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Updated: July 10, 2025
In the course of explorations made to the eastward of here, between the 38th and 40th parallels, I observed glacial phenomena equally fresh and demonstrative on all the higher mountains of the White Pine, Golden Gate, and Snake ranges, varying from those already described only as determined by differences of elevation, relations to the snow-bearing winds, and the physical characteristics of the rock formations.
We find this colour very grateful to the eyes, and as a rule it is possible to see everything through them even more clearly than with naked vision. The hard sastrugi are now all from the W.S.W. and our cairns are drifted up by winds from that direction; mostly, though, there has evidently been a range of snow-bearing winds round to south.
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