Scientific Contradictions to the Book of Genesis
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Texas Co-Op Power • March 2017
LOCAL ELECTRIC COOPERATIVE EDITION MARCH 2017 Blizzard of ’57 Spring Vegetable Salads Palo Duro Pageant 35 35on Brake-worthy stops on highway through co-op country THE TRACTOR THAT STARTED IT ALL. IS CHANGING IT ALL. Metal Hood, Fenders New Deluxe Seat** New Swift-TTaach Loader** New Grille Guard New Dash Panel & Operator Platform & Tilt Steering Wheel & Swift-Connect Backhoe & Front Hitch & Display ALL-NEWW KUBOTTAA BX80 SERIES Low-Rate, Long-TTeerm Financing 6 YYeear Goingg On Noww! Limited Powertrain Warrantyy* kubota.com *Only terms and conditions of Kubota’s standard Limited Warranty applyy.. For warranty terms, see Kubota’s Limited Warranty at www.kubota.com or authorized Kubota Dealers. **Only avvaailable on certain models. Optional equipment may be shown. © Kubota TTrractor Corporation, 2017 Since 1944 March 2017 FAVORITES 5 Letters 6 Currents 18 Local Co-op News Get the latest information plus energy and safety tips from your cooperative. 29 Texas History Panhandle Blizzard of 1957 By Dawn Stephens 31 Recipes Spring Vegetable Salads 35 Focus on Texas Photo Contest: In Motion 36 Around Texas List of Local Events 38 Hit the Road Texas on a Grand Stage in Palo Duro By Sheryl Smith-Rodgers Marker near the northern end ONLINE of Interstate 35 in Texas, just TexasCoopPower.com south of the Red River Find these stories online if they don’t appear in your edition of the magazine. FEATURE Texas USA Odessa Meteor Crater 35 on 35 8 Stops with fascinating food, history and popular By E.R. Bills culture lure travelers from the interstate as it weaves Observations through Texas from Mexico to Oklahoma Another Roadside Attraction Story and photos by Julia Robinson By Ryann Ford ROAD TRIP! See video and photos at TexasCoopPower.com NEXT MONTH Drones: An Overview Texas inno- vators, including electric co-ops, hone drones as tools of today. -
Barringer Meteorite Crater, Coconino County, Arizona
BARRINGERI' METEORITE CRATER, COCONINO COUNTY, ARIZONA Eugene Shoemaker CaliforniaInstitute of Technology David Roddy United States Geological Survey Carleton Moore Arizona State University Robert Dietz Arizona State University A one-day field trip will visit Barringer Meteorite Crater. Partici pants will depart from Tempe in the evening and spend the night in Flagstaff. The field trip will depart from Flagstaff to the Crater and will return to Flagstaff and Phoenix on the same day. At the Crater participants may choose from a number of guided or self-guided op tions to visit this interesting geologic feature. In addition to the road guide included here participants will be provided with a ''Guidebook to the Geology of Meteor Crater, Arizona" prepared for the 37th Annual Meeting of the Meteoritical Society. It has been reprinted and is available from the Center forMeteorite Studies, Arizona State Uni versity, Tempe, Arizona 85281. Access to the Crater is by the courtesy of the Barringer Crater Company and Meteor Crater Enterprises, Inc. Visitors must receive permission to enter nonpublic areas of the Crater. SYNOPSIS OF THE The Supai Formation consists of interbedded red and GEOLOGY OF METEOR CRATER yellow fine-grained argillaceous sandstone and subordinate by Eugene M. Shoemaker siltstone. It is more than 300 meters (1,000 feet) thick in REGIONAL SETTING this region (Pierce, 1958, p. 84), but not more than 100 Meteor Crater lies in north-central Arizona in the Can meters or so (a few hundred feet) have been penetrated by yon Diablo region of the southern part of the Colorado drill holes at the crater. -
Geology, Petrography, Shock Petrography, and Geochemistry of Impactites and Target Rocks from the Kärdla Crater, Estonia
Meteoritics & Planetary Science 39, Nr 3, 425–451 (2004) Abstract available online at http://meteoritics.org Geology, petrography, shock petrography, and geochemistry of impactites and target rocks from the Kärdla crater, Estonia V. PUURA,1* H. HUBER, 2† J. KIRS,1 A. KÄRKI,3 K. SUUROJA, 4 K. KIRSIMÄE, 1 J. KIVISILLA, 4 A. KLEESMENT, 5 M. KONSA,5 U. PREEDEN, 1 S. SUUROJA, 5 and C. KOEBERL 2 1Institute of Geology, University of Tartu, Vanemuise strasse 46, 51014 Tartu, Estonia 2Department of Geological Sciences, University of Vienna, Althanstrasse 14, A-1090 Vienna, Austria 3Institute of Geosciences, University of Oulu, Box 3000, FIN-90401 Oulu, Finland 4Geological Survey of Estonia, Kadaka tee 80/82, 12618 Tallinn, Estonia 5Institute of Geology, Tallinn Technical University, Estonia pst. 7, 10143 Tallinn, Estonia †Present address: Institute of Geophysics and Planetary Physics, University of California Los Angeles, 595 Charles Young Drive, Los Angeles, California 90095, USA *Corresponding author. E-mail: [email protected] (Received 20 December 2002; revision accepted 7 January 2004) Abstract–The Kärdla crater is a 4 km-wide impact structure of Late Ordovician age located on Hiiumaa Island, Estonia. The 455 Ma-old buried crater was formed in shallow seawater in Precambrian crystalline target rocks that were covered with sedimentary rocks. Basement and breccia samples from 13 drill cores were studied mineralogically, petrographically, and geochemically. Geochemical analyses of major and trace elements were performed on 90 samples from allochthonous breccias, sub-crater and surrounding basement rocks. The breccia units do not include any melt rocks or suevites. The remarkably poorly mixed sedimentary and crystalline rocks were deposited separately within the allochthonous breccia suites of the crater. -
Adventists and Genesis
Adventists And Genesis The Primary Time Theory Refuted By Paul Nethercott 2008 Three Angels Website www.CreationismOnline.com 1 Biblical Creationism Genesis 1:1 Genesis 2:3 The Literal Week 168 Hours 4,000 BC 4,000 BC 2 SDA Bible Commentary, Volume 1, Page 218, 1978. The Primary Time Theory Genesis 1:1 Genesis 1:3 Genesis 2:3 Primary Time Creation Week 4,500 Million Years 168 Hours? 4,500,000,000 BC 4,000 BC 4,000 BC Invented By Jehovah’s Witnesses The New Creation, 1904, Pastor Charles Russell, page 18,19. “Creation,” 1927, Judge Rutherford, Page 14, 27, 30, 35, 36, 37, 45 Evolution Or By Creation?, Chapter 3, 1985 Edition Evolution Or Creation, 1985, Page 26 All Scripture Inspired, 1990, Page 14 Aid To Bible Understanding, Page 476 Reasoning From The Scriptures, 1989, Page 88 3 Awake!, May 8, 1997, page 12 The Watchtower, April 1, 1986, pages 12-13 Awake!, March 22, 1983, pages 12-13 Awake, September 2006, Pages 3, 18, 19, 20, 28 4 Primary Time Diagram G Geological Creation Biological Creation Rest Days Rest Days Light Day And Night Plants Snow, Continental Drift, Rivers Dry Land, Volcanoes, Glaciers 1 2 3 4 5 6 7 Mountains, Erosion, Rain Volcanic Ash, Meteor Craters Sun, Work Days Solar System 4,500,000,000 BC 4,0005 BC 4,000 BC Invented By Jehovah’s Witnesses The Creation Week Genesis 1:1 Genesis 1:3 Genesis 2:3 5,000 Million Years Ago 6,000 Years Ago Geological Creation Biological Creation Light Land Day 1 Day And Night Plants Snow, Continental Drift, Rivers Dry Land, Volcanoes, Glaciers Day 3 Day 2 Day 3 Day 5 Day 6 Day 7 Mountains, -
POSTER SESSION 5:30 P.M
Monday, July 27, 1998 POSTER SESSION 5:30 p.m. Edmund Burke Theatre Concourse MARTIAN AND SNC METEORITES Head J. W. III Smith D. Zuber M. MOLA Science Team Mars: Assessing Evidence for an Ancient Northern Ocean with MOLA Data Varela M. E. Clocchiatti R. Kurat G. Massare D. Glass-bearing Inclusions in Chassigny Olivine: Heating Experiments Suggest Nonigneous Origin Boctor N. Z. Fei Y. Bertka C. M. Alexander C. M. O’D. Hauri E. Shock Metamorphic Features in Lithologies A, B, and C of Martian Meteorite Elephant Moraine 79001 Flynn G. J. Keller L. P. Jacobsen C. Wirick S. Carbon in Allan Hills 84001 Carbonate and Rims Terho M. Magnetic Properties and Paleointensity Studies of Two SNC Meteorites Britt D. T. Geological Results of the Mars Pathfinder Mission Wright I. P. Grady M. M. Pillinger C. T. Further Carbon-Isotopic Measurements of Carbonates in Allan Hills 84001 Burckle L. H. Delaney J. S. Microfossils in Chondritic Meteorites from Antarctica? Stay Tuned CHONDRULES Srinivasan G. Bischoff A. Magnesium-Aluminum Study of Hibonites Within a Chondrulelike Object from Sharps (H3) Mikouchi T. Fujita K. Miyamoto M. Preferred-oriented Olivines in a Porphyritic Olivine Chondrule from the Semarkona (LL3.0) Chondrite Tachibana S. Tsuchiyama A. Measurements of Evaporation Rates of Sulfur from Iron-Iron Sulfide Melt Maruyama S. Yurimoto H. Sueno S. Spinel-bearing Chondrules in the Allende Meteorite Semenenko V. P. Perron C. Girich A. L. Carbon-rich Fine-grained Clasts in the Krymka (LL3) Chondrite Bukovanská M. Nemec I. Šolc M. Study of Some Achondrites and Chondrites by Fourier Transform Infrared Microspectroscopy and Diffuse Reflectance Spectroscopy Semenenko V. -
Emplacement of Cretaceous-Tertiary Boundary Shocked Quartz from Chicxulub Crater Walter Alvarez,* Philippe Claeys,T Susan W
ARTICLES Emplacement of Cretaceous-Tertiary Boundary Shocked Quartz from Chicxulub Crater Walter Alvarez,* Philippe Claeys,t Susan W. Kieffer Observations on shocked quartz in Cretaceous-Tertiary (K-T) boundary sediments get rock and with the crystallization age of compellingly tied to Chicxulub crater raise three problems. First, in North America zircons from Chicxulub melt rock (17). It shocked quartz occurs above the main K-T ejecta layer. Second, shocked quartz is now seems clear that both layers were pro- more abundant west than east of Chicxulub. Third, shocked quartz reached distances duced by the Chicxulub impact and that requiring initial velocities up to 8 kilometers per second, corresponding to shock the shocked quartz and other minerals orig- pressures that would produce melt, not the moderate-pressure shock lamellae ob- inated from the basement granite. Iridium served. Shock devolatilization and the expansion of carbon dioxide and water from and quartz are believed to come from dif- impacted wet carbonate, producing a warm, accelerating fireball after the initial hot ferent sources: vaporized meteorite and un- fireball of silicate vapor, may explain all three problems. melted basement rock, respectively. Prob- lem 1 is thus, how did the shocked quartz and the iridium end up together in a sepa- rate layer, above the layer ofkaolinitic clay? In wells and outcrops of uninterrupted ma- impact crater (12) dating precisely from the The geographic distribution of K-T rine sedimentary rocks outside of North K-T boundary at 65.0 Ma (13) and sur- shocked quartz is not fully known, but it America, the K-T boundary is marked by a rounded out to -4000-km radius by proxi- appears to be much more abundant and single 1- to 10-mm clay layer often contain- mal ejecta at the biostratigraphic K-T slightly coarser grained at longitudes west of ing anomalous iridium and altered impact boundary (5, 7, 8) has strongly confirmed Chicxulub. -
Keller 1989 GSA Bull
Downloaded from gsabulletin.gsapubs.org on November 18, 2014 Geological Society of America Bulletin Extended period of extinctions across the Cretaceous /Tertiary boundary in planktonic foraminifera of continental-shelf sections: Implications for impact and volcanism theories GERTA KELLER Geological Society of America Bulletin 1989;101, no. 11;1408-1419 doi: 10.1130/0016-7606(1989)101<1408:EPOEAT>2.3.CO;2 Email alerting services click www.gsapubs.org/cgi/alerts to receive free e-mail alerts when new articles cite this article Subscribe click www.gsapubs.org/subscriptions/ to subscribe to Geological Society of America Bulletin Permission request click http://www.geosociety.org/pubs/copyrt.htm#gsa to contact GSA Copyright not claimed on content prepared wholly by U.S. government employees within scope of their employment. Individual scientists are hereby granted permission, without fees or further requests to GSA, to use a single figure, a single table, and/or a brief paragraph of text in subsequent works and to make unlimited copies of items in GSA's journals for noncommercial use in classrooms to further education and science. This file may not be posted to any Web site, but authors may post the abstracts only of their articles on their own or their organization's Web site providing the posting includes a reference to the article's full citation. GSA provides this and other forums for the presentation of diverse opinions and positions by scientists worldwide, regardless of their race, citizenship, gender, religion, or political viewpoint. Opinions presented in this publication do not reflect official positions of the Society. -
Flynn Creek Crater, Tennessee: Final Report, by David J
1967010060 ASTROGEOLOGIC STUDIES / ANNUAL PROGRESS REPORT " July 1, 1965 to July 1, 1966 ° 'i t PART B - h . CRATERINVESTIGATIONS N 67_1_389 N 57-" .]9400 (ACCEC_ION [4U _" EiER! (THRU} .2_ / PP (PAGLS) (CO_ w ) _5 (NASA GR OR I"MX OR AD NUMBER) (_ATEGORY) DEPARTMENT OF THE INTERIOR UNITED STATES GEOLOQICAL SURVEY • iri i i i i iiii i i 1967010060-002 ASTROGEOLOGIC STUDIES ANNUAL PROGRESS REPORT July i, 1965 to July I, 1966 PART B: CRATER INVESTIGATIONS November 1966 This preliminary report is distributed without editorial and technical review for conformity with official standards and nomenclature. It should not be quoted without permission. This report concerns work done on behalf of the National Aeronautics and Space Administration. DEPARTMENT OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY 1967010060-003 • #' C OING PAGE ,BLANK NO/" FILMED. CONTENTS PART B--CRATER INVESTIGATIONS Page Introduction ........................ vii History and origin of the Flynn Creek crater, Tennessee: final report, by David J. Roddy .............. 1 Introductien ..................... 1 Geologic history of the Flynn Creek crater ....... 5 Origin of the Flynn Creek crater ............ ii Conc lusions ...................... 32 References cited .................... 35 Geology of the Sierra Madera structure, Texas: progress report, by H. G. Wilshire ............ 41_ Introduction ...................... 41 Stratigraphy ...................... 41 Petrography and chemical composition .......... 49 S truc ture ....................... 62 References cited ............. ...... 69 Some aspects of the Manicouagan Lake structure in Quebec, Canada, by Stephen H. Wolfe ................ 71 f Craters produced by missile impacts, by H. J. Moore ..... 79 Introduction ...................... 79 Experimental procedure ................. 80 Experimental results .................. 81 Summary ........................ 103 References cited .................... 103 Hypervelocity impact craters in pumice, by H. J. Moore and / F. -
Contents Page
Contents Page Adventists and Genesis The Primary Time Theory Refuted By Paul Nethercott 2008 Contents Introduction Jehovah Witness Viewpoint Seventh Day Adventist Viewpoint The Age Of the Earth Is the Age Of Mankind Scientific Contradictions To The Book Of Genesis No Gap Between Genesis 1:1 and 1:3 Radioactive Dating Is Whole Rock Dating Radioactive Dating And Fossil Ages Radioactive Dating Of ‘Pre‐Cambrian’ Rocks Genesis Versus Radio‐Active Dating Chronology Controversy Over Radiometric Dating Methods The Days Of Creation Are Literal 24 Hour Days Ellen G. Whites Comments Gunter Faure Brent Dalrymple History Of Modern Creationism The Biblical Account Of Origins In the Beginning Where Did the Light on the First Day Come From? Light On The First Day Of Creation Loma Linda University Conclusions References www.CreationOnTheWeb.org Adventists And Genesis 1 Introduction The Men Behind The Idea The Founders Of The Primary Time Theory Pastor Russell Judge Rutherford Nathan Homer Knorr Jehovah’s Witnesses The Bible does not say how long a period elapsed between the beginning when God created the heaven and the earth, and the Jehovah’s Witnesses beginning of the creative week used in perfecting it for man: nor do Long before the beginning of those Jehovah’s Witnesses geologists agree amongst seven days the molten mass had “In the beginning God created the heavens and the themselves as to the period of this thrown off great quantities of mineral interval‐‐a few extremists indulge in Earth.” (Genesis 1:1) Just how long ago the starry substances in vapor form, and these heavens and the earth were created is not stated In wild speculations of millions of had formed into rings around the years. -
The Tennessee Meteorite Impact Sites and Changing Perspectives on Impact Cratering
UNIVERSITY OF SOUTHERN QUEENSLAND THE TENNESSEE METEORITE IMPACT SITES AND CHANGING PERSPECTIVES ON IMPACT CRATERING A dissertation submitted by Janaruth Harling Ford B.A. Cum Laude (Vanderbilt University), M. Astron. (University of Western Sydney) For the award of Doctor of Philosophy 2015 ABSTRACT Terrestrial impact structures offer astronomers and geologists opportunities to study the impact cratering process. Tennessee has four structures of interest. Information gained over the last century and a half concerning these sites is scattered throughout astronomical, geological and other specialized scientific journals, books, and literature, some of which are elusive. Gathering and compiling this widely- spread information into one historical document benefits the scientific community in general. The Wells Creek Structure is a proven impact site, and has been referred to as the ‘syntype’ cryptoexplosion structure for the United State. It was the first impact structure in the United States in which shatter cones were identified and was probably the subject of the first detailed geological report on a cryptoexplosive structure in the United States. The Wells Creek Structure displays bilateral symmetry, and three smaller ‘craters’ lie to the north of the main Wells Creek structure along its axis of symmetry. The question remains as to whether or not these structures have a common origin with the Wells Creek structure. The Flynn Creek Structure, another proven impact site, was first mentioned as a site of disturbance in Safford’s 1869 report on the geology of Tennessee. It has been noted as the terrestrial feature that bears the closest resemblance to a typical lunar crater, even though it is the probable result of a shallow marine impact. -
Pecos Trail Newsletter Aug-2016
Texas Pecos Trail Region Newsletter August 2016 TPTR Mission The Texas Pecos Trail Region develops and promotes heritage preservation and tourism throughout the richly diverse West Texas area. Inside this Issue: Pecos Trail Partners Event — 1 Midland TX, Petroleum Museum Pecos Trail Partners Event—Midland TPTR Partners Event, Cont’d 2 The Texas Pecos Trail Region held our bi-monthly Partners Event on Travel Itinerary: 2 July 21 in Midland TX at the Permian Basin Petroleum Museum. Guests Outlaws and Lawmen came from Brackettville, Crane, Eldorado, Junction, Langtry, McCamey, Get Ready for State Fair 3 Midland, Monahans, and Sonora. Jordan Resigns, New ED 3 Museum staff led attendees on a guided tour of the museum, which has been recently renovated with immersive, state-of-the-art exhibits to Preservation Spotlight: 3 Odessa Meteor Crater enhance the visitor experience. Attendees were introduced to the new Permian Sea diorama, historic photos and rare artifacts of the Permian Aug Calendar of Events 4 Basin oil fields and communities, oil and gas exploration technology, Contact Information 4 alternative energy sources, mid-20th-Century cultural life, and the near-futuristic Petrotrekker ride. At the business meeting we discussed recent travel guide promotions TPTR Board of Directors at regional events, funding for the current and upcoming fiscal years, and State Fair participation. The board approved heritage tourism grants to Bill Hodges (Chair) Rancher, Eldorado the George W. Bush Childhood Home in Midland for public reading Ellen Crossland (Vice Chair) programs and to the Kimble County Historical Museum for exhibit Mendoza Trail Museum, McCamey development in their new museum facilities in Junction. -
Nördlingen 2010: the Ries Crater, the Moon, and the Future of Human Space Exploration, P
Program and Abstract Volume LPI Contribution No. 1559 The Ries Crater, the Moon, and the Future of Human Space Exploration June 25–27, 2010 Nördlingen, Germany Sponsors Museum für Naturkunde – Leibniz-Institute for Research on Evolution and Biodiversity at the Humboldt University Berlin, Germany Institut für Planetologie, University of Münster, Germany Deutsches Zentrum für Luft- und Raumfahrt DLR (German Aerospace Center) at Berlin, Germany Institute of Geoscience, University of Freiburg, Germany Lunar and Planetary Institute (LPI), Houston, USA Deutsche Forschungsgemeinschaft (German Science Foundation), Bonn, Germany Barringer Crater Company, Decatur, USA Meteoritical Society, USA City of Nördlingen, Germany Ries Crater Museum, Nördlingen, Germany Community of Otting, Ries, Germany Märker Cement Factory, Harburg, Germany Local Organization City of Nördlingen Museum für Naturkunde – Leibniz- Institute for Research on Evolution and Biodiversity at the Humboldt University Berlin Ries Crater Museum, Nördlingen Center of Ries Crater and Impact Research (ZERIN), Nördlingen Society Friends of the Ries Crater Museum, Nördlingen Community of Otting, Ries Märker Cement Factory, Harburg Organizing and Program Committee Prof. Dieter Stöffler, Museum für Naturkunde, Berlin Prof. Wolf Uwe Reimold, Museum für Naturkunde, Berlin Dr. Kai Wünnemann, Museum für Naturkunde, Berlin Hermann Faul, First Major of Nördlingen Prof. Thomas Kenkmann, Freiburg Prof. Harald Hiesinger, Münster Prof. Tilman Spohn, DLR, Berlin Dr. Ulrich Köhler, DLR, Berlin Dr. David Kring, LPI, Houston Dr. Axel Wittmann, LPI, Houston Gisela Pösges, Ries Crater Museum, Nördlingen Ralf Barfeld, Chair, Society Friends of the Ries Crater Museum Lunar and Planetary Institute LPI Contribution No. 1559 Compiled in 2010 by LUNAR AND PLANETARY INSTITUTE The Lunar and Planetary Institute is operated by the Universities Space Research Association under a cooperative agreement with the Science Mission Directorate of the National Aeronautics and Space Administration.