. Elements of geology : a text-book for colleges and for the general reader. Geology. Fig. 222.—Ideal Section of Jura if unaffected by Erosion. Fig. 223.—Section of Jura as modified by Erosion. mashing is so extreme that the sides are driven in under the swol- len central parts, so that the strata are often reversed. This is the case in the Alps (Fig. 226). Fig. 224.—Section of Coast Range, showing Plication by Horizontal Pressure. Proof of Elevation oy Lateral Pressure alone: 1. Folding.—It is evident that foldings such as those represented in all the above figures,. O 7 C B 3 2 / A Fig. 225.

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. Elements of geology : a text-book for colleges and for the general reader. Geology. Fig. 222.—Ideal Section of Jura if unaffected by Erosion. Fig. 223.—Section of Jura as modified by Erosion. mashing is so extreme that the sides are driven in under the swol- len central parts, so that the strata are often reversed. This is the case in the Alps (Fig. 226). Fig. 224.—Section of Coast Range, showing Plication by Horizontal Pressure. Proof of Elevation oy Lateral Pressure alone: 1. Folding.—It is evident that foldings such as those represented in all the above figures,. O 7 C B 3 2 / A Fig. 225.—Generalized and Simplified Section of the Appalachian Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original LeConte, Joseph, 1823-1901. New York : D. Appleton and Co.

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Keywords: ., bookcentury1800, bookdecade1890, booksubjectgeology, bookyear1892