2 edition of Structure and metamorphism in the Mono Craters quadrangle, Sierra Nevada, California found in the catalog.
Structure and metamorphism in the Mono Craters quadrangle, Sierra Nevada, California
Ronald Wayne Kistler
|Statement||by Ronald W. Kistler.|
|Series||Contributions to general geology, Geological Survey bulletin -- 1221-E|
|The Physical Object|
|Pagination||v, 53 p. :|
|Number of Pages||53|
Quadrangle, Boulder and Jefferson Counties, Colorado IE Department of the Interior Structure and Metamorphism in the Mono Craters Quadrangle, Sierra Nevada, California IF Department of the Interior Igneous Geology of the Dry Mountain Quadrangle, Jefferson County, Montana The word "Metamorphism" comes from the Greek: meta = after, morph = form, so metamorphism means the after form. In geology this refers to the changes in mineral assemblage and texture that result from subjecting a rock to conditions such pressures, temperatures, and chemical environments different from those under which the rock originally formed.
A Checklist Flora of the Mono Lake Basin, Mono County, California and Mineral County, Nevada.: definition of Upper Mono Basin; Literature Referring To This Location: Kistler, Ronald W. Structure and Metamorphism in the Mono Craters Quadrangle, Sierra Nevada, California. The Long Valley volcanic field (Bailey, ) is part of an active regional transtensional zone at the Sierra Nevada-Basin and Range eruptive history overlaps in time with smaller mafic-to-silicic volcanic fields along this transition zone, at Big Pine (Bateman, ) and Coso (Duffield and Bacon, ), respectively, 50 and km SSE of Long by:
Understanding the Impact Cratering Process: a Simple Approach At some time in their life nearly every girl, boy (and adult) has thrown pebbles or cobbles into mud and watched nice round form. The force of the impacts create circular structures with raised rimmed wall; spatters of mud and smaller circular secondary craters may be seen (Fig. 1). Schweickert, R.A., and Lahren, M.M., , Tectonics of the east-central Sierra Nevada--Saddlebag Lake and Northern Ritter Range pendants, in Lahren, M.M., Trexler, J.
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Structure and metamorphism in the Mono Craters quadrangle, Sierra Nevada, California / by Ronald W. Kistler. Format Online Resource Book Published [Washington, D.C.]: United States Department of the Interior, Geological Survey, Washington: United States Government Printing Office Description.
Structure and metamorphism in the Mono Craters quadrangle, Sierra Nevada, California (OCoLC) Material Type: Government publication, National government publication: Document Type: Book: All Authors / Contributors: Ronald Wayne Kistler; Geological Survey (U.S.).
Get this from a library. Structure and metamorphism in the Mono Craters quadrangle, Sierra Nevada, California. [Ronald Wayne Kistler; Geological Survey (U.S.),]. complex in the Mono Basin and in part of the Sierra Nevada. The Mono Craters quadrangle map (1: 62,) was photographic ally enlarged toas a base for geologic mapping.
Selected areas of this map were photographically enlarged (1 in. = 1, ft.) to permit detailed mapping in parts of the structurally complex roof by: USGS San Diego Hydrogeology project information Search Search Structure and California book in the Mono Crater quadrangle, Sierra Nevada, California: U.S.
Geological Survey Bulletin E, p. Relationship between seismicity and geologic structure in southern California: Seismological Society of America Bulletinp. USGS Bulletins 1 - USGS Bulletins California book USGS Bulletins - USGS Bulletins - B E / Kistler, R.
/ STRUCTURE AND METAMORPHISM IN THE MONO CRATERS QUADRANGLE, SIERRA NEVADA, CALIFORNIA,pb, 53 pages, 2 plates (in pocket), 6 figs., $ 9. Part I. Experiments on the stability of andalusite.
Part II. Studies of contact metamorphism in the Sierra Nevada, California: EART: KEW: Ph.D. The geology of the Mono Craters Quadrangle, California: NRLF: KNITTLE: and applications to the study of the crustal structure of California Coast Ranges: MAIN: LINN: M.A.
GEOL: Geology of. Most craters are volcanic, and although more than 95% of the world's volcanic rocks are basaltic, there are numerous categories (to be mentioned below). The complex explosion and collapse structures known as calderas (q.v.) often containing secondary craters, are treated separately.
Abstract. Metamorphism may be defined as any significant change in the texture, mineralogy, and/or bulk composition of a chiefly solid rock—not including partial or complete melting on the one hand, and weathering processes on the other—which results from the attendance of physical and chemical conditions different from those present during formation of the by: Metamorphism is driven by heat and pressure.
High heat can cause rock minerals to recrystallize in the process of metamorphism. Rocks that are buried deep in Earth are subjected to equal pressure from all directions. This confining pressure can cause a phase change but does not fold rocks. Click on the book chapter title to read more.
The Inyo Craters are a km-long chain of silicic lava domes, lava flows, and explosion craters along the eastern margin of Sierra Nevada south of Mono Craters near the town of Mammoth. Inyo Craters overtop the NW rim of the Pleistocene Long Valley caldera and extend onto the caldera floor, but are chemically and magmatically part of a different volcanic system.
Located in the Basin and Range province, Mono Basin is a 1 to 3 million year old, structural depression bordered by a fault escarpment on the eastern margin of Sierra Nevada (Mono, ). When the Farallon plate finished subducting under the North American plate 20 m.y.a, the Pacific plate started to slide northwest against the North American plate (Tierney, ).
potassium-argon ages of recent rhyolites sin) [ 11 ]. This suggests a maximum age of approxi- mat years for the southern coulde [ 13]. The available geologic evidence does not indicate whether the Mono and Inyo Craters eruptions oc- curred over a period of a few years or tens of thou- Cited by: Contact metamorphism (also called thermal metamorphism) is the process by which the country rock that surrounds a hot magma intrusion is metamorphosed by the high heat flow coming from the intrusion.
The zone of metamorphism that surrounds the intrusion is called the halo (or aureole) and rarely extends more than meters into the country rock. (D) Geology of the Eldorado Springs quadrangle, Boulder and Jefferson Coun ties, Colorado, by John D.
Wells. (E) Structure and metamorphism in the Mono Craters quadrangle, Sierra Nevada, California, by Ronald W.
Kistler. (F) Igneous geology of the Dry Mountain quadrangle, Jefferson County, Mon tana, by Harold J. by: Geology of Paleozoic Rocks in Eastern Sierra Nevada Roof Pendants, California lar to those of the same age in the Inyo and White Mountains (Stevens and Greene, ; Stevens and Stone, in prep).
Volcanological perspectives on Long Valley, Mammoth Mountain, and Mono Craters: several contiguous but discrete systems. Journal of Volcanology and Geothermal Research.
() Kistler, Ronald W. Structure and Metamorphism in the Mono Craters Quadrangle, Sierra Nevada, California. USGS Bulletin E: Structure and metamorphism in the Mono Craters Quadrangle, Sierra Nevada, California.
By Ronald W. Kistler. 53p., 2 plates in. MS Book and Mineral Company Geology and Mining History of California I - Federal Publications And Mabey, D.
/ STRATIGRAPHY AND STRUCTURE, DEATH VALLEY, CALIFORNIA,pb, pages, 3 plates (in pocket), figs., 26 tables, $ 45 R. / STRUCTURE AND METAMORPHISM IN THE MONO CRATERS QUADRANGLE, SIERRA NEVADA, CALIFORNIA. Full text of "Monthly catalog of United States Government publications" See other formats.Benioff, H., and B.
Gutenberg, The Mammoth "Earthquake Fault" and related features in Mono County, California, Seismol. Soc. Am. Bull., 29,Mono Lake, the Sierra Nevada mountain range, Mono Craters and associated features are all visible from the Panum Crater. A rough trail on pumice (read: squishy footing) leads to the rim and miles of further hiking takes you to the spectacular obsidian core of the volcano which erupted years ago.