Horizon-Vol 21-No 03
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New Chryse and the Provinces
New Chryse and the Provinces The city of New Chryse is actually several connected cities. The Upper City is located on a break in the crater rim, looking down past a steep rock to the Lower City. Inside the da Vinci crater rim lies the Inner City, also known as the Old City – Red Era tunnels and cave shelters, as well as several nanocomposite towers and cupolas on Mona Lys Ridge looking down on the lower parts of the city. The Lower city lies in a valley sloping down to the Harbour City, which fills a crater 20 kilometres to the East. The Harbour City crater is connected to Camiling Bay and the sea through two canyons and is very well protected from both wind and ice. South of the Lower City and Harbour City lies The Slopes, a straight slope into the sea that is covered with sprawl and slums. Mona Lys Ridge is a mixture of palatial estates surrounded by gardens, imposing official imperial buildings and towering ancient structures used by the highest ranks of the Empire. The central imperial administration and especially the Council is housed in the Deimos Needle, a diamondoid tower that together with its sibling the Phobos Needle dominate the skyline. Escalators allow swift and discreet transport down to the lower levels of the city, and can easily be defended by the police force. North of Mona Lys lies a secluded garden city for higher administrators, guild officials and lesser nobility. The Inner City is to a large extent part of Mona Lys, although most of the inhabitants of Mona Lys do not care much for the dusty old tunnels and hidden vaults – that is left to the Guild of Antiquarians who maintain and protect it. -
Observations of the Marker Bed at Gale Crater with Recommendations for Future Exploration by the Curiosity Rover
52nd Lunar and Planetary Science Conference 2021 (LPI Contrib. No. 2548) 1484.pdf OBSERVATIONS OF THE MARKER BED AT GALE CRATER WITH RECOMMENDATIONS FOR FUTURE EXPLORATION BY THE CURIOSITY ROVER. C. M. Weitz1, J. L. Bishop2, B. J. Thomson3, K. D. Seelos4, K. Lewis5, I. Ettenborough3, and R. E. Arvidson6. 1Planetary Science Institute, 1700 East Fort Lowell, Tuc- son, AZ ([email protected]); 2SETI Institute, Carl Sagan Center, Mountain View, CA; 3Dept. of Earth and Planetary Sciences, Univ. Tennessee, Knoxville, TN; 4Planetary Exploration Group, JHU Applied Physics Laboratory, Laurel, MD; 5Dept Earth and Planetary Sciences, John Hopkins University, Baltimore, MD; 6Dept Earth and Planetary Sci- ences, Washington University, St. Louis, Missouri. Introduction: A dark-toned marker bed is ob- pearance across the mound. Most of the sulfates served within the sulfates at Gale crater [1,2]. This above/below the marker bed are stratified, heavily marker bed is characterized by a dark-toned, smooth fractured, and erode into boulder-size blocks, but there surface that appears more indurated and retains more are examples where the sulfates appear massive with craters relative to the sulfate-bearing layers above and limited fracturing and no boulders eroding from the below it. The bed has a distinct physical appearance unit (Fig. 3a). from the sulfates in which it occurs, suggesting a change in the environment or geochemistry for a brief period of time within the depositional sequence that formed the sulfates or post-deposition alteration. In this study, we utilized HiRISE and CTX images to identify and map the occurrence of the marker bed throughout Aeolis Mons. -
Pacing Early Mars Fluvial Activity at Aeolis Dorsa: Implications for Mars
1 Pacing Early Mars fluvial activity at Aeolis Dorsa: Implications for Mars 2 Science Laboratory observations at Gale Crater and Aeolis Mons 3 4 Edwin S. Kitea ([email protected]), Antoine Lucasa, Caleb I. Fassettb 5 a Caltech, Division of Geological and Planetary Sciences, Pasadena, CA 91125 6 b Mount Holyoke College, Department of Astronomy, South Hadley, MA 01075 7 8 Abstract: The impactor flux early in Mars history was much higher than today, so sedimentary 9 sequences include many buried craters. In combination with models for the impactor flux, 10 observations of the number of buried craters can constrain sedimentation rates. Using the 11 frequency of crater-river interactions, we find net sedimentation rate ≲20-300 μm/yr at Aeolis 12 Dorsa. This sets a lower bound of 1-15 Myr on the total interval spanned by fluvial activity 13 around the Noachian-Hesperian transition. We predict that Gale Crater’s mound (Aeolis Mons) 14 took at least 10-100 Myr to accumulate, which is testable by the Mars Science Laboratory. 15 16 1. Introduction. 17 On Mars, many craters are embedded within sedimentary sequences, leading to the 18 recognition that the planet’s geological history is recorded in “cratered volumes”, rather than 19 just cratered surfaces (Edgett and Malin, 2002). For a given impact flux, the density of craters 20 interbedded within a geologic unit is inversely proportional to the deposition rate of that 21 geologic unit (Smith et al. 2008). To use embedded-crater statistics to constrain deposition 22 rate, it is necessary to distinguish the population of interbedded craters from a (usually much 23 more numerous) population of craters formed during and after exhumation. -
Geophysical and Remote Sensing Study of Terrestrial Planets
GEOPHYSICAL AND REMOTE SENSING STUDY OF TERRESTRIAL PLANETS A Dissertation Presented to The Academic Faculty By Lujendra Ojha In Partial Fulfillment Of the Requirements for the Degree Doctor of Philosophy in Earth and Atmospheric Sciences Georgia Institute of Technology August, 2016 COPYRIGHT © 2016 BY LUJENDRA OJHA GEOPHYSICAL AND REMOTE SENSING STUDY OF TERRESTRIAL PLANETS Approved by: Dr. James Wray, Advisor Dr. Ken Ferrier School of Earth and Atmospheric School of Earth and Atmospheric Sciences Sciences Georgia Institute of Technology Georgia Institute of Technology Dr. Joseph Dufek Dr. Suzanne Smrekar School of Earth and Atmospheric Jet Propulsion laboratory Sciences California Institute of Technology Georgia Institute of Technology Dr. Britney Schmidt School of Earth and Atmospheric Sciences Georgia Institute of Technology Date Approved: June 27th, 2016. To Rama, Tank, Jaika, Manjesh, Reeyan, and Kali. ACKNOWLEDGEMENTS Thanks Mom, Dad and Jaika for putting up with me and always being there. Thank you Kali for being such an awesome girl and being there when I needed you. Kali, you are the most beautiful girl in the world. Never forget that! Thanks Midtown Tavern for the hangovers. Thanks Waffle House for curing my hangovers. Thanks Sarah Sutton for guiding me into planetary science. Thanks Alfred McEwen for the continued support and mentoring since 2008. Thanks Sue Smrekar for taking me under your wings and teaching me about planetary geodynamics. Thanks Dan Nunes for guiding me in the gravity world. Thanks Ken Ferrier for helping me study my favorite planet. Thanks Scott Murchie for helping me become a better scientist. Thanks Marion Masse for being such a good friend and a mentor. -
Global Spectral Classification of Martian Low-Albedo Regions with Mars Global Surveyor Thermal Emission Spectrometer (MGS-TES) Data A
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 112, E02004, doi:10.1029/2006JE002726, 2007 Global spectral classification of Martian low-albedo regions with Mars Global Surveyor Thermal Emission Spectrometer (MGS-TES) data A. Deanne Rogers,1 Joshua L. Bandfield,2 and Philip R. Christensen2 Received 4 April 2006; revised 12 August 2006; accepted 13 September 2006; published 14 February 2007. [1] Martian low-albedo surfaces (defined here as surfaces with Mars Global Surveyor Thermal Emission Spectrometer (MGS-TES) albedo values 0.15) were reexamined for regional variations in spectral response. Low-albedo regions exhibit spatially coherent variations in spectral character, which in this work are grouped into 11 representative spectral shapes. The use of these spectral shapes in modeling global surface emissivity results in refined distributions of previously determined global spectral unit types (Surface Types 1 and 2). Pure Type 2 surfaces are less extensive than previously thought, and are mostly confined to the northern lowlands. Regional-scale spectral variations are present within areas previously mapped as Surface Type 1 or as a mixture of the two surface types, suggesting variations in mineral abundance among basaltic units. For example, Syrtis Major, which was the Surface Type 1 type locality, is spectrally distinct from terrains that were also previously mapped as Type 1. A spectral difference also exists between southern and northern Acidalia Planitia, which may be due in part to a small amount of dust cover in southern Acidalia. Groups of these spectral shapes can be averaged to produce spectra that are similar to Surface Types 1 and 2, indicating that the originally derived surface types are representative of the average of all low-albedo regions. -
Water on the Moon, III. Volatiles & Activity
Water on The Moon, III. Volatiles & Activity Arlin Crotts (Columbia University) For centuries some scientists have argued that there is activity on the Moon (or water, as recounted in Parts I & II), while others have thought the Moon is simply a dead, inactive world. [1] The question comes in several forms: is there a detectable atmosphere? Does the surface of the Moon change? What causes interior seismic activity? From a more modern viewpoint, we now know that as much carbon monoxide as water was excavated during the LCROSS impact, as detailed in Part I, and a comparable amount of other volatiles were found. At one time the Moon outgassed prodigious amounts of water and hydrogen in volcanic fire fountains, but released similar amounts of volatile sulfur (or SO2), and presumably large amounts of carbon dioxide or monoxide, if theory is to be believed. So water on the Moon is associated with other gases. Astronomers have agreed for centuries that there is no firm evidence for “weather” on the Moon visible from Earth, and little evidence of thick atmosphere. [2] How would one detect the Moon’s atmosphere from Earth? An obvious means is atmospheric refraction. As you watch the Sun set, its image is displaced by Earth’s atmospheric refraction at the horizon from the position it would have if there were no atmosphere, by roughly 0.6 degree (a bit more than the Sun’s angular diameter). On the Moon, any atmosphere would cause an analogous effect for a star passing behind the Moon during an occultation (multiplied by two since the light travels both into and out of the lunar atmosphere). -
Appendix I Lunar and Martian Nomenclature
APPENDIX I LUNAR AND MARTIAN NOMENCLATURE LUNAR AND MARTIAN NOMENCLATURE A large number of names of craters and other features on the Moon and Mars, were accepted by the IAU General Assemblies X (Moscow, 1958), XI (Berkeley, 1961), XII (Hamburg, 1964), XIV (Brighton, 1970), and XV (Sydney, 1973). The names were suggested by the appropriate IAU Commissions (16 and 17). In particular the Lunar names accepted at the XIVth and XVth General Assemblies were recommended by the 'Working Group on Lunar Nomenclature' under the Chairmanship of Dr D. H. Menzel. The Martian names were suggested by the 'Working Group on Martian Nomenclature' under the Chairmanship of Dr G. de Vaucouleurs. At the XVth General Assembly a new 'Working Group on Planetary System Nomenclature' was formed (Chairman: Dr P. M. Millman) comprising various Task Groups, one for each particular subject. For further references see: [AU Trans. X, 259-263, 1960; XIB, 236-238, 1962; Xlffi, 203-204, 1966; xnffi, 99-105, 1968; XIVB, 63, 129, 139, 1971; Space Sci. Rev. 12, 136-186, 1971. Because at the recent General Assemblies some small changes, or corrections, were made, the complete list of Lunar and Martian Topographic Features is published here. Table 1 Lunar Craters Abbe 58S,174E Balboa 19N,83W Abbot 6N,55E Baldet 54S, 151W Abel 34S,85E Balmer 20S,70E Abul Wafa 2N,ll7E Banachiewicz 5N,80E Adams 32S,69E Banting 26N,16E Aitken 17S,173E Barbier 248, 158E AI-Biruni 18N,93E Barnard 30S,86E Alden 24S, lllE Barringer 29S,151W Aldrin I.4N,22.1E Bartels 24N,90W Alekhin 68S,131W Becquerei -
In Pdf Format
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Nabs 2004 Final
CURRENT AND SELECTED BIBLIOGRAPHIES ON BENTHIC BIOLOGY 2004 Published August, 2005 North American Benthological Society 2 FOREWORD “Current and Selected Bibliographies on Benthic Biology” is published annu- ally for the members of the North American Benthological Society, and summarizes titles of articles published during the previous year. Pertinent titles prior to that year are also included if they have not been cited in previous reviews. I wish to thank each of the members of the NABS Literature Review Committee for providing bibliographic information for the 2004 NABS BIBLIOGRAPHY. I would also like to thank Elizabeth Wohlgemuth, INHS Librarian, and library assis- tants Anna FitzSimmons, Jessica Beverly, and Elizabeth Day, for their assistance in putting the 2004 bibliography together. Membership in the North American Benthological Society may be obtained by contacting Ms. Lucinda B. Johnson, Natural Resources Research Institute, Uni- versity of Minnesota, 5013 Miller Trunk Highway, Duluth, MN 55811. Phone: 218/720-4251. email:[email protected]. Dr. Donald W. Webb, Editor NABS Bibliography Illinois Natural History Survey Center for Biodiversity 607 East Peabody Drive Champaign, IL 61820 217/333-6846 e-mail: [email protected] 3 CONTENTS PERIPHYTON: Christine L. Weilhoefer, Environmental Science and Resources, Portland State University, Portland, O97207.................................5 ANNELIDA (Oligochaeta, etc.): Mark J. Wetzel, Center for Biodiversity, Illinois Natural History Survey, 607 East Peabody Drive, Champaign, IL 61820.................................................................................................................6 ANNELIDA (Hirudinea): Donald J. Klemm, Ecosystems Research Branch (MS-642), Ecological Exposure Research Division, National Exposure Re- search Laboratory, Office of Research & Development, U.S. Environmental Protection Agency, 26 W. Martin Luther King Dr., Cincinnati, OH 45268- 0001 and William E. -
New Double Stars from Asteroidal Occultations, 1971 - 2008
Vol. 6 No. 1 January 1, 2010 Journal of Double Star Observations Page 88 New Double Stars from Asteroidal Occultations, 1971 - 2008 Dave Herald, Canberra, Australia International Occultation Timing Association (IOTA) Robert Boyle, Carlisle, Pennsylvania, USA Dickinson College David Dunham, Greenbelt, Maryland, USA; Toshio Hirose, Tokyo, Japan; Paul Maley, Houston, Texas, USA; Bradley Timerson, Newark, New York, USA International Occultation Timing Association (IOTA) Tim Farris, Gallatin, Tennessee, USA Volunteer State Community College Eric Frappa and Jean Lecacheux, Paris, France Observatoire de Paris Tsutomu Hayamizu, Kagoshima, Japan Sendai Space Hall Marek Kozubal, Brookline, Massachusetts, USA Clay Center Richard Nolthenius, Aptos, California, USA Cabrillo College and IOTA Lewis C. Roberts, Jr., Pasadena, California, USA California Institute of Technology/Jet Propulsion Laboratory David Tholen, Honolulu, Hawaii, USA University of Hawaii E-mail: [email protected] Abstract: Observations of occultations by asteroids and planetary moons can detect double stars with separations in the range of about 0.3” to 0.001”. This paper lists all double stars detected in asteroidal occultations up to the end of 2008. It also provides a general explanation of the observational method and analysis. The incidence of double stars with a separation in the range 0.001” to 0.1” with a magnitude difference less than 2 is estimated to be about 1%. Vol. 6 No. 1 January 1, 2010 Journal of Double Star Observations Page 89 New Double Stars from Asteroidal Occultations, 1971 - 2008 tions. More detail about the method of analysis is set Introduction out in the Appendix. Asteroids and planetary moons will naturally oc- cult many stars as they move through the sky. -
DOUBLE DOME1 I Issued by The
DOUBLE DOME1 i Issued by the MILWAUKEE ASTRONOMICAL SOCIETY - : MAY 1983 t - ÌY ELECTION MEETING: The May meeting will be in two parts. Some time will be taken up by an election of' board members and officers, and some time will be given to Dr. Paul Rybski o± University of Chicago's Yerkes Observatory. Dr. Rybski's talk is entitled "Charge Couple Devices - Their Uses in Contemporary Astronomy. ft Four officers and four board members will be elected. Candidates may be incumbents, nominees volunteers, or recommended members who have agreed to run. Directors serve three-year terms with a two-term limit. Officers serve for one year with unlimited re-election. Let's have a big turnout. Bring a friend and enjoy a good, informative speaker, arid do your duty to the MAS by electing qualified people to help shape the future of the Society. WHEN: Friday, May 20, 8 p.m. WHERE: UWM Physics Bldg., corner of Kenwood and Cramer, room 133. OPEN HOUSES are scheduled for June 17, July 1, 15, 29, August 12, 26, and September 9, all Friday nights. As in the past, each night will feature a different astronomical sub- ject pertaining to the heavens. The June 17 talk will cover eclipses. Since the New Berlin facilities will be open to the general public-- we can also expect the news media to be present--volunteers will be needed to assist the anticipated large crowds by operating 'scopes, guiding, minding the parking lots, or spelling other workers. Perhaps you'd like to give a talk apropos to the topic for that particular night. -
Herschel Celestial Calibration Sources: Four Large Main-Belt Asteroids As
Experimental Astronomy manuscript No. (will be inserted by the editor) Herschel celestial calibration sources Four large main-belt asteroids as prime flux calibrators for the far-IR/sub-mm range Thomas M¨uller Zoltan´ Balog Markus Nielbock Tanya· Lim David Teyssier· Michael Olberg· Ulrich· Klaas Hendrik· Linz Bruno Altieri· Chris Pearson· George Bendo· Esa Vilenius · · · Received: date / Accepted: date Abstract Celestial standards play a major role in observational astrophysics. They are needed to characterise the performance of instruments and are paramount for photometric calibration. During the Herschel Calibration Asteroid Preparatory Pro- gramme approximately 50 asteroids have been established as far-IR/sub-mm/mm calibrators for Herschel. The selected asteroids fill the flux gap between the sub- mm/mm calibrators Mars, Uranus and Neptune, and the mid-IR bright calibration stars. All three Herschel instruments observed asteroids for various calibration pur- poses, including pointing tests, absolute flux calibration, relative spectral response function, observing mode validation, and cross-calibration aspects. Here we present newly established models for the four large and well characterized main-belt aster- oids (1) Ceres, (2) Pallas, (4) Vesta, and (21) Lutetia which can be considered as new prime flux calibrators. The relevant object-specific properties (size, shape, spin- properties, albedo, thermal properties) are well established. The seasonal (distance to T. M¨uller, E. Vilenius Max Planck Institute for Extraterrestrial Physics, PO Box 1312, Giessenbachstrasse, 85741 Garching, Germany Tel.: +49 89 30000-3499 E-mail: [email protected] Z. Balog, M. Nielbock, U. Klaas, H. Linz Max Planck Institute for Astronomy, K¨onigstuhl 17, 69117 Heidelberg, Germany T.