United States Department of the Interior Geological Survey Proceedings of Workshop Xix Active Tectonic and Magmatic Processes Be
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Excesss Karaoke Master by Artist
XS Master by ARTIST Artist Song Title Artist Song Title (hed) Planet Earth Bartender TOOTIMETOOTIMETOOTIM ? & The Mysterians 96 Tears E 10 Years Beautiful UGH! Wasteland 1999 Man United Squad Lift It High (All About 10,000 Maniacs Candy Everybody Wants Belief) More Than This 2 Chainz Bigger Than You (feat. Drake & Quavo) [clean] Trouble Me I'm Different 100 Proof Aged In Soul Somebody's Been Sleeping I'm Different (explicit) 10cc Donna 2 Chainz & Chris Brown Countdown Dreadlock Holiday 2 Chainz & Kendrick Fuckin' Problems I'm Mandy Fly Me Lamar I'm Not In Love 2 Chainz & Pharrell Feds Watching (explicit) Rubber Bullets 2 Chainz feat Drake No Lie (explicit) Things We Do For Love, 2 Chainz feat Kanye West Birthday Song (explicit) The 2 Evisa Oh La La La Wall Street Shuffle 2 Live Crew Do Wah Diddy Diddy 112 Dance With Me Me So Horny It's Over Now We Want Some Pussy Peaches & Cream 2 Pac California Love U Already Know Changes 112 feat Mase Puff Daddy Only You & Notorious B.I.G. Dear Mama 12 Gauge Dunkie Butt I Get Around 12 Stones We Are One Thugz Mansion 1910 Fruitgum Co. Simon Says Until The End Of Time 1975, The Chocolate 2 Pistols & Ray J You Know Me City, The 2 Pistols & T-Pain & Tay She Got It Dizm Girls (clean) 2 Unlimited No Limits If You're Too Shy (Let Me Know) 20 Fingers Short Dick Man If You're Too Shy (Let Me 21 Savage & Offset &Metro Ghostface Killers Know) Boomin & Travis Scott It's Not Living (If It's Not 21st Century Girls 21st Century Girls With You 2am Club Too Fucked Up To Call It's Not Living (If It's Not 2AM Club Not -
Geologic Map of the Central San Juan Caldera Cluster, Southwestern Colorado by Peter W
Geologic Map of the Central San Juan Caldera Cluster, Southwestern Colorado By Peter W. Lipman Pamphlet to accompany Geologic Investigations Series I–2799 dacite Ceobolla Creek Tuff Nelson Mountain Tuff, rhyolite Rat Creek Tuff, dacite Cebolla Creek Tuff Rat Creek Tuff, rhyolite Wheeler Geologic Monument (Half Moon Pass quadrangle) provides exceptional exposures of three outflow tuff sheets erupted from the San Luis caldera complex. Lowest sheet is Rat Creek Tuff, which is nonwelded throughout but grades upward from light-tan rhyolite (~74% SiO2) into pale brown dacite (~66% SiO2) that contains sparse dark-brown andesitic scoria. Distinctive hornblende-rich middle Cebolla Creek Tuff contains basal surge beds, overlain by vitrophyre of uniform mafic dacite that becomes less welded upward. Uppermost Nelson Mountain Tuff consists of nonwelded to weakly welded, crystal-poor rhyolite, which grades upward to a densely welded caprock of crystal-rich dacite (~68% SiO2). White arrows show contacts between outflow units. 2006 U.S. Department of the Interior U.S. Geological Survey CONTENTS Geologic setting . 1 Volcanism . 1 Structure . 2 Methods of study . 3 Description of map units . 4 Surficial deposits . 4 Glacial deposits . 4 Postcaldera volcanic rocks . 4 Hinsdale Formation . 4 Los Pinos Formation . 5 Oligocene volcanic rocks . 5 Rocks of the Creede Caldera cycle . 5 Creede Formation . 5 Fisher Dacite . 5 Snowshoe Mountain Tuff . 6 Rocks of the San Luis caldera complex . 7 Rocks of the Nelson Mountain caldera cycle . 7 Rocks of the Cebolla Creek caldera cycle . 9 Rocks of the Rat Creek caldera cycle . 10 Lava flows premonitory(?) to San Luis caldera complex . .11 Rocks of the South River caldera cycle . -
Hawaii Volcanoes National Park Geologic Resources Inventory Report
National Park Service U.S. Department of the Interior Natural Resource Program Center Hawai‘i Volcanoes National Park Geologic Resources Inventory Report Natural Resource Report NPS/NRPC/GRD/NRR—2009/163 THIS PAGE: Geologists have lloongng been monimonittoorriing the volcanoes of Hawai‘i Volcanoes National Park. Here lalava cascades durduriingng the 1969-1971 Mauna Ulu eruption of Kīlauea VolVolcano. NotNotee the Mauna Ulu fountountaiain in the background. U.S. Geologiogicalcal SurSurvveyey PhotPhotoo by J. B. Judd (12/30/1969). ON THE COVER: ContContiinuouslnuouslyy eruptuptiingng since 1983, Kīllaueaauea Volcano contcontiinues to shapshapee Hawai‘Hawai‘i VoVollccanoes NatiNationalonal ParkPark.. Photo courtesy Lisa Venture/UniversiUniversitty of Cincinnati. Hawai‘i Volcanoes National Park Geologic Resources Inventory Report Natural Resource Report NPS/NRPC/GRD/NRR—2009/163 Geologic Resources Division Natural Resource Program Center P.O. Box 25287 Denver, Colorado 80225 December 2009 U.S. Department of the Interior National Park Service Natural Resource Program Center Denver, Colorado The National Park Service, Natural Resource Program Center publishes a range of reports that address natural resource topics 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. -
Poroelastic Responses of Confined Aquifers to Subsurface Strain And
Solid Earth, 6, 1207–1229, 2015 www.solid-earth.net/6/1207/2015/ doi:10.5194/se-6-1207-2015 © Author(s) 2015. CC Attribution 3.0 License. Poroelastic responses of confined aquifers to subsurface strain and their use for volcano monitoring K. Strehlow, J. H. Gottsmann, and A. C. Rust School of Earth Sciences, University of Bristol, Wills Memorial Building, Bristol BS8 1RJ, UK Correspondence to: K. Strehlow ([email protected]) Received: 11 May 2015 – Published in Solid Earth Discuss.: 9 June 2015 Revised: 18 September 2015 – Accepted: 21 October 2015 – Published: 10 November 2015 Abstract. Well water level changes associated with mag- aquifer and are commonly neglected in analytical models. matic unrest can be interpreted as a result of pore pressure These findings highlight the need for numerical models for changes in the aquifer due to crustal deformation, and so the interpretation of observed well level signals. However, could provide constraints on the subsurface processes caus- simulated water table changes do indeed mirror volumetric ing this strain. We use finite element analysis to demonstrate strain, and wells are therefore a valuable addition to monitor- the response of aquifers to volumetric strain induced by pres- ing systems that could provide important insights into pre- surized magma reservoirs. Two different aquifers are invoked eruptive dynamics. – an unconsolidated pyroclastic deposit and a vesicular lava flow – and embedded in an impermeable crust, overlying a magma chamber. The time-dependent, fully coupled models simulate crustal deformation accompanying chamber pres- 1 Introduction surization and the resulting hydraulic head changes as well as flow through the porous aquifer, i.e. -
Mono County ¡Lanning Commission Agenda
MONO COUNTY PLANNING COMMISSION PO Box 347 PO Box 8 Mammoth Lakes, CA 93546 Bridgeport, CA 93517 760.924.1800, fax 924.1801 760.932.5420, fax 932.5431 [email protected] www.monocounty.ca.gov AGENDA THURSDAY, AUGUST 14, 2014 – 10 a.m. Supervisors Chambers, County Courthouse, Bridgeport *Videoconference: BOS Conference Room, third floor, Sierra Center Mall, Mammoth Lakes Full agenda packets, plus associated materials distributed less than 72 hours prior to the meeting, will be available for public review at the Community Development offices in Bridgeport (Annex 1, 74 N. School St.) or Mammoth Lakes (Minaret Village Mall, above Giovanni’s restaurant). Agenda packets are also posted online at www.monocounty.ca.gov / boards & commissions / planning commission. For inclusion on the e- mail distribution list, interested persons can subscribe on the website. *Agenda sequence (see note following agenda). 1. CALL TO ORDER & PLEDGE OF ALLEGIANCE 2. PUBLIC COMMENT: Opportunity to address the Planning Commission on items not on the agenda 3. MEETING MINUTES: Review and adopt minutes of July 10, 2014 – p. 1 4. CONSENT ITEM 10:10 A.M. FINAL APPROVAL OF PARCEL MAP 13-001/ Hildenbrand-Booth. Approval of Parcel Map 13- 001 will divide APN 026-220-009, totaling 6.30 acres, into four lots of 2.39, 1.19, 1.19, and 1.43 acres, along with an offer of dedication of 0.10 acres along Valley Road. The project is located in the community of Chalfant. Access is via Valley Road, with a proposed private road, Owens Ranch Road. Individual wells and septic systems are proposed. -
Lombok Island, Sumbawa Island, and Samalas Volcano
ECOLE DOCTORALE DE GEOGRAPHIE DE PARIS (ED 4434) Laboratoire de Géographie Physique - UMR 8591 Doctoral Thesis in Geography Bachtiar Wahyu MUTAQIN IMPACTS GÉOMORPHIQUES DE L'ÉRUPTION DU SAMALAS EN 1257 LE LONG DU DÉTROIT D'ALAS, NUSA TENGGARA OUEST, INDONÉSIE Defense on: 11 December 2018 Supervised by : Prof. Franck LAVIGNE (Université Paris 1 – Panthhéon Sorbonne) Prof. HARTONO (Universitas Gadjah Mada) Rapporteurs : Prof. Hervé REGNAULD (Université de Rennes 2) Prof. SUWARDJI (Universitas Mataram) Examiners : Prof. Nathalie CARCAUD (AgroCampus Ouest) Dr. Danang Sri HADMOKO (Universitas Gadjah Mada) 1 Abstract As the most powerful event in Lombok’s recent eruptive history, volcanic materials that were expelled by the Samalas volcano in 1257 CE covered the entire of Lombok Island and are widespread in its eastern part. Almost 800 years after the eruption, the geomorphological impact of this eruption on the island of Lombok remains unknown, whereas its overall climatic and societal consequences are now better understood. A combination of stratigraphic information, present-day topography, geophysical measurement with two-dimensional resistivity profiling technique, local written sources, as well as laboratory and computational analysis, were used to obtain detailed information concerning geomorphic impacts of the 1257 CE eruption of Samalas volcano on the coastal area along the Alas Strait in West Nusa Tenggara Province, Indonesia. This study provides new information related to the geomorphic impact of a major eruption volcanic in coastal areas, in this case, on the eastern part of Lombok and the western coast of Sumbawa. In the first place, the study result shows that since the 1257 CE eruption, the landscape on the eastern part of Lombok is still evolved until the present time. -
Depth of Magma Chamber Determined by Experimental Petrologic Methods
DEPTH OF MAGMA CHAMBER DETERMINED BY EXPERIMENTAL PETROLOGIC METHODS Akihiko Tomiya Geological Survey of Japan, 1-1-3, Higashi, Tsukuba, Ibaraki, Japan Keywords: magma chamber, experimental petrology, Usu magma and, therefore, the composition of the residual melt, volcano, deep-seated geothermal resource that is, the evolved magma. ABSTRACT Thermodynamic conditions of a magma chamber can be estimated using petrographic information (e.g., compositions Depth of magma chamber (or young intrusive body) is one of and modal fractions of phenocrysts and groundmass) from a the most important parameters that determine the thermal representative rock erupted from the chamber. In order to structure and the circulation pattern of fluid around a estimate the pressure of magma chamber, the following geothermal area. The depth is also important when we methods are generally used; (1) geobarometer, (2) water recognize the magma chamber as a deep-seated geothermal content, and (3) melting experiment. One of the examples of resource itself. Here, we introduce an experimental petrologic the first method is an amphibole geobarometer (e.g., method for determining the depth of magma chamber. There Hammarstrom and Zen, 1986) where pressure is estimated are several methods in order to determine the depth (pressure) from the aluminum content of the amphibole crystallized from of a magma chamber. Among them, a melting experiment for the magma. This method, however, is difficult to apply to the rock erupted from the magma chamber is the most reliable natural magma because the geobarometer should be applied method. The method consists of the following procedure: (1) only when the mineral assemblage of the magma is the same as Select a sample (volcanic rock) which is representative of that of experimental products for which the geobarometer was magma in the chamber; (2) Give a petrographic description of calibrated. -
Undiscovered Papua National Mask Festival
UNDISCOVERED PAPUA NATIONAL MASK FESTIVAL One of the world’s most astonishing man-made spectacles, the Papua New Guinea national mask festival celebrates the unique mask cultures of the tribes of East New Britain: the Tolai, Baining, Pomio and Sulka. The festival itself is a four day extravaganza of storytelling, music, cultural dancing, and ritual performance. On the first day at dawn, the Kinavai is held, signalling the arrival of the Tolai Tubuans who arrive on canoes amidst the chanting and beating of kundu drums. Traditional masks will be on display during the festival – some many decades old, brought over from New Ireland Province and other parts of Papua New Guinea. Many of these masks are sacred and are not meant to be viewed, and the opening ceremony acts as a cleansing or appeasement ritual for the broken taboos. The highlight of the evening performances are the spectacular fire dances in which young initiated Baining men perform exhilarating rituals through blazing fires as their elders chant in haunting tones. During our stay we will also have time to visit wartime sites and WWII relics, travel through colourful welcoming villages and tour the rim of an active volcano. Attend the astonishing Kinavai ceremony on Kokopo beach at dawn. Witness the arrival of the Tolai people on canoes with wild drum beats. See traditional masks from all over Papua New Guinea. Be immersed by the performance of the Asaro mud-men warriors from the central highlands. Climb an active volcano and visit a vulcanology research station. Travel to the landing spot of Australian forces in World War One. -
150 Geologic Facts About California
California Geological Survey - 150th Anniversary 150 Geologic Facts about California California’s geology is varied and complex. The high mountains and broad valleys we see today were created over long periods of time by geologic processes such as fault movement, volcanism, sea level change, erosion and sedimentation. Below are 150 facts about the geology of California and the California Geological Survey (CGS). General Geology and Landforms 1 California has more than 800 different geologic units that provide a variety of rock types, mineral resources, geologic structures and spectacular scenery. 2 Both the highest and lowest elevations in the 48 contiguous states are in California, only 80 miles apart. The tallest mountain peak is Mt. Whitney at 14,496 feet; the lowest elevation in California and North America is in Death Valley at 282 feet below sea level. 3 California’s state mineral is gold. The Gold Rush of 1849 caused an influx of settlers and led to California becoming the 31st state in 1850. 4 California’s state rock is serpentine. It is apple-green to black in color and is often mottled with light and dark colors, similar to a snake. It is a metamorphic rock typically derived from iron- and magnesium-rich igneous rocks from the Earth’s mantle (the layer below the Earth’s crust). It is sometimes associated with fault zones and often has a greasy or silky luster and a soapy feel. 5 California’s state fossil is the saber-toothed cat. In California, the most abundant fossils of the saber-toothed cat are found at the La Brea Tar Pits in Los Angeles. -
A Review of Tertiary Climate Changes in Southern South America and the Antarctic Peninsula. Part 1: Oceanic Conditions
Sedimentary Geology 247–248 (2012) 1–20 Contents lists available at SciVerse ScienceDirect Sedimentary Geology journal homepage: www.elsevier.com/locate/sedgeo Review A review of Tertiary climate changes in southern South America and the Antarctic Peninsula. Part 1: Oceanic conditions J.P. Le Roux Departamento de Geología, Facultad de Ciencias Físicas y Matemáticas, Universidad de Chile/Centro de Excelencia en Geotérmia de los Andes, Casilla 13518, Correo 21, Santiago, Chile article info abstract Article history: Oceanic conditions around southern South America and the Antarctic Peninsula have a major influence on cli- Received 11 July 2011 mate patterns in these subcontinents. During the Tertiary, changes in ocean water temperatures and currents Received in revised form 23 December 2011 also strongly affected the continental climates and seem to have been controlled in turn by global tectonic Accepted 24 December 2011 events and sea-level changes. During periods of accelerated sea-floor spreading, an increase in the mid- Available online 3 January 2012 ocean ridge volumes and the outpouring of basaltic lavas caused a rise in sea-level and mean ocean temper- ature, accompanied by the large-scale release of CO . The precursor of the South Equatorial Current would Keywords: 2 fi Climate change have crossed the East Paci c Rise twice before reaching the coast of southern South America, thus heating Tertiary up considerably during periods of ridge activity. The absence of the Antarctic Circumpolar Current before South America the opening of the Drake Passage suggests that the current flowing north along the present western seaboard Antarctic Peninsula of southern South American could have been temperate even during periods of ridge inactivity, which might Continental drift explain the generally warm temperatures recorded in the Southeast Pacific from the early Oligocene to mid- Ocean circulation dle Miocene. -
Slow Rates of Subduction Erosion and Coastal Underplating Along the Andean Margin of Chile and Peru: COMMENT and REPLY
Slow rates of subduction erosion and coastal underplating along the Andean margin of Chile and Peru: COMMENT and REPLY COMMENT: doi: 10.1130/G24305C.1 to Miocene shallow marine and continental strata exposed along the coast of central Chile (33°–35°S). However, if presently exposed Neogene Alfonso Encinas strata in the Caldera basin and central Chile were deposited at depths of Departamento de Ciencias de la Tierra, Universidad de Concepción, ~2000 m, then the paleocoast must have been located tens of kilometers Casilla 160-C, Concepción, Chile to the east. In fact, the easternmost occurrence of shallow marine Pliocene Kenneth L. Finger successions in central Chile is ~40 km from the present coast (Encinas University of California Museum of Paleontology, 1101 Valley Life et al., 2006). Furthermore, marine sequences in central Chile are punc- Sciences Building, Berkeley, California 94720-4780, USA tuated by major unconformities between the Upper Cretaceous, Eocene, and Neogene (Gana et al., 1996). These have been recognized in wells In their article, Clift and Hartley (2007) propose the existence of two drilled on the continental shelf of south-central Chile (~36°–40°S), some alternating modes of subduction erosion for north-central Chile and Peru: located 40 km east of the present coast (Mordojovich, 1981). Whereas the one fast, with steady-state retreat from 150 to 20 Ma, and the other slow, unconformities represent regressive intervals of uplift, nondeposition, and with erosion constrained only in the trench domain from 20 Ma onward. erosion, the position of the paleocoastline must have oscillated widely. The proposed model is intriguing, as it reveals that subduction ero- In conclusion, we share Clift and Hartley’s point of view that there sion is not always by steady-state evolution with mass removal along the are alternating periods of fast and slow tectonic erosion, but we do not entire subduction channel and whole-scale landward retreat. -
Haole Matters: an Interrogation of Whiteness in Hawai'i
l/637 )(jJ~ 263 HAOLE MATTERS: AN INTERROGATION OF WHITENESS IN HAWAI'I A DISSERTATION SUBMITTED TO THE GRADUATE DMSION OF THE UNIVERSITY OF HAWAI'I IN PARTIAL FULFULLMENT OF THE REQUIREMENTS FOR THE DEGREE OF DOCTOR OF PHILOSOPHY IN POLITICAL SCIENCE AUGUST 2005 By Judy L. Rohrer Dissertation Committee: Kathy E. Ferguson, Chairperson Phyllis Turnbull Noenoe K. Silva Jonathan Goldberg-Hiller David Stannard iii © Copyright 2005 by Judy L. Rohrer All Rights Reserved iv This work is dedicated with respect and aloha to the women who were, and are my inspiration my grandmother, mother, and niece: Estella Acevedo Kasnetsis (1908-1975) Georgia Kasnetsis Acevedo (1938- ) Ho'ohila Estella Kawelo (2002-) v ACKNOWLEDGEMENTS It is impossible to thank all who contributed to this dissertation. I can only send a heartfelt mahalo out into the universe and trust it will light in the right places. For their unwavering support and guidance through this process, I thank my outstanding committee. My chair, Kathy Ferguson has been both friend and mentor, nurturing my theoretical growth, challenging stale thinking, and encouraging curiosity over moralizing. For all the parts of this dissertation that deal with Hawaiian culture and history and so many more, I am indebted to Noenoe Silva for her close read, gentle corrections, suggested sources, and inquisitive questions. Phyllis Turnbull has been my compass, always to the point ("rein itin, Bubba") and unfailingly supportive in times of doubt (''Breathe deeply. There is a god and she is still on our side"). Jon Goldberg~Hiller introduced me to critical legal theory and made the revolutionary s~ggestion that I defend ahead of schedule.