Conference Summary and Recommendations
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
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. -
Bul Le Tin of the Global Vol Can Ism Net Work
Bul le tin of the Global Vol can ism Net work Vol ume 28, Num ber 5, May 2003 Ana ta han (Mari ana Is lands) Nearly con tinuous ash plumes through May ....................2 Chiku ra chki (Kur ile Islands) Eruption contin ued through May; long plumes and some ash fall ........5 Karym sky (Kamchatk a) Fre quent ash plumes gener ated from Oc tober 2002 through May 2003 ........6 Har- Togoo (Mon go lia) Fu ma roles and mi nor seis mic ity since Oc to ber 2002 ..................7 Mayon (Phil ip pines) Three small ash- and- steam ex plo sions dur ing April- May 2003 ..............9 Karan ge tang (In do ne sia) Ash explo sions from January through May 2003 ..................10 Lokon- Empung (In do ne sia) In creased ex plo sive ac tiv ity dur ing January- April 2003; lo cal ash fall......11 Ruapehu (New Zea land) Steam plume issued from warm Crater Lake in May, but no erup tion ........12 Mon owai Sea mount (Ker madec Is lands) Volcanic earth quake swarm April-May detec ted by T-wave s ....13 Piton de la Fournaise (Réunion Island) Eruption on 30 May gener ates lava flows within Dolomie u crater ..14 Strom boli (It aly) Lava ef fu sion con tin ues through mid- June; in fra red sat el lite ob ser va tions .........15 Nyi ra gongo (DR Congo) 2002-3 lava lake activity, thermal ra diation, and CO2 and SO2 emis sions......16 Ro bledo (Ar gen tina) Sat el lite sur veys dur ing May 1996- October 2000 in di cate sub si dence ..........22 Utu runcu (Bo livia) De for ma tion de tected by sat el lite sur veys; low- level seis mic ity and ac tive fu ma roles...23 -
Low Resolution
No. 102 June 2021 IAMGIAMG NewsletterNewsletter Official Newsletter of the International Association for Mathematical Geosciences Contents ith the Covid-19 pandemic Wfar from over, most Announcement of the 2021 IAmG AwArds ......................... 1 scientific meetings have been PresIdent’s forum .............................................................. 3 postponed or converted to a member news ...................................................................... 3 digital format. While there are nomInAtIons for IAmG AwArds ........................................... 3 certainly benefits to online meetings (I definitely don’t miss multiple memorAndum wIth codA AssocIAtIon ................................ 3 flights each way and jetlag) they tend reseArch center for solId eArth bIG dAtA to lose the personal interactions. It founded At the chInA unIversIty of GeoscIences ........... 4 is difficult for an online conference rememberInG dr. Peter fox - A tItAn In the eArth to replicate the conversations in the scIence InformAtIcs communIty ........................................ 4 hallways between sessions or during a meal that can bring a community Ieee GeoscIence And remote sensInG socIety (Grss) dIs- together and build new connections and tInGuIshed lecturer (dl) ............................................. 4 ideas. If you have any ideas or examples Professor noel cressIe nAmed A fellow of the of how the IAMG could work to bring the royAl socIety of new south Wales................................... 4 community together, please -
Mercurian Impact Ejecta: Meteorites and Mantle
Meteoritics & Planetary Science 44, Nr 2, 285–291 (2009) Abstract available online at http://meteoritics.org Mercurian impact ejecta: Meteorites and mantle Brett GLADMAN* and Jaime COFFEY University of British Columbia, Department of Physics and Astronomy, 6244 Agricultural Road, Vancouver, British Columbia V6T 1Z1, Canada *Corresponding author. E-mail: [email protected] (Submitted 28 January 2008; revision accepted 15 October2008) Abstract–We have examined the fate of impact ejecta liberated from the surface of Mercury due to impacts by comets or asteroids, in order to study 1) meteorite transfer to Earth, and 2) reaccumulation of an expelled mantle in giant-impact scenarios seeking to explain Mercury’s large core. In the context of meteorite transfer during the last 30 Myr, we note that Mercury’s impact ejecta leave the planet’s surface much faster (on average) than other planets in the solar system because it is the only planet where impact speeds routinely range from 5 to 20 times the planet’s escape speed; this causes impact ejecta to leave its surface moving many times faster than needed to escape its gravitational pull. Thus, a large fraction of Mercurian ejecta may reach heliocentric orbit with speeds sufficiently high for Earth-crossing orbits to exist immediately after impact, resulting in larger fractions of the ejecta reaching Earth as meteorites. We calculate the delivery rate to Earth on a time scale of 30 Myr (typical of stony meteorites from the asteroid belt) and show that several percent of the high-speed ejecta reach Earth (a factor of 2–3 less than typical launches from Mars); this is one to two orders of magnitude more efficient than previous estimates. -
Open Research Online Oro.Open.Ac.Uk
Open Research Online The Open University’s repository of research publications and other research outputs Late movement of basin-edge lobate scarps on Mercury Journal Item How to cite: Fegan, E. R.; Rothery, D. A.; Marchi, S.; Massironi, M.; Conway, S. J. and Anand, M. (2017). Late movement of basin-edge lobate scarps on Mercury. Icarus, 288 pp. 226–324. For guidance on citations see FAQs. c 2017 Elsevier Inc https://creativecommons.org/licenses/by-nc-nd/4.0/ Version: Accepted Manuscript Link(s) to article on publisher’s website: http://dx.doi.org/doi:10.1016/j.icarus.2017.01.005 Copyright and Moral Rights for the articles on this site are retained by the individual authors and/or other copyright owners. For more information on Open Research Online’s data policy on reuse of materials please consult the policies page. oro.open.ac.uk 1 Late movement of basin-edge lobate scarps on Mercury 2 Fegan E.R.1*, Rothery D.A.1, Marchi S.2, Massironi M.3, Conway S.J.1,4, Anand M.1,5, 3 1Department of Physical Sciences, The Open University, Walton Hall, Milton Keynes, MK7 6AA, UK. 2NASA 4 Lunar Science Institute, Southwest Research Institute, Boulder, Colorado 80302, USA. 3Dipartimento di 5 Geoscienze, Università di Padova, Via Giotto 1, 35137 Padova, Italy. 4LPG Nantes - UMR CNRS 6112, 2 rue de la 6 Houssinière - BP 92208, 44322 Nantes Cedex 3, France 5Department of Earth Science, The Natural History 7 Museum, Cromwell Road, London, SW7 5BD, UK. 8 9 *Corresponding author (email: [email protected]) 10 Keywords: Planetary; geology; Mercury; tectonics; model ages; lobate scarps; planetary volcanism. -
The Destruction of Art
1 The destruction of art Solvent form examines art and destruction—through objects that have been destroyed (lost in fires, floods, vandalism, or, similarly, those that actively court or represent this destruction, such as Christian Marclay’s Guitar Drag or Chris Burden’s Samson), but also as an undoing process within art that the object challenges through form itself. In this manner, events such as the Momart warehouse fire in 2004 (in which large hold- ings of Young British Artists (YBA) and significant collections of art were destroyed en masse through arson), as well as the events surrounding art thief Stéphane Breitwieser (whose mother destroyed the art he had stolen upon his arrest—putting it down a garbage disposal or dumping it in a nearby canal) are critical events in this book, as they reveal something about art itself. Likewise, it is through these moments of destruction that we might distinguish a solvency within art and discover an operation in which something is made visible at a time when art’s metaphorical undo- ing emerges as oddly literal. Against this overlay, a tendency is mapped whereby individuals attempt to conceptually gather these destroyed or lost objects, to somehow recoup them in their absence. This might be observed through recent projects, such as Jonathan Jones’s Museum of Lost Art, the Tate Modern’s Gallery of Lost Art, or Henri Lefebvre’s text The Missing Pieces; along with exhibitions that position art as destruction, such as Damage Control at the Hirschhorn Museum or Under Destruction by the Swiss Institute in New York. -
Meeting Program
A A S MEETING PROGRAM 211TH MEETING OF THE AMERICAN ASTRONOMICAL SOCIETY WITH THE HIGH ENERGY ASTROPHYSICS DIVISION (HEAD) AND THE HISTORICAL ASTRONOMY DIVISION (HAD) 7-11 JANUARY 2008 AUSTIN, TX All scientific session will be held at the: Austin Convention Center COUNCIL .......................... 2 500 East Cesar Chavez St. Austin, TX 78701 EXHIBITS ........................... 4 FURTHER IN GRATITUDE INFORMATION ............... 6 AAS Paper Sorters SCHEDULE ....................... 7 Rachel Akeson, David Bartlett, Elizabeth Barton, SUNDAY ........................17 Joan Centrella, Jun Cui, Susana Deustua, Tapasi Ghosh, Jennifer Grier, Joe Hahn, Hugh Harris, MONDAY .......................21 Chryssa Kouveliotou, John Martin, Kevin Marvel, Kristen Menou, Brian Patten, Robert Quimby, Chris Springob, Joe Tenn, Dirk Terrell, Dave TUESDAY .......................25 Thompson, Liese van Zee, and Amy Winebarger WEDNESDAY ................77 We would like to thank the THURSDAY ................. 143 following sponsors: FRIDAY ......................... 203 Elsevier Northrop Grumman SATURDAY .................. 241 Lockheed Martin The TABASGO Foundation AUTHOR INDEX ........ 242 AAS COUNCIL J. Craig Wheeler Univ. of Texas President (6/2006-6/2008) John P. Huchra Harvard-Smithsonian, President-Elect CfA (6/2007-6/2008) Paul Vanden Bout NRAO Vice-President (6/2005-6/2008) Robert W. O’Connell Univ. of Virginia Vice-President (6/2006-6/2009) Lee W. Hartman Univ. of Michigan Vice-President (6/2007-6/2010) John Graham CIW Secretary (6/2004-6/2010) OFFICERS Hervey (Peter) STScI Treasurer Stockman (6/2005-6/2008) Timothy F. Slater Univ. of Arizona Education Officer (6/2006-6/2009) Mike A’Hearn Univ. of Maryland Pub. Board Chair (6/2005-6/2008) Kevin Marvel AAS Executive Officer (6/2006-Present) Gary J. Ferland Univ. of Kentucky (6/2007-6/2008) Suzanne Hawley Univ. -
Dean Cain Bettina Zimmermann
DEAN CAIN BETTINA ZIMMERMANN POST IMPACT POST IMPACT In 2012, a meteor crashes into tion plane to Europe is destroyed Siberia with the force of several by a mysterious satellite signal, thousand nuclear warheads. In controlled from the ruins of Berlin, 2015, a few survivors will travel a city that was considered dead into “the death zone”, to try and and buried – under 30 feet of ice locate a device that could give and snow – the President of the mankind new hope – or forever New United Northern Sates orders finish it… a new expedition to find and destroy the base and the satellite. In 2012, a meteor strikes Earth, Tom Parker (Dean Cain) volunteers causing earthquakes, tidal waves, to lead a group of highly trained and a dust cloud that soon covers specialists on a suicide mission most of the Northern hemisphere, to Berlin – with ground vehicles, turning it into an ice-covered no reliable intel, and zero radio “death-zone”. contact. Three years later, most of the sur- In the ruins of what was once one vivors have settled in the only hab- of the most dynamic cities in itable territories below the equa- Europe, a desperate fight ensues tor. It’s a harsh life, with little hope for the power to change every- of Earth’s climate ever reverting thing – for better or for worse… back to normal. When an expedi- POST IMPACT SNOWBLIND LLC presents a TANDEM PRODUCTIONS GMBH, UFO IPS LLC in co-production with LUCKY 7 PRODUCTIONS LLC and AMERICAN FILM CINEMA in association with RTL TELEVISION GMBH and THE TOWER LIMITED LIABILITY PARTNERSHIP Production -
Complete Production History 2018-2019 SEASON
THEATER EMORY A Complete Production History 2018-2019 SEASON Three Productions in Rotating Repertory The Elaborate Entrance of Chad Deity October 23-24, November 3-4, 8-9 • Written by Kristoffer Diaz • Directed by Lydia Fort A satirical smack-down of culture, stereotypes, and geopolitics set in the world of wrestling entertainment. Mary Gray Munroe Theater We Are Proud to Present a Presentation About the Herero of Namibia, Formerly Known as Southwest Africa, From the German Südwestafrika, Between the Years 1884-1915 October 25-26, 30-31, November 10-11 • Written by Jackie Sibblies Drury • Directed by Eric J. Little The story of the first genocide of the twentieth century—but whose story is actually being told? Mary Gray Munroe Theater The Moors October 27-28, November 1-2, 6-7 • Written by Jen Silverman • Directed by Matt Huff In this dark comedy, two sisters and a dog dream of love and power on the bleak English moors. Mary Gray Munroe Theater Sara Juli’s Tense Vagina: an actual diagnosis November 29-30 • Written, directed, and performed by Sara Juli Visiting artist Sara Juli presents her solo performance about motherhood. Theater Lab, Schwartz Center for the Performing Arts The Tatischeff Café April 4-14 • Written by John Ammerman • Directed by John Ammerman and Clinton Wade Thorton A comic pantomime tribute to great filmmaker and mime Jacques Tati Mary Gray Munroe Theater 2 2017-2018 SEASON Midnight Pillow September 21 - October 1, 2017 • Inspired by Mary Shelley • Directed by Park Krausen 13 Playwrights, 6 Actors, and a bedroom. What dreams haunt your midnight pillow? Theater Lab, Schwartz Center for the Performing Arts The Anointing of Dracula: A Grand Guignol October 26 - November 5, 2017 • Written and directed by Brent Glenn • Inspired by the works of Bram Stoker and others. -
Post-Impact Hydrothermal Activity in Meteorite Impact Craters and Potential Opportunities for Life
Bioastronomy 2002: Life Among the Stars IAU Symposium, Vol. 213, 2004 R.P.Norris and F.H.Stootman (eds.) Post-Impact Hydrothermal Activity in Meteorite Impact Craters and Potential Opportunities for Life Christian Koeberl Department of Geological Sciences, University of Vienna, Althanstrasse 14, A-1090 Vienna, Austria, [email protected] Wolf Uwe Reimold Impact Cratering Research Group, School of Geosciences, University of the Witwatersrand, Johannesburg 2050, South Africa, [email protected] Abstract. Impact craters are prominent landforms on all objects with a solid surface in the solar system. The formation of an impact structure is a high-energy, high-temperature transient event which introduces large amounts of energy into a limited area. This energy can, in part, be expanded on the creation and activation of a hydrothermal system within and even outside of the crater. Depending on the crater size and geology of the target region, this hydrothermal system may persist for extended periods of time. Such impact-induced hydrothermal systems could well have provided conditions supportive of the development of life on the early Earth and it is not unreasonable to assume that similar conditions could have led to life-favoring circumstances on other planets and satellites. 1. Introduction Studies during the last few decades have convinced most workers that the planets formed by collision and hierarchical growth starting from small objects, Le., from dust to planetesimals to planets. All planets and satellites of the solar system that have solid surfaces (e.g., Mercury, Venus, Mars, the asteroids) are covered by craters. Impact cratering has been either the most important, or one of the most important processes that affected the shaping of their surfaces. -
PROJECT STREET from to MORATORIUM START FY09-Slurry
PROJECT STREET FROM TO MORATORIUM START FY09-Slurry 01ST AV W WALNUT AV UPAS ST 5/7/2010 FY09-Slurry 01ST AV UPAS ST THORN ST 5/7/2010 FY09-Slurry 01ST AV THORN ST SPRUCE ST 5/7/2010 FY10-Overlay 01ST AV PENNSYLVANIA AV BROOKES AV 7/12/2010 FY10-Slurry 01ST AV LEWIS ST W WASHINGTON ST 1/9/2012 FY10-Slurry 01ST AV ARBOR DR MONTECITO WY 1/11/2012 FY10-Slurry 01ST AV MONTECITO WY LEWIS ST 1/11/2012 FY10-Slurry 01ST AV W WASHINGTON ST UNIVERSITY AV 1/11/2012 FY10-Slurry 01ST AV UNIVERSITY AV ROBINSON AV 1/11/2012 FY11-Slurry 01ST AV BEECH ST ASH ST 9/9/2012 FY11-Slurry 01ST AV ASH ST A ST 9/9/2012 FY11-Slurry 01ST AV A ST W B ST 9/9/2012 FY11-Slurry 01ST AV W B ST C ST 9/9/2012 FY11-Slurry 01ST AV ELM ST CEDAR ST 9/9/2012 FY11-Slurry 01ST AV CEDAR ST BEECH ST 9/9/2012 FY11-Overlay 01ST AV ROBINSON AV PENNSYLVANIA AV 10/10/2012 FY08-Overlay 02ND AV ASH ST A ST 4/10/2009 FY09-Overlay 02ND AV C ST BROADWAY 11/3/2009 FY09-Slurry 02ND AV WALNUT AV UPAS ST 5/26/2010 FY09-Slurry 02ND AV UPAS ST THORN ST 5/26/2010 FY09-Slurry 02ND AV THORN ST SPRUCE ST 5/26/2010 FY11-Overlay 02ND AV MARKET ST ISLAND AV 10/16/2012 FY11-Overlay 02ND AV ISLAND AV J ST 10/16/2012 FY09-Slurry 03RD AV LEWIS ST WASHINGTON ST 5/7/2010 FY09-Slurry 03RD AV END ARBOR DR 5/27/2010 FY09-Slurry 03RD AV ARBOR DR MONTECITO WY 5/28/2010 FY09-Slurry 03RD AV MONTECITO WY LEWIS ST 5/28/2010 FY10-Slurry 03RD AV WALNUT AV UPAS ST 1/11/2012 FY11-Slurry 03RD AV UNIVERSITY AV ROBINSON AV 6/5/2012 FY11-Slurry 03RD AV ROBINSON AV PENNSYLVANIA AV 6/5/2012 FY11-Slurry 03RD AV PENNSYLVANIA AV -
Research Paper in Nature
Draft version November 1, 2017 Typeset using LATEX twocolumn style in AASTeX61 DISCOVERY AND CHARACTERIZATION OF THE FIRST KNOWN INTERSTELLAR OBJECT Karen J. Meech,1 Robert Weryk,1 Marco Micheli,2, 3 Jan T. Kleyna,1 Olivier Hainaut,4 Robert Jedicke,1 Richard J. Wainscoat,1 Kenneth C. Chambers,1 Jacqueline V. Keane,1 Andreea Petric,1 Larry Denneau,1 Eugene Magnier,1 Mark E. Huber,1 Heather Flewelling,1 Chris Waters,1 Eva Schunova-Lilly,1 and Serge Chastel1 1Institute for Astronomy, 2680 Woodlawn Drive, Honolulu, HI 96822, USA 2ESA SSA-NEO Coordination Centre, Largo Galileo Galilei, 1, 00044 Frascati (RM), Italy 3INAF - Osservatorio Astronomico di Roma, Via Frascati, 33, 00040 Monte Porzio Catone (RM), Italy 4European Southern Observatory, Karl-Schwarzschild-Strasse 2, D-85748 Garching bei M¨unchen,Germany (Received November 1, 2017; Revised TBD, 2017; Accepted TBD, 2017) Submitted to Nature ABSTRACT Nature Letters have no abstracts. Keywords: asteroids: individual (A/2017 U1) | comets: interstellar Corresponding author: Karen J. Meech [email protected] 2 Meech et al. 1. SUMMARY 22 confirmed that this object is unique, with the highest 29 Until very recently, all ∼750 000 known aster- known hyperbolic eccentricity of 1:188 ± 0:016 . Data oids and comets originated in our own solar sys- obtained by our team and other researchers between Oc- tem. These small bodies are made of primor- tober 14{29 refined its orbital eccentricity to a level of dial material, and knowledge of their composi- precision that confirms the hyperbolic nature at ∼ 300σ. tion, size distribution, and orbital dynamics is Designated as A/2017 U1, this object is clearly from essential for understanding the origin and evo- outside our solar system (Figure2).