Glaciers of the Canadian Rockies And Selkirks Smithsonian Expedition of 1904
Glaciers of the Canadian Rockies And Selkirks Smithsonian Expedition of 1904
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2 B -0. 7 C 1. 9 E -i . O F -4. 6 G ii. 8 2-4 4. 8 12 . O Missing.
3-2 20. 4 IS- 1 These figures indicate that the component glaciers are as independent m their movements as in their structure, and that some may be stationary, or in retreat, while others lying alongside are advancing. The question of the frontal be- havior of a. Piedmont glacier is thus seen to be complicated in proportion to the complexity of its structure. Measurements made at single stations can give only very incomplete dat...a concerning the glacier as a whole. There should be at least one such measurement for each commensal stream.
8. FORMER ACTIVITY. A. Bear-den moraines. Along the western front of the Wenkchemna, for a GLACIERS OF THE CANADIAN ROCKIES AND SELKIRKS. 69 distance of over a mile, there occurs a tremendous accumulation of huge mo- rainic blocks of a red and brown sandstone. The blocks are much disintegrated by the weather, and falling apart, but each roughly indicates its former size and shape (plate xxiv, figure 3) .
What to read after Glaciers of the Canadian Rockies And Selkirks Smithsonian Expedition of 1904?
You can find similar books in the "Read Also" column, or choose other free books by W H William Hittell Sherzer to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
2 B -0. 7 C 1. 9 E -i . O F -4. 6 G ii. 8 2-4 4. 8 12 . O Missing.
3-2 20. 4 IS- 1 These figures indicate that the component glaciers are as independent m their movements as in their structure, and that some may be stationary, or in retreat, while others lying alongside are advancing. The question of the frontal be- havior of a. Piedmont glacier is thus seen to be complicated in proportion to the complexity of its structure. Measurements made at single stations can give only very incomplete dat...a concerning the glacier as a whole. There should be at least one such measurement for each commensal stream.
8. FORMER ACTIVITY. A. Bear-den moraines. Along the western front of the Wenkchemna, for a GLACIERS OF THE CANADIAN ROCKIES AND SELKIRKS. 69 distance of over a mile, there occurs a tremendous accumulation of huge mo- rainic blocks of a red and brown sandstone. The blocks are much disintegrated by the weather, and falling apart, but each roughly indicates its former size and shape (plate xxiv, figure 3) .
What to read after Glaciers of the Canadian Rockies And Selkirks Smithsonian Expedition of 1904?
You can find similar books in the "Read Also" column, or choose other free books by W H William Hittell Sherzer to read onlineMoreLess
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