Some Geological Rambles Near Vassar College
Some Geological Rambles Near Vassar College
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Later there came a change, which may have begun while this cementing process was still in progress.
Due to earth forces these beds were compressed and buckled up into folds so as to form an extensive moun- tain system. Finally, erosion acting through long periods of time, has cut these mountains down again almost to sea-level. The small fold shown in this figure and described above, is one of the minor corru- gations, but in its form and development, may be taken as typical of others of much gr...eater dimensions.
REFERENCES.
Geology. Chamberlin and Salisbury. Vol. I, 1905, pp. 501-510.
An Introduction to Geology. Scott. 1897, pp. 233-242.
Text Book of Geology. Geikie. 3rd ed. 1893, pp. 536-543; 4th ed. 1903, pp. 672-681.
(78) ROCK FOLDING NEAR HIGHLAND DIFFERENTIAL CLEAVAGE Location. — The ledge in which this differential cleav- age occurs is situated on the West Shore Railroad, about a mile above Highland and 200 yards north of Clearwater flag station. (Number on map, 18.) Description.
What to read after Some Geological Rambles Near Vassar College?
You can find similar books in the "Read Also" column, or choose other free books by George Burbank Shattuck to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
Later there came a change, which may have begun while this cementing process was still in progress.
Due to earth forces these beds were compressed and buckled up into folds so as to form an extensive moun- tain system. Finally, erosion acting through long periods of time, has cut these mountains down again almost to sea-level. The small fold shown in this figure and described above, is one of the minor corru- gations, but in its form and development, may be taken as typical of others of much gr...eater dimensions.
REFERENCES.
Geology. Chamberlin and Salisbury. Vol. I, 1905, pp. 501-510.
An Introduction to Geology. Scott. 1897, pp. 233-242.
Text Book of Geology. Geikie. 3rd ed. 1893, pp. 536-543; 4th ed. 1903, pp. 672-681.
(78) ROCK FOLDING NEAR HIGHLAND DIFFERENTIAL CLEAVAGE Location. — The ledge in which this differential cleav- age occurs is situated on the West Shore Railroad, about a mile above Highland and 200 yards north of Clearwater flag station. (Number on map, 18.) Description.
What to read after Some Geological Rambles Near Vassar College?
You can find similar books in the "Read Also" column, or choose other free books by George Burbank Shattuck to read onlineMoreLess
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