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" la Beche, has intruded itself into the carboniferous slate and slaty sandstone, twisting and contorting the strata, and sending veins into them. Hence some of the slate rocks have become " micaceous; others more indurated, and with the characters of mica-slate... "
The Student's Elements of Geology - Seite 578
von Sir Charles Lyell - 1878 - 672 Seiten
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A Geological Manual

Henry Thomas De La Beche - 1833 - 662 Seiten
...intrusion, some being simply micaceous, others more indurated and with the characters of mica slate and gneiss, while others again appear converted into a hard zoned rock strongly impregnated with felspar. The alteration of the rocks in this case is of very easy explanation. The grauwackc, which...
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A Treatise on Primary Geology, etc

Henry Samuel BOASE - 1834 - 440 Seiten
...surrounding Dartmoor have been changed," says De la Beche, " by the intrusion of granite; some being simply micaceous, others more indurated and with the characters...converted into a hard zoned rock strongly impregnated with felspar. The alteration of the rocks in this case is of very easy explanation. The greywacke, which...
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Principles of geology, Band 4

sir Charles Lyell (bart.) - 1835 - 480 Seiten
...granite, says Mr. De la Beche, of Dartmoor, in Devonshire, has intruded itself into the greywacke: twisting and contorting the strata, and sending veins...gneiss, while others again appear converted into a hard-zoned rock strongly impregnated with felspar." f We learn from the investigations of M. Dufrenoy,...
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Principles of Geology: Being an Inquiry how Far the Former Changes ..., Band 2

Sir Charles Lyell - 1837 - 584 Seiten
...granite, says Mr. De la Beche, of Dartmoor, in Devonshire, has intruded itself into the greywacke', twisting and contorting the strata, and sending veins...gneiss, while others again appear converted into a hard-zoned rock strongly impregnated with felspar.":): We learn from the investigations of M. Dufrenoy,...
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Elements of Geology

Sir Charles Lyell - 1838 - 582 Seiten
...GKANITE. 245 Mr. De la Beche, has intruded itself into the slate and slaty sandstone called grey wacke, twisting and contorting the strata, and sending veins...gneiss, while others again appear converted into a hard-zoned rock strongly impregnated with felspar." * We learn from the investigations of M. Dufrenoy,...
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Elements of Geology

Sir Charles Lyell - 1838 - 606 Seiten
...Devonshire, says Mr. De la Beche, has intruded itself into the slate and slaty sandstone called greywacke, twisting and contorting the strata, and sending veins...gneiss, while others again appear converted into a hard-zoned rock strongly impregnated with felspar." * We learn from the investigations of M. Dufrenoy,...
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Elements of Geology

Sir Charles Lyell - 1839 - 330 Seiten
...Devonshire, says Mr. De la Beche, has intruded itself into the slate and slaty sandstone called greywacke, twisting and contorting the strata, and sending veins...gneiss, while others again appear converted into a hard-zoned rock strongly impregnated with felspar."* We learn from the investigations of M. Dufrenoy,...
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Elements of Geology, Band 1

Sir Charles Lyell - 1841 - 946 Seiten
...Devonshire, says Mr. De la Bêche, has intruded itself into the slate and slaty sandstone called greywacké, twisting and contorting the strata, and sending veins...gneiss; while others again appear converted into a hard-zoned rock strongly impregnated with felspar."* We learn from the investigations of M. Dufrénoy,...
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Elements of Geology

Sir Charles Lyell - 1845 - 338 Seiten
...Devonshire, says Mr. De la Beche, has intruded itself into the slate and slaty sandstone called greywacké, twisting and contorting the strata, and sending veins...gneiss, while others again appear converted into a hard-zoned rock strongly impregnated with felspar."* We learn from the investigations of M. Dufrénoy,...
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Elements of Geology

Sir Charles Lyell - 1846 - 358 Seiten
...Devonshire, says Mr. De la Beche, has intruded itself into the slate and slaty sandstone called greywacké, twisting and contorting the strata, and sending veins...gneiss, while others again appear converted into a hard-zoned rock strongly impregnated with felspar."* Now the alterations above described as superinduced...
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