A Combined Topographic-Thematic Map of the Centauri and Hellas Montes Area, Mars
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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. -
Geologic Maps of Washington
GEOLOGIC MAPS OF WASHINGTON DGER GM-53 124° 117° 123° 122° 121° 120° CANADA 119° 118° 49° 49° WASHINGTON STATE PEND DGER OFR 2000-5 WHATCOM DGER OFR 90-5 USA FERRY (scale 1:500,000) OREILLE Roche Mount Bellingham Robinson Oroville Republic Colville Harbor Baker Mtn 125° OKANOGAN DGER OFR 2003-17 48°30 USGS Map I-2660 DGER OFR 90-10 DGER OFR 90-13 48°30 CANADA DGER OFR 90-11 SAN USA Port JUAN SKAGIT DGER DGER OFR 90-12 ISLAND OFR 90-9 Cape Angeles Port Sauk Nespelem Chewelah Flattery Townsend River Twisp Omak USGS Map I-1198F DGER OFR 2003-5 DGER OFR 2003-6 DGER DGER OFR 90-14 48° USGS Map I-1198G USGS Map I -2592 OFR 95-3 DGER OFR 90-16 48° CLALLAM USGS OFR 93-233 STEVENS IDAHO SNOHOMISH DOUGLAS JEFFERSON USGS OFR 91-147 CHELAN Mount Coulee Forks Seattle Skykomish Banks Spokane Olympus River Chelan Lake Dam DGER OFR 2000-4 DGER OFR 2003-4 DGER OFR 90-17 47°30 KITSAP USGS Map I-1963 USGS Map I-1661 DGER OFR 90-6 DGER OFR 90-15 47°30 GRAYS GIS data only KING LINCOLN SPOKANE Copalis HARBOR GRANT Snoqualmie Moses Beach Shelton Tacoma Wenatchee Ritzville Rosalia MASON Pass Lake DGER OFR 2003-16 KITTITAS DGER OFR 2003-15 47° DGER OFR 87-3 USGS Map I-2538 USGS Map I-1311 DGER OFR 90-1 DGER OFR 90-2 DGER OFR 90-7 47° WHITMAN PIERCE ADAMS THURSTON Westport Chehalis Mount Priest Pullman River Centralia Yakima Connell LEWIS Rainier Rapids FRANKLIN DGER DGER OFR 87-8 DGER OFR 87-8 DGER 46°30 DGER OFR 87-11 DGER OFR 87-16 OFR 86-4 OFR 94-12 DGER OFR 94-13 DGER OFR 94-14 DGER OFR 94-6 46°30 PACIFIC GARFIELD YAKIMA DGER COLUMBIA OFR 86-3 BENTON Ilwaco WAHKIAKUM Mount Clarkston Mount Richland Walla Walla Astoria St. -
DATING the RESURFACING EVENTS of the HARMAKHIS VALLIS SOURCE REGIONS, MARS: PRELIMINARY RESULTS. S. Kukkonen and V.-P
44th Lunar and Planetary Science Conference (2013) 2140.pdf DATING THE RESURFACING EVENTS OF THE HARMAKHIS VALLIS SOURCE REGIONS, MARS: PRELIMINARY RESULTS. S. Kukkonen and V.-P. Kostama, Astronomy, Department of Physics, P.O. Box 3000, FI-90014 University of Oulu, Finland ([email protected]). Introduction: Harmakhis Vallis is one of the four [e.g., 15–17]. Usually they have been excluded from major outflow channel systems that cut the eastern Hel- the crater counts because of the uncertainty of their las rim region of Mars (Fig. 1). It is ~800 km long and origin (primary vs. secondary crater). However, small located ~450 km south of Hadriaca Patera starting craters accumulate to the surface more quickly than close to the end of another valley, Reull Vallis. Due to larger ones, and thus the high spatial resolution is nec- the close position to the volcanic features, the channels essary in dating younger surfaces or small units where are suggested to have been formed by the mobilization there are only few large craters. In the case of Harma- and release of subsurface volatiles by volcanic heat [1– khis Vallis, the region has experienced significant re- 5]. Because Harmakhis Vallis cuts the surrounding cent modification and degradation, and thus, we can massifs of the cratered terrains, it is clearly one of the assume that the small crater population mostly post- youngest features in the region [6, 7]. dates the secondary craters forming larger impacts lo- cated in the older regions. Therefore, only the obvious clusters of secondary craters were excluded from the counts. -
Cartography. the Definitive Guide to Making Maps, Sample Chapter
Cartograms Cartograms offer a way of accounting for differences in population distribution by modifying the geography. Geography can easily get in the way of making a good Consider the United States map in which thematic map. The advantage of a geographic map is that it states with larger populations will inevitably lead to larger numbers for most population- gives us the greatest recognition of shapes we’re familiar with related variables. but the disadvantage is that the geographic size of the areas has no correlation to the quantitative data shown. The intent However, the more populous states are not of most thematic maps is to provide the reader with a map necessarily the largest states in area, and from which comparisons can be made and so geography is so a map that shows population data in the almost always inappropriate. This fact alone creates problems geographical sense inevitably skews our perception of the distribution of that data for perception and cognition. Accounting for these problems because the geography becomes dominant. might be addressed in many ways such as manipulating the We end up with a misleading map because data itself. Alternatively, instead of changing the data and densely populated states are relatively small maintaining the geography, you can retain the data values but and vice versa. Cartograms will always give modify the geography to create a cartogram. the map reader the correct proportion of the mapped data variable precisely because it modifies the geography to account for the There are four general types of cartogram. They each problem. distort geographical space and account for the disparities caused by unequal distribution of the population among The term cartogramme can be traced to the areas of different sizes. -
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, -
Application of Geologic Mapping and Geographic Information Systems To
APPLICATION OF GEOLOGIC MAPPING AND GEOGRAPHIC INFORMATION SYSTEMS TO DELINEATE SENSITIVE KARST AREAS FOR LAND-USE DECISIONS Jim Cichon, Alex Wood, Alan Baker and Jon Arthur Florida Geological Survey, Hydrogeology Program The Problem: The Floridan aquifer system (FAS), a thick sequence of Tertiary carbonates, is the major fresh water resource in the Florida panhandle. The expanding population of the State places an ever-growing demand on the fresh-water resources through increased land and water use. Overburden comprised of surficial aquifer sediments or intermediate confining unit (ICU) sediments may act to protect the FAS from potential contamination sources where it is present. This overburden can be several hundred feet thick where it provides variable confinement for the FAS, or it can be thin to absent in areas where carbonate units comprising the FAS are exposed at or near land surface. In areas where the overburden is thin to absent, the potential for karst terrain development is increased. Sinkholes and collapse features are more common and occur at a much Figure 1: Generalized geologic map of northwestern Florida (modified from Scott, et al. 2001). greater rate than in well-confined areas. The nature of karst terrain provides preferential flow paths for surface water to enter the underlying aquifer system, and therefore aquifer systems underlying karst terrain are at a greater risk to surface contamination potential. The Geologic Map: In Florida, areas of karst topography are associated with, but not limited to shallow and exposed carbonate rocks. The state geologic map of Florida and associated cross-sections provide this detailed lithologic information (Scott, et al, 2001). -
Chapter 1. Map Study and Interpretation
Chapter 1. Map Study and Interpretation 1.1. Maps A map is a visual representation of an area—a symbolic depiction highlighting relationships between elements of that space such as objects, regions, and themes. Many maps are static two-dimensional, geometrically accurate (or approximately accurate) representations of three-dimensional space, while others are dynamic or interactive, even three-dimensional. Although most commonly used to depict geography, maps may represent any space, real or imagined, without regard to context or scale; e.g. brain mapping, DNA mapping, and extraterrestrial mapping. 1.2. Types of Maps Maps are one of the most important tools researchers, cartographers, students and others can use to examine the entire Earth or a specific part of it. Simply defined maps are pictures of the Earth's surface. They can be general reference and show landforms, political boundaries, water, the locations of cities, or in the case of thematic maps, show different but very specific topics such as the average rainfall distribution for an area or the distribution of a certain disease throughout a county. Today with the increased use of GIS, also known as Geographic Information Systems, thematic maps are growing in importance. A map is a visual representation of an area – a symbolic depiction highlighting relationships between elements of that space such as objects, regions, and themes. There are however applications for different types of general reference maps when the different types are understood correctly. These maps do not just show a city's location for example; instead the different map types can show a plethora of information about places around the world. -
Investigating Adolescents' Interpretations And
INVESTIGATING ADOLESCENTS’ INTERPRETATIONS AND PRODUCTIONS OF THEMATIC MAPS AND MAP ARGUMENT PERFORMANCES IN THE MEDIA By Nathan Charles Phillips Dissertation Submitted to the Faculty of the Graduate School of Vanderbilt University in partial fulfillment of the requirements for the degree of DOCTOR OF PHILOSOPHY in Learning, Teaching and Diversity December, 2013 Nashville, Tennessee Approved: Professor Kevin M. Leander Professor Rogers Hall Professor Pratim Sengupta Professor Jay Clayton Professor Cynthia Lewis To Julee and To Jenna, Amber, Lukas, Isaac, and Esther ! ii ACKNOWLEDGEMENTS My dissertation work was financially supported by the National Science Foundation through the Tangibility for the Teaching, Learning, and Communicating of Mathematics grant (NSF DRL-0816406) and by Peabody College at Vanderbilt University and the Department of Teaching and Learning. I feel most grateful to the young people I worked with. I hope I have done justice to their efforts to learn, laugh, and play with thematic maps. Mr. Norman welcomed me into his classroom and graciously gave me the space and time for this work. He was interested, supportive, and generous throughout. The district and school administrators and office staff at Local County High School were welcoming and accommodating, including the librarians who made some of the technology possible. It would be impossible to express how much my life and scholarship have been directed and supported by Kevin Leander and Rogers Hall over the last six years. Their brilliance, innovative thinking, and academic mentorship are only surpassed by their kind hearts and good friendship. I will forever be blessed by Kevin’s willingness to take me on as a doctoral student and for his invitation to join the SLaMily with Rogers, Katie Headrick Taylor, and Jasmine Ma. -
Evolution of Mars As a Planet, Possible Life on Mars
EVOLUTION OF MARS LECTURE 18 NEEP 533 HARRISON H. SCHMITT NASA HST IMAGE N THARSIS HELLAS S ANDESITE OR WEATHERED SOIL DUST DUST DUST BASALT ~100 KM A C B THEMIS THERMAL IMAGING OF SPIRIT LANDING AREA IN GUSEV CRATER A. SPIRIT LANDING ELLIPSE B. CLOSER VIEW OF SPIRIT LANDING ELLIPSE C. NIGHT IR IMAGE: BRIGHT AREAS ARE MORE ROCKY. ARROW POINTS TO ROCKY SLOPE SPIRIT MOVED TO GUSEV CRATER POSSIBLE LAKE BED IN LARGE BASIN A C B THEMIS THERMAL IMAGING OF OPPORTUNITYLANDING AREA IN MERIDIANI PLANUM A. LANDING ELLIPSE ~120 KM LONG) B. CLOSER VIEW OF LANDING ELLIPSE C. NIGHT IR IMAGE: BRIGHT AREAS ARE MORE ROCKY. ARROW POINTS TO ROCKY SLOPE MAJOR STAGES OF MARS’ EVOLUTION 1 BEGINNING 2 MAGMA OCEAN / CONVECTIVE OVERTURN 3A ? ? CRATERED UPLANDS / VERY LARGE BASINS 3B ? CORE FORMATION/GLOBAL MAGNETIC FIELD 3C 4.5 - 1.3 GLOBAL MAFIC VOLCANISM DENSE WATER / CO2 ATMOSPHERE E ? G 3D EROSION / LAKES / NORTHERN OCEAN A T ? ? S 4 LARGE BASINS CATACLYSM ? THARSIS UPLIFT AND VOLCANISM ? 5 NORTHERN HEMISPHERE BASALTIC / ANDESITIC VOLCANISM ? 1.3 - 0.2 SUBSURFACE HYDROSPHERE / CRYOSPHERE 6 ? PRESENT SURFACE CONDITIONS LUNAR 4.6 4.2? 3.8 ? 5.0 4.0 3.0 2.0 1.0 BILLIONS OF YEARS BEFORE PRESENT ITALICS = SNC DATES RED = MAJOR UNCERTAINTY OLYMPUS TOPOGRAPHY OF MONS THARSIS REGION VALLES MARINERIS THARSIS REGION SHADED RELIEF DETAIL MARS GLOBAL SURVEYOR MOLA OLYMPUS MONS VALLES MARINERIS APOLLO MODEL OF MARS EVOLUTION ELYSIUM MONS ANDESITIC THARSIS EVENTS EXTRUSIONS <3.8 B.Y. THARSIS THICKENING ATMOSPHERE: MAFIC UPPER MANTLE WITH CO2, H20 CRYOSPHERE / INCREASING HYDROSPHERE SI AND FE UPWARDS OLIVINE/ NA- PYROXENE ? ANDESITIC CUMULATE INTRUSIONS? OLIVINE ? CUMULATE RELIC PROTO- GARNET / NA-CPX/ CORE ? NA-BIOTITE?/NA- HORNBLENDE/ ? FExNIySz “RUTILE” (TRANSITION? CORE CUMULATES ? ZONE) RELIC MAGNETIC STRIPING THICKENED SOUTHERN ©Harrison H. -
Heat Maps: Perfect Maps for Quick Reading? Comparing Usability of Heat Maps with Different Levels of Generalization
International Journal of Geo-Information Article Heat Maps: Perfect Maps for Quick Reading? Comparing Usability of Heat Maps with Different Levels of Generalization Katarzyna Słomska-Przech * , Tomasz Panecki and Wojciech Pokojski Department of Geoinformatics, Cartography and Remote Sensing, Faculty of Geography and Regional Studies, University of Warsaw, Krakowskie Przedmiescie 30, 00-927 Warsaw, Poland; [email protected] (T.P.); [email protected] (W.P.) * Correspondence: [email protected] Abstract: Recently, due to Web 2.0 and neocartography, heat maps have become a popular map type for quick reading. Heat maps are graphical representations of geographic data density in the form of raster maps, elaborated by applying kernel density estimation with a given radius on point- or linear-input data. The aim of this study was to compare the usability of heat maps with different levels of generalization (defined by radii of 10, 20, 30, and 40 pixels) for basic map user tasks. A user study with 412 participants (16–20 years old, high school students) was carried out in order to compare heat maps that showed the same input data. The study was conducted in schools during geography or IT lessons. Objective (the correctness of the answer, response times) and subjective (response time self-assessment, task difficulty, preferences) metrics were measured. The results show that the smaller radius resulted in the higher correctness of the answers. A larger radius did not result in faster response times. The participants perceived the more generalized maps as easier to use, although this result did not match the performance metrics. -
Dating the Resurfacing Event of Morpheos Basin (Upper Reull Vallis), Mars: Implications for the Extent of the Basin
EPSC Abstracts Vol. 6, EPSC-DPS2011-1555, 2011 EPSC-DPS Joint Meeting 2011 c Author(s) 2011 Dating the resurfacing event of Morpheos basin (upper Reull Vallis), Mars: Implications for the extent of the basin V.-P. Kostama , S. Kukkonen and J. Raitala Astronomy, Dept. of Physics, University of Oulu, P.O. Box 3000, FIN-90014, Oulu, Finland ([email protected] ) 1. Introduction Morpheos basin question was also addressed when a volumetric re-analysis of the Reull Vallis fluvial The eastern rim of Hellas basin has several large system was completed with the MOLA DEM and channel features which are characteristic to this GRIDVIEW [5]. In this study, Capitoli [5] region. One of these, Reull Vallis, has been studied determined that the previously proposed level of in great detail by earlier works [i.e. 1, 2]. However, filling of the Morpheos basin at 600-650 m [2] was the new data from Mars Express (HRSC) and MRO too high due to the limit of the volume of the (CTX and HiRISE) gives a possibility to still add Segment 1. We agree, as the proposed level in our more details to the general view of the evolution of earlier work was in fact thought to be the absolute the larger Reull fluvial system. We were able to find maximum of possible filling. However, Capitoli and new age constraints for the upper parts of this system Mest [6] proposed that if multiple pulses of water through crater size-frequency distributions using the from Segment 1 were released, a level of 550 m at available images of CTX, HiRISE and HRSC and the Morpheos basin could still be reached. -
Observations on USGS-State Cooperative Mapping
DR.WALLACE W. HACAN Director Kentucky Geological Survey (Ret.) Observations on USGS-State Cooperative Mapping HE DICTIONARY defines the word cooper- selective based on immediate needs of our T ate to mean: to work together willingly country. A state may attract the uscs to map for a common purpose. Thus, when The in it, or accelerate mapping in progress, by United States Geological Survey and a state entrance into a cooperative program. This agency enter into a cooperative agreement, also reduces the cost to the federal govern- they have definite objectives which involve ment, and produces a base map sooner, and both state and federal agencies. The signed consequently enhances economic develop- agreements are quite simple and indicate ment in the State. the nature of the funding, who performs the Fourteen states now have complete 7.5 operations, who owns the original materials, minute topographic map coverage on a the mutual considerations, and the publica- 1:24,000 scale, most of which was done in tion of the results. cooperative programs. Last year in FY 1978, There are several types of cooperative 38 states and Puerto Rico contributed $3.5 programs: million toward the National Mapping Pro- The uses furnishes the personnel, super- -gram, .- primarily for new 7.5 minute topo- vises personnel and operations, in field graphic mapping. Some states' cooperative and ofice, reviews, approves, does cartog- mapping agreements included: raphy, and publishes. Plans and priorities are formulated mutually, and funds are High-altitude aerial photography, photo- matched. inspection, and photorevision of published 7.5 minute maps in the states of Indiana, This is the same, except by agreement the state furnishes some of the personnel and Kansas, Pennsylvania, Ohio, and Virginia.