Physical Geography of the Evanston Waukegan Region
Physical Geography of the Evanston Waukegan Region
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In our eReader you can find the full English version of the book. Read Physical Geography of the Evanston Waukegan Region Online - link to read the book on full screen. Our eReader also allows you to upload and read Pdf, Txt, ePub and fb2 books. In the Mini eReder on the page below you can quickly view all pages of the book - Read Book Physical Geography of the Evanston Waukegan Region
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[BULL. 7 In section 4 (Waukegan) the beach ridge continues northward with characteristic strength, and thence for over six miles is followed by Sheridan road. Near Beach station it has three closely set crests. At Zion City it is double, the two ridges having the same height, 53 feet above the lake, and crossing Shiloh boulevard near Dowie's residence. In places it is raised a few feet by blown sand. Near Withrop Harbor it is again double and not so well defined. Behind it, on the outer slope o...f the till ridge, a low cliff has developed. The beach ridge crosses the State line with a crest which rises and falls several feet because of dune action.
West of this 50 to 55-foot Glen wood beach ridge is another long ridge, from 5 to 15 feet higher, usually much broader, and commonly so till-like in structure as to suggest an ice-front deposit rather than a beach ridge. Locally, however, (as at the gravel pit at the southeast corner of section 9, near Winthrop Harbor), it is seen to be built of well stratified gravels.
What to read after Physical Geography of the Evanston Waukegan Region?
You can find similar books in the "Read Also" column, or choose other free books by Wallace Walter Atwood to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
[BULL. 7 In section 4 (Waukegan) the beach ridge continues northward with characteristic strength, and thence for over six miles is followed by Sheridan road. Near Beach station it has three closely set crests. At Zion City it is double, the two ridges having the same height, 53 feet above the lake, and crossing Shiloh boulevard near Dowie's residence. In places it is raised a few feet by blown sand. Near Withrop Harbor it is again double and not so well defined. Behind it, on the outer slope o...f the till ridge, a low cliff has developed. The beach ridge crosses the State line with a crest which rises and falls several feet because of dune action.
West of this 50 to 55-foot Glen wood beach ridge is another long ridge, from 5 to 15 feet higher, usually much broader, and commonly so till-like in structure as to suggest an ice-front deposit rather than a beach ridge. Locally, however, (as at the gravel pit at the southeast corner of section 9, near Winthrop Harbor), it is seen to be built of well stratified gravels.
What to read after Physical Geography of the Evanston Waukegan Region?
You can find similar books in the "Read Also" column, or choose other free books by Wallace Walter Atwood to read onlineMoreLess
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