This historic book may have numerous typos and missing text. Purchasers can download a free scanned copy of the original book (without typos) from the publisher. Not indexed. Not illustrated. 1910 Excerpt: ...on the south side of the mountain south of Sawtooth Mountain (Pl. VIII, B); these faults are among the most conspicuous features of the near landscape around Rhyolite. VVhere flows closely r e s e m bl e o n e another it is very difficult to trace faults, but fortunately in many such cases basalt dikes or debris ' of ...
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This historic book may have numerous typos and missing text. Purchasers can download a free scanned copy of the original book (without typos) from the publisher. Not indexed. Not illustrated. 1910 Excerpt: ...on the south side of the mountain south of Sawtooth Mountain (Pl. VIII, B); these faults are among the most conspicuous features of the near landscape around Rhyolite. VVhere flows closely r e s e m bl e o n e another it is very difficult to trace faults, but fortunately in many such cases basalt dikes or debris ' of basalt marks the fault plane. An example is the northern portion of the Hobo fault, on the hills northwest of the Las Vegas and Tonopah Railroad s t a tio n. Along a part of its length rhyolite No. 8 forms both the hanging and the foot wall, and abundant and almost continuous b as alt debris along this fault plane becomes a useful guide. VVhen both hanging and foot walls of a fault are the same rock and basalt is absent, it is difficult or impossible 'to trace the faults accurately. These are the conditions along that portion of the Denver fault on Busch Peak north of the outcrop of basalt No. 2, which it displaces. Wash covers up a large number of faults; some partly, others completely. For example, the structure and succession of Ladd and Montgomery mountains show that a fault striking northwest, with a vertical displacement of many hundred feet, occurs between the two mountains, but no part of its outcrop is exposed. The Montgomery-Shoshone fault can be traced accurately along a part of its course, but after it passes into the flat southwest of the Polaris mine only its approximate location can be determined. Since the beds which form Bonanza Mountain have been depressed with respect to those which form Ladd s FIGURE 8.--Dlagram showing strikes of faults. Mountain by about as much as the vertical displacement of the Montgomery-Shoshone fault, it is certain that this fault, or one with approximately equal throw, passes under the was...
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New. Trade paperback (US). Glued binding. 170 p. In Stock. 100% Money Back Guarantee. Brand New, Perfect Condition, allow 4-14 business days for standard shipping. To Alaska, Hawaii, U.S. protectorate, P.O. box, and APO/FPO addresses allow 4-28 business days for Standard shipping. No expedited shipping. All orders placed with expedited shipping will be cancelled. Over 3, 000, 000 happy customers.
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