Workshop on Meteorites from Cold and Hot Deserts
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Meteorite in Den Polargebiefen
Literatur: chemische Untersuchungen in den Alpen. Zb1. 1) Gor h a m , E.: The salt content of some Ice Aerosolforsch. 10, 1962, 97-105. samples from Nordaustlandet, Svalbord, :r. of 6) Tarn a n n , G.: Die Bildung des Gletscher Glaciology, 3, 1957, 181-186. korns, Naturwiss. 17, 1929, 851-854. 2) Gor h a m , E.: Soluble salts in a temperate 7) Renaud, A.: A contribution to the study of glacier Tellus, 10, 1958, 496-497. the glacter-graln. J. of Glaciology, 1, 1949, 3) Renaud, A.: Nouvelle contribution ä l' Hude 328-324. du grain de glacier. IUGG-Konferenzbericht, 8) R e v eIl e, R. und S u e s S, H.: Carbon dio Brüssel 1951, 206-211. xide exehange between atmosphere and ocean 4) Junge, C. E.: Sulfur in the atmosphere. :r of and the question of anincrease of atmospheric Geophys. Res .. 65, 1960, 227-237. CO. during the past decades Tellus, 9, 1957, 5) G e 0 r g 11, H. W. und Web er, E.: Luft- 18-27. Meteorite in den Polargebiefen Von Werner Sandner, Grafing-Bahnhof '}) Gegenüber den Vertretern aller anderen tische Gebiet zu zählen sind und wieviele naturwissenschaftlichen Disziplinen ist der Fundorte bereits südlich desselben liegen. Astronom insofern benachteiligt, als er die Was die benutzten literarischen Unterlagen Objekte seines Forschens nicht im Labora betrifft, so reicht der Katalog von Leonard torium einer Untersuchung unterwerfen, bis zum Jahre 1955, während das Werk von nicht mit ihnen "experimentieren" kann. Er Krinow alle Fälle und Funde bis 1956 ent ist vielmehr auf die Kunde angewiesen, die hält. -
Oettingen Munningen Megesheim Hainsfarth Ehingen Auhausen
VERWALTUNGSGEMEINSCHAFT OETTINGEN IN BAYERN OETTINGEN MUNNINGEN MEGESHEIM HAINSFARTH EHINGEN AUHAUSEN WWW.VG-OETTINGEN.DE Alles aus Edelstahl. Dekoratives und praktisches für Haus und Garten Skulpturen nach Wunsch Sonderanfertigungen Feuer, Grillen, Designerprodukte, Kreativprodukte Pflanzgefäße, Geschenke, Wasserläufe, Spiele, Wasserstationen GL-Design GmbH Kreatives aus Edelstahl Baumetswiese 6 – D-86732 Oettingen Tel. +49 (0)9082 9600-0 Fax +49 (0)9082 9600-15 [email protected] www.kreativesausedelstahl.de Geschäftsführer: Günter Lämmermeier WICHTIGE ARBEITGEBER GRUSSWORT KARL KOLB Liebe Mitbürgerinnen und Mitbürger, liebe Gäste, mit der vorliegenden Informationsbroschüre möchten wir, die Bürgermeister der VG-Gemeinden und die Mitarbeiterinnen und Mitarbeiter der Verwaltung, Ihnen „auf einen Blick“ alles Wissenswerte über die Verwaltungsgemein- schaft Oettingen i. Bay. an die Hand geben. In dieser Broschüre stellt sich unsere Verwaltungsgemeinschaft mit ihren sechs Mitgliedsgemeinden, der Stadt Oettingen i. Bay. sowie den Gemeinden Auhausen, Ehingen a. Ries, Hainsfarth, Megesheim und Munningen auf informative und unterhaltsame Art und Weise vor. Damit Sie sich als Einwohner oder Gast in unseren Gemeinden gut zurecht- finden, haben wir in dieser Broschüre alle grundlegenden Informationen zu Kindertagesstätten, Schulen, medizinischer Versorgung, Kirchen und sozialen Diensten sowie sämtliche Vereinsaktivitäten und kulturelle Events in abwechslungsreicher und illustrer Form zusammengestellt. Die Sammlung von Daten, Adressen -
Oettingen Munningen Megesheim Hainsfarth Ehingen Auhausen
verwaltungsgemeinschaft Oettingen in bayern OETTINGEN MUNNINGEN MEGESHEIM HAINSFARTH EHINGEN AUHAUSEN www.vg-oettingen.de VERWALTUNGSGEMEINSCHAFT Inhaltsverzeichnis OETTINGEN IN BAYERN Die Verwaltungsgemeinschaft 1 Schloßstraße 36 Stadt- und Gemeinderäte 2 86732 Oettingen i. Bay. Was erledige ich wo? 3 Telefon 09082 709-0 Ver- und Entsorgung 6 E-Mail [email protected] Abfallwirtschaft 6 Internet www.vg-oettingen.de Weitere wichtige Behörden und Institutionen 7 Kinderbetreuung und Bildungseinrichtungen 8 Kirchen und Pfarrämter 9 Soziales 9 Gesundheit 9 Vereine 11 Notruftafel 17 in Zusammenarbeit mit: 86732050 /7. Auflage / Dez. 2020 Stadt Oettingen i.Bay. Schloßstraße 36, 86732 Oettingen i.Bay Druck: mediaprint solutions GmbH Redaktion: Verantwortlich für den redaktionellen Teil: Stadt Oettingen i.Bay. und Papier: mediaprint infoverlag gmbh 135 g, weiß, matt, chlor- und säurefrei Herausgeber: Verantwortlich für den Anzeigenteil: mediaprint info verlag gmbh, Goran Petrasevic mediaprint infoverlag gmbh Lechstr. 2, 86415 Mering Angaben nach Art. 8 Abs. 3 BayPrG: Alleinige Gesellschafterin Registergericht Augsburg, HRB 27606 der mediaprint infoverlag gmbh ist die Media-Print Group GmbH, Paderborn IMPRESSUM USt-IdNr.: DE 118515205 Titel, Umschlaggestaltung sowie Art Geschäftsführung: und Anordnung des Inhalts sind zugunsten des Ulf Stornebel Quellennachweis für Fotos / Abbildungen: jeweiligen Inhabers dieser Rechte urheberrecht- Tel.: 08233 384-0 Gemeinden der Verwaltungsgemeinschaft Oettingen, lich geschützt. Nachdruck und Übersetzungen Fax: 08233 384-247 Werner Rensing, Bettina Schramm in Print und Online sind – auch auszugsweise [email protected] Weitere Bildquellen sind direkt am Bild vermerkt. – nicht gestattet. 2 Verwaltungsgemeinschaft Oettingen i. Bay. Karl Kolb Vorsitzender VG Oettingen i. Bay. Schloßstraße 36, 86732 Oettingen i. Bay. Telefon 09082 709-0 E-Mail [email protected] Internet www.vg-oettingen.de Thomas Heydecker Martin Weiß 1. -
Gemeinde Hainsfarth Übereignet, Im Sommer 2005 Zwei Die Kapelle Säumenden Winterlinden Aus Sicherheitsgründen Entfernt (Ehem
Historische Kulturlandschaft im Nördlinger Ries – Erhebungsbogen Kulturlandschaftselemente Objekt: Ackerterrassen N Hainsfarth Aufnahmedatum: 6.11.2006 Gemeinde: Hainsfarth Landkreis: DON Gemarkung: Hainsfarth Lage: N Hainsfarth am Kirchenberg oberhalb B 466 Koordinaten: R: 4399026 H: 5426293 Blattnummer TK 25: 7029 Elementtyp: Ackerterrassensystem Funktionsbereich: Landwirtschaft, Waldwirtschaft, Teichwirtschaft Form: flächenhaft Funktion: rezent Beschreibung: mind. 9 Stufen, schon 1830 Flurname „In den Zeilranken“ beschrieben unter Biotop-Nr. 7029-0065 (Hecken und Altgrasfluren auf dem Kirchberg nördlich Hainsfarth): mäßig steile W- und N-Seite des Kirchbergs terrassenartig gestuft, zwischen Äckern und Mähwiesen zahlreiche Hecken und einige Altgrasfluren, v.a. Schlehe, Altgrasfluren teils mit Fettarten (dann nicht aufgenommen), Brutplatz für Heckenbrüter Analyse: entstanden durch jahrhunderte lange Bewirtschaftung in hängiger Lage oder künstlich angelegt, durch Hecken Ranken befestigt Bedeutung: Notwendigkeit der Bewirtschaftung auch steilerer Hänge wegen geringer Erträge und zunehmender Bevölkerung Kulturlandschaftlicher Wert: hoch Erhaltungszustand: sehr gut, schon von weitem sichtbar, Flächen teils heute noch als Äcker genutzt Bild: Plan: Bisheriger Schutzstatus: Biotop (teilweise) Quellen: FIS-Natur Historische Kulturlandschaft im Nördlinger Ries – Erhebungsbogen Kulturlandschaftselemente Objekt: Allmende Steinhart Aufnahmedatum: 28.9.2006 Gemeinde: Hainsfarth Landkreis: DON Gemarkung: Steinhart Lage: um Steinhart Koordinaten: R: -
Disequilibrium Melting and Melt Migration Driven by Impacts: Implications for Rapid Planetesimal Core Formation
Available online at www.sciencedirect.com Geochimica et Cosmochimica Acta 100 (2013) 41–59 www.elsevier.com/locate/gca Disequilibrium melting and melt migration driven by impacts: Implications for rapid planetesimal core formation Andrew G. Tomkins ⇑, Roberto F. Weinberg, Bruce F. Schaefer 1, Andrew Langendam School of Geosciences, P.O. Box 28E, Monash University, Melbourne, Victoria 3800, Australia Received 20 January 2012; accepted in revised form 24 September 2012; available online 12 October 2012 Abstract The e182W ages of magmatic iron meteorites are largely within error of the oldest solar system particles, apparently requir- ing a mechanism for segregation of metals to the cores of planetesimals within 1.5 million years of initial condensation. Cur- rently favoured models involve equilibrium melting and gravitational segregation in a static, quiescent environment, which requires very high early heat production in small bodies via decay of short-lived radionuclides. However, the rapid accretion needed to do this implies a violent early accretionary history, raising the question of whether attainment of equilibrium is a valid assumption. Since our use of the Hf–W isotopic system is predicated on achievement of chemical equilibrium during core formation, our understanding of the timing of this key early solar system process is dependent on our knowledge of the seg- regation mechanism. Here, we investigate impact-related textures and microstructures in chondritic meteorites, and show that impact-generated deformation promoted separation of liquid FeNi into enlarged sulfide-depleted accumulations, and that this happened under conditions of thermochemical disequilibrium. These observations imply that similar enlarged metal accumu- lations developed as the earliest planetesimals grew by rapid collisional accretion. -
Meteorologia
MINISTÉRIO DA DEFESA COMANDO DA AERONÁUTICA METEOROLOGIA ICA 105-1 DIVULGAÇÃO DE INFORMAÇÕES METEOROLÓGICAS 2006 MINISTÉRIO DA DEFESA COMANDO DA AERONÁUTICA DEPARTAMENTO DE CONTROLE DO ESPAÇO AÉREO METEOROLOGIA ICA 105-1 DIVULGAÇÃO DE INFORMAÇÕES METEOROLÓGICAS 2006 MINISTÉRIO DA DEFESA COMANDO DA AERONÁUTICA DEPARTAMENTO DE CONTROLE DO ESPAÇO AÉREO PORTARIA DECEA N° 15/SDOP, DE 25 DE JULHO DE 2006. Aprova a reedição da Instrução sobre Divulgação de Informações Meteorológicas. O CHEFE DO SUBDEPARTAMENTO DE OPERAÇÕES DO DEPARTAMENTO DE CONTROLE DO ESPAÇO AÉREO, no uso das atribuições que lhe confere o Artigo 1°, inciso IV, da Portaria DECEA n°136-T/DGCEA, de 28 de novembro de 2005, RESOLVE: Art. 1o Aprovar a reedição da ICA 105-1 “Divulgação de Informações Meteorológicas”, que com esta baixa. Art. 2o Esta Instrução entra em vigor em 1º de setembro de 2006. Art. 3o Revoga-se a Portaria DECEA nº 131/SDOP, de 1º de julho de 2003, publicada no Boletim Interno do DECEA nº 124, de 08 de julho de 2003. (a) Brig Ar RICARDO DA SILVA SERVAN Chefe do Subdepartamento de Operações do DECEA (Publicada no BCA nº 146, de 07 de agosto de 2006) MINISTÉRIO DA DEFESA COMANDO DA AERONÁUTICA DEPARTAMENTO DE CONTROLE DO ESPAÇO AÉREO PORTARIA DECEA N° 33 /SDOP, DE 13 DE SETEMBRO DE 2007. Aprova a edição da emenda à Instrução sobre Divulgação de Informações Meteorológicas. O CHEFE DO SUBDEPARTAMENTO DE OPERAÇÕES DO DEPARTAMENTO DE CONTROLE DO ESPAÇO AÉREO, no uso das atribuições que lhe confere o Artigo 1°, alínea g, da Portaria DECEA n°34-T/DGCEA, de 15 de março de 2007, RESOLVE: Art. -
Australian Aborigines and Meteorites
Records of the Western Australian Museum 18: 93-101 (1996). Australian Aborigines and meteorites A.W.R. Bevan! and P. Bindon2 1Department of Earth and Planetary Sciences, 2 Department of Anthropology, Western Australian Museum, Francis Street, Perth, Western Australia 6000 Abstract - Numerous mythological references to meteoritic events by Aboriginal people in Australia contrast with the scant physical evidence of their interaction with meteoritic materials. Possible reasons for this are the unsuitability of some meteorites for tool making and the apparent inability of early Aborigines to work metallic materials. However, there is a strong possibility that Aborigines witnessed one or more of the several recent « 5000 yrs BP) meteorite impact events in Australia. Evidence for Aboriginal use of meteorites and the recognition of meteoritic events is critically evaluated. INTRODUCTION Australia, although for climatic and physiographic The ceremonial and practical significance of reasons they are rarely found in tropical Australia. Australian tektites (australites) in Aboriginal life is The history of the recovery of meteorites in extensively documented (Baker 1957 and Australia has been reviewed by Bevan (1992). references therein; Edwards 1966). However, Within the continent there are two significant areas despite abundant evidence throughout the world for the recovery of meteorites: the Nullarbor that many other ancient civilizations recognised, Region, and the area around the Menindee Lakes utilized and even revered meteorites (particularly of western New South Wales. These accumulations meteoritic iron) (e.g., see Buchwald 1975 and have resulted from prolonged aridity that has references therein), there is very little physical or allowed the preservation of meteorites for documentary evidence of Aboriginal acknowledge thousands of years after their fall, and the large ment or use of meteoritic materials. -
Magnetite Biomineralization and Ancient Life on Mars Richard B Frankel* and Peter R Buseckt
Magnetite biomineralization and ancient life on Mars Richard B Frankel* and Peter R Buseckt Certain chemical and mineral features of the Martian meteorite with a mass distribution unlike terrestrial PAHs or those from ALH84001 were reported in 1996 to be probable evidence of other meteorites; thirdly, bacterium-shaped objects (BSOs) ancient life on Mars. In spite of new observations and up to several hundred nanometers long that resemble fos interpretations, the question of ancient life on Mars remains silized terrestrial microorganisms; and lastly, 10-100 nm unresolved. Putative biogenic, nanometer magnetite has now magnetite (Fe304), pyrrhotite (Fel_xS), and greigite (Fe3S4) become a leading focus in the debate. crystals. These minerals were cited as evidence because of their similarity to biogenic magnetic minerals in terrestrial Addresses magnetotactic bacteria. *Department of Physics, California Polytechnic State University, San Luis Obispo, California 93407, USA; e-mail: [email protected] The ancient life on Mars hypothesis has been extensively tDepartments of Geology and Chemistry/Biochemistry, Arizona State challenged, and alternative non-biological processes have University, Tempe, Arizona 85287-1404, USA; e-mail: [email protected] been proposed for each of the four features cited by McKay et al. [4]. In this paper we review the current situa tion regarding their proposed evidence, focusing on the Abbreviations putative biogenic magnetite crystals. BCM biologically controlled mineralization BIM biologically induced mineralization BSO bacterium-shaped object Evidence for and against ancient Martian life PAH polycyclic aromatic hydrocarbon PAHs and BSOs Reports of contamination by terrestrial organic materials [5°,6°] and the similarity of ALH84001 PAHs to non-bio genic PAHs in carbonaceous chondrites [7,8] make it Introduction difficult to positively identify PAHs of non-terrestrial, bio A 2 kg carbonaceous stony meteorite, designated genic origin. -
Lost Lake by Robert Verish
Meteorite-Times Magazine Contents by Editor Like Sign Up to see what your friends like. Featured Monthly Articles Accretion Desk by Martin Horejsi Jim’s Fragments by Jim Tobin Meteorite Market Trends by Michael Blood Bob’s Findings by Robert Verish IMCA Insights by The IMCA Team Micro Visions by John Kashuba Galactic Lore by Mike Gilmer Meteorite Calendar by Anne Black Meteorite of the Month by Michael Johnson Tektite of the Month by Editor Terms Of Use Materials contained in and linked to from this website do not necessarily reflect the views or opinions of The Meteorite Exchange, Inc., nor those of any person connected therewith. In no event shall The Meteorite Exchange, Inc. be responsible for, nor liable for, exposure to any such material in any form by any person or persons, whether written, graphic, audio or otherwise, presented on this or by any other website, web page or other cyber location linked to from this website. The Meteorite Exchange, Inc. does not endorse, edit nor hold any copyright interest in any material found on any website, web page or other cyber location linked to from this website. The Meteorite Exchange, Inc. shall not be held liable for any misinformation by any author, dealer and or seller. In no event will The Meteorite Exchange, Inc. be liable for any damages, including any loss of profits, lost savings, or any other commercial damage, including but not limited to special, consequential, or other damages arising out of this service. © Copyright 2002–2010 The Meteorite Exchange, Inc. All rights reserved. No reproduction of copyrighted material is allowed by any means without prior written permission of the copyright owner. -
March 21–25, 2016
FORTY-SEVENTH LUNAR AND PLANETARY SCIENCE CONFERENCE PROGRAM OF TECHNICAL SESSIONS MARCH 21–25, 2016 The Woodlands Waterway Marriott Hotel and Convention Center The Woodlands, Texas INSTITUTIONAL SUPPORT Universities Space Research Association Lunar and Planetary Institute National Aeronautics and Space Administration CONFERENCE CO-CHAIRS Stephen Mackwell, Lunar and Planetary Institute Eileen Stansbery, NASA Johnson Space Center PROGRAM COMMITTEE CHAIRS David Draper, NASA Johnson Space Center Walter Kiefer, Lunar and Planetary Institute PROGRAM COMMITTEE P. Doug Archer, NASA Johnson Space Center Nicolas LeCorvec, Lunar and Planetary Institute Katherine Bermingham, University of Maryland Yo Matsubara, Smithsonian Institute Janice Bishop, SETI and NASA Ames Research Center Francis McCubbin, NASA Johnson Space Center Jeremy Boyce, University of California, Los Angeles Andrew Needham, Carnegie Institution of Washington Lisa Danielson, NASA Johnson Space Center Lan-Anh Nguyen, NASA Johnson Space Center Deepak Dhingra, University of Idaho Paul Niles, NASA Johnson Space Center Stephen Elardo, Carnegie Institution of Washington Dorothy Oehler, NASA Johnson Space Center Marc Fries, NASA Johnson Space Center D. Alex Patthoff, Jet Propulsion Laboratory Cyrena Goodrich, Lunar and Planetary Institute Elizabeth Rampe, Aerodyne Industries, Jacobs JETS at John Gruener, NASA Johnson Space Center NASA Johnson Space Center Justin Hagerty, U.S. Geological Survey Carol Raymond, Jet Propulsion Laboratory Lindsay Hays, Jet Propulsion Laboratory Paul Schenk, -
Bez Tytu³u-2
BIULETYN MI£ONIKÓW METEORYTÓW METEORYT Nr 1 (25) Marzec 1998 W numerze: Jawor, Baszkówka, Mt Tazerzait, ¯elazo Pallasa Meteoryt Sikhote-Alin (105 g) bêd¹cy w³asnoci¹ miasta Lidzbarka Warmiñskiego. METEORYT 1/98 1 Od redaktora: Meteoryt biuletyn dla mi³o- ników meteorytów wydawany Wydarzeniem numeru jest rozwi¹zanie zagadki meteorytu przez Olsztyñskie Planetarium Jawor. Cudzys³ów podpowiada ju¿, ¿e wynik jest negatywny. Wro- i Obserwatorium Astronomicz- c³awscy naukowcy potrafili jednak dociec, czym jest kawa³ek ska³y ne, Muzeum Miko³aja Koper- le¿¹cy w muzeum w Jaworze z etykietk¹ meteoryt? i sk¹d do nika we Fromborku i Pallasite muzeum trafi³. Meteoryt czuje siê zaszczycony, ¿e to z jego ³amów Press wydawcê kwartalnika mo¿na siê o tym po raz pierwszy dowiedzieæ. Pe³ne opracowanie Meteorite! z którego pochodzi uka¿e siê w jednym z bardziej fachowych czasopism. wiêksza czêæ publikowanych Z nowym rokiem i z 25 numerem Meteoryt znów zmienia materia³ów. wygl¹d, co tradycyjnie jest zas³ug¹ Jacka Dr¹¿kowskiego. Z przy- Redaguje Andrzej S. Pilski jemnoci¹ odnotowujê te¿ powrót Micha³a Kosmulskiego do t³uma- czenia artyku³ów, oraz do³¹czenie siê Marka Muæka do grona t³uma- Sk³ad: Jacek Dr¹¿kowski czy i wspó³pracowników. Ronie te¿ grono czytelników, czyli nowy Druk: Jan, Lidzbark Warm. rok dobrze siê zapowiada. Adres redakcji: Dobrze zapowiada siê te¿ pozyskiwanie meteorytów dla kolekcjo- skr. poczt. 6, nerów, ale idzie to bardzo powoli. W kontaktach z zagranicznymi 14-530 Frombork, dealerami wystêpuje zjawisko znane naszym kolekcjonerom z kontak- tel. 0-55-243-7392. tów z ni¿ej podpisanym: wysy³a siê zamówienie i.. -
Cape Denison MAWSON CENTENNIAL 1911–2011, Commonwealth Bay
Cape Denison MAWSON CENTENNIAL 1911–2011, Commonwealth Bay Mawson and the Australasian Geology of Cape Denison Landforms of Cape Denison Position of Cape Denison in Gondwana Antarctic Expedition The two dominant rock-types found at Cape Denison Cape Denison is a small ice-free rocky outcrop covering Around 270 Million years ago the continents that we are orthogneiss and amphibolite. There are also minor less than one square kilometre, which emerges from The Australasian Antarctic Expedition (AAE) took place know today were part of a single ancient supercontinent occurrences of coarse grained felsic pegmatites. beneath the continental ice sheet. Stillwell (1918) reported between 1911 and 1914, and was organised and led by called Pangea. Later, Pangea split into two smaller that the continental ice sheet rises steeply behind Cape the geologist, Dr Douglas Mawson. The expedition was The Cape Denison Orthogneiss was described by Stillwell (1918) as supercontinents, Laurasia and Gondwana, and Denison reaching an altitude of ‘1000 ft in three miles and jointly funded by the Australian and British Governments coarse-grained grey quartz-feldspar layered granitic gneiss. These rock Antarctica formed part of Gondwana. with contributions received from various individuals and types are normally formed by metamorphism (changed by extreme heat 1500 ft in five and a half miles’ (approximately 300 metres and pressure) of granites. The Cape Denison Orthogneiss is found around In current reconstructions of the supercontinent Gondwana, the Cape scientific societies, including the Australasian Association to 450 metres over 8.9 kilometres). Photography by Chris Carson Cape Denison, the nearby offshore Mackellar Islands, and nearby outcrops Denison–Commonwealth Bay region was located adjacent to the coast for the Advancement of Science.