FREE BOOKS

Author's List




PREV.   NEXT  
|<   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   62   63   64   65   66   67   68   69   70   71   72   73   74   75   >>  
ly about three-quarters of a mile of river, which is not more than fifty or sixty yards wide, and two or three feet deep, and is so swift and rough that navigation is out of the question. "Lake Lindeman is about five miles long and half a mile wide. It is deep enough for all ordinary purposes. Lake Bennet[3] is twenty-six and a quarter miles long, for the upper fourteen of which it is about half a mile wide. About midway in its length an arm comes in from the west, which Schwatka appears to have mistaken for a river, and named Wheaton River. This arm is wider than the other arm down to that point, and is reported by Indians to be longer and heading in a glacier which lies in the pass at the head of Chilkoot Inlet. This arm is, as far as seen, surrounded by high mountains, apparently much higher than those on the arm we travelled down. Below the junction of the two arms the lake is about one and a half miles wide, with deep water. Above the forks the water of the east branch is muddy. This is caused by the streams from the numerous glaciers on the head of the tributaries of Lake Lindeman. [Footnote 3: A small saw-mill has been erected at the head of Lake Bennet; lumber for boat building sells at $100 per M. Boats 25 feet long and 5 feet beam are $60 each. Last year the ice broke up in the lake on the 12th June, but this season is earlier and the boats are expected to go down the lake about the 1st of June.] "A stream which flows into Lake Bennet at the south-west corner is also very dirty, and has shoaled quite a large portion of the lake at its mouth. The beach at the lower end of this lake is comparatively flat and the water shoal. A deep, wide valley extends northwards from the north end of the lake, apparently reaching to the canon, or a short distance above it. This may have been originally a course for the waters of the river. The bottom of the valley is wide and sandy, and covered with scrubby timber, principally poplar and pitch-pine. The waters of the lake empty at the extreme north-east angle through a channel not more than one hundred yards wide, which soon expands into what Schwatka called Lake Nares.[4] Through this narrow channel there is quite a current, and more than 7 feet of water, as a 6 foot paddle and a foot of arm added to its length did not reach the bottom. [Footnote 4: The connecting waters between Lake Bennet and Tagish Lake constitute what is now called Caribou Crossing.] "The hills at
PREV.   NEXT  
|<   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   62   63   64   65   66   67   68   69   70   71   72   73   74   75   >>  



Top keywords:
Bennet
 

waters

 

channel

 

Schwatka

 
Footnote
 

valley

 
apparently
 

bottom

 

Lindeman

 

called


length

 

portion

 
shoaled
 
paddle
 

expected

 
Tagish
 

season

 
earlier
 

stream

 

corner


connecting

 
constitute
 

timber

 

principally

 
poplar
 

scrubby

 

covered

 

Through

 

expands

 

hundred


extreme

 

narrow

 
extends
 

current

 
northwards
 

comparatively

 

Caribou

 

reaching

 

originally

 
distance

Crossing

 
caused
 

mistaken

 

Wheaton

 

appears

 

midway

 

heading

 

glacier

 

longer

 

reported