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Cross-References ASTEROID IMPACT Definition and Introduction History of Impact Cratering Studies
18 ASTEROID IMPACT Tedesco, E. F., Noah, P. V., Noah, M., and Price, S. D., 2002. The identification and confirmation of impact structures on supplemental IRAS minor planet survey. The Astronomical Earth were developed: (a) crater morphology, (b) geo- 123 – Journal, , 1056 1085. physical anomalies, (c) evidence for shock metamor- Tholen, D. J., and Barucci, M. A., 1989. Asteroid taxonomy. In Binzel, R. P., Gehrels, T., and Matthews, M. S. (eds.), phism, and (d) the presence of meteorites or geochemical Asteroids II. Tucson: University of Arizona Press, pp. 298–315. evidence for traces of the meteoritic projectile – of which Yeomans, D., and Baalke, R., 2009. Near Earth Object Program. only (c) and (d) can provide confirming evidence. Remote Available from World Wide Web: http://neo.jpl.nasa.gov/ sensing, including morphological observations, as well programs. as geophysical studies, cannot provide confirming evi- dence – which requires the study of actual rock samples. Cross-references Impacts influenced the geological and biological evolu- tion of our own planet; the best known example is the link Albedo between the 200-km-diameter Chicxulub impact structure Asteroid Impact Asteroid Impact Mitigation in Mexico and the Cretaceous-Tertiary boundary. Under- Asteroid Impact Prediction standing impact structures, their formation processes, Torino Scale and their consequences should be of interest not only to Earth and planetary scientists, but also to society in general. ASTEROID IMPACT History of impact cratering studies In the geological sciences, it has only recently been recog- Christian Koeberl nized how important the process of impact cratering is on Natural History Museum, Vienna, Austria a planetary scale. -
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. -
Detecting and Avoiding Killer Asteroids
Target Earth! Detecting and Avoiding Killer Asteroids by Trudy E. Bell (Copyright 2013 Trudy E. Bell) ARTH HAD NO warning. When a mountain- above 2000°C and triggering earthquakes and volcanoes sized asteroid struck at tens of kilometers (miles) around the globe. per second, supersonic shock waves radiated Ocean water suctioned from the shoreline and geysered outward through the planet, shock-heating rocks kilometers up into the air; relentless tsunamis surged e inland. At ground zero, nearly half the asteroid’s kinetic energy instantly turned to heat, vaporizing the projectile and forming a mammoth impact crater within minutes. It also vaporized vast volumes of Earth’s sedimentary rocks, releasing huge amounts of carbon dioxide and sulfur di- oxide into the atmosphere, along with heavy dust from both celestial and terrestrial rock. High-altitude At least 300,000 asteroids larger than 30 meters revolve around the sun in orbits that cross Earth’s. Most are not yet discovered. One may have Earth’s name written on it. What are engineers doing to guard our planet from destruction? winds swiftly spread dust and gases worldwide, blackening skies from equator to poles. For months, profound darkness blanketed the planet and global temperatures dropped, followed by intense warming and torrents of acid rain. From single-celled ocean plank- ton to the land’s grandest trees, pho- tosynthesizing plants died. Herbivores starved to death, as did the carnivores that fed upon them. Within about three years—the time it took for the mingled rock dust from asteroid and Earth to fall out of the atmosphere onto the ground—70 percent of species and entire genera on Earth perished forever in a worldwide mass extinction. -
Terrestrial Impact Structures Provide the Only Ground Truth Against Which Computational and Experimental Results Can Be Com Pared
Ann. Rev. Earth Planet. Sci. 1987. 15:245-70 Copyright([;; /987 by Annual Reviews Inc. All rights reserved TERRESTRIAL IMI!ACT STRUCTURES ··- Richard A. F. Grieve Geophysics Division, Geological Survey of Canada, Ottawa, Ontario KIA OY3, Canada INTRODUCTION Impact structures are the dominant landform on planets that have retained portions of their earliest crust. The present surface of the Earth, however, has comparatively few recognized impact structures. This is due to its relative youthfulness and the dynamic nature of the terrestrial geosphere, both of which serve to obscure and remove the impact record. Although not generally viewed as an important terrestrial (as opposed to planetary) geologic process, the role of impact in Earth evolution is now receiving mounting consideration. For example, large-scale impact events may hav~~ been responsible for such phenomena as the formation of the Earth's moon and certain mass extinctions in the biologic record. The importance of the terrestrial impact record is greater than the relatively small number of known structures would indicate. Impact is a highly transient, high-energy event. It is inherently difficult to study through experimentation because of the problem of scale. In addition, sophisticated finite-element code calculations of impact cratering are gen erally limited to relatively early-time phenomena as a result of high com putational costs. Terrestrial impact structures provide the only ground truth against which computational and experimental results can be com pared. These structures provide information on aspects of the third dimen sion, the pre- and postimpact distribution of target lithologies, and the nature of the lithologic and mineralogic changes produced by the passage of a shock wave. -
A Possible Albian Impact Crater at Murshid, Southern Oman
GeoArabia, Vol. 7, No. 4, 2002 Gulf PetroLink, Bahrain A possible Albian impact crater at Murshid, southern Oman Bruce Levell1, Pascal Richard2 and Folco Hoogendijk2, Petroleum Development Oman ABSTRACT During interpretation of a 3-D seismic survey in southern Oman a solitary, 2.5-km-wide circular basin with a central peak and raised rim was identified in the subsurface 35 km west of the Marmul oil field. The feature is the only one of its kind in the area. The basinal structure is probably of Late Cretaceous (Albian) age and the regional geology strongly suggests that it is neither a volcanic crater nor related to salt-dome tectonics or salt dissolution. It possibly represents a crater formed by a terrestrial impact event and has been named the Murshid crater. This report does not constitute a detailed investigation of the possible impact crater but rather records the 3-D seismic observations and the drilling that has taken place near the structure so far. INTRODUCTION During interpretation of a newly acquired 3-D seismic survey for oil exploration in southern Oman, a solitary 2.5-km-diameter circular basinal feature was identified as a possible impact structure and was named the Murshid crater. It lies 35 km west of the Marmul oil field in the South Oman Salt Basin (Figure 1). The center of the structure is at latitude 18º10’59"N, longitude 54º55’08”E, and it is buried at a depth of approximately 380 m below mean sea level (680 m below the ground surface). The authors are petroleum geologists who felt that the Murshid basinal structure needed reporting to the wider scientific community. -
Destination Moon
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Magnetic Properties and Redox State of Impact Glasses: a Review and New Case Studies from Siberia
geosciences Review Magnetic Properties and Redox State of Impact Glasses: A Review and New Case Studies from Siberia Pierre Rochette 1,* , Natalia S. Bezaeva 2,3, Andrei Kosterov 4 ,Jérôme Gattacceca 1, Victor L. Masaitis 5, Dmitry D. Badyukov 6, Gabriele Giuli 7 , Giovani Orazio Lepore 8 and Pierre Beck 9 1 Aix Marseille Université, CNRS, IRD, Coll. France, INRA, CEREGE, 13545 Aix-en-Provence, France; [email protected] 2 Institute of Geology and Petroleum Technologies, Kazan Federal University, 4/5 Kremlyovskaya Str., 420008 Kazan, Russia; [email protected] 3 Institute of Physics and Technology, Ural Federal University, 19 Mira Str., 620002 Ekaterinburg, Russia 4 St. Petersburg State University, 199034 St. Petersburg, Russia; [email protected] 5 A.P. Karpinsky Russian Geological Research Institute (VSEGEI), Sredny prospect 74, 199106 St. Petersburg, Russia; [email protected] 6 V.I. Vernadsky Institute of Geochemistry and Analytical Chemistry, Russian Academy of Sciences, 19 Kosygin str., 119991 Moscow, Russia; [email protected] 7 School of Science and Technology-Geology division, University of Camerino, Via Gentile III da Varano, 62032 Camerino (MC), Italy; [email protected] 8 CNR-IOM-OGG c/o ESRF, 71 Avenue des Martyrs CS 40220, F-38043 Grenoble, France; [email protected] 9 Université Grenoble Alpes, CNRS, IPAG, UMR5274, 38041 Grenoble, France; [email protected] * Correspondence: [email protected]; Tel.: +33-442971562 Received: 26 February 2019; Accepted: 11 May 2019; Published: 15 May 2019 Abstract: High velocity impacts produce melts that solidify as ejected or in-situ glasses. We provide a review of their peculiar magnetic properties, as well as a new detailed study of four glasses from Siberia: El’gygytgyn, Popigai, urengoites, and South-Ural glass (on a total of 24 different craters or strewn-fields). -
Chapter 5: Shock Metamorphism and Impact Melting
5. Shock Metamorphism and Impact Melting ❖❖❖ Shock-metamorphic products have become one of the diagnostic tools of impact cratering studies. They have become the main criteria used to identify structures of impact origin. They have also been used to map the distribution of shock-pressures throughout an impact target. The diverse styles of shock metamorphism include fracturing of crystals, formation of microcrystalline planes of glass through crystals, conversion of crystals to high-pressure polymorphs, conversion of crystals to glass without loss of textural integrity, conversion of crystals to melts that may or may not mix with melts from other crystals. Shock-metamorphism of target lithologies at the crater was first described by Barringer (1905, 1910) and Tilghman (1905), who recognized three different products. The first altered material they identified is rock flour, which they concluded was pulverized Coconino sandstone. Barringer observed that rock flour was composed of fragmented quartz crystals that were far smaller in size than the unaffected quartz grains in normal Coconino sandstone. Most of the pulverized silica he examined passed through a 200 mesh screen, indicating grain sizes <74 µm (0.074 mm), which is far smaller than the 0.2 mm average detrital grain size in normal Coconino (Table 2.1). Fairchild (1907) and Merrill (1908) also report a dramatic comminution of Coconino, although only 50% of Fairchild’s sample of rock flour passed through a 100 mesh screen, indicating grain sizes <149 µm. Heterogeneity of the rock flour is evident in areas where sandstone clasts survive within the rock flour. The rock flour is pervasive and a major component of the debris at the crater. -
The 3D.Y Knom Example Is /1"<
t Sixth International Congress on Glass - Washington, D. C., 1962. Fossil Glasses Produced by Inpact of Meteorites, Asteroids 2nd Possibly Comets with the Planet Xarth* A. J. Zzhen :&uon Insticute, Pittsburgh, ?ennsylvania (U. S. A. ) Sunnary / (to be trmslzted izto Frerzh and German) - i in recent thes one of the nost intriging aysteries of geGlogy has ceen the occurrence of aerodgnasicdly-shaped glasses on five continents of the earth. Tnese glasses mder discussion are obviously not of f-d- guritic origin. 3ecent research indicates that these glasses laom as tektites are the result of meteorite, esteroid, or sossibly comet hpact. Lqact glass?s, io generzl, differ Tram volcanic glasses in that they are lo;;.tr in ?,iater zontent, have laver gallium and germiun ccntents, and are rot necessarily ia mgnaticalljr unstable continental areas. These hpac- tites may be divided as follovs: (1)Glasses found in or near terrestrial neteorite craters. These glasses usually contain numerous s-,'nerules 02 nickel-iron, coesite, chunlks of partially melted meteoritic inatter and even stishovite. Shattered or fractured melted mi-nerals such as quarts are comxonly gresent. Aerodpaaic-shaping nay or nay not be present in this t-ne. &m?les are Canyon Diablo and Wabar Crster glasses. (2) Impzct- glasses zssociated with craters uitn no evidence of meteoritic mterial i? the @.ass or surrounding the explosisn site. The 3d.y knom example is /1"< Tnis vork vas supported by Xatiocal A-eroEautizs and Space P.dministretioq,$ 3esezrch Grant NsG-37-6O Supplement 1-62. Page 2 glass associated with AoueUoul Crater in the Western Sahara Desert. -
EPSC2018-833, 2018 European Planetary Science Congress 2018 Eeuropeapn Planetarsy Science Ccongress C Author(S) 2018
EPSC Abstracts Vol. 12, EPSC2018-833, 2018 European Planetary Science Congress 2018 EEuropeaPn PlanetarSy Science CCongress c Author(s) 2018 Impact melt boulder from northern Sweden from an unknown source Timmu Kreitsmann (1), Satu Hietala (2), Tapio Soukka (3), Jüri Plado (1), Jari Nenonen (2) and Lauri J. Pesonen (4) (1) Department of Geology, University of Tartu, Estonia ([email protected], [email protected]), (2) Geological Survey of Finland, Finland ([email protected], [email protected]), (3) Oulu Mining School, University of Oulu, Finland ([email protected]) (4) Solid Earth Geophysics Laboratory, Physics Department, University of Helsinki, Finland ([email protected]) Abstract We report an impact melt rock finding from northern Sweden, near the village of Kitkiöjärvi. There is no confirmed meteorite impact structure nearby, thus, the source is currently undiscovered. The impact origin of the finding was confirmed by the presence of planar deformation features (PDFs) in quartz. 1. Introduction Impact cratering is a common and frequent process that affects the planetary surfaces across the solar system throughout geologic time. On Earth, there are 191 confirmed impact structures which are distributed unevenly around the globe. The Fennoscandian Shield houses around 10% of them. Here, we report an impact melt rock finding that originates from an unknown structure in northern Sweden. The semi-rounded impactite boulder, sized 10 × 7 cm, was found by Tapio Soukka in 2017 from a gravel pit at the western side of village Kitkiöjärvi (67°46'16"N 23°03'06"E; Fig. 1). Figure 1: Proven impact structures in Fennoscandia. -
A Tomography Approach to Investigate Impactite Structure
3rd International Conference on Tomography of Materials and Structures Lund, Sweden, 26-30 June 2017, ICTMS2017-110 A TOMOGRAPHY APPROACH TO INVESTIGATE IMPACTITE STRUCTURE A. Fedrigo*1,2, K. Marstal1,3, A. Bjorholm Dahl1, M. Lyksborg1, C. Gundlach1, M. Strobl2 & C. Bender Koch4 1Danish Technical University, Denmark 2European Spallation Source ESS ERIC, Sweden 3ERASMUS MC, Netherland 4Copenhagen University, Denmark Keywords: Neutron imaging, image registration, bimodal imaging, computed tomography. Summary: We investigate the structure of impactites from the Wabar iron meteorite impact site in Saudi Arabia. In order to understand the physical and chemical processes involved in the formation of the impactite, we applied a non-destructive investigation approach, which combines X-ray and neutron tomography. This bi-modal imaging method allowed for a better understanding of the impactite’s chemical composition. 1. INTRODUCTION Meteorite impacts have recently been recognised among the most important processes able to modify planetary surfaces. It also happens to be one of the least understood in details. In particular it is a challenge to understand both the extent of impacts and the physical and chemical changes that occur during and following the impact, where materials (e.g., rocks, sand, meteorite fragments, etc.) are subjected to temperatures of several thousands degrees and pressures of several GPa. In addition, most accessible Earth impact areas are highly affected by weathering, which causes extensive secondary chemical alterations. Iron meteorites impact on planetary surfaces cause shock-induced rock deformations that happens both at macroscopic and at microscopic level, e.g. shatter cones (macroscopic) and planar deformation features in quartz (microscopic). Another indicator often correlated to meteoritic impacts is the presence of iridium concentration anomalies [1, 2].