DOCSLIB.ORG

SAVE 29 REGAL MEN'g GHOP Iianrlltfittr Ieutmttg Llrraui

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
SAVE 29 REGAL MEN'g GHOP Iianrlltfittr Ieutmttg Llrraui H • PAGE FORTY-FOUR WEDNESDAY, DECEMBER 8, 1971 m anirliPBter lEoBnins iim U i Most Manchester Stores Open Tonight Until 9 O^Clock fforth Manchester Al-Anon W. Allen Kingsbury, a Man­ Youth Ministry family group will meet tonight chester native, recently was Av«rag« DaUg N«t PrtM Ran About Town at 8 at the Second Congregation­ awarded the U.S. Public Health ’ Hie annual businesa meeting al Church palish house. The Service Commissioned Corps Conference Set For Iho Week Ended The Weather o( Uriel Lodge of Masons, in­ Thursday group will meet to­ Commendation Medal for his November M, 1971 Cloudy and mild through to­ cluding elecUmi of officers, will morrow at 8:30 p.m. at tho leadership In maintaining the At St. Mary’s morrow morning with light bo held at the Masonic Temple Pathfinders Club, 10? Norman federal program In New Eng­ rain/drlnle; tonight’* low near "Which Way, St. Mary’s," a lit Merrow on Saturilay at 7:30 SI. Both groups meet weekly land for certifying Interstate 15 ,5 9 0 iianrllTfitTr iEuTmttg llrraUi 40. Partial clearing Friday af­ p.m., followed by a meeting of and are open to friends and ro- milk carriers. A sanitarian, he conference on Youth Ministry ternoon; high In 40a. Uriel Temple Corporation. Re­ lutives living with a drinking is. now stationed in the San for the whole parish, will be MancheMter— A City of ViUago Charm freshments wrlll be served after problem. Francisco, Calif., office of the conducted Saturday from 9:30 the meeting. Public Health Service. a.m. to 3 p.m. In Neill Hall and VOL. LXXXXI, NO. S9 (TWENTY-EIGHT PAGES—TWO SECTIONS) MANCHESTER, CONN., THURSDAY, DECEMBER 9, 1971 (OlMeifled AdvwthdM ea Phfiit M ) The commission on missions PRICE FIFTEEN CENTS Registration closes tomorrow tho Old Parish Hall of St, Matys of South united Methodist The Church of tho Nazarene for the annual VFW CSilldren’s Episcopal Church. Church will meet tonight at 7:30 will have a midweek service of Christmas party on Dec. H and at the church. Bible study and prayer tonight A light lunch .will be served may be made by contacting at 7:30 In the lower auditorium after a midday informal Euchar­ Mrs. Jessie Turell of 312 Oak­ of the church. ist. The conference slogan Is The Sunday School staff of land St. or Cary Crane of 06 “ There's a new you coming the Choppers, Allies Zion Evangelical Lutheran Essex St. The property committee of great Christ way,” and Its Church will meet tonight at 7 :30 Soldiers Jam Ganges theme Is "What realistically at the church. Center Congregational Church First Church of Christ, Scien­ will meet tonight at 7:30 In the could happen In youth ministry, tist, will have its regular mid­ church office. and what would be Involved In Batter Reds In week testimony meeting tonight Emanuel Lutheran Church making It happen?” at 8 at the church, 447 N. Main Choir will rehearse tonight at The Senior Choir of Commun­ Tho conference Is open to all St. The meeting Is open to the 7:30 In' Luther Hall of the ity Baptist Church will rehearse members of St. Mary’s Church In Retreat to Dacca public. church. tonight at 7:30 at the church. free of charge. Registrations will bo accepted through Fri­ Cambodia Clash The evangelism committee of day afternoon at the church of­ By THE ASSOCIATED PRESS they were In a building in the given to Bast Pakistan by the rear. rebels and IiuUa. Emanuel Lutheran Church will fice. SAIOON (AP) — U.S. hcli- tack from two aides. But fight­ India claimed today Its troops meet tonight at 7:30 in the Advisors and consultants for coptor gunahlpa and South Vlet- ing near a prison camp 10 had pressed to within 26 miles Associated Press correspond­ "The forces of our army and the Mukti Bahlni guerrillas act­ tm ind It at church board room. the conference are the Rev. nameae troope battered North mUes south of the Chmbodian of Dacca, that thousands a t ent Peter O’Loughlin reported Douglas T. Cooke, diocesan con­ Vletnameae force* In Cambodia capital ended as the North Viet­ fleeing Pakistani soldiers were that the feeling in Dacca “was ing not only in concert but un­ 1^1 i o m Wesley Circle of South United sultant on youth ministries; and today, and a apokanman report­ namese troops pulled out under trying to cross the Ganges Riv­ that the Indians, attacking der a unified command are kWithoursto. Methodist Church will have a the Rev. Russell H. Allen, as­ ed 7S Nmth Vletnameae Mlled a heavy bombardment that de­ er to that East Pakistan capi­ from several directions, are forcing the Pakistani forcss to m r m and ao weapon* captured. tightening the noose.” India pull out from their strongholds \ dinner party tonight at 6:80 at sistant to the rector at St. stroyed the village of Kleah tal, and that enemy planes had the WtVaelc of malaltriUt the home of Mrs. John Muschko, Mary’s. The apokeaman, Lt. Col. Do Sanday. been driven from the skies. claim ed Wednesday It* forces In conflision,” R am aaasrtod. dowfltown maneheitet*. Ram aald ComlUa, southeast 277 Spring St. There will be a The Rei3^ 'Mr. Cooke has Viet, aald there were no South Most cf the fighting was Indian troope were reported were within 28 miles of Dacca. of Dacca, and Bylhet, in the discussion of "The Christmas worked in parishes In New Mil­ tnetnameae coaualtlea. south and southwest of the cap­ holding their ground in Kash­ Defense Minister Jagjivon northeast comer of the territo­ Spirit— Commercialism versus ford and Oakville and has led It was the second big enemy ital, with some as close as mir on the western front. Ram told the Indian parUament ry, toll Wednesday. Ho r^Mrted opM tonight till 9, and the Religrious Aspect." high school conferences, ad­ loss in aa many days claimed eight miles to the city, but Pakistan's eastern command that Indian troop* and their al­ that the capture cf Rangpur vised area youth programs and by the South Vietnamese north most of the cldshes were small in Dacca countered with re­ lies in the East Pakistani seces­ and Dlnajpur In the north­ every night till Christmas! The ways and means commit­ of Highway 7 In the enemy’s and scattered. ports of fierce fighting cn most sion movement have “freed led inner-city youth conferences western part of the province tee of Center Congregational Dam Be base camp area about Meanwhile, some 280 U.S. fronts in the east and said large areas of Bangla Desk we have a fantastic assortment of chlrstmas decora­ In New York City. was Imminent. Church will meet tonight at 7 :30 80 miles from the V^tnameae warplanes attacked the Ho Chi “ enemy thrusts are stlU being from the occupying forces of t tions tor inside and out! The Rev. Mr. Allen, directed The Pakistani command in Mlnh trail In Laos, keeping up successfully countered by Paki­ Pakistan.’’ Bangla Deah—the o tree • mantle In the church library. Manchester’s Slimmer ’66 and border. Another 80 North Viet­ ’70, and has advised two coffee namese were reported killed the strong air effort to Inter­ stani troops.” Bengali nation—Is the name (See Page Two) o doorway s window A midweek service of prayer houses and was the assistant at Wednesday by South Vletnam- cept Norih • Vietnamese war An Indian army communique will be held tonight at 7:30 at Calvary House In New York SM ground farces and U.S. taell- materials and reinforcements reported Its troops had ad­ Calvary Church. City. He now coordinates youth, q ^ r a . The South Vietnamese moving south to Cambodia and vanced to the Meghna River 26 we have everything at fairway prices | urban, ecumenical, and liturgi­ toU than was two kUled and 28 Soutti Vietnam, miles from .Dacca. Boy Scout Troop 123 will meet cal ministries at St. Mary’s wounded. “ With improved weather Lt. Gen. Jagjlt Singh Aurora, Sabers Silencing for your hofiday deeoratiens! | tonight at 6:46 at Community Church. there is more truck traffic commander of India’s eastern Baptist Church. along the trail, and a strong fnmt, said in Calcutta that U.S. air effort Is being made to 'organiMtional discounts, too!' thousands of Pakistani troops I The Senior Citbir of Center Southeast Intercept and Interdict the ene­ under air attack were trying to Mail Deadlines m y,’’ said one Informant. Cbngregatlcmal Church will re­ t n R e t r ^ t reach Dacca or the port cf Tashkent Pledge hearse tonight at 7:80 in Mem- Help Deliveries Scores cf support planes also Chittagong in the east In an ar­ ' orlal Hall of the church. were In the skies over Lajos, In­ mada of sampans, barges and B y 8PENOEB DAV18 cluding rescue aircraft and es­ Tashkent Declaration died kxig Manchester Postmaster Ed­ river boats. ago because Pakistan never Im- Ool. Viet sold It was the most cort fighters on the lookout for WASHINGTON (AP) — ward Sauter today remlned Of these eight Pakistani bat­ pCemented its provisions for a significant acU<m since the 28,- North Vietnamese MIQ’s. Whatever tu^pened to the residents of the mailing dates talions, about 7,000 men, were Tashkent Declaration in which ministerial meeting. OOO-man South Vietnamese One P106 escort fired a recommended by the postal Of attempting to cross the Ganges American officials say no force drove Into eastern Cam- Shrike mlssfie at a North Viet­ India and Pakistan solemnly service for Christmas parcels from the west to make a stand Ifledged after a six-day war In major power la oUe to {flay a I ^i/teAaAAl-BilEYER'S iCE CREAM SALE bodU on Nov.
Load more

Recommended publications
  • Columbus Crater HLS2 Hangout: Exploration Zone Briefing
    Columbus Crater HLS2 Hangout: Exploration Zone Briefing Kennda Lynch1,2, Angela Dapremont2, Lauren Kimbrough2, Alex Sessa2, and James Wray2 1Lunar and Planetary Institute/Universities Space Research Association 2Georgia Institute of Technology Columbus Crater: An Overview • Groundwater-fed paleolake located in northwest region of Terra Sirenum • ~110 km in diameter • Diversity of Noachian & Hesperian aged deposits and outcrops • High diversity of aqueous mineral deposits • Estimated 1.5 km depth of sedimentary and/or volcanic infill • High Habitability and Biosignature Preservation Potential LZ & Field Station Latitude: 194.0194 E Longitude: 29.2058 S Altitude: +910 m SROI #1 RROI #1 LZ/HZ SROI #4 SROI #2 SROI #5 22 KM HiRISE Digital Terrain Model (DTM) • HiRISE DTMs are made from two images of the same area on the ground, taken from different look angles (known as a stereo-pair) • DTM’s are powerful research tools that allow researchers to take terrain measurements and model geological processes • For our traversability analysis of Columbus: • The HiRISE DTM was processed and completed by the University of Arizona HiRISE Operations Center. • DTM data were imported into ArcMap 10.5 software and traverses were acquired and analyzed using the 3D analyst tool. • A slope map was created in ArcMap to assess slope values along traverses as a supplement to topography observations. Slope should be ≤30°to meet human mission requirements. Conclusions Traversability • 9 out of the 17 traverses analyzed met the slope criteria for human missions. • This region of Columbus Crater is traversable and allows access to regions of astrobiological interest. It is also a possible access point to other regions of Terra Sirenum.
    [Show full text]
  • Identification of Volcanic Rootless Cones, Ice Mounds, and Impact 3 Craters on Earth and Mars: Using Spatial Distribution As a Remote 4 Sensing Tool
    JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 111, XXXXXX, doi:10.1029/2005JE002510, 2006 Click Here for Full Article 2 Identification of volcanic rootless cones, ice mounds, and impact 3 craters on Earth and Mars: Using spatial distribution as a remote 4 sensing tool 1 1 1 2 3 5 B. C. Bruno, S. A. Fagents, C. W. Hamilton, D. M. Burr, and S. M. Baloga 6 Received 16 June 2005; revised 29 March 2006; accepted 10 April 2006; published XX Month 2006. 7 [1] This study aims to quantify the spatial distribution of terrestrial volcanic rootless 8 cones and ice mounds for the purpose of identifying analogous Martian features. Using a 9 nearest neighbor (NN) methodology, we use the statistics R (ratio of the mean NN distance 10 to that expected from a random distribution) and c (a measure of departure from 11 randomness). We interpret R as a measure of clustering and as a diagnostic for 12 discriminating feature types. All terrestrial groups of rootless cones and ice mounds are 13 clustered (R: 0.51–0.94) relative to a random distribution. Applying this same 14 methodology to Martian feature fields of unknown origin similarly yields R of 0.57–0.93, 15 indicating that their spatial distributions are consistent with both ice mound or rootless 16 cone origins, but not impact craters. Each Martian impact crater group has R 1.00 (i.e., 17 the craters are spaced at least as far apart as expected at random). Similar degrees of 18 clustering preclude discrimination between rootless cones and ice mounds based solely on 19 R values.
    [Show full text]
  • Geologic Map of Mars 1: 600 000 Gusev Crater Region M 600K 14.00S/175.50E G
    Geologic Map of Mars 1: 600 000 Gusev Crater Region M 600k 14.00S/175.50E G GEOLOGIC UNITS 188°00’ West 187°30’ 187°00’ 186°30’ 186°00’ 185°30’ 185°00’ 184°30’ 184°00’ 183°30’ 183°00’ 182°30’ 182°00’ 181°30’ 181°00’ West 172°00’ East 172°30’ 173°00’ 173°30’ 174°00’ 174°30’ 175°00’ 175°30’ 176°00’ 176°30’ 177°00’ 177°30’ 178°00’ 178°30’ 179°00’ East -10°00’ -10°00’ Highlands -10°07’ A -10°07’ v Modified Gusev highland formation (MGHf) e r n Durius formation (Df) u -10°30’ -10°30’ s Gusev highland formation (GHf) -10°30’ R -10°30’ Himalaya formation (Hf) u p Lowlands e s A p o l l i n a r i s P a t e r a Suici formation (2) (Sf2) -11°00’ -11°00’ Suici formation (1) (Sf1) -11°00’ Zutphen Galdakao formation (ZGf) Death Valley formation (DVf) A p o l l i n a r i s S u l c i Bermuda formation (Bf) -11°30’ -11°30’ Z e p h y r i a M e n s a e -11°30’ -11°30’ Apollinaris formation (Af) Vaucouleurs formation-mesas (Vfm) Vaucouleurs formation (1) (Vf1) -12°00’ -12°00’ Vaucouleurs formation (2) (Vf2) -12°00’ -12°00’ Gusev Crater Gusev Crivitz formation (GCf) Ma'adim Vallis formation (MVf) -12°30’ -12°30’ Manhattan formation (Mf) -12°30’ -12°30’ Thira formation(Tf) Paris formation (Pf) -13°00’ -13°00’ Zandfoort formation (Zf) Gusev rim formation (Grf) -13°00’ -13°00’ Features G a l d a k a o Groove -13°30’ -1330’ Ridge -13°30’ Channel Crater rim d e V a u c o u l e u r s Degraded, buried crater rim -14°00’ -14°00’ Z u t p h e n Central peak of impact crater -14°00’ -14°00’ Landslide G u s e v Contacts Certain -14°30’ -14°30’ Approximate T h i r a -14°30’
    [Show full text]
  • Distribution of Rocks on the Gusev Plains and on Husband Hill, Mars J
    GEOPHYSICAL RESEARCH LETTERS, VOL. 33, L16202, doi:10.1029/2006GL026964, 2006 Click Here for Full Article Distribution of rocks on the Gusev Plains and on Husband Hill, Mars J. A. Grant,1 S. A. Wilson,1 S. W. Ruff,2 M. P. Golombek,3 and D. L. Koestler4 Received 19 May 2006; revised 12 July 2006; accepted 21 July 2006; published 29 August 2006. [1] The population of rocks larger than 15 cm in diameter al., 2000, Greeley et al., 2005], but perhaps Noachian) was measured at 36 locations imaged by the Spirit rover and of uncertain origin [Squyres et al., 2006; Arvidson et al., over 4 km of the traverse across the Gusev plains and 2006]. We examined the rock population of the surfaces at Husband Hill in Gusev crater on Mars. The rock population regular intervals along the traverse of the Spirit rover observed on plains surfaces is consistent with impact (Figure 1) to determine whether there was any significant fragmentation of rubbly/fractured volcanics and reveals variability among presumably different geomorphic surfa- little evidence for modification by secondary processes or ces that might reflect a fluvial/alluvial contribution to the weathering. Interpretation of counts from Husband Hill impact-derived blocks and/or modification by weathering or suggest an influence by bedrock for rocks larger than 0.5 m alternate geomorphic processes. across, but the distribution of smaller rocks is consistent with ejecta possessing contributions from pre-plains impact 2. Measuring the Rock Population events. Results indicate plains surfaces experienced only tens of centimeters of eolian erosion/deposition since the [4] The rock population was characterized by measuring Hesperian, whereas meters rather than tens of meters of the maximum visible axis of all rocks larger than 15 cm at erosion modified Husband Hill since the early Hesperian.
    [Show full text]
  • Geologic Mapping of Gusev Crater, Mars: Gusev Rim and Floor Characteristics
    Planetary Geologic Mappers 2021 (LPI Contrib. No. 2610) 7020.pdf GEOLOGIC MAPPING OF GUSEV CRATER, MARS: GUSEV RIM AND FLOOR CHARACTERISTICS. David A. Crown1, Frank C. Chuang1, James W. Rice1, Steven W. Ruff2, and Stephen P. Scheidt1,3,4, 1Planetary Science Institute, 1700 E. Ft. Lowell Rd., Suite 106, Tucson, AZ 85719 ([email protected]), 2Arizona State University, Tempe, AZ 85287, 3Howard University, Washington, DC 20059, 4Center for Research & Exploration in Space Science and Technology, Greenbelt, MD 20771. Introduction: The geologic complexity of Gusev the crater floor. crater (~160 km diameter; 14.53°S, 175.52°E) and its Gusev Crater Floor: Gusev floor materials have surroundings have been revealed through orbital been attributed to aeolian deposits overlying lava flows remote sensing coupled with in situ exploration of the [11]; mass-wasting and channel deposits [12]; fluvio- Columbia Hills and adjacent volcanic plains by the lacustrine deposits [6-7]; and basaltic lava flows [8, MER Spirit rover [e.g., 1-4]. Gusev crater’s geologic 13-15]. Although Spirit confirmed the presence of history has been attributed to the combined effects of a basalt, questions remain regarding the overall geologic variety of geologic processes that span much of evolution of Gusev. Martian history. We have initiated a new geologic Figure 1 shows our preliminary geologic map of mapping investigation of Gusev crater, designed to Gusev floor materials. Using 5-6 m/pixel CTX images, produce a 1:250K-scale, formal geologic map focused we have identified eight geologic units, including: two on the geologic evolution of the Gusev rim and floor ridged volcanic plains, Ma’adim debris flow, dissected (Figures 1-3).
    [Show full text]
  • Columbus Crater HLS2 Hangout: Exploration Zone Briefing
    Columbus Crater HLS2 Hangout: Exploration Zone Briefing Kennda Lynch1,2, Angela Dapremont2, Lauren Kimbrough2, Alex Sessa2, and James Wray2 1Lunar and Planetary Institute/Universities Space Research Association 2Georgia Institute of Technology Columbus Crater: An Overview • Groundwater-fed paleolake located in northwest region of Terra Sirenum • ~110 km in diameter • Diversity of Noachian & Hesperian aged deposits and outcrops • High diversity of aqueous mineral deposits • Estimated 1.5 km depth of sedimentary and/or volcanic infill • High Habitability and Biosignature Preservation Potential LZ & Field Station Latitude: 194.0194 E Longitude: 29.2058 S Altitude: +910 m SROI #1 RROI #1 LZ/HZ SROI #4 SROI #2 SROI #5 22 KM HiRISE Digital Terrain Model (DTM) • HiRISE DTMs are made from two images of the same area on the ground, taken from different look angles (known as a stereo-pair) • DTM’s are powerful research tools that allow researchers to take terrain measurements and model geological processes • For our traversability analysis of Columbus: • The HiRISE DTM was processed and completed by the University of Arizona HiRISE Operations Center. • DTM data were imported into ArcMap 10.5 software and traverses were acquired and analyzed using the 3D analyst tool. • A slope map was created in ArcMap to assess slope values along traverses as a supplement to topography observations. Slope should be ≤30°to meet human mission requirements. Conclusions Traversability • 9 out of the 17 traverses analyzed met the slope criteria for human missions. • This region of Columbus Crater is traversable and allows access to regions of astrobiological interest. It is also a possible access point to other regions of Terra Sirenum.
    [Show full text]
  • Chapter Vi Report of Divisions, Commissions, and Working
    CHAPTER VI REPORT OF DIVISIONS, COMMISSIONS, AND WORKING GROUPS Downloaded from https://www.cambridge.org/core. IP address: 170.106.33.42, on 24 Sep 2021 at 09:23:58, subject to the Cambridge Core terms of use, available at https://www.cambridge.org/core/terms. https://doi.org/10.1017/S0251107X00011937 DIVISION I FUNDAMENTAL ASTRONOMY Division I provides a focus for astronomers studying a wide range of problems related to fundamental physical phenomena such as time, the intertial reference frame, positions and proper motions of celestial objects, and precise dynamical computation of the motions of bodies in stellar or planetary systems in the Universe. PRESIDENT: P. Kenneth Seidelmann U.S. Naval Observatory, 3450 Massachusetts Ave NW Washington, DC 20392-5100, US Tel. + 1 202 762 1441 Fax. +1 202 762 1516 E-mail: [email protected] BOARD E.M. Standish President Commission 4 C. Froeschle President Commisison 7 H. Schwan President Commisison 8 D.D. McCarthy President Commisison 19 E. Schilbach President Commisison 24 T. Fukushima President Commisison 31 J. Kovalevsky Past President Division I PARTICIPATING COMMISSIONS: COMMISSION 4 EPHEMERIDES COMMISSION 7 CELESTIAL MECHANICS AND DYNAMICAL ASTRONOMY COMMISSION 8 POSITIONAL ASTRONOMY COMMISSION 19 ROTATION OF THE EARTH COMMISSION 24 PHOTOGRAPHIC ASTROMETRY COMMISSION 31 TIME Downloaded from https://www.cambridge.org/core. IP address: 170.106.33.42, on 24 Sep 2021 at 09:23:58, subject to the Cambridge Core terms of use, available at https://www.cambridge.org/core/terms. https://doi.org/10.1017/S0251107X00011937 COMMISSION 4: EPHEMERIDES President: H. Kinoshita Secretary: C.Y. Hohenkerk Commission 4 held one business meeting.
    [Show full text]
  • Ebook < Impact Craters on Mars # Download
    7QJ1F2HIVR # Impact craters on Mars « Doc Impact craters on Mars By - Reference Series Books LLC Mrz 2012, 2012. Taschenbuch. Book Condition: Neu. 254x192x10 mm. This item is printed on demand - Print on Demand Neuware - Source: Wikipedia. Pages: 50. Chapters: List of craters on Mars: A-L, List of craters on Mars: M-Z, Ross Crater, Hellas Planitia, Victoria, Endurance, Eberswalde, Eagle, Endeavour, Gusev, Mariner, Hale, Tooting, Zunil, Yuty, Miyamoto, Holden, Oudemans, Lyot, Becquerel, Aram Chaos, Nicholson, Columbus, Henry, Erebus, Schiaparelli, Jezero, Bonneville, Gale, Rampart crater, Ptolemaeus, Nereus, Zumba, Huygens, Moreux, Galle, Antoniadi, Vostok, Wislicenus, Penticton, Russell, Tikhonravov, Newton, Dinorwic, Airy-0, Mojave, Virrat, Vernal, Koga, Secchi, Pedestal crater, Beagle, List of catenae on Mars, Santa Maria, Denning, Caxias, Sripur, Llanesco, Tugaske, Heimdal, Nhill, Beer, Brashear Crater, Cassini, Mädler, Terby, Vishniac, Asimov, Emma Dean, Iazu, Lomonosov, Fram, Lowell, Ritchey, Dawes, Atlantis basin, Bouguer Crater, Hutton, Reuyl, Porter, Molesworth, Cerulli, Heinlein, Lockyer, Kepler, Kunowsky, Milankovic, Korolev, Canso, Herschel, Escalante, Proctor, Davies, Boeddicker, Flaugergues, Persbo, Crivitz, Saheki, Crommlin, Sibu, Bernard, Gold, Kinkora, Trouvelot, Orson Welles, Dromore, Philips, Tractus Catena, Lod, Bok, Stokes, Pickering, Eddie, Curie, Bonestell, Hartwig, Schaeberle, Bond, Pettit, Fesenkov, Púnsk, Dejnev, Maunder, Mohawk, Green, Tycho Brahe, Arandas, Pangboche, Arago, Semeykin, Pasteur, Rabe, Sagan, Thira, Gilbert, Arkhangelsky, Burroughs, Kaiser, Spallanzani, Galdakao, Baltisk, Bacolor, Timbuktu,... READ ONLINE [ 7.66 MB ] Reviews If you need to adding benefit, a must buy book. Better then never, though i am quite late in start reading this one. I discovered this publication from my i and dad advised this pdf to find out. -- Mrs. Glenda Rodriguez A brand new e-book with a new viewpoint.
    [Show full text]
  • Meter-Scale Slopes of Candidate MER Landing Sites from Point Photoclinometry Ross A
    JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 108, NO. E12, 8085, doi:10.1029/2003JE002120, 2003 Meter-scale slopes of candidate MER landing sites from point photoclinometry Ross A. Beyer and Alfred S. McEwen Department of Planetary Sciences, University of Arizona, Tucson, Arizona, USA Randolph L. Kirk Astrogeology Team, U.S. Geological Survey, Flagstaff, Arizona, USA Received 13 May 2003; revised 16 July 2003; accepted 22 August 2003; published 4 December 2003. [1] Photoclinometry was used to analyze the small-scale roughness of areas that fall within the proposed Mars Exploration Rover (MER) 2003 landing ellipses. The landing ellipses presented in this study were those in Athabasca Valles, Elysium Planitia, Eos Chasma, Gusev Crater, Isidis Planitia, Melas Chasma, and Meridiani Planum. We were able to constrain surface slopes on length scales comparable to the image resolution (1.5 to 12 m/pixel). The MER 2003 mission has various engineering constraints that each candidate landing ellipse must satisfy. These constraints indicate that the statistical slope values at 5 m baselines are an important criterion. We used our technique to constrain maximum surface slopes across large swaths of each image, and built up slope statistics for the images in each landing ellipse. We are confident that all MER 2003 landing site ellipses in this study, with the exception of the Melas Chasma ellipse, are within the small-scale roughness constraints. Our results have provided input into the landing hazard assessment process. In addition to evaluating the safety of the landing sites, our mapping of small-scale roughnesses can also be used to better define and map morphologic units.
    [Show full text]
  • Amir's Visit Gives Fresh Impetus to Qatar-China Ties
    BUSINESS | Page 1 SPORT | Page 8 Weiss strike helps Gharafa QFZA signs three retain MoUs with top QSL Cup entities in China published in QATAR since 1978 FRIDAY Vol. XXXIX No. 11081 February 1, 2019 Jumada I 26, 1440 AH GULF TIMES www. gulf-times.com 2 Riyals In brief ARAB WORLD | Politics Lebanese leaders agree Amir’s visit gives fresh on new govt: sources Lebanese leaders reached a deal yesterday to set up a new unity government, three political sources from diff erent factions said, ending nine months of wrangling over how to share out cabinet portfolios in the impetus to Qatar-China ties heavily indebted state. It will be the third government led by the Western- backed Saad al-Hariri. Page 4 zSheikh Tamim, President Xi witness signing of several MoUs REGION | Confl ict UN ‘deeply concerned’ zAmir expresses Qatar’s willingness to invest more in China about Yemen hostilities United Nations Special Envoy for Yemen Martin Griff iths is deeply concerned about recent hostilities in the country and is urging all sides to reduce tensions, his off ice said on its Twitter account yesterday. Yemen’s Houthis have agreed with the Saudi- backed government to implement a ceasefire in Hodeidah province and withdraw their respective forces as part of a UN-sponsored peace agreement signed in Sweden in December. REGION | Sanctions Iran welcomes new EU trade entity as ‘fi rst step’ Tehran yesterday cautiously welcomed as a “first step” the expected launch of an EU trade entity aimed at saving Iran’s nuclear deal by His Highness the Amir Sheikh Tamim bin Hamad al-Thani and Chinese President bypassing US sanctions.
    [Show full text]
  • Karadag Nature Reserve of National Academy of Science of Ukraine
    Interpretative Trails on the Ground: Support to the Management of Natural Protected Areas in the Black Sea Region “InterTrails” GUIDELINES ON NATURE INTERPRETATION Odessa-2013 GUIDELINES ON NATURE INTERPRETATION Edited by Oleg Rubel, Anastasiya Snigirova Authors: Natalia Fedoronchuk, Vladimir Poltorak, Galina Bezvushko, Oleh Derkach, Tatyana Balatskaya, Mykola Rozhenko, Julia Nazarchuk This book has been prepared in the frame of the Project “Interpretative Trails on the Ground: Support to the Management of Natural Protected Areas in the Black Sea Region” (InterTrails) funded by European Union. The authors have developed methodological and methodical basis of interpretation of nature protected areas. The structure and detailed description of four ecological trails located in protected areas of the Black Sea coast: Karadag Natural Reserve of NAS of Ukraine, Danube Biosphere Reserve of NAS of Ukraine, Lower Dniester National Nature Park, Regional Landscape Park "Kinburn Sand-spit". The book is designed for tour guides, travel managers and campaigns, staff of protected area, researchers, students and wide range of readers. Reviewers: Alexander Voloshkevich, PhD, director of Danube Biosphere Reserve of National Academy of Science of Ukraine Natalia Gorіap, director of touristic company "Salіx" Michael Zhmud, Ph.D., director of the touristic company "Pelican-Vilkovo-Tour" Ivan Rusev, Ph.D., Ukrainian Anti-Plague Research Institute named after I. I. Mechnikov Vasiliy Fedorenko, PhD, deputy director of the Danube Biosphere Reserve of National
    [Show full text]
  • Structure, Stratigraphy, and Origin of Husband Hill, Columbia Hills, Gusev Crater, Mars T
    JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 113, E06S03, doi:10.1029/2007JE003041, 2008 Click Here for Full Article Structure, stratigraphy, and origin of Husband Hill, Columbia Hills, Gusev Crater, Mars T. J. McCoy,1 M. Sims,2 M. E. Schmidt,1 L. Edwards,2 L. L. Tornabene,3 L. S. Crumpler,4 B. A. Cohen,5 L. A. Soderblom,6 D. L. Blaney,7 S. W. Squyres,8 R. E. Arvidson,9 J. W. Rice Jr.,10 E. Tre´guier,11 C. d’Uston,11 J. A. Grant,12 H. Y. McSween Jr.,13 M. P. Golombek,7 A. F. C. Haldemann,14 and P. A. de Souza Jr.15,16 Received 15 November 2007; revised 26 February 2008; accepted 7 April 2008; published 17 June 2008. [1] The strike and dip of lithologic units imaged in stereo by the Spirit rover in the Columbia Hills using three-dimensional imaging software shows that measured dips (15– 32°) for bedding on the main edifice of the Columbia Hill are steeper than local topography (8–10°). Outcrops measured on West Spur are conformable in strike with shallower dips (7–15°) than observed on Husband Hill. Dips are consistent with observed strata draping the Columbia Hills. Initial uplift was likely related either to the formation of the Gusev Crater central peak or ring or through mutual interference of overlapping crater rims. Uplift was followed by subsequent draping by a series of impact and volcaniclastic materials that experienced temporally and spatially variable aqueous infiltration, cementation, and alteration episodically during or after deposition. West Spur likely represents a spatially isolated depositional event.
    [Show full text]