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PDF Files Are Openly Distributed for the Educational Purpose Only. Reuse And/Or Modifications of Figures and Tables in the PDF Files Are Not Allowed
PDF files are openly distributed for the educational purpose only. Reuse and/or modifications of figures and tables in the PDF files are not allowed. 3. Ancient landforms: Understanding the early Mars environment 3.1 Erosional landforms 3.1.1 Outflow channels 3.1.2 Valley networks 3.1.3 Erosional processes on early Mars 3.2 Standing bodies of water 3.2.1 Ocean and shorelines 3.2.2 Crater lakes and deltas 3.2.3 Layered deposits 3.3 Composition of sediments: from geomorphology to geology 3.3.1 MER rover discoveries 3.3.2 Exobiological issues 3.1.1 Outflow channels Length: 100 to 1000 km Width: 1 to 30 km Low gradient (<0.1) Anastomosing patterns, braided systems Teardrop-shaped islands Discharge rate :107 –109 m3 s-1 (Baker, 1981; Komar, 1986) 20 km Mangala valles 500 m Ares Valles Terrestrial floods: high discharge (here due to a storm) The Channeled Scabland analogy (Baker and Milton, 1974) ------- 40 km Columbia Basin (eastern Washington, USA) A glacial dam releases the subglacial lake Discharges of 2 x107 m3 s-1 Geographic distribution: Correlation with volcanic regions Role of geothermal activity Outflow channels (red) and valley networks (yellow) Elysium Mons Tharsis bulge From Carr, 1979 Relationship between chaotic terrains and outflow channels Chryse Planitia Kasei dfg Valles +Viking 1 + Pathfinder Ares Vallis Disruption of the permafrost at the source? Valles Marineris MOLA data Altitude (m) A recent outflow channel: Athabasca Vallis Outflow from fractures Very young: ~10 million years ago (Burr et al, 2002) (Berman and Hartmann, 2003) 6 km Origin of outflow channels 1 -Ground water under pressure confined within the permafrost (M. -
Introduction to Astronomy from Darkness to Blazing Glory
Introduction to Astronomy From Darkness to Blazing Glory Published by JAS Educational Publications Copyright Pending 2010 JAS Educational Publications All rights reserved. Including the right of reproduction in whole or in part in any form. Second Edition Author: Jeffrey Wright Scott Photographs and Diagrams: Credit NASA, Jet Propulsion Laboratory, USGS, NOAA, Aames Research Center JAS Educational Publications 2601 Oakdale Road, H2 P.O. Box 197 Modesto California 95355 1-888-586-6252 Website: http://.Introastro.com Printing by Minuteman Press, Berkley, California ISBN 978-0-9827200-0-4 1 Introduction to Astronomy From Darkness to Blazing Glory The moon Titan is in the forefront with the moon Tethys behind it. These are two of many of Saturn’s moons Credit: Cassini Imaging Team, ISS, JPL, ESA, NASA 2 Introduction to Astronomy Contents in Brief Chapter 1: Astronomy Basics: Pages 1 – 6 Workbook Pages 1 - 2 Chapter 2: Time: Pages 7 - 10 Workbook Pages 3 - 4 Chapter 3: Solar System Overview: Pages 11 - 14 Workbook Pages 5 - 8 Chapter 4: Our Sun: Pages 15 - 20 Workbook Pages 9 - 16 Chapter 5: The Terrestrial Planets: Page 21 - 39 Workbook Pages 17 - 36 Mercury: Pages 22 - 23 Venus: Pages 24 - 25 Earth: Pages 25 - 34 Mars: Pages 34 - 39 Chapter 6: Outer, Dwarf and Exoplanets Pages: 41-54 Workbook Pages 37 - 48 Jupiter: Pages 41 - 42 Saturn: Pages 42 - 44 Uranus: Pages 44 - 45 Neptune: Pages 45 - 46 Dwarf Planets, Plutoids and Exoplanets: Pages 47 -54 3 Chapter 7: The Moons: Pages: 55 - 66 Workbook Pages 49 - 56 Chapter 8: Rocks and Ice: -
Drainage Network Development in the Keanakāko'i
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 117, E08009, doi:10.1029/2012JE004074, 2012 Drainage network development in the Keanakāko‘i tephra, Kīlauea Volcano, Hawai‘i: Implications for fluvial erosion and valley network formation on early Mars Robert A. Craddock,1 Alan D. Howard,2 Rossman P. Irwin III,1 Stephen Tooth,3 Rebecca M. E. Williams,4 and Pao-Shin Chu5 Received 1 March 2012; revised 11 June 2012; accepted 4 July 2012; published 22 August 2012. [1] A number of studies have attempted to characterize Martian valley and channel networks. To date, however, little attention has been paid to the role of lithology, which could influence the rate of incision, morphology, and hydrology as well as the characteristics of transported materials. Here, we present an analysis of the physical and hydrologic characteristics of drainage networks (gullies and channels) that have incised the Keanakāko‘i tephra, a basaltic pyroclastic deposit that occurs mainly in the summit area of Kīlauea Volcano and in the adjoining Ka‘ū Desert, Hawai‘i. The Keanakāko‘i tephra is up to 10 m meters thick and largely devoid of vegetation, making it a good analog for the Martian surface. Although the scales are different, the Keanakāko‘i drainage networks suggest that several typical morphologic characteristics of Martian valley networks may be controlled by lithology in combination with ephemeral flood characteristics. Many gully headwalls and knickpoints within the drainage networks are amphitheater shaped, which results from strong-over-weak stratigraphy. Beds of fine ash, commonly bearing accretionary lapilli (pisolites), are more resistant to erosion than the interbedded, coarser weakly consolidated and friable tephra layers. -
A Collection of Curricula for the STARLAB Greek Mythology Cylinder
A Collection of Curricula for the STARLAB Greek Mythology Cylinder Including: A Look at the Greek Mythology Cylinder Three Activities: Constellation Creations, Create a Myth, I'm Getting Dizzy by Gary D. Kratzer ©2008 by Science First/STARLAB, 95 Botsford Place, Buffalo, NY 14216. www.starlab.com. All rights reserved. Curriculum Guide Contents A Look at the Greek Mythology Cylinder ...................3 Leo, the Lion .....................................................9 Introduction ......................................................3 Lepus, the Hare .................................................9 Andromeda ......................................................3 Libra, the Scales ................................................9 Aquarius ..........................................................3 Lyra, the Lyre ...................................................10 Aquila, the Eagle ..............................................3 Ophuichus, Serpent Holder ..............................10 Aries, the Ram ..................................................3 Orion, the Hunter ............................................10 Auriga .............................................................4 Pegasus, the Winged Horse..............................11 Bootes ..............................................................4 Perseus, the Champion .....................................11 Cancer, the Crab ..............................................4 Phoenix ..........................................................11 Canis Major, the Big Dog -
Kinematics of Antlia 2 and Crater 2 from the Southern Stellar Stream Spectroscopic Survey (S5)
Draft version September 23, 2021 Typeset using LATEX twocolumn style in AASTeX63 Kinematics of Antlia 2 and Crater 2 from The Southern Stellar Stream Spectroscopic Survey (S5) Alexander P. Ji ,1, 2, 3 Sergey E. Koposov ,4, 5, 6 Ting S. Li ,1, 7, 8, 9 Denis Erkal ,10 Andrew B. Pace ,11 Joshua D. Simon ,1 Vasily Belokurov ,5 Lara R. Cullinane ,12 Gary S. Da Costa ,12, 13 Kyler Kuehn ,14, 15 Geraint F. Lewis ,16 Dougal Mackey ,12 Nora Shipp ,2, 3 Jeffrey D. Simpson ,17, 13 Daniel B. Zucker ,18, 19 Terese T. Hansen 20, 21 And Joss Bland-Hawthorn 16, 13 (S5 Collaboration) 1Observatories of the Carnegie Institution for Science, 813 Santa Barbara St., Pasadena, CA 91101, USA 2Department of Astronomy & Astrophysics, University of Chicago, 5640 S Ellis Avenue, Chicago, IL 60637, USA 3Kavli Institute for Cosmological Physics, University of Chicago, Chicago, IL 60637, USA 4Institute for Astronomy, University of Edinburgh, Royal Observatory, Blackford Hill, Edinburgh EH9 3HJ, UK 5Institute of Astronomy, University of Cambridge, Madingley Road, Cambridge CB3 0HA, UK 6Kavli Institute for Cosmology, University of Cambridge, Madingley Road, Cambridge CB3 0HA, UK 7Department of Astrophysical Sciences, Princeton University, Princeton, NJ 08544, USA 8Department of Astronomy and Astrophysics, University of Toronto, 50 St. George Street, Toronto ON, M5S 3H4, Canada 9NHFP Einstein Fellow 10Department of Physics, University of Surrey, Guildford GU2 7XH, UK 11McWilliams Center for Cosmology, Carnegie Mellon University, 5000 Forbes Ave, Pittsburgh, PA 15213, -
Mars-Match-Slides.Pdf
MA RS Clouds A B Clouds A Eastern 2/3 of the U.S. Clouds Clouds on Mars are made of _____ . A. water B. carbon dioxide C. water and carbon dioxide Clouds on Mars are made of _____ . A. water B. carbon dioxide C. water and carbon dioxide Ice cap, Antarctica A B Ice cap, Antarctica Sout A h Nort B h Ice cap, Antarctica The northern ice cap on Mars consists of frozen _____ . A. water B. carbon dioxide C. water and carbon dioxide The northern ice cap on Mars consists of frozen _____ . A. water B. carbon dioxide C. water and carbon dioxide Dust storm A B Dust storm A Sahara dust storm Polar dust storm True or False? Dust storms on Mars can cover the entire planet. True! Dust storms on Mars can cover the entire planet. 2018 Dust Devil A B Dust Devil A Seen from the ground by the Opportunity rover B Dust Devil Seen from above by the Mars Reconnaissance Orbiter Barchan dunes, Mawrth Valles A B Barchan dunes, Mawrth Valles A Sahara Desert Barchan dunes, Mawrth Valles Aorounga impact crater, Chad A B Aorounga impact crater, Chad B Lowell Crater Aorounga impact crater, Chad River Delta, Jezero Crater A B River Delta, Jezero Crater B Horton River Delta, Canada River Delta, Jezero Crater What is the name of the rover that will land in Jezero crater in 2021? A. Perseverance B. Curiosity C. Spirit What is the name of the rover that will land in Jezero crater in 2021? A. Perseverance B. -
Glossary of Lunar Terminology
Glossary of Lunar Terminology albedo A measure of the reflectivity of the Moon's gabbro A coarse crystalline rock, often found in the visible surface. The Moon's albedo averages 0.07, which lunar highlands, containing plagioclase and pyroxene. means that its surface reflects, on average, 7% of the Anorthositic gabbros contain 65-78% calcium feldspar. light falling on it. gardening The process by which the Moon's surface is anorthosite A coarse-grained rock, largely composed of mixed with deeper layers, mainly as a result of meteor calcium feldspar, common on the Moon. itic bombardment. basalt A type of fine-grained volcanic rock containing ghost crater (ruined crater) The faint outline that remains the minerals pyroxene and plagioclase (calcium of a lunar crater that has been largely erased by some feldspar). Mare basalts are rich in iron and titanium, later action, usually lava flooding. while highland basalts are high in aluminum. glacis A gently sloping bank; an old term for the outer breccia A rock composed of a matrix oflarger, angular slope of a crater's walls. stony fragments and a finer, binding component. graben A sunken area between faults. caldera A type of volcanic crater formed primarily by a highlands The Moon's lighter-colored regions, which sinking of its floor rather than by the ejection of lava. are higher than their surroundings and thus not central peak A mountainous landform at or near the covered by dark lavas. Most highland features are the center of certain lunar craters, possibly formed by an rims or central peaks of impact sites. -
Snake in the Clouds: a New Nearby Dwarf Galaxy in the Magellanic Bridge ∗ Sergey E
MNRAS 000, 1{21 (2018) Preprint 19 April 2018 Compiled using MNRAS LATEX style file v3.0 Snake in the Clouds: A new nearby dwarf galaxy in the Magellanic bridge ∗ Sergey E. Koposov,1;2 Matthew G. Walker,1 Vasily Belokurov,2;3 Andrew R. Casey,4;5 Alex Geringer-Sameth,y6 Dougal Mackey,7 Gary Da Costa,7 Denis Erkal8, Prashin Jethwa9, Mario Mateo,10, Edward W. Olszewski11 and John I. Bailey III12 1McWilliams Center for Cosmology, Carnegie Mellon University, 5000 Forbes Ave, 15213, USA 2Institute of Astronomy, University of Cambridge, Madingley road, CB3 0HA, UK 3Center for Computational Astrophysics, Flatiron Institute, 162 5th Avenue, New York, NY 10010, USA 4School of Physics and Astronomy, Monash University, Clayton 3800, Victoria, Australia 5Faculty of Information Technology, Monash University, Clayton 3800, Victoria, Australia 6Astrophysics Group, Physics Department, Imperial College London, Prince Consort Rd, London SW7 2AZ, UK 7Research School of Astronomy and Astrophysics, Australian National University, Canberra, ACT 2611, Australia 8Department of Physics, University of Surrey, Guildford, GU2 7XH, UK 9European Southern Observatory, Karl-Schwarzschild-Str. 2, 85748 Garching, Germany 10Department of Astronomy, University of Michigan, 311 West Hall, 1085 S University Avenue, Ann Arbor, MI 48109, USA 11Steward Observatory, The University of Arizona, 933 N. Cherry Avenue., Tucson, AZ 85721, USA 12Leiden Observatory, Leiden University, Niels Bohrweg 2, 2333 CA Leiden, The Netherlands Accepted XXX. Received YYY; in original form ZZZ ABSTRACT We report the discovery of a nearby dwarf galaxy in the constellation of Hydrus, between the Large and the Small Magellanic Clouds. Hydrus 1 is a mildy elliptical ultra-faint system with luminosity MV 4:7 and size 50 pc, located 28 kpc from the Sun and 24 kpc from the LMC. -
Constraints on Overland Fluid Transport Through Martian Valley Networks. M
Lunar and Planetary Science XXXI 1189.pdf CONSTRAINTS ON OVERLAND FLUID TRANSPORT THROUGH MARTIAN VALLEY NETWORKS. M. C. Malin and K. S. Edgett, Malin Space Science Systems, Box 910148, San Diego, CA 92191-0148, USA. Introduction: Since their discovery in Mariner 9 networks. images [1,2], Òrunoff channelsÓ [3], or more properly, Flow Integration: Arguably the best example Òmartian valley networksÓ [4,5] have been almost uni- found on Mars of an arborescent network are the War- versally cited as the best evidence that Mars once rego Valles. Earlier Viking data, and now MGS im- maintained an environment capable of supporting the ages, raise serious questions concerning the interpreta- flow of liquid water across its surface. Unlike Òoutflow tion of these valleys as surficial drainage. First, the channels,Ó that appear to indicate brief, catastrophic valleys are not Òthrough-going,Ó but rather consist of releases of fluid from very localized sources, valley transecting, elongate, occasionally isolated depres- networks often display arborescent patterns, sinuosity sions. Second, mass movements appear to have played and occasionally meandering patterns that imply proc- a role in both extending and widening the valleys. esses of overland flow: drainage basin development Third, the valley walls are extremely subdued, reflect- and sustained surficial transport of fluid. As part of the ing either mantling or an origin by collapse. These on-going Mars Global Surveyor (MGS) Mars Orbiter attributes suggest that collapse may have played the Camera (MOC) imaging activities, many observations dominant role in formation of valley networks of valley networks have been planned and executed; the Discussion: Groundwater follows topographic gra- results of some of these observations have been previ- dients nearly as effectively as surface water. -
Valley Formation on Early Mars by Subglacial and Fluvial Erosion
ARTICLES https://doi.org/10.1038/s41561-020-0618-x Valley formation on early Mars by subglacial and fluvial erosion Anna Grau Galofre! !1,2 ✉ , A. Mark Jellinek1 and Gordon R. Osinski! !3,4 The southern highlands of Mars are dissected by hundreds of valley networks, which are evidence that water once sculpted the surface. Characterizing the mechanisms of valley incision may constrain early Mars climate and the search for ancient life. Previous interpretations of the geological record require precipitation and surface water runoff to form the valley networks, in contradiction with climate simulations that predict a cold, icy ancient Mars. Here we present a global comparative study of val- ley network morphometry, using a principal-component-based analysis with physical models of fluvial, groundwater sapping and glacial and subglacial erosion. We found that valley formation involved all these processes, but that subglacial and fluvial erosion are the predominant mechanisms. This is supported by predictions from models of steady-state erosion and geomor- phological comparisons to terrestrial analogues. The inference of subglacial channels among the valley networks supports the presence of ice sheets that covered the southern highlands during the time of valley network emplacement. alley networks are ancient (3.9–3.5 billion years ago (Ga)) angle between tributaries and main stem (γ), (2) streamline fractal 1–4 systems of tributaries with widely varying morphologies dimension (Df), (3) maximum network stream order (Sn), (4) width Vpredominately incised on the southern hemisphere high- of first-order tributaries (λ), (5) length-to-width aspect ratio (R) lands of Mars (Fig. 1). -
Statistika 2018
NASLOV + AVTOR (SKUPINE) + DRŽAVA DATUM IN URA DEJAVNOST / ZVRSTPRODUKCIJATIP PROGRAMA PREDPRODAJNADVORANA CENACENA ( €NA) DAN (€OBISK) KULTURNI(n) EVRO (n)ZASEDENOST (%)ŠT. STATUS GOSTOVANJE UROŠ WEINBERGER: Die Drohnen (SLO) 8.1.2018 ob 20:00 razstava P SP Kamera prost vstop prost vstop 1022 / / Otvoritev 35+16+11+7+548+189+111+105JZ UMETNICA NA MESEC | ANJA JELOVŠEK: Air-lines (SLO) 11.1.2018 ob 18:00 pogovor + razstava P SP DobraVaga prost vstop prost vstop 95 / / JZ ŠPIL LIGA: 3. tekmovalni večer (SLO) 12.1.2018 ob 20:00 koncert: rock P OP Komuna prost vstop prost vstop 80 / 40,0 80/200 JZ DON'T BREAK DOWN: Film o Jawbreaker - premiera 13.1.2018 ob 19:00 film KP SP Katedrala 5 5 26 / 52,0 26/50 NVO REAL LIFE VERSION (SLO) 13.1.2018 ob 21:00 koncert: rock KP OP Komuna 5 5 56 / 93,0 56/60 NVO IMPRONEDELJEK (SLO) 15.1.2018 ob 20:00 improsešn P OP Kavarna Kino Šiška prost vstop prost vstop 35 / 116,7 35/30 JZ KREATOR + VADER + Dagoba (GER, FR) 18.1.2018 ob 20:00 koncert: metal ZP OP Katedrala 28 32 750 33 84,0 783/932 GO MANCA UDOVIČ ft. NINA KRALJIĆ: Romanca (SLO/HR) 19.1.2018 ob 20:00 koncert: jazz, pop P OP Katedrala 10 12 260 10 90,0 270/300 JZ ZINE VITRINE | JURE ŠAJN: Picking up lines (SLO) 23.1.2018 ob 19:00 razstava P SP DobraVaga prost vstop prost vstop 65 / / JZ BURDEN (2016) - premiera 23.1.2018 ob 20:00 film KP SP Katedrala 3 5 89 70 72,3 159/220 NVO BOBRI | Svetlana Makarovič, Jure Novak: PASJA PROCESIJA (SLO) 24.1.2018 ob 11:00 koncertna urpizoritev za šole KP OP Slovensko mladinsko gledališče 120 JZ izven šiške APPOINTMENT -
The Mars Global Surveyor Mars Orbiter Camera: Interplanetary Cruise Through Primary Mission
p. 1 The Mars Global Surveyor Mars Orbiter Camera: Interplanetary Cruise through Primary Mission Michael C. Malin and Kenneth S. Edgett Malin Space Science Systems P.O. Box 910148 San Diego CA 92130-0148 (note to JGR: please do not publish e-mail addresses) ABSTRACT More than three years of high resolution (1.5 to 20 m/pixel) photographic observations of the surface of Mars have dramatically changed our view of that planet. Among the most important observations and interpretations derived therefrom are that much of Mars, at least to depths of several kilometers, is layered; that substantial portions of the planet have experienced burial and subsequent exhumation; that layered and massive units, many kilometers thick, appear to reflect an ancient period of large- scale erosion and deposition within what are now the ancient heavily cratered regions of Mars; and that processes previously unsuspected, including gully-forming fluid action and burial and exhumation of large tracts of land, have operated within near- contemporary times. These and many other attributes of the planet argue for a complex geology and complicated history. INTRODUCTION Successive improvements in image quality or resolution are often accompanied by new and important insights into planetary geology that would not otherwise be attained. From the variety of landforms and processes observed from previous missions to the planet Mars, it has long been anticipated that understanding of Mars would greatly benefit from increases in image spatial resolution. p. 2 The Mars Observer Camera (MOC) was initially selected for flight aboard the Mars Observer (MO) spacecraft [Malin et al., 1991, 1992].