The Geological Record
The Geological Record
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. Geology of Southern New Brunswick. Proc. Amer. Assoc.
vol. xxii. B. pp. 116, 117 (abstract).
. Breaks in the American Palaeozoic Series. Proc. Amer. Assoc.
vol. xxii. B. pp. 117, X19 (abstract).
• On the crystalline Bocks of the Blue Eidge, and on their decomposed condition. Proc. Boston Nat. Hist. Soc. vol. xvi.
part 2, pp. 116, 117.
These consist of homblendic and micaceons schists, completely de- composed to a depth of 50 feet and more, being changed to u reddish unctuous clay, with interb...edded layers of quartz, showing the original inclination of the rocks. The removal of the iron-oxide is said to be the source of the large deposits of hydrous iron-ores found at the foot of the Blue Bidge in the Appalachian valley. The decomposition is supposed to have taken place in very ancient times, when there was a highly carbonated atmosphere. To the N.E. an absence of decom- posed rocks is held to be due to subsequent denudation, the soft parts being swept away, and the unchanged rock exposed and glaciated.
What to read after The Geological Record?
You can find similar books in the "Read Also" column, or choose other free books by Crookes, William, Sir, 1832-1919 to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
. Geology of Southern New Brunswick. Proc. Amer. Assoc.
vol. xxii. B. pp. 116, 117 (abstract).
. Breaks in the American Palaeozoic Series. Proc. Amer. Assoc.
vol. xxii. B. pp. 117, X19 (abstract).
• On the crystalline Bocks of the Blue Eidge, and on their decomposed condition. Proc. Boston Nat. Hist. Soc. vol. xvi.
part 2, pp. 116, 117.
These consist of homblendic and micaceons schists, completely de- composed to a depth of 50 feet and more, being changed to u reddish unctuous clay, with interb...edded layers of quartz, showing the original inclination of the rocks. The removal of the iron-oxide is said to be the source of the large deposits of hydrous iron-ores found at the foot of the Blue Bidge in the Appalachian valley. The decomposition is supposed to have taken place in very ancient times, when there was a highly carbonated atmosphere. To the N.E. an absence of decom- posed rocks is held to be due to subsequent denudation, the soft parts being swept away, and the unchanged rock exposed and glaciated.
What to read after The Geological Record?
You can find similar books in the "Read Also" column, or choose other free books by Crookes, William, Sir, 1832-1919 to read onlineMoreLess
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