Geology
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In our eReader you can find the full English version of the book. Read Geology 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 Geology
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XIX, 1892; and Woodworth, Bull. 84 N. Y. State Mus.
4 Dana, Manual of Geology, 4th ed., p. 982; and Store, Jour, of Geol., Vol. I, pp. 246-254.
5 Bell. Am. Jour Sci , 4th ser., Vol. I, pp 219-228, 1896.
■101 GEOLOGY.
THE PLEISTOCENE OR GLACIAL PERIOD. 405 of post-glacial submergence are reported at still greater heights in Labrador.
The Loess.
The term loess is used with not a little latitude, both as a text- ural and a formational name. Lithologically, loess is a variety cf silt intermediate b...etween the finest sand and clay. In general, it is free from stones of all sorts, except the concretions which have been developed in it since its deposition. In the exceptional cases where stones occur in it, they are confined to its extreme basal portion. At its base, too, it is sometimes interstratified with sand, especially where it is thick.
The composition 1 of the loess is significant in that it contains angular, undecomposed particles of the commoner carbonates, calcite and dolomite, and silicates, such as the feldspars, the amphiboles, the micas, etc.
What to read after Geology?
You can find similar books in the "Read Also" column, or choose other free books by Thomas C Thomas Chrowder Chamberlin to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
XIX, 1892; and Woodworth, Bull. 84 N. Y. State Mus.
4 Dana, Manual of Geology, 4th ed., p. 982; and Store, Jour, of Geol., Vol. I, pp. 246-254.
5 Bell. Am. Jour Sci , 4th ser., Vol. I, pp 219-228, 1896.
■101 GEOLOGY.
THE PLEISTOCENE OR GLACIAL PERIOD. 405 of post-glacial submergence are reported at still greater heights in Labrador.
The Loess.
The term loess is used with not a little latitude, both as a text- ural and a formational name. Lithologically, loess is a variety cf silt intermediate b...etween the finest sand and clay. In general, it is free from stones of all sorts, except the concretions which have been developed in it since its deposition. In the exceptional cases where stones occur in it, they are confined to its extreme basal portion. At its base, too, it is sometimes interstratified with sand, especially where it is thick.
The composition 1 of the loess is significant in that it contains angular, undecomposed particles of the commoner carbonates, calcite and dolomite, and silicates, such as the feldspars, the amphiboles, the micas, etc.
What to read after Geology?
You can find similar books in the "Read Also" column, or choose other free books by Thomas C Thomas Chrowder Chamberlin to read onlineMoreLess
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