Geology of the Eureka District Nevada With An Atlas
Geology of the Eureka District Nevada With An Atlas
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From Weber Peak southward they overlie conformably the Lower Coal-measures, although not extending southward out into the open valley quite as far as the limestone, being buried beneath either basaltic flows or the alluvial deposits of Pinto Creek. Along the line of contact the Weber conglomerates form a well defined series of ridges parallel with the Alpha and Fusilina ridges, the two formations standing out sharply contrasted by their surface forms, atmospheric agencies acting quite different...ly on the fine crystalline limestones and the coarse conglomerates. In like manner erosion acting upon the more easily disintegrated conglom- erates has worn out a number of narrow drainage channels along the con- tact which serve still more sharply to define tin- boundaries. The conglom- MON xx 11 162 GEOLOGY OF THE EUKEKA DISTRICT.
erates stretch out toward the west until cut off by the broad basaltic table- land of the Strahleuberg, which, concealing- everything over a wide area, leaves to conjecture the probable structural relations of the Carboniferous rocks of the Diamond Range to the immense block of Devonian limestone of the County Peak uplift.
What to read after Geology of the Eureka District Nevada With An Atlas?
You can find similar books in the "Read Also" column, or choose other free books by A Arnold Hague to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
From Weber Peak southward they overlie conformably the Lower Coal-measures, although not extending southward out into the open valley quite as far as the limestone, being buried beneath either basaltic flows or the alluvial deposits of Pinto Creek. Along the line of contact the Weber conglomerates form a well defined series of ridges parallel with the Alpha and Fusilina ridges, the two formations standing out sharply contrasted by their surface forms, atmospheric agencies acting quite different...ly on the fine crystalline limestones and the coarse conglomerates. In like manner erosion acting upon the more easily disintegrated conglom- erates has worn out a number of narrow drainage channels along the con- tact which serve still more sharply to define tin- boundaries. The conglom- MON xx 11 162 GEOLOGY OF THE EUKEKA DISTRICT.
erates stretch out toward the west until cut off by the broad basaltic table- land of the Strahleuberg, which, concealing- everything over a wide area, leaves to conjecture the probable structural relations of the Carboniferous rocks of the Diamond Range to the immense block of Devonian limestone of the County Peak uplift.
What to read after Geology of the Eureka District Nevada With An Atlas?
You can find similar books in the "Read Also" column, or choose other free books by A Arnold Hague to read onlineMoreLess
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