated immediately north of Behring's Straits, which was named after Dr. Eschscholz, medical officer during Kotzebue's famous voyage.[346] Immediately after the anchor fell we were visited by several very large skin boats and a large number of _kayaks_. The latter were larger than the Greenlanders', being commonly intended for two persons, who sat back to back in the middle of the craft. We even
PREV.   NEXT  
|<   542   543   544   545   546   547   548   549   550   551   552   553   554   555   556   557   558   559   560   561   562   563   564   565   566  
567   568   569   570   571   572   573   574   575   576   577   578   579   580   581   582   583   584   585   586   587   588   589   590   591   >>   >|  



Top keywords:
metres
 

stratified

 

traces

 

height

 

mountains

 

glaciers

 
voyage
 

consisted

 

reaching

 

preceding


opportunity

 

fossils

 

collection

 

formed

 

fjords

 

Kolyutschin

 

Lawrence

 

excavate

 

contributed

 
considerable

covered
 
opposite
 
Asiatic
 

Metschigme

 

Konyam

 
cliffs
 

approached

 
American
 

discovered

 
number

kayaks

 
anchor
 
Immediately
 

visited

 
larger
 
middle
 

persons

 
Greenlanders
 

commonly

 

intended


famous

 
remarkable
 

mammoth

 

bearing

 

schists

 

animal

 
vegetable
 
remains
 

strata

 
period