On the Lakes of Southeastern Wisconsin
On the Lakes of Southeastern Wisconsin
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A similar mass two miles north of the village is being cut away hy the Wisconsin Central railroad. Kames lie at in- tervals on the low strip west of the moraine, or appear as islands in the swamps. They are similarly developed along the drain- age line at the east base. A very prominent kame area reaches southeast in a tongue between Little Cedar and Silver lakes, abutting at the northwest against the high moraine ridge. The plain which lies east of the Silver creek line is at places deeply and... beautifully pitted. Such a pitted area lies on the east side of Little Silver lake. On the site of this plain the remnants of the retreating glacier became isolated blocks of ice. The inter- spaces were filled to a plane with sand and gravel from tEe gla- cier to the east.
THE LAKE BASIN'S.
The trough which is partly filled by the waters of Big Cedar lake is one of those already described as involved in the structure of the moraine. Kame gravels partly filled it to a plane above the level of the lake and it is probable that the whole valley would have been filled to the same depth, had not the present lake basin been occupied by a mass of ice.
What to read after On the Lakes of Southeastern Wisconsin?
You can find similar books in the "Read Also" column, or choose other free books by N M Nevin Melancthon 1865 1945 Fenneman to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
A similar mass two miles north of the village is being cut away hy the Wisconsin Central railroad. Kames lie at in- tervals on the low strip west of the moraine, or appear as islands in the swamps. They are similarly developed along the drain- age line at the east base. A very prominent kame area reaches southeast in a tongue between Little Cedar and Silver lakes, abutting at the northwest against the high moraine ridge. The plain which lies east of the Silver creek line is at places deeply and... beautifully pitted. Such a pitted area lies on the east side of Little Silver lake. On the site of this plain the remnants of the retreating glacier became isolated blocks of ice. The inter- spaces were filled to a plane with sand and gravel from tEe gla- cier to the east.
THE LAKE BASIN'S.
The trough which is partly filled by the waters of Big Cedar lake is one of those already described as involved in the structure of the moraine. Kame gravels partly filled it to a plane above the level of the lake and it is probable that the whole valley would have been filled to the same depth, had not the present lake basin been occupied by a mass of ice.
What to read after On the Lakes of Southeastern Wisconsin?
You can find similar books in the "Read Also" column, or choose other free books by N M Nevin Melancthon 1865 1945 Fenneman to read onlineMoreLess
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