December 19, 2012 the Sutter's Mill Meteorite Fall In
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Handbook of Iron Meteorites, Volume 3
Sierra Blanca - Sierra Gorda 1119 ing that created an incipient recrystallization and a few COLLECTIONS other anomalous features in Sierra Blanca. Washington (17 .3 kg), Ferry Building, San Francisco (about 7 kg), Chicago (550 g), New York (315 g), Ann Arbor (165 g). The original mass evidently weighed at least Sierra Gorda, Antofagasta, Chile 26 kg. 22°54's, 69°21 'w Hexahedrite, H. Single crystal larger than 14 em. Decorated Neu DESCRIPTION mann bands. HV 205± 15. According to Roy S. Clarke (personal communication) Group IIA . 5.48% Ni, 0.5 3% Co, 0.23% P, 61 ppm Ga, 170 ppm Ge, the main mass now weighs 16.3 kg and measures 22 x 15 x 43 ppm Ir. 13 em. A large end piece of 7 kg and several slices have been removed, leaving a cut surface of 17 x 10 em. The mass has HISTORY a relatively smooth domed surface (22 x 15 em) overlying a A mass was found at the coordinates given above, on concave surface with irregular depressions, from a few em the railway between Calama and Antofagasta, close to to 8 em in length. There is a series of what appears to be Sierra Gorda, the location of a silver mine (E.P. Henderson chisel marks around the center of the domed surface over 1939; as quoted by Hey 1966: 448). Henderson (1941a) an area of 6 x 7 em. Other small areas on the edges of the gave slightly different coordinates and an analysis; but since specimen could also be the result of hammering; but the he assumed Sierra Gorda to be just another of the North damage is only superficial, and artificial reheating has not Chilean hexahedrites, no further description was given. -
NASA Ames Jim Arnold, Craig Burkhardt Et Al
The re-entry of artificial meteoroid WT1190F AIAA SciTech 2016 1/5/2016 2008 TC3 Impact October 7, 2008 Mohammad Odeh International Astronomical Center, Abu Dhabi Peter Jenniskens SETI Institute Asteroid Threat Assessment Project (ATAP) - NASA Ames Jim Arnold, Craig Burkhardt et al. Michael Aftosmis - NASA Ames 2 Darrel Robertson - NASA Ames Next TC3 Consortium http://impact.seti.org Mission Statement: Steve Larson (Catalina Sky Survey) “Be prepared for the next 2008 TC3 John Tonry (ATLAS) impact” José Luis Galache (Minor Planet Center) Focus on two aspects: Steve Chesley (NASA JPL) 1. Airborne observations of the reentry Alan Fitzsimmons (Queen’s Univ. Belfast) 2. Rapid recovery of meteorites Eileen Ryan (Magdalena Ridge Obs.) Franck Marchis (SETI Institute) Ron Dantowitz (Clay Center Observatory) Jay Grinstead (NASA Ames Res. Cent.) Peter Jenniskens (SETI Institute - POC) You? 5 NASA/JPL “Sentry” early alert October 3, 2015: WT1190F Davide Farnocchia (NASA/JPL) Catalina Sky Survey: Richard Kowalski Steve Chesley (NASA/JPL) Marco Michelli (ESA NEOO CC) 6 WT1190F Found: October 3, 2015: one more passage Oct. 24 Traced back to: 2013, 2012, 2011, …, 2009 Re-entry: Friday November 13, 2015 10.61 km/s 20.6º angle Bill Gray 11 IAC + UAE Space Agency chartered commercial G450 Mohammad Odeh (IAC, Abu Dhabi) Support: UAE Space Agency Dexter Southfield /Embry-Riddle AU 14 ESA/University Stuttgart 15 SETI Institute 16 Dexter Southfield team Time UAE Camera Trans-Lunar Insertion Stage Leading candidate (1/13/2016): LUNAR PROSPECTOR T.L.I.S. Launch: January 7, 1998 UT Lunar Prospector itself was deliberately crashed on Moon July 31, 1999 Carbon fiber composite Spin hull thrusters Titanium case holds Amonium Thiokol Perchlorate fuel and Star Stage 3700S HTPB binder (both contain H) P.I.: Alan Binder Scott Hubbard 57-minutes later: Mission Director Separation of TLIS NASA Ames http://impact.seti.org 30 . -
Tree-Ring Dating of Meteorite Fall in Sikhote-Alin, Eastern Siberia – Russia
International Journal of Astrobiology, Page 1 of 6 1 doi:10.1017/S1473550411000309 © Cambridge University Press 2011 Tree-ring dating of meteorite fall in Sikhote-Alin, Eastern Siberia – Russia R. Fantucci1, Mario Di Martino2 and Romano Serra3 1Geologi Associati Fantucci e Stocchi, 01027 Montefiascone (VT), Italy e-mail: [email protected] 2INAF-Osservatorio Astronomico di Torino, 10025 Pino Torinese, Italy 3Dipartimento di Fisica, Università di Bologna, via Irnerio 46, 40126 Bologna, Italy Abstract: This research deals with the fall of the Sikhote-Alin iron meteorite on the morning of 12 February 1947, at about 00:38 h Utrecht, in a remote area in the territory of Primorsky Krai in Eastern Siberia (46°09′ 36″N, 134°39′22″E). The area engulfed by the meteoritic fall was around 48 km2, with an elliptic form and thousands of craters. Around the large craters the trees were torn out by the roots and laid radially to the craters at a distance of 10–20 m; the more distant trees had broken tops. This research investigated through dendrocronology n.6 Scots pine trees (Pinus Sibirica) close to one of the main impact craters. The analysis of growth anomalies has shown a sudden decrease since 1947 for 4–8 years after the meteoritic impact. Tree growth stress, detected in 1947, was analysed in detail through wood microsection that confirmed the winter season (rest vegetative period) of the event. The growth stress is mainly due to the lost crown (needle lost) and it did not seem to be caused due to direct damages on trunk and branches (missing of resin ducts). -
Radar-Enabled Recovery of the Sutter's Mill Meteorite, A
RESEARCH ARTICLES the area (2). One meteorite fell at Sutter’sMill (SM), the gold discovery site that initiated the California Gold Rush. Two months after the fall, Radar-Enabled Recovery of the Sutter’s SM find numbers were assigned to the 77 me- teorites listed in table S3 (3), with a total mass of 943 g. The biggest meteorite is 205 g. Mill Meteorite, a Carbonaceous This is a tiny fraction of the pre-atmospheric mass, based on the kinetic energy derived from Chondrite Regolith Breccia infrasound records. Eyewitnesses reported hearing aloudboomfollowedbyadeeprumble.Infra- Peter Jenniskens,1,2* Marc D. Fries,3 Qing-Zhu Yin,4 Michael Zolensky,5 Alexander N. Krot,6 sound signals (table S2A) at stations I57US and 2 2 7 8 8,9 Scott A. Sandford, Derek Sears, Robert Beauford, Denton S. Ebel, Jon M. Friedrich, I56US of the International Monitoring System 6 4 4 10 Kazuhide Nagashima, Josh Wimpenny, Akane Yamakawa, Kunihiko Nishiizumi, (4), located ~770 and ~1080 km from the source, 11 12 10 13 Yasunori Hamajima, Marc W. Caffee, Kees C. Welten, Matthias Laubenstein, are consistent with stratospherically ducted ar- 14,15 14 14,15 16 Andrew M. Davis, Steven B. Simon, Philipp R. Heck, Edward D. Young, rivals (5). The combined average periods of all 17 18 18 19 20 Issaku E. Kohl, Mark H. Thiemens, Morgan H. Nunn, Takashi Mikouchi, Kenji Hagiya, phase-aligned stacked waveforms at each station 21 22 22 22 23 Kazumasa Ohsumi, Thomas A. Cahill, Jonathan A. Lawton, David Barnes, Andrew Steele, of 7.6 s correspond to a mean source energy of 24 4 24 2 25 Pierre Rochette, Kenneth L. -
Characteristics of a Bright Fireball and Meteorite Fall at Buzzard Coulee, Saskatchewan, Canada, November 20, 2008
40th Lunar and Planetary Science Conference (2009) 2505.pdf CHARACTERISTICS OF A BRIGHT FIREBALL AND METEORITE FALL AT BUZZARD COULEE, SASKATCHEWAN, CANADA, NOVEMBER 20, 2008. A. R. Hildebrand1, E. P. Milley1 , P. G. Brown2, P. J. A. McCausland2, W. Edwards2, M. Beech3, A. Ling4, G. Sarty5, M. D. Paulson4, L. A. Maillet1, S. F. Jones1 and M. R. Stauffer5. 1Department of Geoscience, 2500 University Drive NW, University of Calgary, Calgary, AB T2N 1N4 ([email protected], [email protected]), 2Department of Physics and Astronomy, The University of Western Ontario, London, ON, N6A 3K7, 3Department of Physics, Campion College at the University of Regina, Regina, SK S4S 0A2, 4Edmonton Centre, Royal Astronomical Society of Canada, 5Departments of Physics and En- gineering Physics and Department of Geological Sciences, University of Saskatchewan, Saskatoon, SK S7N 5E2. Introduction: A bright fireball was widely ob- tion surfaces (angular shapes with numerous small served across Alberta, Saskatchewan and Manitoba piezoglypts) presumably reflecting the meteoroids’ during late twilight on November 20, 2008. Interviews significant fragmentation extending deep into the at- of eyewitnesses and crude calibrations of security cam- mosphere; a larger proportion of mature ablation sur- eras constrained the fall region and the first search faces and oriented individuals may occur up range in attempt recovered meteorites off the ice of a manmade the strewn field. Fusion crusts are a typical dark gray pond in Buzzard Coulee, SK, Nov. 27, 2008. for an ordinary chondrite fall with more vitreous crusts Trajectory and Pre-fall Orbit: The fireball and on the back of some oriented specimens. The fall is subsequent dust trail, or shadows cast by the fireball, also distinguished by the large proportion of meteor- were widely recorded by all-sky (4) and security video ites that exhibit freshly broken surfaces with no fusion cameras (at least 19) establishing that its brightest por- crust; broken surfaces with variable amounts of “paint- tion occurred from 17:26:40 to 17:26:45 MST. -
Chelyabinsk Airburst, Damage Assessment, Meteorite Recovery and Characterization
O. P. Popova, et al., Chelyabinsk Airburst, Damage Assessment, Meteorite Recovery and Characterization. Science 342 (2013). Chelyabinsk Airburst, Damage Assessment, Meteorite Recovery, and Characterization Olga P. Popova1, Peter Jenniskens2,3,*, Vacheslav Emel'yanenko4, Anna Kartashova4, Eugeny Biryukov5, Sergey Khaibrakhmanov6, Valery Shuvalov1, Yurij Rybnov1, Alexandr Dudorov6, Victor I. Grokhovsky7, Dmitry D. Badyukov8, Qing-Zhu Yin9, Peter S. Gural2, Jim Albers2, Mikael Granvik10, Läslo G. Evers11,12, Jacob Kuiper11, Vladimir Kharlamov1, Andrey Solovyov13, Yuri S. Rusakov14, Stanislav Korotkiy15, Ilya Serdyuk16, Alexander V. Korochantsev8, Michail Yu. Larionov7, Dmitry Glazachev1, Alexander E. Mayer6, Galen Gisler17, Sergei V. Gladkovsky18, Josh Wimpenny9, Matthew E. Sanborn9, Akane Yamakawa9, Kenneth L. Verosub9, Douglas J. Rowland19, Sarah Roeske9, Nicholas W. Botto9, Jon M. Friedrich20,21, Michael E. Zolensky22, Loan Le23,22, Daniel Ross23,22, Karen Ziegler24, Tomoki Nakamura25, Insu Ahn25, Jong Ik Lee26, Qin Zhou27, 28, Xian-Hua Li28, Qiu-Li Li28, Yu Liu28, Guo-Qiang Tang28, Takahiro Hiroi29, Derek Sears3, Ilya A. Weinstein7, Alexander S. Vokhmintsev7, Alexei V. Ishchenko7, Phillipe Schmitt-Kopplin30,31, Norbert Hertkorn30, Keisuke Nagao32, Makiko K. Haba32, Mutsumi Komatsu33, and Takashi Mikouchi34 (The Chelyabinsk Airburst Consortium). 1Institute for Dynamics of Geospheres of the Russian Academy of Sciences, Leninsky Prospect 38, Building 1, Moscow, 119334, Russia. 2SETI Institute, 189 Bernardo Avenue, Mountain View, CA 94043, USA. 3NASA Ames Research Center, Moffett Field, Mail Stop 245-1, CA 94035, USA. 4Institute of Astronomy of the Russian Academy of Sciences, Pyatnitskaya 48, Moscow, 119017, Russia. 5Department of Theoretical Mechanics, South Ural State University, Lenin Avenue 76, Chelyabinsk, 454080, Russia. 6Chelyabinsk State University, Bratyev Kashirinyh Street 129, Chelyabinsk, 454001, Russia. -
ELEMENTAL ABUNDANCES in the SILICATE PHASE of PALLASITIC METEORITES Redacted for Privacy Abstract Approved: Roman A
AN ABSTRACT OF THE THESIS OF THURMAN DALE COOPER for theMASTER OF SCIENCE (Name) (Degree) in CHEMISTRY presented on June 1, 1973 (Major) (Date) Title: ELEMENTAL ABUNDANCES IN THE SILICATE PHASE OF PALLASITIC METEORITES Redacted for privacy Abstract approved: Roman A. Schmitt The silicate phases of 11 pallasites were analyzed instrumen- tally to determine the concentrations of some major, minor, and trace elements.The silicate phases were found to contain about 98% olivine with 1 to 2% accessory minerals such as lawrencite, schreibersite, troilite, chromite, and farringtonite present.The trace element concentrations, except Sc and Mn, were found to be extremely low and were found primarily in the accessory phases rather than in the pure olivine.An unusual bimodal Mn distribution was noted in the pallasites, and Eagle Station had a chondritic nor- malized REE pattern enrichedin the heavy REE. The silicate phases of pallasites and mesosiderites were shown to be sufficiently diverse in origin such that separate classifications are entirely justified. APPROVED: Redacted for privacy Professor of Chemistry in charge of major Redacted for privacy Chairman of Department of Chemistry Redacted for privacy Dean of Graduate School Date thesis is presented June 1,1973 Typed by Opal Grossnicklaus for Thurman Dale Cooper Elemental Abundances in the Silicate Phase of Pallasitic Meteorites by Thurman Dale Cooper A THESIS submitted to Oregon State University in partial fulfillment of the requirements for the degree of Master of Science June 1974 ACKNOWLEDGMENTS The author wishes to express his gratitude to Prof. Roman A. Schmitt for his guidance, suggestions, discussions, and thoughtful- ness which have served as an inspiration. -
Numerical Modeling of the 2013 Meteorite Entry in Lake Chebarkul, Russia
Nat. Hazards Earth Syst. Sci., 17, 671–683, 2017 www.nat-hazards-earth-syst-sci.net/17/671/2017/ doi:10.5194/nhess-17-671-2017 © Author(s) 2017. CC Attribution 3.0 License. Numerical modeling of the 2013 meteorite entry in Lake Chebarkul, Russia Andrey Kozelkov1,2, Andrey Kurkin2, Efim Pelinovsky2,3, Vadim Kurulin1, and Elena Tyatyushkina1 1Russian Federal Nuclear Center, All-Russian Research Institute of Experimental Physics, Sarov, 607189, Russia 2Nizhny Novgorod State Technical University n. a. R. E. Alekseev, Nizhny Novgorod, 603950, Russia 3Institute of Applied Physics, Nizhny Novgorod, 603950, Russia Correspondence to: Andrey Kurkin ([email protected]) Received: 4 November 2016 – Discussion started: 4 January 2017 Revised: 1 April 2017 – Accepted: 13 April 2017 – Published: 11 May 2017 Abstract. The results of the numerical simulation of possi- Emel’yanenko et al., 2013; Popova et al., 2013; Berngardt et ble hydrodynamic perturbations in Lake Chebarkul (Russia) al., 2013; Gokhberg et al., 2013; Krasnov et al., 2014; Se- as a consequence of the meteorite fall of 2013 (15 Febru- leznev et al., 2013; De Groot-Hedlin and Hedlin, 2014): ary) are presented. The numerical modeling is based on the – the meteorite with a diameter of 16–19 m flew into the Navier–Stokes equations for a two-phase fluid. The results of ◦ the simulation of a meteorite entering the water at an angle earth’s atmosphere at about 20 to the horizon at a ve- ∼ −1 of 20◦ are given. Numerical experiments are carried out both locity of 17–22 km s . when the lake is covered with ice and when it is not. -
The Chelyabinsk Meteorite Fall on February 15, 2013 Attracted Much
46th Lunar and Planetary Science Conference (2015) 2686.pdf MINERALOGY, PETROLOGY, CHRONOLOGY, AND EXPOSURE HISTORY OF THE CHELYABINSK METEORITE AND PARENT BODY. K. Righter1, P. Abell1, D. Agresti2, E. L. Berger3, A.S. Burton1, J.S. Delaney4, M.D. Fries1, E.K. Gibson1, R. Harrington5, G. F. Herzog4, L.P. Keller1, D. Locke6, F. Lindsay4, T.J. McCoy7, R.V. Morris1, K. Nagao8, K. Nakamura-Messenger1, P.B. Niles1, L. Nyquist1, J. Park4, Z.X. Peng9, C.- Y.Shih10, J.I. Simon1, C.C. Swisher, III4, M. Tappa11, and B. Turrin4. 1NASA-JSC, Houston, TX 77058; 2Department of Physics, University of Alabama at Birmingham, Birmingham, AL 35294-1170; 3GeoControl Systems Inc.– Jacobs JETS contract – NASA JSC; 4Rutgers Univ., Wright Labs-Chemistry Dept., Piscataway, NJ; 5UTAS – Jacobs JETS Contract, NASA-JSC; 6HX5 – Jacobs JETS Contract, NASA-JSC; 7Smithsonian Institution, PO Box 37012, MRC 119, Washington, DC; 8Laboratory for Earthquake Chemistry, University of Tokyo, Hongo, Bunkyo- ku, Tokyo 113-0033, Japan; 9Barrios Tech – Jacobs JETS Contract, NASA-JSC; 10Jacobs JETS Contract, NASA- JSC; 11Aerodyne Industries – Jacobs JETS Contract, NASA-JSC. Introduction: The Chelyabinsk meteorite fall in impact melt veins (Figure 2), as compared to on February 15, 2013 attracted much more atten- results of shock experiments [20]. tion worldwide than do most falls [1-3]. A con- Chronology: Portions of light and dark lithol- sortium led by JSC received 3 masses of Chelya- ogies from Chel-101, and the impact melt brecci- binsk (Chel-101, -102, -103) that were collected as (Chel-102 and Chel-103) were prepared and shortly after the fall and handled with care to analyzed for Rb-Sr, Sm-Nd, and Ar-Ar dating. -
Sikhote-Alin Meteorite, Elemental Composition Analysis Using CF LIBS
WDS'12 Proceedings of Contributed Papers, Part II, 123–127, 2012. ISBN 978-80-7378-225-2 © MATFYZPRESS Sikhote-Alin Meteorite, Elemental Composition Analysis Using CF LIBS J. Plavčan,1 M. Horňáčková,1 Z. Grolmusová,1,2 M. Kociánová,1 J. Rakovský,1 P. Veis1,2 1 Department of Experimental Physics, Faculty of Mathematics Physics and Informatics Comenius University, Mlynská dolina, 84248 Bratislava, Slovakia. 2 Laboratory of Isotope Geology, State Geological Institute of Dionyz Stur, Mlynská dolina 1, 817 04 Bratislava, Slovakia. Abstract. Calibration free laser induced breakdown spectroscopy (CF-LIBS) method was used for determination of elements presented in meteorite Sikhote Alin as well as its quantities. As a source of ablation, Q-switched Nd: YAG laser operating at 532 nm was used. Emission from plasma was collected by optical fiber that was connected with slit of Echelle spectrometer (ME 5000, Andor) coupled with iCCD camera (iSTAR DH734i-18F- 03, Andor). Optimal experimental conditions, i.e. time delay, gate width, energy per pulse were found. The measured spectra were recorded 2.5 μs after laser pulse and gate width of iCCD camera was set to 0.5 μs. Electron concentration was calculated from broadening of hydrogen Hα line (656 nm).A Saha-Boltzmann plot method was used for determination of electron temperature, assuming the local thermodynamic equilibrium. Apart from iron, which is the main elemental constituent of examined meteorite, elements like nickel, cobalt, phosphor, potassium, sodium, calcium and manganese, were also detected. In comparison with official Sikhote Alin elemental quantitative measurements, some elements like sodium, calcium, potassium and manganese were not mentioned, it is expected that these elements were added to the surface of meteorite after the meteorite fall. -
Team Studies Rare Meteorite Possibly from the Outer Asteroid Belt 20 December 2012
Team studies rare meteorite possibly from the outer asteroid belt 20 December 2012 The asteroid approached on an orbit that still points to the source region of CM chondrites. From photographs and video of the fireball, Jenniskens calculated that the asteroid approached on an unusual low-inclined almost comet-like orbit that reached the orbit of Mercury, passing closer to the sun than known from other recorded meteorite falls. "It circled the sun three times during a single orbit of Jupiter, in resonance with that planet," Jenniskens said. Based on the unusually short time that the asteroid was exposed to cosmic rays, there was not much time to go slower or faster around the sun. That puts the original source asteroid very (Phys.org)—Scientists found treasure when they close to this resonance, in a low inclined orbit. studied a meteorite that was recovered April 22, 2012 at Sutter's Mill, the gold discovery site that "A good candidate source region for CM chondrites led to the 1849 California Gold Rush. Detection of now is the Eulalia asteroid family, recently the falling meteorites by Doppler weather radar proposed as a source of primitive C-class asteroids allowed for rapid recovery so that scientists could in orbits that pass Earth," adds Jenniskens. study for the first time a primitive meteorite with little exposure to the elements, providing the most pristine look yet at the surface of primitive asteroids. An international team of 70 researchers reported in today's issue of Science that this meteorite was classified as a Carbonaceous-Mighei or CM-type carbonaceous chondrite and that they were able to identify for the first time the source region of these meteorites. -
Career Pages of Astronomer Dr. Peter Jenniskens Peter Jenniskens, Ph.D
10/8/2014 Career pages of astronomer Dr. Peter Jenniskens Peter Jenniskens, Ph.D. Meteor astronomer Carl Sagan Center, The SETI Institute. E-mail: Petrus.M.Jenniskens [at] nasa.gov, Tel: 1 (650) 810 0216; Fax: 1 (650) 962 9419 Last update: December 08, 2008; List of Publications Curriculum vitae Astronomer Dr. Peter Jenniskens [Portrait (3.2 Mbyte)] is a Research Scientist with the Carl Sagan Center at the SETI Institute and works on mission projects at NASA/Ames Research Center in Moffett Field, California, and on research topics that relate to interstellar and interplanetary matter. Research Interests: Meteor showers - Jenniskens is an expert on meteor showers, and is known for identifying the parent body of the Quadrantid shower: a minor planet called 2003 EH1. Main belt asteroid 1999 TY224 was named (42981) "Jenniskens". He is the Principal Investigator of ASIMA - the Asteroid Impact Analyzer, a proposed satellite mission (2014-2016) to measure the carbon content of meteors from space and study the diversity of comets and asteroids. He predicted the return of the unusual Aurigid shower from dust ejected around 4 AD by long-period comet Kiess on September 1, 2007, and was the Principal Investigator of the Aurigid Multi-Instrument Aircraft Campaign (Aurigid MAC), an airborne mission that deployed from NASA Ames to study this meteor outburst. This was followed by a study of dust ejected by comet 8P/Tuttle (Ursid MAC) in December 2007, and a mission in January 2008 to study the Quadrantid meteor shower for clues to its date of origin (Quadrantid MAC). Before that, Jenniskens was the Principal Investigator of NASA's first Astrobiology mission, Leonid MAC, an airborne campaign to explore the 1998 - 2002 Leonid storms and study meteoroids and their paths from extra-terrestrial to terrestrial matter.