mz 
-»y-r •» ' 
tended such lower down formerly, There are moraine inside of morains, 
The glacier at present has several sources covering a large share of 
this side of the mountain, Hear the top these unite and run to a point 
a short distance above timber line. In the crevasses and near the 
sumlt near rooks where the mum has broken off leaving the faces bare, 
strata showing deposit® of shot# for at least 10 years can bo seen. Large 
rocks arc floating on the surface and indentations may be seen where 
rocks from above have become loosened and went thundering dos m until they 
reached a crevasse wide enough to eatch thorn, The largest crevasses are 
about SO feet across and some of them must be at least 100 feet la depth, 
mile descending, Mr*, Kelson detached a rock weighing probably 200 pounds; 
it broke into several pieces and gathering aewnfctto as it wont, it would 
bound at times 50 feet or more in the air and finally left the glacier 
and brought up in a lot of pcarphyritie boulders below it, 
There ere no signs of volcanic action about this mountain. It is 
composed of solid porphyry. 
Stopping the night of larch 1 in our camp in the cave we rod© to 
Jhaeea the following day, Ife wore ao glasses cm the mountain and Mr, I, 
and I suffered severely for several days from snowblisdnesa* % could 
not us© our eye® and were obliged to stay in a dark room. 
About March 5 we left Jaaeca for Mcac, with all our outfit, where we 
stayed a couple of days and continued our travels as described in smother 
place , 
la addition to the mammals given from this place (Ameeameec) we after- 
ward took tbs following: Mephitis: A few of these live about Sect© 
Monte. One specimen ms trapped, Dipodgaw® a 1 discovered a few of 
their holes near the railroad about a ail© fresi town toward Morelos, 
The ground her© is vary sandy and is, I should think, well suited to 
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