Quantcast

Appendix I: Glaciation in Great New York

Appendix I: Glaciation in Great New York Page of 281 Appendix I: Glaciation in Great New York Text size:minus plus Restore normal size   Mail page  Print this page
EVIDENCES OF GLACIATION                195
where, and, as in the case of the Dedham granite distributed to the south, invariably show northern origin. In Berkshire County, Massachusetts, these traveled rocks lie in long align­ments, passing over the Lenox Hills, and extending in a gen­erally southeasterly direction for fifteen or twenty miles, and have been filched from the Canaan and Richmond Hills across the line in New York, being of chloritic slate, with angular specimens of limestone intermixed.
Some granites from Vermont, on the west of the Green Mountains, have been lifted over these barriers and trans­ferred to the southern margins of Massachusetts; while in Vermont a boulder weighing over 3,400 tons, and known as the Green Mountain Giant, has been drifted from the Green Mountains easterly across the valley of the Deerfield River, and planted 500 feet above that stream. In Michigan, near the Menominee River, a field upon the northern slope of a mountain is densely covered with boulders, so that a mile can be traversed without once touching the ground. Again, huge nuggets of copper, torn from the immense deposits of native copper at Keweenaw Point, Portage Lake, and the Ontonagon district, on the southern shore of Lake Superior, are found widely disseminated to the south of these localities in Michi­gan, Wisconsin, Ohio, and Minnesota, a few of which have weighed 300, 800, and one, 3,000 pounds. From the sides of the White Mountains fragments of rock have been carried away, and not only conveyed southward, but, as Agassiz first pointed out, distributed northward, though only at compara­tively slight distances.
Throughout Ohio boulders are found which are composed of rock utterly foreign to their present surroundings—indeed, of material not known within the limits of the State. These are found perched over declivities, buried in the soil with their exposed edges showing above the surface, or else lying unencumbered in slight depressions of the ground. In In­diana, Michigan, Illinois, Wisconsin, etc., they are omni­present, and the streets of Cincinnati are paved with the
Appendix I: Glaciation in Great New York Page of 281 Appendix I: Glaciation in Great New York
Suggested Illustrations
Other Chapters you may find useful
Other Books on this topic
bullet Tag
This Page