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Cenozoic Volcanic Rocks of the Devils Postpile Quadrangle, Eastern Sierra Nevada California

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Cenozoic Volcanic Rocks of the Devils Postpile Quadrangle, Eastern Sierra Nevada California Cenozoic Volcanic Rocks of the Devils Postpile Quadrangle, Eastern Sierra Nevada California By N. KING HUBER and C. DEAN RINEHART SHORTER CONTRIBUTIONS TO GENERAL GEOLOGY GEOLOGICAL SURVEY PROFESSIONAL PAPER 554-D Prepared in cooperation with the California Division of Mines and Geology UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1967 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 CONTENTS Page Tuff of Reds Meadow Continued Abstract______________________________ Dl Zonation in the tuff Continued Page Introduction. ___________________________ 1 Upper flow unit- _ _____ Dll Petrologic and chemical data_____________ 2 Lower zone of partial welding- 11 Microscopic petrography___________ 2 ____ 11 Chemical data______________________ 2 12 Classification______________________ __ 12 Andesite of Deadman Pass___-________ _____ 13 _ __ 14 Quartz latite of Two Teats__________ i7 Andesite from Deadman-Glass Creeks area- 9 Andesite from Dry Creek area__ _ __ _ _ _____ 15 Andesite of Pumice Butte. ._._._ - - ___ 16 Tuff of Reds Meadow_-----__---_-------- 10 __ __ 16 Zonation in the tuff_----_--__-----___- 10 Basalt of the Red Cones. _____ 16 Lower flow unit________________. 10 Rhyolite _ _ _ __ _ __- _____ 17 Lower zone of no welding____ 10 Pumice- _ _____ 19 Lower zone of partial welding- 10 __ _ 19 Zone of intense welding_____ 10 _____ 20 Upper zone of partial welding. 11 References. _ _ _ 20 ILLUSTRATIONS Page FKONTISPIECE. Photograph showing well-developed columnar jointing in andesite at the Devils Postpile. PLATE 1. Geologic map showing Cenozoic volcanic rocks of the Devils Postpile quadrangle, Sierra Nevada, Calif __ In pocket FIGTJBE 1. Index map of the Devils Postpile quadrangle.________________________________--------_----------- D2 2. Variation diagram of the Mammoth Lakes volcanic suite showing classification according to the "alkali- lime index"________________________________________________________________________________ 4 3. "Differentiation trend" diagram for the Mammoth Lakes volcanic suite.____________-_-____----------- 6 4. Silica-refractive-index diagram for volcanic rocks of the Mammoth Lakes area_______________---------- 7 5. Diagram showing range in percentage of silica of some of the mapped volcanic units as inferred from refrac­ tive indices of fused samples________________________-_________--__-_--_--__-----__-----_--__- 7 6. Photograph of basal part of quartz latite of Two Teats on east side of San Joaquin Mountain-____-___-_- 9 7, 8. Photomicrographs of tuff of Reds Meadow 7. Lower flow unit ______________________________________________________________-_--__ 11 8. Upper flow unit_________________________________________________-_-_-__-_------ -_ 12 9. West-east section in vicinity of Rainbow Falls showing reconstructed surface of the tuff of Reds Meadow 13 10-13. Photographs of 10. Polygonal joint pattern displayed by tops of columns in the Devils Postpile___----------- -_ 14 11. Northernmost of the two Red Cones as viewed from the southern cone______---___------- _ 17 12. Rhyolite dome south of Deadman Creek as seen from Deer Mountain-_____--__-__-_------ _ 17 13. Upper surface of rhyolite dome south of Glass Creek showing typical irregular blocky surface __ 17 14. Vertical aerial photographs of Deer Mountain area, mounted as a stereopair_____________________ ___ 18 15. Photograph showing view of Inyo Craters from Deer Mountain____________________________________ 19 TABLES Page TABLE 1. Ages of Cenozoic volcanic rocks of the Devils Postpile quadrangle__-_-_---_-_----------------_-_-_--- Dl 2. Petrographic summary of the volcanic rocks_____________________________________--__----_-------_- 3 3. Chemical analyses and norms of the volcanic rocks______________________________________________ 5 SHORTER CONTRIBUTIONS TO GENERAL GEOLOGY CENOZOIC VOLCANIC ROCKS OF THE DEVILS POSTPILE QUADRANGLE, EASTERN SIERRA NEVADA, CALIFORNIA By N. KING HUBER and C. DEAN KINEHART ABSTRACT rangle to the east (Rinehart and Ross, 1964) allows the Cenozoic volcanic rocks of the Devils Postpile quadrangle are division of the Cenozoic volcanic rocks of the Devils of late Pliocene to Recent age and are divided into 11 map units. Postpile quadrangle into 11 mappable units. Scattered The suite is alkalic-calcic and ranges in composition from basalt erosional remnants of uncertain stratigraphic position to rhyolite. It includes a rhyolitic welded ash-flow tuff which is have tentatively been assigned to these units, although probably correlative with the Bishop Tuff, although the two some of the remnants may represent additional episodes units are geographically isolated by the Sierra Nevada drainage divide. The Devils Postpile itself is a classic example of co­ of volcanic activity not otherwise recognized. Table 1 lumnar jointing in the lower part of a lava flow. lists the 11 units and their radiometric ages where avail­ able, and plate 1 shows their distribution. INTRODUCTION TABLE 1. Ages of Cenozoic volcanic rocks of the Devils Postpile The Devils Postpile quadrangle straddles the crest of quadrangle the Sierra Nevada southeast of Yosemite National Park [See text for source and other data regarding individual age determinations] and contains the Devils Postpile National Monument Potassium-argon age (fig. 1). The pre-Cenozoic rocks of the quadrangle in­ Age and unit determination 1 clude Paleozoic and Mesozoic metasedimentary and met- (million years) avolcanic rocks. The metamorphic rocks have been in­ Recent: Rhyolite-_ . __. ._.... truded by various granitoid igneous rocks, which form Basalt of the Red Cones___________ Pleistocene or Recent: a part of the composite Sierra Nevada batholith (Bate- Olivine-bearing quartz latite________ Pleistocene: man and others, 1963; Huber and Rinehart, 1965a). By Andesite of Pumice Butte___....____ Andesite from Dry Creek area_._____ late Tertiary time the Sierra Nevada had attained ap­ Quartz latite of Mammoth Mountain_.... 0.37±0.04; 0.18±0.09 Andesite of the Devils Postpile.. ..... 0.94±0.15; 0.63±0.35 proximately its present overall configuration, except for Tuff of Reds Meadow__..__......__. 0.66±0.04; (1.1); (1.4) Pliocene or Pleistocene: later modifications caused by faulting, uplift, and in­ Andesite from Deadman-Glass Creeks area- Pliocene: creased dissection. Regional volcanism began during Quartz latite of Two Teats._.__-___ 3.0±0.1 the late Tertiary and has continued spasmodically to the Andesite of Deadman Pass..________ 3.1±0.1; 3.3±0.1; 3.5±0.1 present. 1 The plus-or-minus figure that accompanies these age determinations is not an estimate of accuracy but rather an estimate of analytical precision at the 68-percent The Cenozoic volcanic rocks of the Devils Postpile confidence interval. Figures in parentheses are two older ages from samples con­ quadrangle resulted from several types of eruption taminated with granite; youngest age is accepted as most reliable. throughout late Tertiary and Quaternary time; the In order to provide a background for description of forms of eruption include domes, lava flows, ash flows, the individual volcanic units, a general summary of and extensive pumice falls. The volcanic rocks range in petrologic and chemical data is presented for the entire composition from basalt to rhyolite, the oldest being ba­ volcanic suite. Following this, field relationships and saltic to andesitic and the youngest, rhyolitic; however, general characteristics of each volcanic unit are de­ most mafic and felsic rocks alternate haphazardly with­ scribed in order of decreasing age, rather than by pet­ out regard to stratigraphic position. For this reason rologic type, to provide a clearer picture of the sequence and because many of the volcanic units remain only as of events. scattered erosional remnants, correlations are difficult. We wish to thank G. B. Dalrymple for making his Interpretation of the volcanic history has been greatly potassium-argon age determinations available to us in assisted by potassium-argon age dating. advance of their being published and Gerhard Schu- Mapping in the Devils Postpile quadrangle (Huber macher for the use of some of his excellent photographs and Rinehart, 1965a) and in the Mount Morrison quad­ of the Mammoth Lakes region. We also express our Dl D2 SHORTER CONTRIBUTIONS TO GENERAL GEOLOGY FIGURE 1. Location of the Devils Postpile quadrangle and the adjacent Mount Morrison quadrangle. appreciation to R. J. Janda for many stimulating dis­ ents and to reveal the large proportion of indeterminate cussions of the interrelations of volcanic and glacial material occult in the groundmass of most of the rocks. events. Minerals listed in groups of two or more are given in order of decreasing abundance. In most specimens PETROLOGIC AND CHEMICAL DATA range in anorthite content of the plagioclase was deter­ MICROSCOPIC PETROGRAPHY mined from twinning relationships. Olivine is typi­ cally magnesium rich. Data obtained from the petrographic study of the volcanic rocks are recorded in table 2. Percentages CHEMICAL DATA of constituents are based upon visual estimates obtained Table 3 presents chemical analyses and norms for from thin-section study and are little more than rough seven samples of volcanic rock from the Devils Postpile approximations. The percentages, however, can be ef­ quadrangle and one from the Mount Morrison quad­ fectively used to distinguish major and minor
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