1888AJ 8. . .97H the ASTRONOMICAL JOURNAL. No

Total Page:16

File Type:pdf, Size:1020Kb

1888AJ 8. . .97H the ASTRONOMICAL JOURNAL. No .97H . 8. THE ASTRONOMICAL JOURNAL. 1888AJ No. 181. VOL. VIII. BOSTON, 1888 SEPTEMBER 14. NO. 13* PHYSICAL OBSERVATIONS OF MARS DURING THE OPPOSITION OF 1888, AT THE LICE OBSERVATORY, By EDWARD S. HOLDEN. The opposition of 'Mars took place April 11, 1888. The cellent ephemerides of Mars which have regularly appeared Lick Observatory was transferred to the University 6f Cali- from his hand, and which have done so much to stimulate fornia on June 1. Previous to this time Mr. Keeler was and to systematize such observations as these. the only member of the astronomical staff at the Observatory, The drawings themselves are simple diagrams, as accurate and he utilized all opportunities for observation in making a as they could be made by eye estimations alone. Circum- series of measures of the satellites of Mars, which have stances did not permit of more exact determinations of the already been printed in the Astronomical Journal. positions of the various markings of the disc. No attempt It was not until July 16, however, that the work of the at pictorial representation is made. machinists and others on the dome and elevating floor was Plate II gives seven drawings of Mars made by me with sufficiently advanced to allow of regular observations. the 26-inch equatorial at Washington in 1875, 1877 and On every suitable night since that time at least one draw- 1879. The first five of these were redrawn by Monsieur ing of Mars has been made, either by myself, Mr. Schae- F. Terby, and printed in Mémoires Couronnés de VAcademie berle, or Mr. Keeler. A list of all the drawings made Royale de Belgique, tome XXXI (1880) ; but they are com- follows : paratively unknown in America, although they are interest- ing as confirming some of the discoveries of Professor E. S. H. J. M. S. J. E. K. Schiaparelli. The other two figures are printed for the h. m h. m h m July 16 9 00P.S.T. first time. 17 9 25 44 The twenty-one drawings of Plate I (1888) form a reason- 44 July 18 8 85P.S.T. 18 8 50 44 ably complete representation of the disc when the unfavor- 19 8 25 “ 19 9 00 able circumstances of the opposition are considered. All of 20 - “ 20 - 44 44 them were made when the disc of the planet was less than 23 8 45 July 23 8 45P.S.T. ;/ 2L8 13 24 8 45 44 24 8 45 44 9 , and when the zenith distance was nearly 60° ; and all 25 7 45 u 25 7 50 44 25 8 00 44 of them were made in the early evening before the large ob- 25 8 20 “ 25 8 40 44 u 44 44 jective was cooled to the temperature of the surrounding air. 26 8 10 26 9 10 26 8 40 Magnifying powers of 350 to 700 diameters have been em- 26 8 21 44 27 8 00 44 27 8 15 44 ployed according to the various conditions of vision. 29 7 28 44 29 7 52 44 29 8 20 44 The inner satellite (Phobos) was seen on July 18, when 31 7 24 “ 44 44 it was only .22 of its brilliancy at mean opposition, and Aug. 1 7 22 Aug. 1 7 52 only ¿ as bright as at the time of discovery by Professor 2 7 23 44 2 8 00 44 5 7 28 44 5 8 20 44 Hall. 5 7 40 44 It is very unfortunate that the great telescope was not 8 7 33 44 8 7 35 44 available for these observations until three months after 44 44 9 7 38 9 8 03 opposition, and that it will be necessary to wait until 1890 9 8 30 44 10 7 30 44 10 8 00 44 to form a map of the planet based upon our owm work. Still it appears to me that the drawings here given, present Plate I gives a series of these drawings arranged in the important evidence relating to the canals of M. Schiaparelli, order of longitude of the central meridian of each drawing. and to the submergence of the 4 4 continent ” Libya reported I desire to express my obligation to Mr. Marth for the ex- and confirmed by M. Perrotin in May last. © American Astronomical Society Provided by the NASA Astrophysics Data System 97H Plate I. 8 88AJ »» ;íVm £¿±- JL^nuAyjy.gtjtrnh. £^ff. ^*o, /mJLj^M, 7 V* /#rl V» * e.iM 3**+jtr v*t^ fi+mr. Sri *t~ ^ L¿¿¿~1. fÁ+~*J ¿, JL ¿tur ¿5* » ¡ w^j "b ^tn¿f , 3* *« îi. ÍmJ«^ c-.^ji-A+iLu^, > — i ^i«4.A . a-4 •/ MULS^ j>*i'/uT-. ^ ■ v<k^ S ; V>«j Lyjíh. I 4ä;«Ä,^^. 74¿í-PxA £¿j?. 'M~lmx~rníjtn-ti*. c.j.H. ■Mza ,iai , •¿trPs t f Í.M. \*xjr à* Mj, * °+tj'. 1~Ws, ^.+xr. XtH’j'.jf. ■ y« +*/*. —«'»-SV',v tía J-«*»« K*^ A/W> « i 7*Äw 4. f w“^'í'‘rj ^ = í«r , .^. -‘ ; i*ÍA -, . 4; i ff/f44* V*Uj LjiJ. ¿: !ut ( T r 5. e; Y“*—¿ ;*u¿. ->: W Uj LrL à*. _ j 'kll- !"*■ 0*1»u,turf* , fwpxi. cm. r^r-nr. **x \ L. je*:/*, *¿jtr. JLX. JLrtXjJjUymr JTJX. m * ‘VT-^y+tv x -si*’ r \. jxr* - T7»*' I .j0j * •i ÄI {¿uútjuS ^?v ^r4*' .■ —rr^J ítuc ■ * s- *. 04* i** i r^- M~ct^ J fi,4 c~ L. ¡Mr. l r*~ í ; M« u¿L*3, u ih 4^.4 h*Üy ot >at . !• ~WP l. i Plate. II. : 1*77 etlU^cj x*t iokio'. SrSX •fe /áT? í./lVW^ \ ‘jo’t y. Z?-* Jiwu2^ \^3ír J*nx7>/j ÜJS* jfit d-o^~k 4p.d Lth, e.z~3-t~aJl X« L 9 c 0° ^/ <} so~'W¿UÍ^lt^. Jlsf.ii.fc~ ir».« í, ®f Wftdi 2¿oümc4s. Bl/m'ivrim.tf tvJu. ¿X< ;?£, £ Awafi fe cfew, . "Xe. - iAT«iwn_ ly ír- « fe r.Tefl,^ ¿fer 7 .fe-/-’.; wfe^ fer — 4 © American Astronomical Society • Provided by the NASA Astrophysics Data System 98 THE ASTRONOMICAL JOURNAL. N°- 181. 97H . With regard to the canals it appears that we have not seen PARELLi in 1877 and 1878, pot to speak of later drawings. 8. any of them double, although many of the more important It is much to be regretted that the series of drawings at have been sketched as broad bands covering the spaces on the Lick Observatory begins at so late a date ; but so far as M. Schiaparelli's map which are occupied by pairs of the evidence of our work goes, it may be said that during canals and by the space separating the members of each this opposition we have seen no double canal, and do not pair. find any important changes in the 44 continent" Libya. At 1888AJ With regard to the “ continent" Libya the observations the same time no one is more sensible than myself of the here show nothing before July 16. After that date we have highly unfavorable conditions under which our work on Mars eight drawings (July 31, July 29, July 27, July 27, July 27, has been done. We have, however, seen enough of the July 26, July 25, July 25, July 26), which exhibit this working of the great telescope on Mars and on other objects marking in various aspects, all of which are in substantial to know that its powers are amply adequate under favorable agreement with each other, and each of which differs ma- conditions ; and we confidently expect the next two oppositions terially from the observations made at Nice during April, to furnish the most conclusive evidence on these highly inter- and May, as given in L'Astronomie for June 1888, page 214. esting questions. No more could have been done here during M. Perrotin says that Libya, which was plainly visible this year than was done, but the opportunities of even a two years ago, u does not exist to-day" (April and May, single favorable opposition, diligently improved, will suffice 1888). to perfect our knowledge of the topography of Mars to a The eight drawings above mentioned show it, however, in most important degree, and two such should present us with essentially the form in which it was drawn by M. Schia- a map of the planet, which may fairly be called complete. Mount Hamilton, 1888 August 17. OBSERVATIONS ON MARS, By A. HALL. [Communicated by the Superintendent of the Naval Observatory.] Observations op the Satellites. Date W.M.T. Ap W.M.T. As Bemarks Deimos. h m h 1888 Mar. 30 12 16.1 122.91 0-53 12 27.1 50.51 —0.10 Faint Apr. 4 12 41.4 118.11 1.02 12 52.4 50.21 + 0.21 Haze, very faint 6 11 19.1 304.13 0.26 11 28.4 52.81 —0.24 8 10 4.3 130.71 0.54 10 12.3 51.26 + 0.18 11 10 42.2 296.03 0.27 13 10 10.7 125.97 0.40 10 18.2 52.78 + 0.52 16 11 13.1 292.27 0.43 11 22.6 49.67 —1.15 Very faint 20 9 0.5 306.51 0.26 9 7.5 53.73 —0.89 Faint 25 9 19.4 303.31 0.55 9 27.9 52.81 + 0.02 Extremely faint May 2 8 53.2 127.65 0.11 9 1.3 51.55 —1.10 Faint 5 9 39,7 292.61 + 0.02 9 48.7 48.69 —0.84 Extremely faint Phobos.
Recommended publications
  • Copyrighted Material
    Index Abulfeda crater chain (Moon), 97 Aphrodite Terra (Venus), 142, 143, 144, 145, 146 Acheron Fossae (Mars), 165 Apohele asteroids, 353–354 Achilles asteroids, 351 Apollinaris Patera (Mars), 168 achondrite meteorites, 360 Apollo asteroids, 346, 353, 354, 361, 371 Acidalia Planitia (Mars), 164 Apollo program, 86, 96, 97, 101, 102, 108–109, 110, 361 Adams, John Couch, 298 Apollo 8, 96 Adonis, 371 Apollo 11, 94, 110 Adrastea, 238, 241 Apollo 12, 96, 110 Aegaeon, 263 Apollo 14, 93, 110 Africa, 63, 73, 143 Apollo 15, 100, 103, 104, 110 Akatsuki spacecraft (see Venus Climate Orbiter) Apollo 16, 59, 96, 102, 103, 110 Akna Montes (Venus), 142 Apollo 17, 95, 99, 100, 102, 103, 110 Alabama, 62 Apollodorus crater (Mercury), 127 Alba Patera (Mars), 167 Apollo Lunar Surface Experiments Package (ALSEP), 110 Aldrin, Edwin (Buzz), 94 Apophis, 354, 355 Alexandria, 69 Appalachian mountains (Earth), 74, 270 Alfvén, Hannes, 35 Aqua, 56 Alfvén waves, 35–36, 43, 49 Arabia Terra (Mars), 177, 191, 200 Algeria, 358 arachnoids (see Venus) ALH 84001, 201, 204–205 Archimedes crater (Moon), 93, 106 Allan Hills, 109, 201 Arctic, 62, 67, 84, 186, 229 Allende meteorite, 359, 360 Arden Corona (Miranda), 291 Allen Telescope Array, 409 Arecibo Observatory, 114, 144, 341, 379, 380, 408, 409 Alpha Regio (Venus), 144, 148, 149 Ares Vallis (Mars), 179, 180, 199 Alphonsus crater (Moon), 99, 102 Argentina, 408 Alps (Moon), 93 Argyre Basin (Mars), 161, 162, 163, 166, 186 Amalthea, 236–237, 238, 239, 241 Ariadaeus Rille (Moon), 100, 102 Amazonis Planitia (Mars), 161 COPYRIGHTED
    [Show full text]
  • Asymmetric Terracing of Lunar Highland Craters: Influence of Pre-Impact Topography and Structure
    Proc. L~lnorPli~nel. Sci. Corrf. /Of11 (1979), p. 2597-2607 Printed in the United States of America Asymmetric terracing of lunar highland craters: Influence of pre-impact topography and structure Ann W. Gifford and Ted A. Maxwell Center for Earth and Planetary Studies, National Air and Space Museum, Smithsonian Institition, Washington, DC 20560 Abstract-The effects of variable pre-impact topography and substrate on slumping and terrace for- mation have been studied on a group of 30 craters in the lunar highlands. These craters are charac- terized by a distinct upper slump block and are all situated on the rim of a larger, older crater or a degraded rim segment. Wide, isolated terraces occur where the rim of the younger crater coincides with a rim segment of the older crater. The craters are all located in Nectarianlpre-Nectarian highland units, and range in age from Imbrian to Copernican. A proposed model for formation of slump blocks in these craters includes the existence of layers with different competence in an overturned rim of the pre-existing crater. Such layering could have resulted from overturning of more coherent layers during formation of the Nectarian and pre-Nec- tarian craters. A combination of material and topographic effects is therefore responsible for terrace formation. Similar terrain effects may be present on other planets and should be considered when interpreting crater statistics in relation to morphology. INTRODUCTION Slumping, terracing or wall failure is an important process in formation and mod- ification of lunar craters. The process of slumping has been investigated by both geometrical (Cintala et a1 ., 1977) and theoretical models (Melosh, 1977; Melosh and McKinnon, 1979); however, these studies are dependent on morphologic constraints imposed by the geologic setting of the craters.
    [Show full text]
  • 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
    [Show full text]
  • Lunar Impact Basins Revealed by Gravity Recovery and Interior
    Lunar impact basins revealed by Gravity Recovery and Interior Laboratory measurements Gregory Neumann, Maria Zuber, Mark Wieczorek, James Head, David Baker, Sean Solomon, David Smith, Frank Lemoine, Erwan Mazarico, Terence Sabaka, et al. To cite this version: Gregory Neumann, Maria Zuber, Mark Wieczorek, James Head, David Baker, et al.. Lunar im- pact basins revealed by Gravity Recovery and Interior Laboratory measurements. Science Advances , American Association for the Advancement of Science (AAAS), 2015, 1 (9), pp.e1500852. 10.1126/sci- adv.1500852. hal-02458613 HAL Id: hal-02458613 https://hal.archives-ouvertes.fr/hal-02458613 Submitted on 26 Jun 2020 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. RESEARCH ARTICLE PLANETARY SCIENCE 2015 © The Authors, some rights reserved; exclusive licensee American Association for the Advancement of Science. Distributed Lunar impact basins revealed by Gravity under a Creative Commons Attribution NonCommercial License 4.0 (CC BY-NC). Recovery and Interior Laboratory measurements 10.1126/sciadv.1500852 Gregory A. Neumann,1* Maria T. Zuber,2 Mark A. Wieczorek,3 James W. Head,4 David M. H. Baker,4 Sean C. Solomon,5,6 David E. Smith,2 Frank G.
    [Show full text]
  • GRAIL Gravity Observations of the Transition from Complex Crater to Peak-Ring Basin on the Moon: Implications for Crustal Structure and Impact Basin Formation
    Icarus 292 (2017) 54–73 Contents lists available at ScienceDirect Icarus journal homepage: www.elsevier.com/locate/icarus GRAIL gravity observations of the transition from complex crater to peak-ring basin on the Moon: Implications for crustal structure and impact basin formation ∗ David M.H. Baker a,b, , James W. Head a, Roger J. Phillips c, Gregory A. Neumann b, Carver J. Bierson d, David E. Smith e, Maria T. Zuber e a Department of Geological Sciences, Brown University, Providence, RI 02912, USA b NASA Goddard Space Flight Center, Greenbelt, MD 20771, USA c Department of Earth and Planetary Sciences and McDonnell Center for the Space Sciences, Washington University, St. Louis, MO 63130, USA d Department of Earth and Planetary Sciences, University of California, Santa Cruz, CA 95064, USA e Department of Earth, Atmospheric and Planetary Sciences, MIT, Cambridge, MA 02139, USA a r t i c l e i n f o a b s t r a c t Article history: High-resolution gravity data from the Gravity Recovery and Interior Laboratory (GRAIL) mission provide Received 14 September 2016 the opportunity to analyze the detailed gravity and crustal structure of impact features in the morpho- Revised 1 March 2017 logical transition from complex craters to peak-ring basins on the Moon. We calculate average radial Accepted 21 March 2017 profiles of free-air anomalies and Bouguer anomalies for peak-ring basins, protobasins, and the largest Available online 22 March 2017 complex craters. Complex craters and protobasins have free-air anomalies that are positively correlated with surface topography, unlike the prominent lunar mascons (positive free-air anomalies in areas of low elevation) associated with large basins.
    [Show full text]
  • Science Concept 3: Key Planetary
    Science Concept 6: The Moon is an Accessible Laboratory for Studying the Impact Process on Planetary Scales Science Concept 6: The Moon is an accessible laboratory for studying the impact process on planetary scales Science Goals: a. Characterize the existence and extent of melt sheet differentiation. b. Determine the structure of multi-ring impact basins. c. Quantify the effects of planetary characteristics (composition, density, impact velocities) on crater formation and morphology. d. Measure the extent of lateral and vertical mixing of local and ejecta material. INTRODUCTION Impact cratering is a fundamental geological process which is ubiquitous throughout the Solar System. Impacts have been linked with the formation of bodies (e.g. the Moon; Hartmann and Davis, 1975), terrestrial mass extinctions (e.g. the Cretaceous-Tertiary boundary extinction; Alvarez et al., 1980), and even proposed as a transfer mechanism for life between planetary bodies (Chyba et al., 1994). However, the importance of impacts and impact cratering has only been realized within the last 50 or so years. Here we briefly introduce the topic of impact cratering. The main crater types and their features are outlined as well as their formation mechanisms. Scaling laws, which attempt to link impacts at a variety of scales, are also introduced. Finally, we note the lack of extraterrestrial crater samples and how Science Concept 6 addresses this. Crater Types There are three distinct crater types: simple craters, complex craters, and multi-ring basins (Fig. 6.1). The type of crater produced in an impact is dependent upon the size, density, and speed of the impactor, as well as the strength and gravitational field of the target.
    [Show full text]
  • Directory of Research Projects
    NASA Technical Memorandum 4211 Directory of Research Projects Planetary Geology and Geophysics Program Henry Holt, Editor NASA Office of Space Science and Applications Washington, D.C. NI A National Aeronautics and Space Administration Office of Management Scientific and Technical Information Division 1990 INTRODUCTION This directory of research projects provides information about currently funded scientific research within the Planetary Geology and Geophysicss (PGG) Program. The directory consists of the proposal summary sheet from each proposal funded under the PGG Program during fiscal year 1990, covering the period from October I, 1989 through September 30, 1990. The summary sheets provide information about the research project including: title, principal investigator, institution, summary of research objectives, past accomplishments, and proposed new investigations. This directory is intended to inform scientists in the PGG Program about other research projects supported by the program and can also be utilized by others as a PGG Program information source. The research projects funded under the PGG Program include investigation over a broad range of topics including geological and geophysics studies of: terrestrial planets and satellites; outer planet satellites and rings; comets and asteroids; planetary interiors; lithosphere-atmosphere relationships; impact cratering processes and chronologies; planetary surface modification by fluvial, aeolian, periglacial, masswasting, and volcanic processes; planetary structure and tectonics; multispectral and radar remote sensing; and solar system dynamics. Also, cartographic and geologic maps of the solid surfaces of planets and satellites are produced and distributed. Statistical information about the PGG Program is presented the next two pages. The following four pages are an alphabetical listing of all program principal investigators.
    [Show full text]
  • LPIB Issue No. 149 Now Available
    Cassini’s Swan Song L Paul Schenk, Lunar and Planetary Institute On September 15 of this year, the mission of the Cassini orbiter at Saturn will come to its official end. Early that morning, the spacecraft’s radio signal will cease as Cassini enters the giant ringed planet’s atmosphere, and the 2-metric-ton vehicle will undergo “molecular dissociation” (in other words, it will burn up). But that date will signify more than just the destruction of a spacecraft. For the hundreds of Pengineers, scientists, and officials who have worked for as much as a quarter of a century on this project, it will be the end of a personal journey to Saturn. The Cassini project officially began in 1990 with solicitations for researchers to participate in it, and many people have joined and left the project since then. The great discoveries of Pioneer and Voyager in 1979–1981 provided a glimpse of the marvels of Saturn, but it is doubtful that anyone working on Cassini prior to its arrival in July 2004 could have anticipated the revolution in our understanding of Saturn and its satellites that this mission has provided. Nor could they have guessed just how much the mission would affect them personally. As Cassini’s radio signal fades out for the last time, there probably won’t be Imany dry eyes in the house. With its fuel supply running low, Cassini began its “Grand Finale” on April 26 of this year, beginning the process that will end its 13-year-long tour of the Saturn system.
    [Show full text]
  • Whatcom County Council Agenda Bill No
    WHATCOM COUNTY COUNCIL AGENDA BILL NO. 2018 -- 28 CLEARANCES Initial Date Date Received in Council Office Al(enda Date Assigned to: Weimer 1/8/2018 1/16/2018 Council lntroductio OriJ<inator: Division Head: v Dept. Head: i~) l•(().l'i\( Prosecutor: PurchasinJ<IBudJ<et: Executive: TITLE OF DOCUMENT: Appointments to Climate Impact Advisory Committee ATTACHMENTS: Applications SEPA review required? ( ) Yes ( ) NO Should Clerk schedule a hearing ? ( ) Yes ( X ) NO SEPA review completed? ( ) Yes ( ) NO Requested Date: SUMMARY STATEMENT OR LEGAL NOTICE LANGUAGE: (Ifthisitem isanordinanceorrequiresapuhlic hearing, you must provide the language for use in the required public notice. Be specific and cite RCW or WCC as appropriate. Be clear in explaining the intent of the action.) Ordinance 2017-080 was adopted establishing the Whatcom County Climate Impact Advisory Committee on December 5, 2017. The Whatcom County Council established the goal of 100% renewable energy use within County Operations and larger Whatcom County community, and directs the Whatcom County Climate Impact Advisory Committee to work diligently toward that goal. COMMITTEE ACTION: COUNCIL ACTION: Related County Contract #: Related File Numbers: Ordinance or Resolution Number: Please Note: Once adopted and signed, ordinances and resolutions are available for viewing and printing on the County's website at: www.co.whatcom.wa.us/council. CLERK OF THE COUNCIL COUNCILMEMBERS Dana Brown-Davis, C.M.C. Barbara E. Brenner Rud Browne COUNTY COURTHOUSE Barry Buchanan 311 Grand Avenue, Suite #105 Todd Donovan Bellingham, WA 98225-4038 Ken Mann (360) 778-5010 Satpal Sidhu Carl Weimer WHATCOM COUNTY COUNCIL BOARDS AND COMMISSION VACANCY Application deadline is 10:00 a.m.
    [Show full text]
  • Galactic Observer
    alactic Observer John J. McCarthy Observatory GVolume 5, No. 9 September 2012 As Curiosity Rover makes its first baby steps for mankind, NASA is already planning for future missions to Mars. Cutting to The InSight lander ("Interior Exploration using Seismic Investigations, Geodesy and Heat the Core Transport" will employ a German-made internal hammer - or "tractor mole" - to probe the Martian crust and descend up to 16 feet (five meters) below the surface. The mission will attempt to find out why Earth and its half-sister have evolved so differently. For more information, go to http://discovery.nasa.gov/index.cfml Image credit: NASA/JPL-Caltech The John J. McCarthy Observatory Galactic Observvvererer New Milford High School Editorial Committee 388 Danbury Road Managing Editor New Milford, CT 06776 Bill Cloutier Phone/Voice: (860) 210-4117 Production & Design Phone/Fax: (860) 354-1595 Allan Ostergren www.mccarthyobservatory.org Website Development JJMO Staff John Gebauer It is through their efforts that the McCarthy Observatory Marc Polansky has established itself as a significant educational and Josh Reynolds recreational resource within the western Connecticut Technical Support community. Bob Lambert Steve Barone Allan Ostergren Dr. Parker Moreland Colin Campbell Cecilia Page Dennis Cartolano Joe Privitera Mike Chiarella Bruno Ranchy Josh Reynolds Jeff Chodak Route Bill Cloutier Barbara Richards Charles Copple Monty Robson Randy Fender Don Ross John Gebauer Gene Schilling Elaine Green Diana Shervinskie Tina Hartzell Katie Shusdock Tom Heydenburg Jon Wallace Jim Johnstone Bob Willaum Bob Lambert Paul Woodell Parker Moreland, PhD Amy Ziffer In This Issue SILENCED FOOTFALLS ................................................... 3 SUNRISE AND SUNSET .................................................. 13 END OF THE YEAR OF THE SOLAR SYSTEM ......................
    [Show full text]
  • 13. Martian Cratering and Implications for the Chronostratigraphy
    13. Martian Cratering and Implications for the Chronostratigraphy The record of large impact basins on differ- ent planetary bodies allows us to compare the characteristics of the heavy bombardment pe- riod and the end of planetary formation. Both the cratering record itself and the age distri- bution of the impact basins represent the pe- riod of highest impactor flux, decaying rapidly within the first half billion years of our solar system. In order to test the plausibility of the Martian chronology model (see Chapter 5), the ages of the large Martian impact basins, using the derived Martian production function, were determined and compared to lunar basin ages. For the Moon, the large basins were produced no later than about 3.8 to 3.9 Ga ago and a similar situation should exist for Mars, follow- ing the marker horizon idea (Wetherill, 1975). This idea is based on the assumption that solar system bodies have undergone a similar evo- lution since planetary formation. In the cra- Figure 13.1.: The crater size frequency distribu- tering record on any solid surface body, which tion measured for one of the oldest regions on Mars: has representative large old surface units, this Noachis Terra (map nomenclature: unit Npl1). first period of heavy bombardment is present in the general crater size–frequency distribution as well as the large basin record itself. According to our investigation, the oldest surface areas on than the visible highland surface, where crater Mars, roughly the Martian southern highlands, count ages are based on craters clearly recog- e. g. Noachis Terra, were formed between 4.0 nized by their morphology.
    [Show full text]
  • Kevin W. Lewis [email protected] — Planetary.Johnshopkins.Edu/Klewis Dept
    Kevin W. Lewis [email protected] | planetary.johnshopkins.edu/klewis Dept. of Earth and Planetary Sciences, Johns Hopkins University, Baltimore, Maryland ||||||||||||||||||||||||||||||||||||||{ Positions 9/2014{ Assistant Professor Johns Hopkins University Department of Earth and Planetary Sciences 2011-2014 Associate Research Scholar Princeton University Department of Geosciences 2009{2011 Harry Hess Postdoctoral Fellow Princeton University Department of Geosciences Education 2009 California Institute of Technology (Pasadena, CA) Ph. D., Planetary Science 2003 Tufts University (Medford, MA) B.S., Physics, Mathematics, Astrophysics Awards 2015 Outstanding Reviewer, Icarus 2014 NASA Group Achievement Award, MSL Science Team 2011 NASA Group Achievement Award, HiRISE Science Team 2009{2011 Harry Hess Postdoctoral Fellowship 2008 NASA Group Achievement Award, MER Science Team 2007{2009 NASA Earth and Space Science Fellowship 2006, 2007 Richard H. Jahns Teaching Prize, Caltech 2007 Recognition of Excellence in Teaching, Caltech Acad. Res. Council 2003 Henshaw Fellowship, Caltech 2003 Amos Emerson Dolbear Prize in Physics, Tufts Univ. 2002 F. W. Pote Memorial Fund Scholarship in Physics, Tufts Univ. Service 2015{ Diversity Champion, JHU Earth & Planetary Sciences Department 2017{ JHU EPS Equity, Diversity, and Inclusivity Committee 2017{ PDS Geosciences Node Advisory Group 2009{10 Lunar and Planetary Science Conference Organizing Committee Reviewer Geophysical Review Letters, Journal of Geophysical Research, Planetary and Space Sciences, Icarus, Science, Nature Geoscience, Geological Society of America Bulletin, Geology, Eos Reviewer Mars Data Analysis Program, Mars Fundamental Research Program, Bilateral Science Foundation, Planetary Geology & Geophysics Reviewer Planetary Data System (PDS) 1 Publications N=49, h-index=31 (via Google Scholar); *member of Lewis research group [1] K. W. Lewis, S. F. Peters, K.
    [Show full text]