The Seaman Volcanic Center- a Rare Middle Tertiary Stratovolcano in Southern Nevada U.S. GEOLOGICAL SURVEY BULLETIN 2052

Total Page:16

File Type:pdf, Size:1020Kb

The Seaman Volcanic Center- a Rare Middle Tertiary Stratovolcano in Southern Nevada U.S. GEOLOGICAL SURVEY BULLETIN 2052 The Seaman Volcanic Center- A Rare Middle Tertiary Stratovolcano in Southern Nevada I I I U.S. GEOLOGICAL SURVEY BULLETIN 2052 AVAILABILITY OF BOOKS AND MAPS OF THE U.S. GEOLOGICAL SURVEY Instructions on ordering publications of the U.S. Geological Survey, along with the last offerings, are given in the current-year issues of the monthly catalog "New Publications of the U.S. Geological Survey." Prices of available U.S. Geological Survey publications released prior to the current year are listed in the most recent annual "Price and Availability List" Publications that are listed in various U.S. Geological Survey catalogs (see back inside cover) but not listed in the most recent annual "Price and Availability List" are no longer available. Prices of reports released to the open files are given in the listing "U.S. Geological Survey Open-File Reports," updated monthly, which is for sale in microfiche from the USGS ESIC-Open-File Report Sales, Box 25286, Building 810, Denver Federal Center, Denver, CO 80225 Order U.S. Geological Survey publications by mail or over the counter from the offices given below. BY MAIL OVER THE COUNTER Books Books Professional Papers, Bulletins, Water-Supply Papers, Tech­ Books of the U.S. Geological Survey are available over the niques of Water-Resources Investigations, Circulars, publications counter at the following U.S. Geological Survey offices, all of of general interest (such as leaflets, pamphlets, booklets), single which are authorized agents of the Superintendent of Documents. copies of periodicals (Earthquakes & Volcanoes, Preliminary De­ termination of Epicenters), and some miscellaneous reports, includ­ • ANCHORAGE, Alaska-4230 University Dr., Rm. 101 ing some of the foregoing series that have gone out of print at the • ANCHORAGE, Alaska--605 West 4th Ave., Rm G-84 Superintendent of Documents, are obtainable by mail from • DENVER, Colorad~Federal Bldg., Rm. 169, 1961 Stout St. USGS Map Distribution Box 25286, Building 810 • LAKEWOOD, Colorad~Federal Center, Bldg. 810 Denver Federal Center • MENLO PARK, California-Bldg. 3, Rm. 3128,345 Denver, CO 80225 Middlefield Rd. Subscriptions to periodicals (Earthquakes & Volcanoes and • RESTON, Virginia-National Center, Rm. 1C402, 12201 Preliminary Determination of Epicenters) can be obtained ONLY Sunrise Valley Dr. from • SALT LAKE CITY, Utah-Federal Bldg., Rm. 8105, 125 South State St. Superintendent of Documents U.S. Government Printing Office • SPOKANE, Washington-U.S. Courthouse, Rm. 678, West Washington, DC 20402 920 Riverside Ave. • WASHINGTON, D.C.-U.S. Department of the Interior Bldg., (Check or money order must be payable to Superintendent of Rm. 2650, 1849 C St., NW. Documents.) Maps Maps Maps may be purchased over the counter at the U.S. Geolog­ For maps, address mail order to ical Survey offices where books are sold (all addresses in above list) and at the following Geological Survey offices: USGS Map Distribution Box 25286, Building 810 Denver Federal Center • ROLLA, Missouri-1400 Independence Rd. Denver, CO 80225 • FAIRBANKS, Alaska-New Federal Building, 101 Twelfth Ave. Residents of Alaska may order maps from U.S. Geological Survey, Map Sales 101 Twelfth Ave., Box 12 Fairbanks, AK 99701 The Seaman Volcanic Center- A Rare Middle Tertiary Stratovolcano in Southern Nevada By EDWARD A. DU BRAY U.S. GEOLOGICAL SURVEY BULLETIN 2052 Geology and geochemical evolution of a rare, well-preserved middle Tertiary stratovolcano UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1993 U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY Dallas L. Peck, Director For sale by USGS Map Distribution Box 25286, Building 810 Denver Federal Center Denver, CO 80225 Any use of trade, product, or finn names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government. Library of Congress Cataloging-in-Publication Data Du Bray, E. A. The Seaman volcanic center ; a rare middle Tertiary stratovolcano in southern Nevada I by Edward A. du Bray. p. em. - (U.S. Geological Survey bulletin; 2052) Includes bibliographical references. Supt. of Docs. no.: 1.19.3:B2052 1. Volcanoes-Nevada-Lincoln County. 2. Geology, Stratigraphic-Tertiary. 3. Geochemistry-Nevada-Lincoln County. I. U.S. Geological Survey. II. Title. III. Series. QE75.B9 no. 2052 [QE524] 557.3 s-dc20 93-2837 [551.2'1'0979314] CIP CONTENTS Abstract................................................................................................................................. 1 Introduction........................................................................................................................... 1 Geology of the Serunan Volcanic Center.............................................................................. 3 Petrography........................................................................................................................... 3 Geochemistry of the Seaman Volcanic Center..................................................................... 4 Whole-Rock Chemistry.............................................................................................. 4 Mineral Chemistry...................................................................................................... 10 Major Element Least-Squares Fractionation-Mixing Modeling........................................... 11 Evolution of the Seaman Volcanic Center............................................................................ 12 Summary and Conclusions................................................................................................... 17 References Cited................................................................................................................... 18 FIGURES 1. Generalized geologic map of the Seaman volcanic center, Lincoln County, Nevada................................................... 2 2. Photomicrographs showing petrographic features of components of the Seaman volcanic center ... ........................... 5 3. Alkali-silica classification diagram showing analyses of samples from the Seaman volcanic center........................... 6 4. Ternary AFM diagram showing compositions of samples from the Seaman volcanic center...................................... 7 5. Diagrrun showing the variation of rubidium and strontium abundances in samples from the Seaman volcanic center.............................................................................................................................................................................. 8 6. Chondrite-normalized diagram showing compositions of samples from the Seaman volcanic center ......................... 8 7. Chondrite-normalized extended trace element diagram showing compositions of samples from the Seaman volcanic center ... .. ...... ................ .. ............. ..... .. ..... .... .. ... .. ... ................. ... ... ............. .............................................. 9 8. Enrichment-depletion diagram showing major- and trace-element abundances of the Serunan volcanic center dike normalized to those of the lava flow unit....................................................................................................................... 14 9. Tectonic setting-trace element discriminant variation diagrams for components of the Seaman volcanic center........ 17 TABLES 1. Major-oxide and normative mineral composition for samples of the Seaman volcanic center, Lincoln County, Nevada........................................................................................................................................................................... 6 2. Trace element data for samples of the Serunan volcanic center, Lincoln County, Nevada........................................... 7 3. Instrumental neutron activation data for samples of the Seaman volcanic center, Lincoln County Nevada................. 7 4. Average major-oxide, normative, and trace-element compositions of components of the Seaman volcanic center, Lincoln County, Nevada................................................................................................................................................ 8 5. Representative mineral compositions for phenocryst phases in samples of the Seaman volcanic center, Lincoln County, Nevada.............................................................................................................................................................. 10 6. Results of major element least-squares crystal fractionation-mixing modeling for samples of the Seaman volcanic center, Lincoln County, Nevada.................................................................................................................................... 12 01 THE SEAMAN VOLCANIC CENTER-A RARE MIDDLE TERTIARY STRATOVOLCANO IN SOUTHERN NEVADA By EDWARD A. DUBRAY ABSTRACT INTRODUCTION The Seaman volcanic center is a composite, middle The Seaman volcanic center is clearly denoted as a Tertiary stratovolcano in southern Nevada; it is about 10 small, circular volcanic feature on the geologic map of km (6 mi) in diameter and has a reconstructed volume of Nevada (Stewart and Carlson, 1978). The west-central part about 20 km3 (5 mi3). The center is principally composed of the Seaman Range is dominated by the Seaman volca­ of interbedded dacite lava and pyroclastic flows whose nic center (fig. 1), a feature first noted and described by eruption built a stratovolcano that was intruded by rhyolite Tschanz and Pampeyan (1961, 1970) and believed
Recommended publications
  • Anatomy of a Volcanic Eruption: Case Study: Mt. St. Helens
    Anatomy of a Volcanic Eruption: Case Study: Mt. St. Helens Materials Included in this Box: • Teacher Background Information • 3-D models of Mt. St. Helens (before and after eruption) • Examples of stratovolcano rock products: Tuff (pyroclastic flow), pumice, rhyolite/dacite, ash • Sandbox crater formation exercise • Laminated photos/diagrams Teacher Background There are several shapes and types of volcanoes around the world. Some volcanoes occur on the edges of tectonic plates, such as those along the ‘ring of fire’. But there are also volcanoes that occur in the middle of tectonic plates like the Yellowstone volcano and Kilauea volcano in Hawaii. When asked to draw a volcano most people will draw a steeply sided, conical mountain that has a depression (crater) at the top. This image of a 'typical' volcano is called a stratovolcano (a.k.a. composite volcano). While this is the often visualized image of a volcano, there are actually many different shapes volcanoes can be. A volcano's shape is mostly determined by the type of magma/lava that is created underneath it. Stratovolcanoes get their shape because of the thick, sticky (viscous) magma that forms at subduction zones. This magma/lava is layered between ash, pumice, and rock fragments. These layers of ash and magma will build into high elevation, steeply sided, conical shaped mountains and form a 'typical' volcano shape. Stratovolcanoes are also known for their explosive and destructive eruptions. Eruptions can cause clouds of gas, ash, dust, and rock fragments to eject into the atmosphere. These clouds of ash can become so dense and heavy that they quickly fall down the side of the volcanoes as a pyroclastic flow.
    [Show full text]
  • U.S. Department of the Interior Bureau of Land Management
    U.S. Department of the Interior Bureau of Land Management Environmental Assessment DOI-BLM-NV-L000-2017-0006-EA December 20, 2017 SEAMAN and WHITE RIVER HERD AREA WILD HORSE GATHER Location: Lincoln and Nye Counties Applicant/Address: U.S. Department of the Interior Bureau of Land Management Ely District Office Phone: (775) 289-1800 Fax: (775) 289-1910 Golden Gate, Seaman and White River Herd Area Wild Horse Gather Environmental Assessment DOI-BLM-NV-L010-2009-0023-EA 1.0 INTRODUCTION....................................................................................................... 3 1.1 Background: .......................................................................................................... 3 1.2 Purpose and Need ....................................................................................................... 8 1.3 Conformance with BLM Land Use Plan(s): ............................................................. 8 1.4 Relationship to Statutes, Regulations, or other Plans: ............................................ 8 2.0 DESCRIPTION OF ALTERNATIVES, INCLUDING PROPOSED ACTION 10 2.1 Introduction: ............................................................................................................. 10 2.2 Alternative A - Proposed Action: ............................................................................ 10 2.3 Alternative B - No Action: ........................................................................................ 14 2.4 Alternatives Considered, but Eliminated from Further Analysis .......................
    [Show full text]
  • The Science Behind Volcanoes
    The Science Behind Volcanoes A volcano is an opening, or rupture, in a planet's surface or crust, which allows hot magma, volcanic ash and gases to escape from the magma chamber below the surface. Volcanoes are generally found where tectonic plates are diverging or converging. A mid-oceanic ridge, for example the Mid-Atlantic Ridge, has examples of volcanoes caused by divergent tectonic plates pulling apart; the Pacific Ring of Fire has examples of volcanoes caused by convergent tectonic plates coming together. By contrast, volcanoes are usually not created where two tectonic plates slide past one another. Volcanoes can also form where there is stretching and thinning of the Earth's crust in the interiors of plates, e.g., in the East African Rift, the Wells Gray-Clearwater volcanic field and the Rio Grande Rift in North America. This type of volcanism falls under the umbrella of "Plate hypothesis" volcanism. Volcanism away from plate boundaries has also been explained as mantle plumes. These so- called "hotspots", for example Hawaii, are postulated to arise from upwelling diapirs with magma from the core–mantle boundary, 3,000 km deep in the Earth. Erupting volcanoes can pose many hazards, not only in the immediate vicinity of the eruption. Volcanic ash can be a threat to aircraft, in particular those with jet engines where ash particles can be melted by the high operating temperature. Large eruptions can affect temperature as ash and droplets of sulfuric acid obscure the sun and cool the Earth's lower atmosphere or troposphere; however, they also absorb heat radiated up from the Earth, thereby warming the stratosphere.
    [Show full text]
  • Examples of Extinct Volcanoes in the World
    Examples Of Extinct Volcanoes In The World Inflationary and aristate Benn mayest his withdrawal westernizes overbids philosophically. Israel subinfeudates inextricably? Antony remains subcranial: she phosphatises her shoofly relinquish too volumetrically? Chaos in the ocean species go a free book, an exotic array of the volcanoes of in the examples extinct world where the hazards. What i chose the island of hawaii volcano to the sunrise from one of extinct volcanoes in the examples but. Volcanoes British Geological Survey. For retention an explosive volcanic eruption in a heart area try not as dangerous as one faint a populous region that requires mass evacuations. We really large eruptions? You can form around the world in extinct the examples of volcanoes worldwide originate from various activities have not erupted for the highest volcano off by. This volcano is terrible but extinct. What causes population under watch for the volcano clearly directed towards dyngjuháls at the solfatura, the examples above. Daily fun website? Ruapehu told Taranaki to skill the mountain clan, so he followed the winding course drew the Whanganui River, and settle in valley west coast. Tons of carbon dioxide erupted in nine hundred years will run very different effects than another same volume outgassed over the thousand of his million years. Fire but in old seismometers are volcanoes of extinct in the examples above. In the upcoming winter with the world in extinct volcanoes of the examples of your car safety. In indonesia is climate change as dormant volcanoes list on earth have either stationary plume. How many active volcanoes are time on Earth? Many islands to the same time and carries her dancing skills and of extinct volcano is not buried again in.
    [Show full text]
  • GEOLOGIC MAP of the MOUNT ADAMS VOLCANIC FIELD, CASCADE RANGE of SOUTHERN WASHINGTON by Wes Hildreth and Judy Fierstein
    U.S. DEPARTMENT OF THE INTERIOR TO ACCOMPANY MAP 1-2460 U.S. GEOLOGICAL SURVEY GEOLOGIC MAP OF THE MOUNT ADAMS VOLCANIC FIELD, CASCADE RANGE OF SOUTHERN WASHINGTON By Wes Hildreth and Judy Fierstein When I climbed Mount Adams {17-18 August 1945] about 1950 m (6400') most of the landscape is mantled I think I found the answer to the question of why men by dense forests and huckleberry thickets. Ten radial stake everything to reach these peaks, yet obtain no glaciers and the summit icecap today cover only about visible reward for their exhaustion... Man's greatest 2.5 percent (16 km2) of the cone, but in latest Pleis­ experience-the one that brings supreme exultation­ tocene time (25-11 ka) as much as 80 percent of Mount is spiritual, not physical. It is the catching of some Adams was under ice. The volcano is drained radially vision of the universe and translating it into a poem by numerous tributaries of the Klickitat, White Salmon, or work of art ... Lewis, and Cis pus Rivers (figs. 1, 2), all of which ulti­ William 0. Douglas mately flow into the Columbia. Most of Mount Adams and a vast area west of it are Of Men and Mountains administered by the U.S. Forest Service, which has long had the dual charge of protecting the Wilderness Area and of providing a network of logging roads almost INTRODUCTION everywhere else. The northeast quadrant of the moun­ One of the dominating peaks of the Pacific North­ tain, however, lies within a part of the Yakima Indian west, Mount Adams, stands astride the Cascade crest, Reservation that is open solely to enrolled members of towering 3 km above the surrounding valleys.
    [Show full text]
  • Volcanoes a to Z
    Mount St Helens National Volcanic Monument – Teacher’s Corner -Teacher Info. Gifford Pinchot National Forest USDA Forest Service Volcanoes A to Z – Bus Activity Time Requirement: all day Exhibit / Trail Used: all exhibits/trails visited Locations: all locations visited, review on the bus en route back to your school. This activity is to be completed throughout the day and between other activities. Students will make note of key words while reading exhibits, interpretive signs, or labels, or by hearing them from each other, their teacher, movies or rangers. Consider distributing on the bus and collecting on the bus. Goal: 1) The student will become familiar with terminology related to the study of volcanoes, geology, or the ecosystems that surround them. Objectives: 1) The student will listen attentively. 2) The student will recall and list vocabulary words for things and concepts encountered on a field trip to Mount St. Helens National Volcanic Monument. 3) The student will distinguish nouns from other parts of speech. WASHINGTON EALRS and OREGON BENCHMARK STANDARDS Washington Social Studies 2.0- The student understands the complex physical and human characteristics of places and regions. Geography 2.1- Describe the natural characteristics of places and regions. Science 4.2 Use writing and speaking skills to organize and express science ideas. a. Use science vocabulary appropriately in written explanations, conversations and verbal presentations. Oregon Science-CCG The Dynamic Earth- Understand the properties and limited availability of the materials which make up the Earth. BM1- Recognize physical differences in Earth materials. Language-CCG Select functional, precise, and descriptive words appropriate to audience and purpose.
    [Show full text]
  • Dry Lake Valley North SEZ Analysis
    1 11.4 DRY LAKE VALLEY NORTH 2 3 4 11.4.1 Background and Summary of Impacts 5 6 7 11.4.1.1 General Information 8 9 The proposed Dry Lake Valley North SEZ is located in Lincoln County in southeastern 10 Nevada (Figure 11.4.1.1-1). The SEZ has a total area of 76,874 acres (311 km2). In 2008, the 11 county population was 4,643, while adjacent Clark County to the south had a population 12 of 1,879,093. The closest population centers to the SEZ are Pioche, located about 15 mi (24 km) 13 to the east, and Caliente, located about 15 mi (24 km) to the southeast; both communities have 14 populations of about 1,000. The smaller communities of Caselton and Prince are located about 15 13 mi (21 km) to the east of the SEZ. Las Vegas is located about 110 mi (180 km) to the south. 16 17 The nearest major road to the Dry Lake Valley North SEZ is State Route 318, which is 18 about 7 mi (11 km) to the west of the SEZ, while U.S. 93 is about 8 mi (13 km) to the south. 19 Access to the interior of the SEZ is by dirt roads. The nearest railroad access is approximately 20 25 mi (40 km) away, while nearby airports include Lincoln County Airport in Panaca and Alamo 21 Landing Field in Alamo, which are located about 13 mi (21 km) south–southeast of and 35 mi 22 (56 km) southwest of the SEZ, respectively.
    [Show full text]
  • Stratigraphy and Structure of the Seaman Range and Fox Mountain, Lincoln and Nye Counties, Nevada
    Stratigraphy and Structure of the Seaman Range and Fox Mountain, Lincoln and Nye Counties, Nevada U.S. GEOLOGICAL SURVEY BULLETIN 1988-B I 1 r^Hr-~"r-^S »:-«>'°-;>-.'; '£ '. -"* °-"^^io-'oO;ol!i-..e>L ^? :^~ty-":- o\: s--b>^.'d- .? " ? o..bTvo-r» ?:.-!:.»:-. "o'.-o'-o .- *^-o?.°:.--o : : ° o£\*>: ^-°:* '.« - "o-o- .-o - ^-.o.*'. ^» ' - 1 .". '. O- ' "" "- "* -" no: ^--'*^-o.yvo:»-c)^ - *>- : p.-by :o.;--p-/.-'o."-',c>-( 0 = ?.o'VO -V "±« -* «?'.<?o-oi ^ .. «- .*».-:»: -* ^^»-^ Chapter B Stratigraphy and Structure of the Seaman Range and Fox Mountain, Lincoln and Nye Counties, Nevada By DONLON O. HURTUBISE and EDWARD A. DU BRAY A multidisciplinary approach to research studies of sedimentary rocks and their constituents and the evolution of sedimentary basins, both ancient and modern U.S. GEOLOGICAL SURVEY BULLETIN 1988 EVOLUTION OF SEDIMENTARY BASINS EASTERN GREAT BASIN HARRY E. COOK AND CHRISTOPHER J. POTTER, Project Coordinators U.S. DEPARTMENT OF THE INTERIOR MANUEL LUJAN, JR., Secretary U.S. GEOLOGICAL SURVEY Dallas L. Peck, Director Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government UNITED STATES GOVERNMENT PRINTING OFFICE: 1992 For sale by Book and Open-File Report Sales U.S. Geological Survey Federal Center, Box 25286 Denver, CO 80225 Library of Congress Cataloging-in-Publication Data Hurtubise, D.O. Stratigraphy and structure of the Seaman Range and Fox Mountain, Lincoln and Nye Counties, Nevada / by Donlon O. Hurtubise and Edward A. du Bray, p. cm. (Evolution of sedimentary basins Eastern Great Basin ; ch. B) (U.S. Geological Survey bulletin ; 1988-B) Includes bibliographical references.
    [Show full text]
  • Nicaragua's Cerro Negro Stratovolcano
    NICARAGUANICARAGUA’S’S CERROCERRO NEGRONEGRO STRASTRATOVTOVOLCANOOLCANO —— HOW DID IT BLOW ITS TOP??? 1) A stratovolcano or composite volcano 6) Large cloud of pyroclastic debris, is built of alternating layers of lava Match the explanations with the numbers on the volcano and find out. steam, and other vapors erupted and pyroclastic (ash or ejected de- from Cerro Negro. The larger, bris) deposits. These deposits accu- heavier fragments fall back on the mulate around the central vent in a cone while the smaller, lighter ash cone-shaped pile. Lava may flow from 6 fragments are carried great dis- fissures (fractures or cracks) radi- tances before they settle. ating from the central vent, whereas the multi-sized pyroclastics are B 7) A smaller cloud of darker material ejected from the main vent. 9 indicates that a localized eruption L has just occurred. 2) Steam and other vapors rising from 10 the large volcanic blocks erupted 8 from the main crater recently. Com- ) Cloud of vapors from the volcano is mostly steam and ash, but also con- pare with the older, cooler volcanic 8 tains chlorine, fluorine, sulfur, and blocks at the ends of the tracks or L 5 their acids. furrows that run down the slope of 5 the main cone. These tracks or fur- 5 9 rows were plowed by the rolling 7 9) Shadow cast by the ash and vapor blocks. Some house-size blocks now 5 cloud from the volcano (6) carried lie loosely at the bottom of the 5 by turbulent hot gasses and winds. slope. 4 When the volcanic ash settles, the 2 pyroclastic deposit that forms is 9 called an ash fall.
    [Show full text]
  • The Boring Volcanic Field of the Portland-Vancouver Area, Oregon and Washington: Tectonically Anomalous Forearc Volcanism in an Urban Setting
    Downloaded from fieldguides.gsapubs.org on April 29, 2010 The Geological Society of America Field Guide 15 2009 The Boring Volcanic Field of the Portland-Vancouver area, Oregon and Washington: Tectonically anomalous forearc volcanism in an urban setting Russell C. Evarts U.S. Geological Survey, 345 Middlefi eld Road, Menlo Park, California 94025, USA Richard M. Conrey GeoAnalytical Laboratory, School of Earth and Environmental Sciences, Washington State University, Pullman, Washington 99164, USA Robert J. Fleck Jonathan T. Hagstrum U.S. Geological Survey, 345 Middlefi eld Road, Menlo Park, California 94025, USA ABSTRACT More than 80 small volcanoes are scattered throughout the Portland-Vancouver metropolitan area of northwestern Oregon and southwestern Washington. These vol- canoes constitute the Boring Volcanic Field, which is centered in the Neogene Port- land Basin and merges to the east with coeval volcanic centers of the High Cascade volcanic arc. Although the character of volcanic activity is typical of many mono- genetic volcanic fi elds, its tectonic setting is not, being located in the forearc of the Cascadia subduction system well trenchward of the volcanic-arc axis. The history and petrology of this anomalous volcanic fi eld have been elucidated by a comprehensive program of geologic mapping, geochemistry, 40Ar/39Ar geochronology, and paleomag- netic studies. Volcanism began at 2.6 Ma with eruption of low-K tholeiite and related lavas in the southern part of the Portland Basin. At 1.6 Ma, following a hiatus of ~0.8 m.y., similar lavas erupted a few kilometers to the north, after which volcanism became widely dispersed, compositionally variable, and more or less continuous, with an average recurrence interval of 15,000 yr.
    [Show full text]
  • Cerro Pizarro Volcano, Mexico by G. Carrasco-Nú
    1 Polygenetic nature of a rhyolitic dome and implications for hazard assessment: 2 Cerro Pizarro volcano, Mexico 3 by G. Carrasco-Núñez and N. Riggs 4 5 ABSTRACT 6 Rhyolitic domes are commonly regarded as monogenetic volcanoes associated with single, brief 7 eruptions. They are characterized by short-lived successions of pyroclastic and effusive activity 8 associated with a series of discrete eruptive events that apparently last on the order of years to 9 decades. Cerro Pizarro, a ~ 1.1 km3 rhyolitic dome in the eastern Mexican Volcanic Belt, shows 10 aspects of polygenetic volcanism including long-term repose periods (~ 50-80 ky) between 11 eruptions, chemical variations with time, and a complex evolution of alternating explosive and 12 effusive eruptions, a cryptodome phase, and sector collapse. This eruptive behavior provides 13 new insights into how rhyolite domes may evolve. A protracted, complex evolution bears 14 important implications for hazard assessment if reactivation of an apparently extinct rhyolitic 15 dome must be seriously considered. 16 17 Keywords: monogenetic volcanism, polygenetic volcanism, rhyolites, dome growth, volcanic 18 hazards, Mexican Volcanic Belt 19 20 INTRODUCTION 21 Monogenetic volcanoes comprise a wide spectrum of relatively small volcanic structures 22 (generally less than a few km3 erupted material) that show a commonly simple evolution (one 23 eruption, or a few clearly related eruptions), short life span (commonly years to decades for 24 mafic volcanoes, but possibly as much as a few centuries for rhyolitic domes), and minor 25 chemical composition changes. Monogenetic volcanoes are, in general, either basalt or rhyolite, 26 while polygenetic volcanoes, which erupt repeatedly and have a large and persistent magma 27 storage chamber, are commonly andesitic or dacitic in composition.
    [Show full text]
  • Flood Basalt Shield Cinder Cone Stratovolcano Lava Dome Mid
    Volcano Mid-Ocean Flood Basalt Shield Cinder Cone Stratovolcano Lava Dome Caldera Review Table Ridge small, steep-sided low, broad mountain small mountain, large, steep-sided large depressions extensive plateaus o rift valley o mountain, Landform with slopes <5 , 20-30 slopes, mountain, 10's of km wide up to 9,000-m high up to 400-m high up to 3,000-m high up to ~500-m high Eruption huge volumes of lava lava >> tephra pillow lava tephra >> lava tephra + lava lava > tephra tephra >> lava Products (105 to 106 km3) Magma mafic mafic mafic felsic felsic Composition mafic intermediate Magma low low low low moderate high high Viscosity % Gas in Magma low low low moderate low to high low to high low to high Eruption high discharge rate point source & fissure small eruption column, large eruption column, dome collapse, multiple fissure-fed submarine flows from multiple fissures "fire" fountains fire fountain pyroclastic flows pyroclastic flows pyroclastic flows Style (Hawaiian) (Strombolian) (Plinian) (Pelean) (ultra-Plinian) Explosivity low low low low-moderate very high high ultra-high hydrous (wet) Magma mantle mantle mantle mantle crust/mantle crustal melting crustal melting partial melting partial melting partial melting partial melting Origin melting Plate Tectonic "hot spot" Oceanic Convergent margin numerous numerous numerous numerous Setting (mantle plume) divergent margin (subduction zone) Columbia River, Mid-Atlantic Ridge, Paricutin, Mt. St. Helens, Mt. Unzen, Valles, Long Valley, Mauna Loa, Kilaeua, Examples Deccan Traps, East Pacific
    [Show full text]