Relating the Lava Creek Ash to the Post-Flood Boundary
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Newsletter of the PANHANDLE ARCHEOLOGY SOCIETY Volume 35 Number 4 April 2015
PAsTIMES Newsletter of the PANHANDLE ARCHEOLOGY SOCIETY Volume 35 Number 4 April 2015 PRESIDENT Donna Otto VICE PRES- IDENT Scott Brosowske SECRETARY Mary Ruthe Carter The timing of the arrival of Paleo-Indians in the Great Plains TREASURER and in North America, in general, is under renewed investiga- Pam Allison tion. Recent genetic studies based on mitochondrial DNA sug- gest that a founding population composed of four distinct ge- netic lineages appeared in the Western Hemisphere between PUBLICATIONS 37,000 and 23,000 years before present (B.P.). It appears that Rolla Shaller all contemporary Native Americans are descendants of these Paleo-Indian lineages, including the hunter-gatherers who made their appearance in the Great Plains 18,000 years ago or NEWSLETTER earlier. EDITOR (Paleo Indians, Encyclopedia of the Great Plains. David J. Beryl C. Hughes Wishart, editor.) 1 TABLE OF CONTENTS PAGE 2a Upcoming Events; Amarillo Public Library Programs 3 Minutes of the Last Meeting 4 From the Editor’s Desk 5 Program for April 6 Early Inhabitants and Temporal Sequence 7 Clovis First? Chronology of Thought and Discoveries 8-12 Program SWFAS UPCOMING EVENTS SWFAS April 25, 2015, Hobbs NM. 5th Annual Perryton Stone Age Fair, April 28, 2015, Museum of the Plains, Perryton. [email protected] 806-434-0157 Science Day May 1, Lamar Elementary TAS Field School, June 13-20, Colorado County TX. AMARILLO PUBLIC LIBRARY PROGRAMS The Library has programs planned throughout April to enhance reading Empire of the Summer Moon, culminating with a visit by the author on May 4. These include: Adobe Walls: Saturday, April 11– Doors open at 9:30 and the program begins at 10. -
Related Magmatism in the Upper Wind River Basin, Wyoming (USA), GEOSPHERE; V
Research Paper THEMED ISSUE: Cenozoic Tectonics, Magmatism, and Stratigraphy of the Snake River Plain–Yellowstone Region and Adjacent Areas GEOSPHERE The leading wisps of Yellowstone: Post–ca. 5 Ma extension- related magmatism in the upper Wind River Basin, Wyoming (USA), GEOSPHERE; v. 14, no. 1 associated with the Yellowstone hotspot tectonic parabola doi:10.1130/GES01553.1 Matthew E. Brueseke1, Anna C. Downey1, Zachary C. Dodd1, William K. Hart2, Dave C. Adams3, and Jeff A. Benowitz4 12 figures; 2 tables; 1 supplemental file 1Department of Geology, Kansas State University, 108 Thompson Hall, Manhattan, Kansas 66506, USA 2Department of Geology and Environmental Earth Science, Miami University, 118C Shideler Hall, Oxford, Ohio 45056, USA 3Box 155, Teton Village, Wyoming 83025, USA CORRESPONDENCE: brueseke@ ksu .edu 4Geophysical Institute and Geochronology Laboratory, University of Alaska Fairbanks, Fairbanks, Alaska 99775, USA CITATION: Brueseke, M.E., Downey, A.C., Dodd, Z.C., Hart, W.K., Adams, D.C., and Benowitz, J.A., 2018, The leading wisps of Yellowstone: Post–ca. 5 Ma ABSTRACT the issue of linking volcanic events to a specific driving mechanism (Fouch, extension-related magmatism in the upper Wind River 2012; Kuehn et al., 2015). Complicating matters, magmatism often continues Basin, Wyoming (USA), associated with the Yellow- The upper Wind River Basin in northwest Wyoming (USA) is located ~80– long after (e.g., millions of years) the upper plate has been translated away stone hotspot tectonic parabola: Geosphere, v. 14, no. 1, p. 74–94, doi:10.1130/GES01553.1. 100 km southeast of the Yellowstone Plateau volcanic field. While the upper from an upwelling plume (Bercovici and Mahoney, 1994; Sleep, 2003; Shervais Wind River Basin is a manifestation of primarily Cretaceous to Eocene Lara- and Hanan, 2008; Jean et al., 2014). -
Water Development Office 6920 YELLOWTAIL ROAD TELEPHONE: (307) 777-7626 CHEYENNE, WY 82002 FAX: (307) 777-6819 TECHNICAL MEMORANDUM
THE STATE OF WYOMING Water Development Office 6920 YELLOWTAIL ROAD TELEPHONE: (307) 777-7626 CHEYENNE, WY 82002 FAX: (307) 777-6819 TECHNICAL MEMORANDUM TO: Water Development Commission DATE: December 13, 2013 FROM: Keith E. Clarey, P.G. REFERENCE: Snake/Salt River Basin Plan Update, 2012 SUBJECT: Available Groundwater Determination – Tab XI (2012) Contents 1.0 Introduction .............................................................................................................................. 1 2.0 Hydrogeology .......................................................................................................................... 4 3.0 Groundwater Development .................................................................................................... 15 4.0 Groundwater Quality ............................................................................................................. 21 5.0 Geothermal Resources ........................................................................................................... 22 6.0 Groundwater Availability ...................................................................................................... 22 References ..................................................................................................................................... 23 Appendix A: Figures and Table ....................................................................................................... i 1.0 Introduction This 2013 Technical Memorandum is an update of the September 10, 2003, -
Coexisting Discrete Bodies of Rhyolite and Punctuated Volcanism Characterize 1
RESEARCH ARTICLE Coexisting Discrete Bodies of Rhyolite and Punctuated 10.1029/2019GC008321 Volcanism Characterize Yellowstone's Post‐Lava Key Points: • Zircons from Yellowstone's Upper Creek Tuff Caldera Evolution ‐ Basin Member rhyolites yield U Pb Christy B. Till1 , Jorge A. Vazquez2 , Mark E. Stelten2 , Hannah I. Shamloo1 , dates defining crystallization 1,3 populations at ~750–550 and and Jamie S. Shaffer ~350–250 ka 1 2 • Discrete bodies of magma School of Earth and Space Exploration, Arizona State University, Tempe, AZ, USA, U.S. Geological Survey, Menlo Park, characterized the subvolcanic CA, USA, 3Now at Arizona State Geological Sciences, Now at New Mexico State University, Las Cruces, NM, USA system during the Upper Basin Member period and during storage of the Lava Creek Tuff ‐ 206 238 • Abstract Ion microprobe Pb/ U geochronology and trace element geochemistry of the unpolished The geochemical and isotopic ‐ evolution of Yellowstone's rims and sectioned interiors of zircons from Yellowstone caldera's oldest post caldera lavas provide post‐caldera rhyolites suggests a insight into the magmatic system during the prelude and aftermath of the caldera‐forming Lava Creek shift in the magmatic supereruption. The post‐caldera lavas compose the Upper Basin Member of the Plateau Rhyolite and fall assimilation/recharge ratio into two groups based on zircon crystallization age: early lavas with zircon ages between ~750 and 550 ka ‐ Supporting Information: and late lavas with zircon ages between ~350 and 250 ka. Zircons from the early erupted East Biscuit Basin • Supporting Information S1 flow yield U‐Pb dates and trace element compositions, which when considered with the Pb isotopic • Table S1 compositions of their coexisting feldspars and pyroxenes, point to an isotopically distinct parental melt • Table S2 • Table S3 present during crystallization of the Lava Creek magma but untapped by the supereruption. -
Texas Roadside Park Study
Texas Roadside Parks Study Historic Context & National Register Requirements An historic overview of the development and evolution of roadside parks and rest areas in Texas constructed by the Texas Department of Transportation from 1930 to 2015 and evaluation criteria for listing in the National Register of Historic Places. Prepared by: Sara Gredler, Megan Ruiz, Heather Goodson and Rick Mitchell, Mead & Hunt, Inc. The environmental review, consultation, and other actions required by applicable Federal environmental laws for this project are being, or have been, carried-out by TxDOT pursuant to 23 U.S.C. 327 and a Memorandum of Understanding dated 12-16-14, and executed by the FHWA and TxDOT . TxDOT Environmental Affairs Division Released: May 2015 420.14.GUI Table of Contents Page Part I Historic Context ........................................................................................................................... 4 A. Introduction ............................................................................................................................... 4 B. Setting the Stage for Roadside Parks, 1860s – 1930 ........................................................... 11 1. The Idea of the Park ......................................................................................................... 11 2. Importance of the Highway and the Rise of Automobile – Good Roads Movement ... 16 3. Introduction of the State Highway Systems ................................................................... 17 4. Early State Highways -
Formation of Low-Δ18o Rhyolites After Caldera Collapse at Yellowstone, Wyoming, USA
Formation of low-δ18O rhyolites after caldera collapse at Yellowstone, Wyoming, USA Ilya N. Bindeman John W. Valley Department of Geology and Geophysics, University of Wisconsin, 1215 West Dayton Street, Madison, Wisconsin 53706, USA ABSTRACT We present a new model for the genesis of low-δ18O rhyolites of the Yellowstone caldera based on analyses of zircons and individual quartz phenocrysts. Low-δ18O rhyolites were erupted soon after the massive caldera-forming Lava Creek Tuff eruption (602 ka, ~1000 km3) and contain xenocrysts of quartz and zircon inherited from precaldera rhyolites. These zircons are iso- topically zoned and out of equilibrium with their host low-δ18O melts and quartz. Diffusion modeling predicts that magmatic disequilibria of oxygen isotopes persists for as much as tens of thousands of years following nearly total remelting of the hydrothermally altered igneous roots of the depressed cauldron, in which the alteration-resistant quartz and zircon initially retained their δ18O values. These results link melting to caldera collapse, rule out rapid or catastrophic magma–meteoric water interaction, and indicate wholesale melting rather than assimilation or partial melting. Keywords: Yellowstone, zircon, oxygen isotopes, caldera, low δ18O. INTRODUCTION rock major and trace element composition is simi- (Spicuzza et al., 1998b). We measured four to Meteoric water plays an important role in the lar to that of isotopically normal high-silica rhyo- seven aliquots of UWG-2 garnet standard on each genesis of ore deposits, explosive volcanism, and lites of precaldera lavas or lavas erupted simul- day of analysis. Nine analyses of NBS-28 quartz hydrothermal activity. Low values of δ18O un- taneously outside the caldera. -
Basic Seismological Characterization for Sublette County, Wyoming By
Basic Seismological Characterization for Sublette County, Wyoming by James C. Case, Rachel N. Toner, and Robert Kirkwood Wyoming State Geological Survey September 2002 BACKGROUND Seismological characterizations of an area can range from an analysis of historic seismicity to a long-term probabilistic seismic hazard assessment. A complete characterization usually includes a summary of historic seismicity, an analysis of the Seismic Zone Map of the Uniform Building Code, deterministic analyses on active faults, “floating earthquake” analyses, and short- or long- term probabilistic seismic hazard analyses. Presented below, for Sublette County, Wyoming, are an analysis of historic seismicity, an analysis of the Uniform Building Code, deterministic analyses of nearby active faults, an analysis of the maximum credible “floating earthquake”, and current short- and long-term probabilistic seismic hazard analyses. Historic Seismicity in Sublette County The enclosed map of “Earthquake Epicenters and Suspected Active Faults with Surficial Expression in Wyoming” (Case and others, 1997) shows the historic distribution of earthquakes in Wyoming. Eighteen magnitude 2.5 or intensity III and greater earthquakes have been recorded in Sublette County. On October 24, 1936, two earthquakes occurred in western Wyoming. The U.S.G.S. National Earthquake Information Center reported these two intensity III earthquakes as occurring in Sublette County, approximately 3 miles southwest of Cora. The original reference and description of these events, however, indicates that these earthquakes originated in the Star Valley of Lincoln County (Neumann, 1936). In June of 1945, two earthquakes occurred in southwestern Sublette County. These intensity III earthquakes were recorded on June 7, 1945, approximately 4 miles northwest of Calpet, and on June 23, 1945, approximately 3 miles northeast of Calpet. -
Water Resources of Teton County, Wyoming, Exclusive of Yellowstone National Park
WATER RESOURCES OF TETON COUNTY, WYOMING, EXCLUSIVE OF YELLOWSTONE NATIONAL PARK 105° 104° U.S. GEOLOGICAL SURVEY Water-Resources Investigations Report 95-4204 Prepared in cooperation with the WYOMING STATE ENGINEER WATER RESOURCES OF TETON COUNTY, WYOMING, EXCLUSIVE OF YELLOWSTONE NATIONAL PARK by Bernard T. Nolan and Kirk A. Miller U.S. GEOLOGICAL SURVEY Water-Resources Investigations Report 95-4204 Prepared in cooperation with the WYOMING STATE ENGINEER Cheyenne, Wyoming 1995 U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY GORDON P. EATON, Director The use of trade, product, industry, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. For additional information Copies of this report can be write to: purchased from: District Chief U.S. Geological Survey U.S. Geological Survey Earth Science Information Center Water Resources Division Open-File Reports Section 2617 E. Lincolnway, Suite B Box 25286, Denver Federal Center Cheyenne, Wyoming 82001 -5662 Denver, Colorado 80225 CONTENTS Page Abstract................................................................................................................................................................................. 1 Introduction........................................................................................................................................................................... 2 Purpose and scope...................................................................................................................................................... -
GEOLOGIC MAP of the HEBGEN LAKE 30' X 60' QUADRANGLE
GEOLOGIC MAP OF THE HEBGEN LAKE 30' x 60' QUADRANGLE, BEAVERHEAD, MADISON, AND GALLATIN COUNTIES, MONTANA, PARK AND TETON COUNTIES, WYOMING, AND CLARK AND FREMONT COUNTIES, IDAHO by J. Michael O’Neill1 and Robert L. Christiansen2 Montana Bureau of Mines and Geology Open-File Report 464 2002 Revisions: 8/03 Map edge-matched and text revised to provide continuity with adjacent Ennis and Gardiner 30’ x 60’ quadrangles. 1 U.S. Geological Survey, P.O. Box 25046, M.S. 964, Federal Center, Denver, CO 80225 2 U.S. Geological Survey, M.S. 910, 345 Middlefield Rd., Menlo Park, CA 94025 This report has had preliminary reviews for conformity with Montana Bureau of Mines and Geology’s technical and editorial standards CORRELATION OF MAP UNITS HEBGEN LAKE 30 x 60 QUADRANGLE CENOZOIC and MESOZOIC Qaf 1 Qfp Qal Qc Qac Qaf Qe Qta Qrg Qbo Qat Quaternary Holocene Qlk Qgo Qgt Qaf 2 Qls Qcpu Qlcu Qpg Qgr Qmr Pleistocene Qatc Qmb QTgr Qpcl Qlcl CENOZOIC Thru Pliocene Thr Thrl unconformity Tsg Tsc Tertiary Miocene Tv Tmv Tfv Tmi Oligocene Tav Tre Eocene unconformity Tda TKgr Paleocene Kbe 1 Kbe 2 Kbe 3 Kevv Ktc Cretaceous Kco Kf MESOZOIC Km Kmd Kt Kk Jurassic Jm Jme Je Triassic Tr w Tr wd Tr d 1 CORRELATION OF MAP UNITS HEBGEN LAKE 30’ x 30’ QUADRANGLE PALEOZOIC and PRECAMBRIAN Psh Permian IP q Pennsylvanian IP M a Mm Mississippian MDt PALEOZOIC Devonian Dj unconformity Ordovician OЄs Єp Єpm Єm Cambrian Єw Єwf Єf unconformity Xmy pЄms pЄgg Xgbc Xgb Xq4 PROTEROZOIC Xph3 Xph2 Xq3 Xks Xif Xph1 Xq21 Xqms Xq 1 Xqfb Xpm pЄgq ARCHEAN XAgd XAam XAm XAq XAms XAcs XAbs Aqfg Aum Ag Aqfbg Adi At 2 3 DESCRIPTION OF MAP UNITS HEBGEN LAKE 30’ x 60’ QUADRANGLE SEDIMENT AND SEDIMENTARY ROCKS Qfp Floodplain deposits (Holocene)—Sand, silt, and clay deposited in broad, open stream valleys and in confined ephemeral stream channels. -
Lava Creek Tuff Love
Goldschmidt2018 Abstract Lava Creek Tuff Love K.S. BEFUS*, R.H. BRUYERE1, M. MANGA2 1Baylor University, One Bear Place #97354 Waco TX 76798 (*[email protected]) 2UC-Berkeley, 307 McCone Hall Berkeley CA 94720 Yellowstone caldera’s most recent supereruption generated ~1000 km3 of rhyolitic ash-fall and ignimbrites. Together the deposits are named the Lava Creek Tuff, but the eruptive sequence is separated into Lava Creek Tuff A and B based on stratigraphic and compositional differences. Primary among these differences is the presence of Fe-rich amphibole as the mafic phase in Lava Creek Tuff A. Hydrous mineral phases are very rare at Yellowstone, thus amphibole in Lava Creek Tuff A may indicate a unique petrologic condition prior to the supereruption. To better understand the pre- eruptive storage conditions of both of the Lava Creek Tuff magmas, we collected pumice clasts from the unwelded basal ignimbrite of Lava Creek Tuff A and the unwelded basal fall of Lava Creek Tuff B. We were restricted to unwelded ignimbrite because no fall deposits of Lava Creek Tuff A are described in the literature or field trip guides. We hope to identify outcrops in future field work. We crushed pumice clasts from both units and handpicked crystals to produce mineral separates. We then analyzed plagioclase (Ab70), T sanidine (Or53±2), amphibole (Al =1.4), fayalite (Fa94±1), clinopyroxene (Wo42±1En15±3Fs43±2), and Fe-Ti oxides using an electron microprobe. Fe-Ti oxides in both units have pronounced exsolution lamellae and cannot be used for thermometry. Thermobarometry and Rhyolite-MELTS modeling using glass and mineral compositions suggest the magma was stored at 800±50 °C and <250 MPa. -
Hispanic Texans
texas historical commission Hispanic texans Journey from e mpire to Democracy a GuiDe for h eritaGe travelers Hispanic, spanisH, spanisH american, mexican, mexican american, mexicano, Latino, Chicano, tejano— all have been valid terms for Texans who traced their roots to the Iberian Peninsula or Mexico. In the last 50 years, cultural identity has become even more complicated. The arrival of Cubans in the early 1960s, Puerto Ricans in the 1970s, and Central Americans in the 1980s has made for increasing diversity of the state’s Hispanic, or Latino, population. However, the Mexican branch of the Hispanic family, combining Native, European, and African elements, has left the deepest imprint on the Lone Star State. The state’s name—pronounced Tay-hahs in Spanish— derives from the old Spanish spelling of a Caddo word for friend. Since the state was named Tejas by the Spaniards, it’s not surprising that many of its most important geographic features and locations also have Spanish names. Major Texas waterways from the Sabine River to the Rio Grande were named, or renamed, by Spanish explorers and Franciscan missionaries. Although the story of Texas stretches back millennia into prehistory, its history begins with the arrival of Spanish in the last 50 years, conquistadors in the early 16th cultural identity century. Cabeza de Vaca and his has become even companions in the 1520s and more complicated. 1530s were followed by the expeditions of Coronado and De Soto in the early 1540s. In 1598, Juan de Oñate, on his way to conquer the Pueblo Indians of New Mexico, crossed the Rio Grande in the El Paso area. -
Montana Bureau of Mines and Geology
Montana Bureau of Mines and Geology GEOLOGIC MAP OF THE GARDINER 30' x 60' QUADRANGLE, SOUTH-CENTRAL MONTANA By Richard B. Berg, Jeffrey D. Lonn, and William W. Locke* Montana Bureau of Mines and Geology Open File Report MBMG 387 1999 REVISIONS Map: 9/01 11/08 Map and text: 12/02 9/03 4/07 This report has been reviewed for conformity with Montana Bureau of Mines and Geology’s technical and editorial standards. Partial support has been provided by the STATEMAP component of the National Cooperative Geologic Mapping Program of the U.S. Geological Survey under Contract Number 98- HQ-AG 2080. (*) Department of Earth Sciences, Montana State University, Bozeman, MT 59701 Correlation Chart of Cenozoic and Mesozoic Map Units Gardiner 30’ x 60’ Quadrangle Holocene Qls Qal Quaternary Quaternary Qao Qta Pleistocene Qg Qgt Qgl Qtr Qba Qlc Miocene Pliocene/ Unconformity Cenozoic Ts Thr Tb a Tg Tr Tl Tfpy Tmz Tdaf Tdap Td Tdip Ta Tanf Tavv d a e TpCi Ti Tav Tms Unconformity Eocene Tertiary Tgcb Tgcf Tgcs Tse Tslc 1 Tsec Unconformity Cretaceous ? Kdi Ks Klf Upper Lower ? Kclf Kmfr Kk Triassic Triassic Jurassic/ Mesozoic Mesozoic JTRs Correlation of Paleozoic and Precambrian Map Units Gardiner 30’ x 60’ Quadrangle PMpa Psh Permian PMs IPMqa Pennsylvanian Mm Mississippian Pzs Paleozoic DOs Devonian and Ordovician Єsrp Єs Cambrian Єpf Unconformity ? TpCi pЄim pЄmy Proterozoic Unconformity Precambrian Asw1 Asw2 Asw3 Asw4 Asw5 Asw6 Asw7 Archean Aamh Aga Agn Agr Anc Aqa As Ash 2 Description of Map Units Qls Landslide deposit (Holocene) - Landslides are typically developed at the unconformity between Tertiary volcanic units and the Precambrian basement, possibly in bentonite beds situated at the base of the Tertiary volcaniclastic sequence.