2009 Landscape Evolution at an Active Plate Margin
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
AR4000 Laser Rangefinder Users Manual
AccuRange 4000™ Laser Rangefinder AccuRange™ Line Scanner User’s Manual LLL004001 – Rev. 2.7 For use with AR4000™ and Line Scanner September 5, 2008 Acuity A product of Schmitt Industries, Inc. 2765 NW Nicolai St. Portland, OR 97210 www.acuitylaser.com Limited Use License Agreement YOU SHOULD CAREFULLY READ THE FOLLOWING TERMS AND CONDITIONS BEFORE OPENING THE PACKAGE CONTAINING THE COMPUTER SOFTWARE AND HARDWARE LICENSED HEREUNDER. CONNECTING POWER TO THE MICROPROCESSOR CONTROL UNIT INDICATES YOUR ACCEPTANCE OF THESE TERMS AND CONDITIONS. IF YOU DO NOT AGREE WITH THEM, YOU SHOULD PROMPTLY RETURN THE UNIT WITH POWER SEAL INTACT TO THE PERSON FROM WHOM IT WAS PURCHASED WITHIN FIFTEEN DAYS FROM DATE OF PURCHASE AND YOUR MONEY WILL BE REFUNDED BY THAT PERSON. IF THE PERSON FROM WHOM YOU PURCHASED THIS PRODUCT FAILS TO REFUND YOUR MONEY, CONTACT SCHMITT INDUSTRIES INCORPORATED IMMEDIATELY AT THE ADDRESS SET OUT BELOW. Schmitt Industries Incorporated provides the hardware and computer software program contained in the microprocessor control unit, and licenses the use of the product to you. You assume responsibility for the selection of the product suited to achieve your intended results, and for the installation, use and results obtained. Upon initial usage of the product your purchase price shall be considered a nonrefundable license fee unless prior written waivers are obtained from Schmitt Industries incorporated. LICENSE a. You are granted a personal, nontransferable and non-exclusive license to use the hardware and software in this Agreement. Title and ownership of the hardware and software and documentation remain in Schmitt Industries, Incorporated; b. the hardware and software may be used by you only on a single installation; c. -
The Bearhead Rhyolite, Jemez Volcanic Field, NM
Journal of Volcanology and Geothermal Research 107 32001) 241±264 www.elsevier.com/locate/jvolgeores Effusive eruptions from a large silicic magma chamber: the Bearhead Rhyolite, Jemez volcanic ®eld, NM Leigh Justet*, Terry L. Spell Department of Geosciences, University of Nevada, Las Vegas, NV, 89154-4010, USA Received 23 February 2000; accepted 6 November 2000 Abstract Large continental silicic magma systems commonly produce voluminous ignimbrites and associated caldera collapse events. Less conspicuous and relatively poorly documented are cases in which silicic magma chambers of similar size to those associated with caldera-forming events produce dominantly effusive eruptions of small-volume rhyolite domes and ¯ows. The Bearhead Rhyolite and associated Peralta Tuff Member in the Jemez volcanic ®eld, New Mexico, represent small-volume eruptions from a large silicic magma system in which no caldera-forming event occurred, and thus may have implications for the genesis and eruption of large volumes of silicic magma and the long-term evolution of continental silicic magma systems. 40Ar/39Ar dating reveals that most units mapped as Bearhead Rhyolite and Peralta Tuff 3the Main Group) were erupted during an ,540 ka interval between 7.06 and 6.52 Ma. These rocks de®ne a chemically coherent group of high-silica rhyolites that can be related by simple fractional crystallization models. Preceding the Main Group, minor amounts of unrelated trachydacite and low silica rhyolite were erupted at ,11±9 and ,8 Ma, respectively, whereas subsequent to the Main Group minor amounts of unrelated rhyolites were erupted at ,6.1 and ,1.5 Ma. The chemical coherency, apparent fractional crystallization-derived geochemical trends, large areal distribution of rhyolite domes 3,200 km2), and presence of a major hydrothermal system support the hypothesis that Main Group magmas were derived from a single, large, shallow magma chamber. -
Stratigraphy and Geochemistry of Volcanic Rocks in the Lava Mountains, California: Implications for the Miocene Development of the Garlock Fault
Geological Society of America Memoir 195 2002 Stratigraphy and geochemistry of volcanic rocks in the Lava Mountains, California: Implications for the Miocene development of the Garlock fault Eugene I. Smith Alexander Sa´nchez Deborah L. Keenan Department of Geoscience, University of Nevada, Las Vegas, Nevada 89154-4010, USA Francis C. Monastero Geothermal Program Office, Naval Air Weapons Station, China Lake, California 93555-6001, USA ABSTRACT Volcanism in the Lava Mountains occurred between 11.7 and 5.8 Ma and was contemporaneous with sinistral motion on the Garlock fault. Volcanic rocks, equiv- alent in age and chemistry to those in the Lava Mountains, crop out 40 km to the southwest in the El Paso Mountains across the Garlock fault. Three chemical groups of volcanic rocks erupted in the Lava Mountains over a period of 5 m.y. These are (1) andesite of Summit Diggings, Almond Mountain volcanic section, and Lava Moun- tains Andesite, (2) basalt of Teagle Wash, and (3) tuffs in the northeastern Lava Moun- tains and dacite in the Summit Range. Volcanic rocks of each group have distinctive chemical signatures useful for correlation of units across the Garlock fault. Our work demonstrated that tuffs in the Almond Mountain volcanic section may be equivalent to a tuff in member 5 of the Miocene Dove Spring Formation, El Paso Mountains. The basalt of Teagle Wash probably correlates with basalt flows in member 4, and tuffs in the northeast Lava Mountains may be equivalent to tuff of member 2. Cor- relation of these units across the Garlock fault implies that the Lava Mountains were situated south of the El Paso Mountains between 10.3 and 11.6 Ma and that 32–40 km of offset occurred on the Garlock fault in ϳ10.4 m.y., resulting in a displacement rate of 3.1 to 3.8 mm/yr. -
Acknowledgments
DATING TECHNIQUES 3 Schultz's definition (1937, p.79) of the Coso should be clarified because the lava flows in the Coso Range have a wide age range. We believe that the lava flows referred to by Schultz are the rhyodacite flows on the Haiwee Ridge (fig. 1) described in the section on Pliocene rhyodacite lava flows. Parts of the Coso Formation have been described by Hopper (1947), Power (1959, 1961), Bacon and Duffield (1978), Duffield, Bacon, and Roquemore (1979), Duffield, Bacon, and Dalrymple (1980), and Giovannetti (1979a, b). Deposits mapped as the Coso (fig. 1) Occur in the Haiwee Reservoir (Stinson, 1977a), Keeler (Stinson, 1977b), and Darwin (Hall and MacKevett, 1962) 15-minute quadrangles and have been mapped in the Coso volcanic field (Duffield and Bacon, 1981). Potassium-argon dating of volcanic rocks intercalated with, and overlying, the Coso Formation has been used by Evernden, Savage, Curtis, and James (1964), Bacon, Giovannetti, Duffield, and Dalrymple (1979), and Duffield, Bacon, and Dalrymple (1980) to constrain the age of the Coso. In this report, we review these potassium-argon ages and present additional data that provide more accurate limits on the age of the Coso Formation. ACKNOWLEDGMENTS We thank C. A. Repenning for advice on paleontologic aspects of this study. G. R. Roquemore contributed valuable observations offieldrela- tions of pyroclastic rocks near Sugar Loaf. J. Metz painstakingly prepared and analyzed glass fractions of tuffs. C. E. Meyer and M. J. Woodward kindly determined fission-track ages of zircons. Part of this report is based on the second author's M. S. -
"A Review of Pertinent Literature on Volcanic-Magmatic and Tectonic
CNWRA 92 025 ~~~_- _ -N A A0on 0 ~~~~~~~~- 0 -~~~ A I M Prepared for Nuclear Regulatory Commission Contract NRC-02-88-005 Prepared by Center for Nuclear Waste Regulatory Analyses San Antonio, Texas September 1992 462.2 --- T1993032400 0 1 A Review of Pertinent Lite-rture on Volcanic-Magmatic and Tectonic History of the Basin CNWRA 92-025 Property of CNWRA Library A REVIEW OF PERTINENT LITERATURE ON VOLCANIC- MAGMATIC AND TECTONIC HISTORY OF THE BASIN AND RANGE Prepared for Nuclear Regulatory Commission Contract NRC-02-88-005 Prepared by Gerry L. Stirewalt Stephen R. Young Kenneth D. Mahrer Center for Nuclear Waste Regulatory Analyses San Antonio, Texas September 1992 ABSTRACT The long-range goal of the Volcanism Research Project is to assess likelihood of volcanic and magmatic activity in the Yucca Mountain area and the potential for disruption of a repository at Yucca Mountain by that activity. To this end, this report discusses extent of available volcanic and tectonic data for the Basin and Range Physiographic Province, assesses usefulness of these data for constraining conceptual models of tectonism and associated volcanism in the Basin and Range, and addresses use of nonlinear dynamics for analyzing patterns of volcanism. Based on data from review of existing literature, the following conclusions and recommendations are drawn to provide guidance for future work in the remaining tasks of this project: (i) middle to late Cenozoic (i.e., less than 55 million years ago) volcanism in the Basin and Range Province can be broadly correlated -
2021 Magazine
July 2021 Welcome to the July 2021 edition of BADWATER® Magazine! We are AdventureCORPS®, producers of ultra-endurance sports events and adventure travel across the globe, and the force behind the BADWATER® brand. This magazine celebrates the entire world-wide Badwater® / AdventureCORPS® series of races, all the Badwater Services, Gear, Drinks, and Clothing, and what we like to call the Badwater Family and the Badwater Way of Life. Adventure is our way of life, so – after the sad and disastrous 2020 when we were not able to host any of our life-changing events – we are pleased to be fully back in action in 2021! Well, make that almost fully: Due to pandemic travel bans still in place, international participation in our USA-based events is not where we want it and that’s really unfortunate. Badwater 135 is the de facto Olympics of Ultrarunning and the 135-Mile World Championship, so we always want as many nationalities represented as possible. (The inside front cover of this magazine celebrates all sixty-one nationalities which have been represented on the Badwater 135 start line over the years.) Our new six-day stage race across Armenia – Artsakh Ultra – will have to wait yet another year to debut in 2022, two years later than planned. But it will be incredible, the ultimate stage race with six days of world-class trail running through several millennia of incredible culture and history, and across the most dramatic and awe-inspiring landscapes. This year, we are super excited to have brought two virtual races to life, first for the 31 days of January, and then for 16 days in April. -
The Archaeology of the Prussian Crusade
Downloaded by [University of Wisconsin - Madison] at 05:00 18 January 2017 THE ARCHAEOLOGY OF THE PRUSSIAN CRUSADE The Archaeology of the Prussian Crusade explores the archaeology and material culture of the Crusade against the Prussian tribes in the thirteenth century, and the subsequent society created by the Teutonic Order that lasted into the six- teenth century. It provides the first synthesis of the material culture of a unique crusading society created in the south-eastern Baltic region over the course of the thirteenth century. It encompasses the full range of archaeological data, from standing buildings through to artefacts and ecofacts, integrated with writ- ten and artistic sources. The work is sub-divided into broadly chronological themes, beginning with a historical outline, exploring the settlements, castles, towns and landscapes of the Teutonic Order’s theocratic state and concluding with the role of the reconstructed and ruined monuments of medieval Prussia in the modern world in the context of modern Polish culture. This is the first work on the archaeology of medieval Prussia in any lan- guage, and is intended as a comprehensive introduction to a period and area of growing interest. This book represents an important contribution to promot- ing international awareness of the cultural heritage of the Baltic region, which has been rapidly increasing over the last few decades. Aleksander Pluskowski is a lecturer in Medieval Archaeology at the University of Reading. Downloaded by [University of Wisconsin - Madison] at 05:00 -
Core Sampling for Plant Belowground Biomass Date: 02/17/2017
Title: TOS Protocol and Procedure: Core Sampling for Plant Belowground Biomass Date: 02/17/2017 NEON Doc. #: NEON.DOC.014038 Author: C. Meier Revision: E TOS PROTOCOL AND PROCEDURE: CORE SAMPLING FOR PLANT BELOWGROUND BIOMASS PREPARED BY ORGANIZATION DATE Courtney Meier SCI 03/25/2013 APPROVALS ORGANIZATION APPROVAL DATE Andrea Thorpe SCI 01/27/2017 Mike Stewart SYS 02/15/2017 RELEASED BY ORGANIZATION RELEASE DATE Judy Salazar CM 02/17/2017 See configuration management system for approval history. The National Ecological Observatory Network is a project solely funded by the National Science Foundation and managed under cooperative agreement by Battelle. Any opinions, findings, and conclusions or recommendations expressed in this material are those of the author(s) and do not necessarily reflect the views of the National Science Foundation. Template NEON.DOC.050006 Rev F Title: TOS Protocol and Procedure: Core Sampling for Plant Belowground Biomass Date: 02/17/2017 NEON Doc. #: NEON.DOC.014038 Author: C. Meier Revision: E Change Record REVISION DATE ECO # DESCRIPTION OF CHANGE A 03/25/2011 ECO-00148 Initial release Production release, template change, method B 01/20/2015 ECO-02273 improvements C 02/26/2015 ECO-02702 Migration to new protocol template Major changes to protocol include: All SOPs now implemented together every time protocol is executed, previously SOP D implemented 1X per site Timing information updated, and preservation of cores prior to core processing eliminated. Equipment list updates for lab work SOP C.1 sieving methods updated based on megapit sampling experience Roots from 2 cores within a clipCell are now pooled after D 1/28/2016 ECO-03547 weighing takes place and prior to grinding for chemical analysis / archive. -
Fish Terminologies
FISH TERMINOLOGIES Monument Type Thesaurus Report Format: Hierarchical listing - class Notes: Classification of monument type records by function. -
The Evolution of Trilobite Body Patterning
ANRV309-EA35-14 ARI 20 March 2007 15:54 The Evolution of Trilobite Body Patterning Nigel C. Hughes Department of Earth Sciences, University of California, Riverside, California 92521; email: [email protected] Annu. Rev. Earth Planet. Sci. 2007. 35:401–34 Key Words First published online as a Review in Advance on Trilobita, trilobitomorph, segmentation, Cambrian, Ordovician, January 29, 2007 diversification, body plan The Annual Review of Earth and Planetary Sciences is online at earth.annualreviews.org Abstract This article’s doi: The good fossil record of trilobite exoskeletal anatomy and on- 10.1146/annurev.earth.35.031306.140258 togeny, coupled with information on their nonbiomineralized tis- Copyright c 2007 by Annual Reviews. sues, permits analysis of how the trilobite body was organized and All rights reserved developed, and the various evolutionary modifications of such pat- 0084-6597/07/0530-0401$20.00 terning within the group. In several respects trilobite development and form appears comparable with that which may have charac- terized the ancestor of most or all euarthropods, giving studies of trilobite body organization special relevance in the light of recent advances in the understanding of arthropod evolution and devel- opment. The Cambrian diversification of trilobites displayed mod- Annu. Rev. Earth Planet. Sci. 2007.35:401-434. Downloaded from arjournals.annualreviews.org ifications in the patterning of the trunk region comparable with by UNIVERSITY OF CALIFORNIA - RIVERSIDE LIBRARY on 05/02/07. For personal use only. those seen among the closest relatives of Trilobita. In contrast, the Ordovician diversification of trilobites, although contributing greatly to the overall diversity within the clade, did so within a nar- rower range of trunk conditions. -
5 Day Itinerary
by a grant from Travel Nevada. Travel from grant a by possible made brochure This JUST 98 MILES NORTH OF LAS VEGAS ON HIGHWAY 95. HIGHWAY ON VEGAS LAS OF NORTH MILES 98 JUST www.beattynevada.org Ph: 1.866.736.3716 Ph: Studio 401 Arts & Salon & Arts 401 Studio Mama’s Sweet Ice Sweet Mama’s Smash Hit Subs Hit Smash VFW Chow VFW Smokin’ J’s BBQ J’s Smokin’ shoot out or two performed by our local cowboys. cowboys. local our by performed two or out shoot Gema’s Café Gema’s historical area you might catch a glimpse of a a of glimpse a catch might you area historical Death Valley Coffee Time Coffee Valley Death of our local eateries. If you are in the downtown downtown the in are you If eateries. local our of Roadhouse 95 Roadhouse After your day trips into the Valley, relax at one one at relax Valley, the into trips day your After Sourdough Saloon & Eatery & Saloon Sourdough lunch at Beatty’s Cottonwood Park. Park. Cottonwood Beatty’s at lunch Hot Stuff Pizza Stuff Hot Store or enjoy walking your dog or having a picnic picnic a having or dog your walking enjoy or Store Mel’s Diner Mel’s Town, the Famous Death Valley Nut and Candy Candy and Nut Valley Death Famous the Town, Happy Burro Chili & Beer & Chili Burro Happy open daily from 10 am to 3 pm, Rhyolite Ghost Ghost Rhyolite pm, 3 to am 10 from daily open The Death Valley Nut & Candy Store Candy & Nut Valley Death The can find in our little town, the Beatty Museum, Museum, Beatty the town, little our in find can LOCAL SHOPS & EATERIES & SHOPS LOCAL Day area, be sure to visit the unique businesses that you you that businesses unique the visit to sure be area, BEATTY Between trips to explore the Death Valley Valley Death the explore to trips Between your plan for each day, and set up a check in time. -
Ridgecrest BUREAU of LAND MANAGEMENT
BLM SPECIAL EDITION 1998 EXAMPLES OF AGENCY SIGNS SURFACE MANAGEMENT STATUS DESERT ACCESS GUIDE Ridgecrest BUREAU OF LAND MANAGEMENT USDA FOREST SERVICE l:100,0()0-Scale topographic map showing: Highways, roads and other manmade structures Water features • Contours and elevations in meters Recreation sites • Coverage of former desert access guide #4 Ridgecrest NATIONAL PARK SERVICE UNITED STATES DEPARTMENT OF THE INTERIOR BUREAU OF LAND MANAGEMENT CALIFORNIA STATE PARKS Edited and published by the Bureau of Land Management National Applied Resource Sciences Center, Denver, Colorado in cooperation with the Bureau of Land Management California State Office. Planimetry partially revised by BLM from various source material. Revised information not field . he. i-rd Base map prepared by the U.S. Geological Survey. Compiled from USGS 1:24,000 and l:62,5O0-scale topographic maps dated 1949-1973, and from advance materials. Partially revised from aerial photographs taken 1973-1989 and other source data. Revised information not CALIFORNIA STATE field checked. Map edited 1993. VEHICULAR RECREATION AREA Help protect your public lands by observing posted Projection and 10,000-meter grid, zone 11: Universal OHV designations. Watch for OHV signs and read hari'.verse Mercator. 25,000-foot grid licks based on them carefully. California coordinate system, zone 4 and 5. 1927 North American Datum. For more information contact the HIM, USDA Forest Service, National Park Service, California State Park, or California State Motorized Vechicle Recreation Area Land lines are omitted in areas of extensive tract surveys. Office (see back panel for address and phone There may be private inholdings within the boundaries of numbers).