Fourth Australian Regolith Geoscientists Association Conference 1
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Planetary Geologic Mappers Annual Meeting
Program Lunar and Planetary Institute 3600 Bay Area Boulevard Houston TX 77058-1113 Planetary Geologic Mappers Annual Meeting June 12–14, 2018 • Knoxville, Tennessee Institutional Support Lunar and Planetary Institute Universities Space Research Association Convener Devon Burr Earth and Planetary Sciences Department, University of Tennessee Knoxville Science Organizing Committee David Williams, Chair Arizona State University Devon Burr Earth and Planetary Sciences Department, University of Tennessee Knoxville Robert Jacobsen Earth and Planetary Sciences Department, University of Tennessee Knoxville Bradley Thomson Earth and Planetary Sciences Department, University of Tennessee Knoxville Abstracts for this meeting are available via the meeting website at https://www.hou.usra.edu/meetings/pgm2018/ Abstracts can be cited as Author A. B. and Author C. D. (2018) Title of abstract. In Planetary Geologic Mappers Annual Meeting, Abstract #XXXX. LPI Contribution No. 2066, Lunar and Planetary Institute, Houston. Guide to Sessions Tuesday, June 12, 2018 9:00 a.m. Strong Hall Meeting Room Introduction and Mercury and Venus Maps 1:00 p.m. Strong Hall Meeting Room Mars Maps 5:30 p.m. Strong Hall Poster Area Poster Session: 2018 Planetary Geologic Mappers Meeting Wednesday, June 13, 2018 8:30 a.m. Strong Hall Meeting Room GIS and Planetary Mapping Techniques and Lunar Maps 1:15 p.m. Strong Hall Meeting Room Asteroid, Dwarf Planet, and Outer Planet Satellite Maps Thursday, June 14, 2018 8:30 a.m. Strong Hall Optional Field Trip to Appalachian Mountains Program Tuesday, June 12, 2018 INTRODUCTION AND MERCURY AND VENUS MAPS 9:00 a.m. Strong Hall Meeting Room Chairs: David Williams Devon Burr 9:00 a.m. -
Back Matter (PDF)
Index Page numbers in italics refer to Tables or Figures Acasta gneiss 137, 138 Chladni, Ernst 94, 97 Adam, Robert 8, 11 chlorite 70, 71 agriculture, Hutton on 177 chloritoid stability 70 Albritton, Claude C. 100 Clerk Jnr, John 3 alumina (A1203), reaction in metamorphism 67-71 Clerk of Odin, John 5, 6, 7, 10, 11 andalusite stability 67 Clerk-Maxwell, George 10 anthropic principle 79-80 climate change 142 Apex basalt 140 Lyell on 97-8 Archean cratons (archons) 28, 31-2 coal as Earth heat source 176 Arizona Crater 98-9 coesite stability 65 Arran, Isle of 170 Columbia River basalts 32 asthenosphere 22 comets 89-90, 147-8 astrobleme 101 short v. long period 92 atmospheric composition 83-6 as source of life 148-9 Austral Volcanic Chain 24 continental flood basalt (CFB) 20, 23, 32 cordierite stability 67 craters, impact Bacon, Francis 21 Chixulub 109, 110, 143 Baldwin, Ralph 102 early ideas on 90, 98 Banks, Sir Joseph 96 modern occurrences 91, 98-101 Barringer, Daniel Moreau 99 Morokweng 142 Barringer Crater 99, 102, 103 modern research 102-3 basalt periodicity of 111-12 described by Hall 40-1 creation, Hutton's views on 76 mid-ocean ridge (MORB) 16-17, 20-1, 22, 23, 30-1 Creech, William 5 modern experiments on 44-7 Cretaceous-Tertiary impacts 141 ocean island (OIB) 20, 23 crust formation 17 see also flood basalt cryptoexplosion structures 101 Benares (India) meteorite shower 96 cryptovolcanic structures 100-1 Biot, Jean-Baptiste 97 Black, Joseph 4, 9, 10, 11, 42, 171 Boon, John D. -
Exploring Comets and Modeling for Mission Success
Exploring Comets and Modeling for Mission Success National Science Education Standards Alignment Created for Deep Impact, A NASA Discovery mission Maura Rountree-Brown and Art Hammon Educator-Enrichment Grades 5 – 8 Science as Inquiry Abilities necessary to do scientific inquiry − Identify questions that can be answered through scientific investigations. • Exploring Comets: Reflections on comets, missions and modeling − Develop descriptions, explanations, predictions, and models using evidence. • Make a Comet and Eat It!, Chemistry and Thermodynamics of Ice Cream, Comet on a Stick, Paper Comet with a Deep Impact, and Comet Models Based on the Deep Impact Mission − Think critically and logically to make the relationships between evidence and explanations. • Make a Comet and Eat It!, Comet on a Stick, Paper Comet with a Deep Impact, and Comet Models Based on the Deep Impact Mission − Communicate scientific procedures and explanations. • Make a Comet and Eat It! Understandings about scientific inquiry − Different kinds of questions suggest different kinds of scientific investigations. Some investigations involve observing and describing objects, or events; some involve experiments; some involve seeking more information; some involve discovery of new objects and phenomena; and some involve making models. • Make a Comet and Eat It!, Chemistry and Thermodynamics of Ice Cream, Comet on a Stick, Paper Comet with a Deep Impact, Comet Models Based on the Deep Impact Mission, and Deep Impact Comet Modeling − Current scientific knowledge and understanding guide scientific investigations. Different scientific domains employ different methods, core theories, and standards to advance scientific knowledge and understanding. • A Comet’s Place in the Solar System, Exploring Comets: Reflections on comets, missions and modeling, Deep Impact Comet Modeling, Deep Impact: Interesting Comet Facts, and Small Bodies Missions − Scientific explanations emphasize evidence, have logically consistent arguments, and use scientific principles, models, and theories. -
Lexiconordica
LexicoNordica Forfatter: Hannu Tommola og Arto Mustajoki [Den förnyade rysk-finska storordboken] Anmeldt værk: Martti Kuusinen, Vera Ollikainen og Julia Syrjäläinen. 1997. Venäjä- suomi-suursanakirja (Bol ´šoj russko-finskij slovar´) yli 90.000 hakusanaa ja sanontaa. Porvoo/Helsinki/Juva: WSOY og Moskva: Russkij jazyk, 1997. Kilde: LexicoNordica 5, 1998, s. 239-260 URL: http://ojs.statsbiblioteket.dk/index.php/lexn/issue/archive © LexicoNordica og forfatterne Betingelser for brug af denne artikel Denne artikel er omfattet af ophavsretsloven, og der må citeres fra den. Følgende betingelser skal dog være opfyldt: Citatet skal være i overensstemmelse med „god skik“ Der må kun citeres „i det omfang, som betinges af formålet“ Ophavsmanden til teksten skal krediteres, og kilden skal angives, jf. ovenstående bibliografiske oplysninger. Søgbarhed Artiklerne i de ældre LexicoNordica (1-16) er skannet og OCR-behandlet. OCR står for ’optical character recognition’ og kan ved tegngenkendelse konvertere et billede til tekst. Dermed kan man søge i teksten. Imidlertid kan der opstå fejl i tegngenkendelsen, og når man søger på fx navne, skal man være forberedt på at søgningen ikke er 100 % pålidelig. 239 Hannu Tommola & Arto Mustajoki Den förnyade rysk-finska storordboken Martti Kuusinen, Vera Ollikainen, Julia Syrjäläinen: Venäjä-suomi- suursanakirja (Bol´soj russko-finskij slovar´) yli 90.000 hakusanaa ja sanontaa. Toim. M. Kuusinen. Porvoo, Helsinki, Juva: WSOY & Moskva: Russkij jazyk, 1997, XXXI + 1575 s. Pris: FIM 554. The dictionary reviewed in this article is a revised edition of a Russian-Finnish dictionary compiled by scholars in the former Soviet Karelia. The dictionary was first published in 1963 in Moscow, then reprinted twice by the Finnish publishing house WSOY. -
Widespread Crater-Related Pitted Materials on Mars: Further Evidence for the Role of Target Volatiles During the Impact Process ⇑ Livio L
Icarus 220 (2012) 348–368 Contents lists available at SciVerse ScienceDirect Icarus journal homepage: www.elsevier.com/locate/icarus Widespread crater-related pitted materials on Mars: Further evidence for the role of target volatiles during the impact process ⇑ Livio L. Tornabene a, , Gordon R. Osinski a, Alfred S. McEwen b, Joseph M. Boyce c, Veronica J. Bray b, Christy M. Caudill b, John A. Grant d, Christopher W. Hamilton e, Sarah Mattson b, Peter J. Mouginis-Mark c a University of Western Ontario, Centre for Planetary Science and Exploration, Earth Sciences, London, ON, Canada N6A 5B7 b University of Arizona, Lunar and Planetary Lab, Tucson, AZ 85721-0092, USA c University of Hawai’i, Hawai’i Institute of Geophysics and Planetology, Ma¯noa, HI 96822, USA d Smithsonian Institution, Center for Earth and Planetary Studies, Washington, DC 20013-7012, USA e NASA Goddard Space Flight Center, Greenbelt, MD 20771, USA article info abstract Article history: Recently acquired high-resolution images of martian impact craters provide further evidence for the Received 28 August 2011 interaction between subsurface volatiles and the impact cratering process. A densely pitted crater-related Revised 29 April 2012 unit has been identified in images of 204 craters from the Mars Reconnaissance Orbiter. This sample of Accepted 9 May 2012 craters are nearly equally distributed between the two hemispheres, spanning from 53°Sto62°N latitude. Available online 24 May 2012 They range in diameter from 1 to 150 km, and are found at elevations between À5.5 to +5.2 km relative to the martian datum. The pits are polygonal to quasi-circular depressions that often occur in dense clus- Keywords: ters and range in size from 10 m to as large as 3 km. -
Sa Abá, ¡Ay! ¡Chito! Ó ¡Chiton!. Sht...! ¡Chiton! ¡Silencio!
English_Spanish_Tagalog_Dictionary_Project_Gutenberg_cd3wd !Vaya! ¡que vergüenza!. Ayan! kahiyâhiyâ! ¡Ah! ¡ay!. Ah! abá! ahá! ¡Ay!. Sa abá, ¡ay! ¡Chito! ó ¡chiton!. Sht...! ¡Chiton! ¡silencio!. ¡Marahan! ¡Fuera! ¡fuera de aquí! ¡quita! ¡quita allá!. Sulong! tabì! lumayas ka! alis diyan! ¡He! ¡oye!. Hoy! pakinggan mo! ¡He!. Ehé. ¡Oh!. Abá! ¡Quita de ahí! ¡vete allá!. Tabì! sulong! ¡Vaya!. ¡Ayan! A bordo. Nakasakay sa sasakyán. A cada hora. Oras-oras. Á cada momento. Sa bawa't sangdalî. A Dios. Paalam, adyos. A Dios; despedida. Paalam. Á él mismo. Sa kanya ngâ, sa kanya man, sa kanya rin (lalake). Á eso, á ello. Diyan sa, doon sa. Á eso, á ello. Diyan sa, doon sa. A este ó esta, por eso. Dahil dito. A esto. Dito sa; hanggang dito. A esto. Dito sa, hanggang dito. Á horcajadas. Pahalang. A la mar, fuera del navio. Sa tubig. A la moda. Ayon sa ugalí, sunod sa moda. A la temperatura de la sangre. Kasing-init ng dugô. Á lo ancho. Sa kalwangan. Á lo cual. Dahil dito, sa dahilang ito. A lo largo. Sa gawî, sa hinabahabà. Á lo largo. Sa hinabahabà. Á lo que, á que. Na saan man. Á mas, ademas. Bukod sa rito, sakâ. A medio camino. Sa may kalagitnaan ng lakarín. Á menos que; si no. Maliban, kung dî. A pedacitos. Tadtad. Á pie. Lakád. A poca distancia, cercanamente. Malapítlapít, halos. Spanish_Tagalog Page 1 English_Spanish_Tagalog_Dictionary_Project_Gutenberg_cd3wd Á poco precio. May kamurahan. A popa, en popa. Sa gawíng likod, sa gawíng hulí. A popa. Sa gawíng likod. Á propósito. Bagay. A punto de, dispuesto á, en accion. Kauntî na, handâ na, hala. -
16. Ice in the Martian Regolith
16. ICE IN THE MARTIAN REGOLITH S. W. SQUYRES Cornell University S. M. CLIFFORD Lunar and Planetary Institute R. O. KUZMIN V.I. Vernadsky Institute J. R. ZIMBELMAN Smithsonian Institution and F. M. COSTARD Laboratoire de Geographie Physique Geologic evidence indicates that the Martian surface has been substantially modified by the action of liquid water, and that much of that water still resides beneath the surface as ground ice. The pore volume of the Martian regolith is substantial, and a large amount of this volume can be expected to be at tem- peratures cold enough for ice to be present. Calculations of the thermodynamic stability of ground ice on Mars suggest that it can exist very close to the surface at high latitudes, but can persist only at substantial depths near the equator. Impact craters with distinctive lobale ejecta deposits are common on Mars. These rampart craters apparently owe their morphology to fluidhation of sub- surface materials, perhaps by the melting of ground ice, during impact events. If this interpretation is correct, then the size frequency distribution of rampart 523 524 S. W. SQUYRES ET AL. craters is broadly consistent with the depth distribution of ice inferred from stability calculations. A variety of observed Martian landforms can be attrib- uted to creep of the Martian regolith abetted by deformation of ground ice. Global mapping of creep features also supports the idea that ice is present in near-surface materials at latitudes higher than ± 30°, and suggests that ice is largely absent from such materials at lower latitudes. Other morphologic fea- tures on Mars that may result from the present or former existence of ground ice include chaotic terrain, thermokarst and patterned ground. -
In Pdf Format
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Durham Research Online
Durham Research Online Deposited in DRO: 02 June 2020 Version of attached le: Accepted Version Peer-review status of attached le: Peer-reviewed Citation for published item: Heap, Michael J. and Gilg, H. Albert and Byrne, Paul K. and Wadsworth, Fabian B. and Reuschl¡e,Thierry (2020) 'Petrophysical properties, mechanical behaviour, and failure modes of impact melt-bearing breccia (suevite) from the Ries impact crater (Germany).', Icarus., 349 . p. 113873. Further information on publisher's website: https://doi.org/10.1016/j.icarus.2020.113873 Publisher's copyright statement: c 2020 This manuscript version is made available under the CC-BY-NC-ND 4.0 license http://creativecommons.org/licenses/by-nc-nd/4.0/ Use policy The full-text may be used and/or reproduced, and given to third parties in any format or medium, without prior permission or charge, for personal research or study, educational, or not-for-prot purposes provided that: • a full bibliographic reference is made to the original source • a link is made to the metadata record in DRO • the full-text is not changed in any way The full-text must not be sold in any format or medium without the formal permission of the copyright holders. Please consult the full DRO policy for further details. Durham University Library, Stockton Road, Durham DH1 3LY, United Kingdom Tel : +44 (0)191 334 3042 | Fax : +44 (0)191 334 2971 https://dro.dur.ac.uk Journal Pre-proof Petrophysical properties, mechanical behaviour, and failure modes of impact melt-bearing breccia (suevite) from the Ries impact crater (Germany) Michael J. -
El Cerebro De Broca
El cerebro de Broca es un libro escrito por Carl Sagan formado por discursos o artículos publicados entre 1974 y 1979 en muchas revistas incluyendo Atlantic Monthly, New Republic, Physics Today, Playboy, y Scientific American. El ensayo que titula el libro lleva su nombre en honor del físico, anatomista y antropólogo francés, Paul Broca (1824-1880). Generalmente se recuerda a Broca por su descubrimiento de que distintas partes físicas del cerebro corresponden a distintas funciones. Una gran parte del libro está dedicada a desacreditar el trabajo de los «fabricantes de paradojas», como llama a los divulgadores de la pseudociencia, ya sea quienes se encuentran al borde de las disciplinas científicas o simplemente son rotundos charlatanes. Otra gran parte del libro discute los convencionalismos en la nomenclatura de los miembros de nuestro sistema solar, así como sus características físicas. Sagan también expone sus puntos de vista sobre la Ciencia Ficción, mencionando especialmente a Robert A. Heinlein, quien fue uno de sus escritores favoritos durante su infancia. Las experiencias cercanas a la muerte, y sus controversias culturales también son discutidas en el libro, así como la crítica de las teorías desarrolladas en el libro de Robert K. Temple The Sirius Mystery publicado tres años antes en 1975. Carl Sagan El cerebro de Broca ePub r1.3 Horus 05.08.16 Título original: Broca´s Brain Carl Sagan, 1974, 1975, 1976, 1977, 1978, 1979 Traducción: Doménech Bregada (Cap 1 al 7) y José Chabás (Cap 8 al 25) Diseño de portada: Horus Editor digital: Horus Colaborador: epubsagan (apéndices y tablas) Corrección de erratas: el nota, heutorez, Autillo ePub base r1.2 Para Rachel y Samuel Sagan, mis padres, que introdujeron en mí la alegría de la comprensión del mundo, con gratitud, admiración y amor AGRADECIMIENTOS EN CUANTO A DISCUSIÓN de puntos específicos abordados en el texto, estoy en deuda con un buen número de amigos, corresponsales y colegas, entre los que se incluyen Diane Ackerman, D.W.G. -
Drought Impact on Fish Communities and River Health in the Corangamite Region
Drought impact on fish communities and river health in the Corangamite Region An isolated pool in Painkalac Creek. Tom Ryan and John McGuckin Report prepared for Corangamite Catchment Management Authority August 2007 Drought impact on fish communities and river health in the Corangamite Region Executive Summary This study provides a rapid assessment of river condition and aims to determine the key issues affecting aquatic health including the relative impact of drought. It is designed to help prioritise potential management actions in the drought response plan. Pre-existing catchment issues, such as water extraction, extensive land clearing and lack of riparian vegetation can directly affect river health and compounds impacts caused directly by drought. Where catchments have been degraded by past management practices, the severity of the drought upon stream health has been the most extreme. Waters examined in this study have been classified into 3 distinct classes of river health, streams with minor stress, streams with moderate stress and streams that have severe stress. Waterways with minor drought stress had lower streamflows than normal as a result of the drought but were in no immediate threat of becoming severely stressed by the drought. Waters classified as having moderate stress are ones in which the existing aquatic fauna is expected to be experiencing some stress, however, the stress is unlikely to have caused the loss of species. Streamflow may have ceased in freshwater reaches and water deterioration may have occurred in remaining refuge habitat, however, the duration of the stress upon aquatic fauna has only been for a relatively short period. -
Anglesea River Estuary Flow Assessment Final Approved Report January 2016
Corangamite CMA Anglesea River Estuary Flow Assessment Final Approved Report January 2016 Table of contents Executive Summary ................................................................................................................................. v 1. Introduction..................................................................................................................................... 1 1.1 Anglesea River estuary ........................................................................................................ 1 1.2 Purpose of this report........................................................................................................... 3 1.3 Scope and limitations ........................................................................................................... 4 Part 1: Physical, ecological and social changes to the Anglesea River estuary ...................................... 5 2. Predicted physical changes to Anglesea River estuary ................................................................. 5 2.1 Objective .............................................................................................................................. 5 2.2 Approach .............................................................................................................................. 5 2.3 Review of Relevant Literature and Data .............................................................................. 6 2.4 Conceptual Models and Modelling Framework ................................................................