Name: The Geology and Remarkable Thermal Activity of Norris Geyser Basin, Yellowstone National Park, Wyoming: Usgs Professional Paper 1456 (en Inglés)
Price: 84617.00 COP
Availability: InStock
Author: White, Donald Edward
ISBN: 9781287014072

portada The Geology and Remarkable Thermal Activity of Norris Geyser Basin, Yellowstone National Park, Wyoming: Usgs Professional Paper 1456 (en Inglés)

The Geology and Remarkable Thermal Activity of Norris Geyser Basin, Yellowstone National Park, Wyoming: Usgs Professional Paper 1456 (en Inglés)

Formato

Libro Físico

Autor

Donald Edward White

Editorial

Bibliogov

Idioma

Inglés

N° páginas

Encuadernación

Tapa Blanda

Dimensiones

24.6 x 18.9 x 0.5 cm

Peso

0.19 kg.

ISBN13

9781287014072

Categorías

Política y gobierno

The Geology and Remarkable Thermal Activity of Norris Geyser Basin, Yellowstone National Park, Wyoming: Usgs Professional Paper 1456 (en Inglés)

Donald Edward White (Autor) · Bibliogov · Tapa Blanda

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Reseña del libro "The Geology and Remarkable Thermal Activity of Norris Geyser Basin, Yellowstone National Park, Wyoming: Usgs Professional Paper 1456 (en Inglés)"

Norris Geyser Basin, normally shortened to Norris Basin, is adjacent to the north rim of the Yellowstone caldera at the common intersection of the caldera rim and the Norris-Mammoth Corridor, a zone of faults, volcanic vents, and thermal activity that strikes north from the caldera rim to Mammoth Hot Springs. An east-west fault zone terminates the Gallatin Range at its southern end and extends from Hebgen Lake, west of the park, to Norris Basin. No local evidence exists at the surface in Norris Basin for the two oldest Yellowstone volcanic caldera cycles ( 2.0 and 1.3 m.y.B.P.). The third and youngest cycle formed the Yellowstone caldera, which erupted the 600,000-year-old Lava Creek Tuff. No evidence is preserved of hydrothermal activity near Norris Basin during the first 300,000.years after the caldera collapse. Glaciation probably removed most of the early evidence, but erratics of hot-spring sinter that had been converted diagenetically to extremely hard, resistant chalcedonic sinter are present as cobbles in and on some moraines and till from the last two glacial stages, here correlated with the early and late stages of the Pinedale glaciation