California Paper - Glacial Erosion and the Origin of the Yosemite Valley

- Organization:
- The American Institute of Mining, Metallurgical, and Petroleum Engineers
- Pages:
- 13
- File Size:
- 1043 KB
- Publication Date:
- Jan 1, 1900
Abstract
It is scarcely necessary to point out the important functions of water in the mining operations of man, especially in the State of California, where sluicing and hydraulic mining have been practiced on such a grand scale as to arouse the opposition of the agricultural interests. But the role which water and ice have played in mining or excavating on their own account is not so apparent. The alluvions of existing rivers, and the higher gravel-beds left by ancient streams, are doubtless the result of running water; but how far these gravelly materials owe their origin primarily as rocky debris and fragments of veins to glacial erosion, it is difficult .to determine. Yet we see on every side in our higher mountains unmistakable evidences of the cutting, crushing and eroding effects of glacial ice. We note that mountain-summits have been reduced in height and shaped into rounded and dome-like summits. We know that the general contour of the hills of New England, of the Highlands of the Hudson, and of the mountains of northern New Jersey, is due to glacial carving. The same is true of the Laurentian hills of Canada and of the mountains of all northern regions. And we recognize in the vast deposits of so-called " drift," which are spread out over the surface of the northern States, the chips and debris from the glacial workshops. Thus we cannot avoid the conclusion that there was an enormous amount of cutting and excavating in glacial times, and that vast quantities of veinmaterial and of ores and metals must have been liberated by ice-action.
Citation
APA:
(1900) California Paper - Glacial Erosion and the Origin of the Yosemite ValleyMLA: California Paper - Glacial Erosion and the Origin of the Yosemite Valley. The American Institute of Mining, Metallurgical, and Petroleum Engineers, 1900.