Fishery and Riparian Resources of Devils Postpile National Monument and Surrounding Waters
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Insights Into Rhyolite Magma Dome Systems Based on Mineral and Whole Rock Compositions at the Mono Craters, Eastern California
ABSTRACT INSIGHTS INTO RHYOLITE MAGMA DOME SYSTEMS BASED ON MINERAL AND WHOLE ROCK COMPOSITIONS AT THE MONO CRATERS, EASTERN CALIFORNIA The Mono Craters magmatic system, found in a transtensional tectonic setting, consists of small magmatic bodies, dikes, and sills. New sampling of the Mono Craters reveals a wider range of magmatic compositions and a more complex storage and delivery system than heretofore recognized. Space compositional patterns, as well as crystallization temperatures and pressures taken from olivine-, feldspar-, orthopyroxene-, and clinopyroxene-liquid equilibria, are used to create a new model for the Mono Craters magmatic system. Felsic magmas erupted throughout the entire Mono Craters chain, whereas intermediate batches only erupted at Domes 10-12 and 14. Mafic magmas are spatially restricted, having erupted only at Domes 10, 12 and 14. Data from the new whole rock analyses illustrates a linear trend. Fractional crystallization does not replicate this trend but rather the linear trend indicates magma mixing. This study also analyzes samples from the Mono Lake Islands and the June Lake Basalts and compares them to the Mono Craters. Although the Mono Lake Islands fall into the intermediate to felsic group, they contain distinctly higher Al2O3 and Na2O at a given SiO2. Therefore, this study concludes that the Mono Craters represent a distinct magmatic system not directly related to the magmatic activity that created the Mono Lake Islands. Michelle Ranee Johnson May 2017 INSIGHTS INTO RHYOLITE MAGMA DOME SYSTEMS BASED -
Visitor Guide to Devils Postpile and the Reds Meadow Valley
National Forest Service Visitor Guide to Devils Postpile and U.S. Department of Agriculture the Reds Meadow Valley National Park Service U.S. Department of the Interior The Post 2009-2010 What’s Inside Information and Services.................. 2 Ranger-led Activities Shuttle Bus Information.................... 3 Hiking ................................................ 4 Making the Most of Your Time Bear Safety......................................... 5 Maps .................................................. 6 Science and Resources Student Conservation Association Welcome to Devils Postpile Junior Ranger Program..................... 7 Volcanic Landscape Aquatic Hitchhikers and the Reds Meadow Valley Bookstores and Partners................... 8 Welcome to Reds Meadow Valley and Southern Sierra species of plants as “wanton destruction of scenery” displayed as an exhibit in the valley or and Devils Postpile in the spectacu- and animals converge along the river and enlisted the support of District in Mammoth. If you have any pho- lar Upper Middle Fork of the San corridor and in the many wetlands. Forester F.E. Olmsted and Univer- tos or stories you would like to share, Joaquin River Valley. Beauty abounds sity of California Professor Joseph N. please feel free to contribute these for in the forms of unusually rich and The value of the natural and recre- LeConte to evaluate the situation with possible inclusion in this exhibit. diverse flora and fauna, traditional ational resources was recognized in the hope of denying the permit and recreational opportunities and a 1890 with its inclusion in the initial protecting the area. Devils Postpile is also embarking on fascinating cultural history. boundaries of Yosemite National Park. its first ever general management plan, Their efforts, along with the support of in cooperation with the Inyo National Researchers, writers, visitors, and In 1905 the Devils Postpile formation, the Sierra Club, resulted in President Forest. -
Forested Communities of the Upper Montane in the Central and Southern Sierra Nevada
United States Department Forested Communities of the Upper of Agriculture Forest Service Montane in the Central and Southern Pacific Southwest Sierra Nevada Research Station Donald A. Potter General Technical Report PSW-GTR-169 Publisher: Pacific Southwest Research Station Albany, California Forest Service Mailing address: U.S. Department of Agriculture PO Box 245, Berkeley CA 94701-0245 Abstract (510) 559-6300 Potter, Donald A. 1998. Forested communities of the upper montane in the central and southern http://www.psw.fs.fed.us Sierra Nevada. Gen. Tech. Rep. PSW-GTR-169. Albany, CA: Pacific Southwest Research Station, Forest Service, U.S. Department of Agriculture; 319 p. September 1998 Upper montane forests in the central and southern Sierra Nevada of California were classified into 26 plant associations by using information collected from 0.1-acre circular plots. Within this region, the forested environment including the physiographic setting, geology, soils, and vegetation is described in detail. A simulation model is presented for this portion of the Sierra Nevada that refines discussions of climate, and disturbance regimes are described to illustrate the interaction between these features of the environment and vegetation in the study area. In the classification, plant associations are differentiated by floristic composition, environmental setting, and measurements of productivity. Differences in elevation, aspect, topographic setting, and soil properties generally distinguish each plant association described. A detailed description is presented for each plant association, including a discussion of the distribution, environment, vegetation, soils, productivity, coarse woody debris, range, wildlife, and management recommendations. A complete species list and tables for cross referencing specific characteristics of each association are provided. -
2011-2012 U.S
National Forest Service Visitor Guide to Devils Postpile and the U.S. Department of Agriculture Reds Meadow Valley National Park Service 2011-2012 U.S. Department of the Interior What’s Inside The Post Welcome A Century of Conservation 1911-2011 Shuttle Bus Information.................... 2 Information and Services.................. 3 Hiking ................................................ 4 Making the Most of Your Time Be Bear Aware................................... 5 Map ................................................... 6 First Bloom Ranger Led Programs Junior Ranger Program..................... 7 Volcanic Landscape Protecting Special Places Bookstores and Partners................... 8 SPECIAL CENTENNIAL INSERT: Articles and information about Devils Postpile National Monument’s 100th anniversary. Park the Car and Ride the Bus! Shuttle Bus and Fee Information Schedule The bus is mandatory for most visitors. Buses leave from the Village at Mam- See the chart below for prices. Tickets moth Lakes at 7:00am, 8:00am, 9:00am, can be purchased at any Mammoth 10:00am, 11:00am. Mountain ticket sales outlet including the Adventure Center, located in the Buses leave from the Mammoth Moun- main gondola building. tain Adventure Center at the following At which stop will I find... National Park Service times: U.S. Department of the Interior Parking for the shuttle bus is along the • 7:15am – 8:15 a.m. once an hour roadside near Mammoth Mountain • 9:00am – 5:00 p.m. every 20 min- Food and Bottled Water....... Main Lodge. Leashed and muzzled utes or less Devils Postpile Wildflower Walk................. National Monument dogs are welcome on buses. Please • 5:00pm – 7:00pm every 30 minutes be careful walking along the roadside Shadow Lake Trail............... -
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. -
Geologic Field-Trip Guide to Long Valley Caldera, California
Geologic Field-Trip Guide to Long Valley Caldera, California Scientific Investigations Report 2017–5022–L U.S. Department of the Interior U.S. Geological Survey COVER View southwestward across Long Valley Caldera and Sierra Nevada. Caldera depression, as wide as 30 km, formed during eruption of Bishop Tuff at 767 ka. Sierra consists of Mesozoic plutonic rocks, Mesozoic metavol- canic rocks, and Paleozoic marine metasedimentary strata. Patchy white exposures in caldera are lacustrine siltstones of middle Pleistocene age that are the top of a 700-m-thick accumulation of intracaldera lake sedi- ment. Sedimentation in the deep closed depression took 600,000 years to raise lake level to its threshold for overflow around 150 ka. Outlet arm of Lake Crowley reservoir leads into Owens River Gorge, which extends 30 km southeast across a welded Bishop Tuff outflow sheet. Overflow and draining of the caldera lake reincised a 200-m-deep precaldera gorge (in Mesozoic granodiorite) that had been diverted by 3.3-Ma basalt and later blanketed by the Bishop Tuff. Round Valley Fault is 2-km-high east-facing scarp at left. At lower center of image, precaldera Glass Mountain rhyolite edifice was truncated by caldera collapse and draped by complexly incised apron of Bishop Tuff. Photo is a NaturalVue satellite image mosaic, which has been extracted from a global dataset of natural-color Landsat-7 multispectral images compiled by MDA Information Systems, Inc. Cover image produced and processed by Joel E. Robinson. Imagery copyright 2010, MDA Information Systems, USGS, NASA. Geologic Field-Trip Guide to Long Valley Caldera, California By Wes Hildreth and Judy Fierstein With sections on A Refreshing Overview of the Bishop Tuff By Wes Hildreth Concealed Ring-Fault Zone of Long Valley Caldera By Wes Hildreth Overview of the Long Valley Hydrothermal System After Decades of Study By William C. -
Inyo National Forest
INYO NATIONAL FOREST WHITNEY PORTAL Alternative Transportation Study 2013 Form Approved REPORT DOCUMENTATION PAGE OMB No. 0704-0188 Publi c report i ng burden for thi s co ll ect ion of i nformat i on is est i mated to average 1 hour per response, i nc l uding the t i me for rev i ewing instructi ons, searchi ng data sources, gathering and mai nta ini ng the data needed, and compl et ing and reviewing the coll ect ion of i nformat ion. Send comments regarding thi s burden esti mate or any other aspect of thi s co ll ect i on of informat ion, i nc l uding suggesti ons for reduci ng th i s burden to Washi ngton Headquarters Servi ce, Directorate for Informati on Operat i ons and Reports, 1215 Jefferson Davi s Highway, Sui te 1204, Ar li ngton, VA 22202-4302, and to the Offi ce of Management and Budget, Paperwork Reducti on Project (0704-0188) Washi ngton, DC 20503. PLEASE DO NOT RETURN YOUR FORM TO THE ABOVE ADDRESS. 1. REPORT DATE (DD-MM-YYYY) 2. REPORT DATE 3. DATES COVERED (From - To) 15-12-2013 Study July 2010 - December 2013 4. TITLE AND SUBTITLE 5a. CONTRACT NUMBER Inyo National Forest Mt. Whitney Portal Alternative Transportation 09-IA-11132429-098 System Study 5b. GRANT NUMBER 5c. PROGRAM ELEMENT NUMBER 6. AUTHOR(S) 5d. PROJECT NUMBER Deborah Tyrone NFXF01 5e. TASK NUMBER 5f. WORK UNIT NUMBER 7. PERFORMING ORGANIZATION NAME(S) AND ADDRESS(ES) 8. PERFORMING ORGANIZATION USDA - Forest Service, Inyo National Forest REPORT NUMBER 9. -
Natural Resource Condition Assessment for Devils Postpile National Monument
National Park Service U.S. Department of the Interior Natural Resource Stewardship and Science Natural Resource Condition Assessment for Devils Postpile National Monument Natural Resource Report NPS/DEPO/NRR—2014/889 ON THE COVER Soda Springs Meadow Photograph courtesy of Devils Postpile National Monument Natural Resource Condition Assessment for Devils Postpile National Monument Natural Resource Report NPS/DEPO/NRR—2014/889 Bill Kuhn National Park Service Yosemite National Park PO Box 700 El Portal, CA 95318 Terressa Whitaker National Park Service Yosemite National Park PO Box 700 El Portal, CA 95318 December 2014 U.S. Department of the Interior National Park Service Natural Resource Program Center Fort Collins, Colorado The National Park Service, Natural Resource Stewardship and Science office in Fort Collins, Colorado, publishes a range of reports that address natural resource topics. These reports are of interest and applicability to a broad audience in the National Park Service and others in natural resource management, including scientists, conservation and environmental constituencies, and the public. The Natural Resource Report Series is used to disseminate high-priority, current natural resource management information with managerial application. The series targets a general, diverse audience, and may contain NPS policy considerations or address sensitive issues of management applicability. All manuscripts in the series receive the appropriate level of peer review to ensure that the information is scientifically credible, technically accurate, appropriately written for the intended audience, and designed and published in a professional manner. This report received informal and formal peer review by administrative staff and subject-matter experts, some of whom were not directly involved in the collection, analysis, or reporting of the data, and whose background and expertise put them on a par technically and scientifically with the authors of the information. -
Devils Postpile Story N
Devils Postpile Story N. King Huber Geologist U.S. Geological Survey Wymond W. Eckhardt Ranger and Park Manager National Park Service Illustrated by Joseph L. Medeiros CONTENTS Introduction 1 Geologic Story 3 Monument History 21 Plants and Animals 25 Selected References 29 Epilogue 31 Copyright© 1985 by INTRODUCTION Devils Postpile National Monument The Sequoia Natural History Association Three Rivers, California 93271 Devils Postpile National Monument ·Iies on the in cooperation with the western slope of the Sierra Nevada near the resort National Park Service community of Mammoth Lakes, California. The Department of the Interior BOO-acreMonument is two and one-half miles long, one-half mile wide, and is at an elevation of about 7,600 feet. The Monument includes one feature of dominant significance: a volcanic formation known as Devils Postpile. Also in the area are Soda Springs and Rainbow Falls. Pumice is the dominant rock- type encountered by the visitor, however, basalt and granite are just under the surface and crop out in many places throughout the area. The plants and animals in the Monument are those typical of the lodgepole pine-red fir forests of the western slope of the Sierra Nevada. The approach road to the Monument passes through Mammoth Lakes from U.S. Highway 395 on the east side of the Sierra Nevada. Beyond Minaret Summit is a paved mountain road that is passable only during the summer months. In the winter the area is closed - the snow may be more than fifteen feet deep. Food and lodging can be obtained at Mammoth Lakes or at nearby Reds Meadow. -
Download Manuscript 4 9 17 Bbray Bullvolc Manuscript.Docx Click Here to View Linked References
4 9 17 BBray BullVolc manuscript Click here to download Manuscript 4 9 17 BBray BullVolc manuscript.docx Click here to view linked References 1 Mafic replenishment of multiple felsic reservoirs at the Mono domes and Mono 2 Lake islands, California 3 4 Brandon Bray1, John Stix1, and Brian Cousens2 5 6 1. Department of Earth & Planetary Sciences, McGill University, 3450 University Street, 7 Montreal, Quebec H3A 0E8, Canada 8 2. Ottawa-Carleton Geoscience Centre, Department of Earth Sciences, Carleton 9 University, 1125 Colonel By Drive, Ottawa, Ontario K1S 5B6, Canada 10 11 Abstract 12 The Mono Basin has been the site of frequent volcanic activity over the past 60,000 13 years, including the emplacement of the Mono domes and Mono Lake islands. The Mono 14 Basin lavas are the youngest and most poorly understood products of the Long Valley 15 Volcanic Field. We have undertaken a study of Mono Basin volcanism encompassing 16 whole-rock major and trace element, Sr, Nd, Pb, and O isotopic, and electron microprobe 17 glass, plagioclase, and amphibole analyses. Variations in major and trace elements 18 suggest that fractional crystallization of feldspar (Sr, K2O), apatite (P2O5), 19 titanomagnetite (V), zircon (Zr), and allanite (La, Ce) has influenced the evolution of the 20 Mono Basin lavas. Field observations, petrography, and chemistry together demonstrate 21 that injection of more mafic magma is a common process throughout the Mono Basin. 22 Mafic enclaves of the Mono domes are stretched and rounded, with chilled margins 23 between enclave and host rhyolite. Thin sections reveal millimeter-scale inclusions of 1 24 rhyolite in the enclaves and vice versa along the host-enclave border. -
Geological Society of America Bulletin
Downloaded from gsabulletin.gsapubs.org on December 8, 2010 Geological Society of America Bulletin Eruption chronology and petrologic reconstruction of the ca. 8500 yr B.P. eruption of Red Cones, southern Inyo chain, California Brandon Browne, Marcus Bursik, Justin Deming, Michael Louros, Antonio Martos and Scott Stine Geological Society of America Bulletin 2010;122;1401-1422 doi: 10.1130/B30070.1 Email alerting services click www.gsapubs.org/cgi/alerts to receive free e-mail alerts when new articles cite this article Subscribe click www.gsapubs.org/subscriptions/ to subscribe to Geological Society of America Bulletin Permission request click http://www.geosociety.org/pubs/copyrt.htm#gsa to contact GSA Copyright not claimed on content prepared wholly by U.S. government employees within scope of their employment. Individual scientists are hereby granted permission, without fees or further requests to GSA, to use a single figure, a single table, and/or a brief paragraph of text in subsequent works and to make unlimited copies of items in GSA's journals for noncommercial use in classrooms to further education and science. This file may not be posted to any Web site, but authors may post the abstracts only of their articles on their own or their organization's Web site providing the posting includes a reference to the article's full citation. GSA provides this and other forums for the presentation of diverse opinions and positions by scientists worldwide, regardless of their race, citizenship, gender, religion, or political viewpoint. Opinions presented in this publication do not reflect official positions of the Society.