OF MR. TEBBUTT's OBSERVATORY, Fellow of the Royal Astronomical Society, Londo

Total Page:16

File Type:pdf, Size:1020Kb

OF MR. TEBBUTT's OBSERVATORY, Fellow of the Royal Astronomical Society, Londo m, ETC. 8. W. BurnhaM* Astron. (Yerkw) R E P o R T OF MR. TEBBUTT'S OBSERVATORY, WINDSOR, NEW SOUTH WALES, FOR THK YEAR 1888, JOHN TEBBUTT, Fellow of the Royal Astronomical Society, London; Member of the Royal Society of New South Wales, and Corresponding Member of the Ethnographic - Institute, Paris, and of the Queensland Branch of the Royal Geographical Society of Australasia. !Syrltic^i : GEORGE MURE AY & CO., PRINTERS, 91 CLAKE3SCE STREET. 1889. REPORT OF MR. TEBBUTT'S OBSERVATORY, WINDSOR, NEW SOUTH WALES, FOR THE VICAR 1888, \ 13 Y JOHN TEBBUTT, Fellow of the Royal Astronomical Society, London; Member of the Royal Society of 2\eiv South JFales, and Corresponding Member of the Ethnographic Institute, Paris, and of the Queensland Branch of the Royal Geographical Society of Australasia. JSytlncy : GEORGE MURRAY & CO., PRINTERS, 91 CLARENCE STREET. 1880. CONTENTS. ♦ PAGE. Buildings and Instruments 5 Geographical Position of the Observatory 6 Meridian Work 7 Instrumental Errors and Chronometer Errors and Hates 11 Extra-Meridian Work 19 Meteorological Observations 22 Publications "• 22 The Library 25 Personal Establishment 26 Proposed Work for year 1889 26 Observations Utilised since 1887 27 Conclusion 27 Presents received for the Library from September 1st, 1887, to December 31st, 1888 28 REPORT OF THE WINDSOR OBSERVATORY. For 1Q88. ♦ At the close of the year 1887, a pamphlet of 74 pages was published, entitled a "History and Description of Mr. Tebbutt's Observatory, Windsor, New South "Wales." This little volume contains a detailed account of the Observatory buildings and of their instrumental equip¬ ment, and furnishes a list of all the scientific papers published by the proprietor, and of presents to the Observatory library, down to the close of August, 1887. The present Report will bring down the History of the Observatory to the close of the year 1888, under various heads, as follow :— Buildings and Instruments. These remain as they were at the close of August, 1887, so that a description of them will be unnecessary here. A general notion of the buildings can be formed from the frontispiece of the publication referred to. It will suffice to state that the principal instruments are a 3-inch transit instrument, by Cooke and Sons of York ; a sidereal and a mean-time chronometer, by Parkinson and Prodsham and by Poole, respectively; an 8-inch equatorial, by Grubb of Dublin; a 4^-inch equatorial, by Cooke and Sons; and a SJ-inch refractor, by Jones. [ 6 ] Geographical Position of the Observatory. The best local determination of the longitude is that published by the author in R. Ast. Society's Monthly Notices, Yol. XL., p. 440. The result is lOh. 3m. 21.81s. E. of Greenwich, and is derived from twenty-three occultation phases, namely, nineteen disappearances and four reappearances. The occulted stars are well known ones, and the moon's tabular places were corrected from meridian observations at Greenwich, Radcliffe, and Washington. With a view to obtain a fundamental meridian for the Australian Colonies from absolute methods, Dr. Auwers of Berlin, in 1884, discussed a series of seventy-six disappearances of stars at the moon's dark limb, observed at Windsor in the years 1873, 1874, 1875, and 1876, and arrived at lOh. 3m. 21.25s. E. as the longitude of Windsor, a result which differs only 0.56s. from that just mentioned. Combining this value with that derived for Melbourne from ten disappearances and two reappearances in the years 1874 and 1875, with moon-culmination results at Sydney and Melbourne, and approximate values of the telegraphic differences of longitude between Sydney and Melbourne and Sydney and Windsor, he derived lOh. 4m. 49.60s. E. as the longitude of Sydney. Subtracting 1m. 28.83s. from this result, he gets lOh. 3m. 20.77s. E. as the longitude of Windsor. In 1887, Professor Harkness of Washington, recognising the great importance of the result derived for Windsor from the occultations of 1873-76, suggested to me the desirability of determining with all possible accuracy the differences of longitude between the Windsor Observatory and the Government Observatories at Sydney and Melbourne. Immediately on the receipt of Professor Harkness' letter, I communi¬ cated with Mr. Lenehan, the Acting Government Astronomer at Sydney, and Mr. Ellery, the Government Astronomer at Melbourne, and the result was that exchanges of telegraphic signals were made with the most satisfactory results, as described in a paper read before the Royal Astronomical Society in April, 1888, and published in the Society's Notices, Yol. XLVIIL, p. 313. The Windsor observations, in full detail, were [ 7 ] forwarded to Professor Harkness, together Avitk the Sydney and Melbourne signals, clock-errors, and rates. He proposes to work out the Windsor chronometer errors and rates by the method of least squares, in order to get the best possible values from the observations. Mean¬ while, adopting 1m. 29.39s. and 24m. 55.26s. as the differences of longitude between Sydney and "Windsor and Sydney and Melbourne respectively (see the author's paper above referred to), and applying these amended differences according to the combination employed by Dr. Auwers, we get lOh. 4m. 49.90s. E. and lOh. 3m. 20.51s. E. as the longitudes of Sydney and Windsor from Greenwich. Considering the number of links in the whole chain of telegraphic connection with Greenwich, this result is probably as trustworthy as that derived from the late telegraphic connection with Singapore. The most reliable value of the latitude is — 33° 36 30.8 , which was derived from a series of prime vertical observations, in 1881, of well- determined stars close to the zenith with the 3-inch transit instrument. (See the author's paper in R.A.S. Monthly Notices, Yol. XLIY., p. 101.) Nothing further has been done in the way of investigating the latitude, if we except the circumstance that in 1887 the" author made a trigonometrical connection between the Obser¬ vatory transit-instrument and the north terminal of the Government base-line, about three miles nearly due west of the Observatory. This connection, which was estab¬ lished with an ordinary steel tape and a 5-inch theodolite reading to minutes of arc, gave - 33° 36' 30.5" as the latitude of the transit and equatorial piers, which differs only 0.3" from the value obtained directly from the prime vertical observations of 1881. The geographical latitude of the terminal as furnished by the head of the Trigonometrical Survey is —33° 35' 58.07". Meridian Work. This has been done throughout with the 3-inch transit instrument in connection with sidereal chrono¬ meter (Parkinson and Erodsham) No. 1042. The transit system consists of five wires, designated A, B, C, D, and [ 8 ] E, in the order of transit above the pole when the clamp is east. The equatorial distances in sidereal time of the four outer wires from the middle wire were re-determined from all the transits of circumpolar stars observed in 1887, with the following results:—Ah- 19.492s. B+9.782s. D—10.001s. E —19.656s., which have been employed throughout the reductions of 1888. The reduction for a complete observation of an equatorial star at the upper culmination, clamp east, has therefore been—0.077s. The reduction for any other star is this quantity multi¬ plied by the secant of the star's declination, and has been taken from a MS. table having for its argument the star's declination. For incomplete transits the reduction for an equatorial star is taken from a MS. table giving the algebraic means of the observed wires. The observations have all been made by the eye and ear method. The level and azimuth errors of the transit instrument, considering the founda¬ tion of the pier, which consists of clay and loam, have been pretty steady throughout the year. The level employed is a striding one of 1130 feet radius, each division being equal to 0.8". The inclination was determined once at least on each evening of observation by four readings of each extremity of the bubble, the level being twice reversed during the operation. On some occasions, and always when the transit instrument has been reversed, two or more sets of readings have been taken. When the western pivot is the higher, the level error is regarded as positive. The collimation error was determined at intervals of a few days by comparing the middle wire in both positions of the axis of rotation with the corresponding wire of a two-inch transit instru¬ ment on a pier a little north of the transit-room. The middle wire of the collimator is slightly inclined for the purpose, and the comparison is always made near the horizontal wires. As there is no micrometer in connec¬ tion with the transit system, the distance of the middle wire from that of the collimator is estimated for each position of the axis of rotation in terms of the diameter of the wire. Half the total displacement reduced to seconds of arc from the known diameter of the wire is [ 9 ] regarded as the collimation error. "When the middle wire falls east of the collimation axis of the telescope with the clamp east, the collimation error is regarded as positive. On every occasion when the instrument has been reversed, star transits have been observed in both positions of the rotation axis, and by allowing for chronometer rate, it has been found that the estimations for collimation error are quite as reliable as the results which might be obtained by the application of the micro¬ meter to so small an instrument. The collimation errors for dates between those on which the reversals were made are simply interpolated.
Recommended publications
  • 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]
  • VV D C-A- R 78-03 National Space Science Data Center/ World Data Center a for Rockets and Satellites
    VV D C-A- R 78-03 National Space Science Data Center/ World Data Center A For Rockets and Satellites {NASA-TM-79399) LHNAS TRANSI]_INT PHENOMENA N78-301 _7 CATAI_CG (NASA) 109 p HC AO6/MF A01 CSCl 22_ Unc.las G3 5 29842 NSSDC/WDC-A-R&S 78-03 Lunar Transient Phenomena Catalog Winifred Sawtell Cameron July 1978 National Space Science Data Center (NSSDC)/ World Data Center A for Rockets and Satellites (WDC-A-R&S) National Aeronautics and Space Administration Goddard Space Flight Center Greenbelt) Maryland 20771 CONTENTS Page INTRODUCTION ................................................... 1 SOURCES AND REFERENCES ......................................... 7 APPENDIX REFERENCES ............................................ 9 LUNAR TRANSIENT PHENOMENA .. .................................... 21 iii INTRODUCTION This catalog, which has been in preparation for publishing for many years is being offered as a preliminary one. It was intended to be automated and printed out but this form was going to be delayed for a year or more so the catalog part has been typed instead. Lunar transient phenomena have been observed for almost 1 1/2 millenia, both by the naked eye and telescopic aid. The author has been collecting these reports from the literature and personal communications for the past 17 years. It has resulted in a listing of 1468 reports representing only slight searching of the literature and probably only a fraction of the number of anomalies actually seen. The phenomena are unusual instances of temporary changes seen by observers that they reported in journals, books, and other literature. Therefore, although it seems we may be able to suggest possible aberrations as the causes of some or many of the phenomena it is presumptuous of us to think that these observers, long time students of the moon, were not aware of most of them.
    [Show full text]
  • Geomorphologic Mapping and Mineralogy of Pits in Intercrater Plains, Northwest Circum-Hellas Region, Mars
    46th Lunar and Planetary Science Conference (2015) 2542.pdf GEOMORPHOLOGIC MAPPING AND MINERALOGY OF PITS IN INTERCRATER PLAINS, NORTHWEST CIRCUM-HELLAS REGION, MARS. F. C. Chuang, E. Z. Noe Dobrea, S. C. Mest, and D. A. Crown, Planetary Science Institute, 1700 E. Ft. Lowell Road, Suite 106, Tucson, AZ 85719 USA ([email protected]). Introduction: The circum-Hellas region has intercrater plains [8]. These occur in pits, or irregular received much attention due to the area's potential for depressions by [3]. A total of 39 irregular depressions, past habitable conditions on Mars. In particular, there 17 within intracrater deposits and 22 within intercrater is evidence for both marine/lacustrine [1-3] and plains were identified in an area between 45°-65° E hydrothermal systems [4] around Hellas sometime after and 22.5°-32.5° S [3]. The pits provide windows into its formation. Regional spectroscopic studies of Hellas the history of the upper crust and(or) the depositional [5,6] support the interpretation for aqueous activity by processes of the materials that infilled the plains. Here providing evidence for phyllosilicates and sulfates we present detailed mapping of geomorphologic units associated with geological features on and near the rim within one of these pits along the NW circum-Hellas of Hellas [7-9]. Evidence has also been found for rim. hydrothermally-altered products on plains near Hellas Data and Methods: Geomorphologic mapping was [8] and in the circum-Hellas region [9]. performed digitally using ArcGIS 10.2.2 software. All Although recent studies have surveyed regions for mapped geomorphologic units were stored as mapped aqueously-altered minerals near Hellas, the abundance polygons.
    [Show full text]
  • Dental Hygienist List 01/01/2019 1
    DENTAL HYGIENIST LIST 01/01/2019 Full Name First Name Middle Name Last Name Suffix Professional Title License Type License Maby Araceli Abarca Maby Araceli Abarca RDH Dental Hygienist 101108 Daveadele M Abel Daveadele M Abel RDH Dental Hygienist 2116 Yohel Berhane Abraha Yohel Berhane Abraha RDH Dental Hygienist 102202 Dawnetta Kay Abraham Dawnetta Kay Abraham RDH Dental Hygienist 2782 Christle Joie Abuan Christle Joie Abuan RDH Dental Hygienist 102423 Merilyn Abundis Merilyn Abundis RDH Dental Hygienist 102405 Vanessa Acevedo Vanessa Acevedo RDH Dental Hygienist 101723 Liezl Lachica Acosta Liezl Lachica Acosta RDH Dental Hygienist 102397 Jennifer Lynn Adamo Jennifer Lynn Adamo RDH Dental Hygienist 101582 Emily Fouse Adams Emily Fouse Adams RDH Dental Hygienist 101416 Grace R Adams Grace R Adams RDH Dental Hygienist 969 Mary Rita Adams Mary Rita Adams RDH Dental Hygienist 2915 Veronica Anne Adams Veronica Anne Adams RDH Dental Hygienist 101803 Mary Alice Adelberg Mary Alice Adelberg RDH Dental Hygienist 2080 Jennifer Ann Agao Jennifer Ann Agao RDH Dental Hygienist 3453 Josselyn Daniela Aguilar Josselyn Daniela Aguilar RDH Dental Hygienist 101925 Gretchen Jessenia Aguirre Gretchen Jessenia Aguirre RDH Dental Hygienist 101171 Ingeborg Agnes Aigner Ingeborg Agnes Aigner RDH Dental Hygienist 2995 Craig Alcantara Alanguilan Craig Alcantara Alanguilan RDH Dental Hygienist 102307 Keosha Aneilia Alcinnat Keosha Aneilia Alcinnat RDH Dental Hygienist 102395 Cam Thi Thuy Aldana Cam Thi Thuy Aldana RDH Dental Hygienist 4212 Valerie Lynn Alexander
    [Show full text]
  • A Sedimentary Origin for Intercrater Plains North of the Hellas Basin
    A sedimentary origin for intercrater plains north of the Hellas basin: Implications for climate conditions and erosion rates on early Mars Francesco Salese, Veronique Ansan, Nicolas Mangold, John Carter, Anouck Ody, François Poulet, Gian Gabriele Ori To cite this version: Francesco Salese, Veronique Ansan, Nicolas Mangold, John Carter, Anouck Ody, et al.. A sedimentary origin for intercrater plains north of the Hellas basin: Implications for climate conditions and erosion rates on early Mars. Journal of Geophysical Research. Planets, Wiley-Blackwell, 2016, 121 (11), pp.2239-2267. 10.1002/2016JE005039. hal-02305998 HAL Id: hal-02305998 https://hal.archives-ouvertes.fr/hal-02305998 Submitted on 4 Oct 2019 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. PUBLICATIONS Journal of Geophysical Research: Planets RESEARCH ARTICLE A sedimentary origin for intercrater plains north of the Hellas 10.1002/2016JE005039 basin: Implications for climate conditions Key Points: and erosion rates on early Mars • Intercrater plains on the northern rim of Hellas basin are
    [Show full text]
  • The Geomorphic and Stratigraphic Analysis of Crater Terby And
    1 The geomorphic and stratigraphic 2 analysis of Crater Terby and layered 3 deposits north of Hellas basin, Mars 4 5 6 Sharon A. Wilson 7 Center for Earth and Planetary Studies, National Air and Space Museum, Smithsonian 8 Institution, Washington, D.C., USA 9 10 Alan D. Howard 11 Department of Environmental Sciences, University of Virginia, Charlottesville, 12 Virginia, USA 13 14 Jeffrey M. Moore 15 Space Sciences Division, NASA Ames Research Center, Moffett Field, California, USA 16 17 John A. Grant 18 Center for Earth and Planetary Studies, National Air and Space Museum, Smithsonian 19 Institution, Washington, D.C., USA 20 21 22 Keywords: layered deposits, Mars, sediment, stratigraphy 23 24 Index Terms: 5470 Surface materials and properties; 5415 Erosion and weathering; 25 5416 Glaciation; 1861 Sedimentation; 1824 Geomorphology 26 27 28 Revised version submitted to JGR-Planets, February 13, 2007 29 1 29 Abstract 30 The geologic history of Crater Terby is developed through geomorphic and 31 stratigraphic analyses within the regional context of the Hellas basin. Terby exhibits ~2 32 km-thick sequences of layers that consist of repetitive, sub-horizontal and laterally 33 continuous beds. The layers are predominantly fine-grained based on their ease of 34 aeolian erosion although a few consolidated layers weather to form rubbly talus. The 35 grain size or composition of the deposited materials fluctuated, producing layering, but 36 the overall properties of the deposits are similar throughout the sequence and are 37 comparable to layered deposits in other crater basins around Hellas. The original 38 depositional geometry, physical and geological characteristics of the layers in Terby and 39 the other basins leads us to favor a lacustrine origin, but a loess-like origin cannot be 40 ruled out.
    [Show full text]
  • General Disclaimer One Or More of the Following Statements May Affect
    https://ntrs.nasa.gov/search.jsp?R=19680018720 2020-03-12T10:00:05+00:00Z General Disclaimer One or more of the Following Statements may affect this Document This document has been reproduced from the best copy furnished by the organizational source. It is being released in the interest of making available as much information as possible. This document may contain data, which exceeds the sheet parameters. It was furnished in this condition by the organizational source and is the best copy available. This document may contain tone-on-tone or color graphs, charts and/or pictures, which have been reproduced in black and white. This document is paginated as submitted by the original source. Portions of this document are not fully legible due to the historical nature of some of the material. However, it is the best reproduction available from the original submission. Produced by the NASA Scientific and Technical Information Program ·• NASA TECHNICAL NASA TR R-277 REPORT < V, < z: CHRONOLOGICAL CATALOG OF REPORTED LUNAR EVENTS by Barbara M. Middlehurst University of Arizona Jaylee M. Burley Goddard Space Flight Center Patrick Moore Armagh Planetarium and Barbara L. Welther Smithsonian Astrophysical Observatory NATIONAL AERONAUTICS AND SPACE ADMINISTRATION • WASHINGTON, D. C. • JULY 1968 NASA TR R-277 CHRONOLOGICAL CATALOG OF REPORTED LUNAR EVENTS By Barbara M. Middlehurst University of Arizona Tucson, Ariz. Jaylee M. Burley Goddard Space Flight Center Greenbelt, Md. Patrick Moore Armagh Planetarium Armagh, Northern Ireland and Barbara L. Welther Smithsonian Astrophysical Observatory Cambridge, Mass. NATIONAL AERONAUTICS AND SPACE ADMINISTRATION For sale by the Clearinghouse for Federal Scientific and Technical Information Springfield, Virginia 22151 - CFSTI price $3.00 ABSTRACT A catalog of reports of lunar events, or temporary changes on the moon, has been compiled based on literature covering more than four centuries.
    [Show full text]
  • Topographic Map of Mars
    U.S. DEPARTMENT OF THE INTERIOR OPEN-FILE REPORT 02-282 U.S. GEOLOGICAL SURVEY Prepared for the NATIONAL AERONAUTICS AND SPACE ADMINISTRATION 180° 0° 55° –55° Russell Stokes 150°E NOACHIS 30°E 210°W 330°W 210°E NOTES ON BASE smooth global color look-up table. Note that the chosen color scheme simply 330°E Darwin 150°W This map is based on data from the Mars Orbiter Laser Altimeter (MOLA) 30°W — 60° represents elevation changes and is not intended to imply anything about –60° Chalcoporous v (Smith and others 2001), an instrument on NASA’s Mars Global Surveyor Milankovic surface characteristics (e.g. past or current presence of water or ice). These two (MGS) spacecraft (Albee and others 2001). The image used for the base of this files were then merged and scaled to 1:25 million for the Mercator portion and Rupes map represents more than 600 million measurements gathered between 1999 1:15,196,708 for the two Polar Stereographic portions, with a resolution of 300 and 2001, adjusted for consistency (Neumann and others 2001 and 2002) and S dots per inch. The projections have a common scale of 1:13,923,113 at ±56° TIA E T converted to planetary radii. These have been converted to elevations above the latitude. N S B LANI O A O areoid as determined from a martian gravity field solution GMM2 (Lemoine Wegener a R M S s T u and others 2001), truncated to degree and order 50, and oriented according to IS s NOMENCLATURE y I E t e M i current standards (see below).
    [Show full text]
  • Craters of Volcanic Origin at the Ground Surface of Mars (Collapse
    www.biogenericpublishers.com Article Type: Research Article Received: 12/01/2021 Published: 21/01/2021 DOI: 10.46718/JBGSR.2021.07.000165 Craters of Volcanic Origin at the Ground Surface of Mars (Collapse Calderas and Volcanic Pipes) Khaled Abdel-Kader Ouda* and Nadia Abdel-Fattah Sharara Geology Department, Faculty of Science, Assiut University, Assiut 71516, Egypt *Corresponding author: Khaled Abdel-Kader Ouda, Geology Department, Faculty of Science, Assiut University, Assiut 71516, Egypt Abstract A thorough examination of 300 craters on the Martian surface by satellite remote sensing (via Google Mars) has revealed that these craters which previously assumed to have been formed by meteorites are actually volcanic craters which were formed at the ground surface around a volcanic vent by lava flow or fragments of lava thrown out during eruption on Mars. The study clearly shows that all of these craters are volcanic in origin and represented by independent collapse calderas and volcanic pipes. These volcanic landforms are variable in size, morphology, topography, topographic elevation, relative age concept and history of volcanic eruption. They are occurring as independent landforms or as parasitic landforms on the flanks of shield and composite volcanoes or at the bottom floor of larger pre-existing calderas. For means of graphical correlation between different types of volcanoes on Mars the topographic and morphologic characters of 150 independent volcanoes were subjected to a detailed statistical analysis using manual cross sections across the width of each volcano. The analysis reveals the recognition of six different types of volcanic calderas and two types of volcanic pipes. The topography, morphology and relative age of these types are given.
    [Show full text]
  • Colonization: a Permanent Habitat for the Colonization of Mars
    COLONIZATION A PERMANENT HABITAT FOR THE COLONIZATION OF MARS A thesis submitted in fulfilment of the requirements of the degree of Master in Engineering Science (Research) in Mechanical Engineering BY MATTHEW HENDER THE UNIVERSITY OF AD ELAIDE SCHOOL OF MECHANICAL ENGINEERING SUPERVISOR S – DR. GERALD SCHNEIDER & COLIN HANSEN A u g u s t 2 0 0 9 315°E (45°W) 320°E (40°W) 325°E (35°W) 330°E (30°W) 335°E (25°W) 340°E (20°W) 345°E (15°W) 350°E (10°W) 355°E (5°W) 360°E (0°W) 0° 0° HYDRAOTES CHAOS . llis Dia-Cau Va vi Ra . Camiling Aromatum Chaos . Rypin Chimbote . Mega . IANI MERIDIANI PLANUM* . v Wicklow Windfall Zulanka Pinglo . Oglala Tuskegee . Bamba . CHAOS . Bahn . Locana. Tarata . Spry Manti Balboa ARABIA Huancayo . AUREUM . Groves . Vaals . Conches _ . Sitka Berseba . Kaid . Chinju Lachute . Manah Rakke CHAOS . Stobs . Byske -5° . Airy-0 . -5° Butte. Azusa Kong Timbuktu . Quorn Airy . Creel . Innsbruck XANTHE Wink TERRA TERRA A . Kholm M . Daet S A Ganges .Sfax . Paks H Batoka C Chasma . Rincon I Arsinoes . Glide R P AURORAE CHAOS A Chaos C I S E R M R I N A E R R F G A I T I A R -10° -10° M Pyrrhae C H A O S S Chaos E L L A V MARGARITIFER Eos Mensa* EOS CHASMA Beer -15° -15° alles V L o i r e Osuga Eos TERRA Chaos V a Jones l l e s Vinogradov -20° Lorica Polotsk -20° s Sigli . Kimry . Lebu Valle S Kansk .
    [Show full text]
  • Thedatabook.Pdf
    THE DATA BOOK OF ASTRONOMY Also available from Institute of Physics Publishing The Wandering Astronomer Patrick Moore The Photographic Atlas of the Stars H. J. P. Arnold, Paul Doherty and Patrick Moore THE DATA BOOK OF ASTRONOMY P ATRICK M OORE I NSTITUTE O F P HYSICS P UBLISHING B RISTOL A ND P HILADELPHIA c IOP Publishing Ltd 2000 All rights reserved. No part of this publication may be reproduced, stored in a retrieval system or transmitted in any form or by any means, electronic, mechanical, photocopying, recording or otherwise, without the prior permission of the publisher. Multiple copying is permitted in accordance with the terms of licences issued by the Copyright Licensing Agency under the terms of its agreement with the Committee of Vice-Chancellors and Principals. British Library Cataloguing-in-Publication Data A catalogue record for this book is available from the British Library. ISBN 0 7503 0620 3 Library of Congress Cataloging-in-Publication Data are available Publisher: Nicki Dennis Production Editor: Simon Laurenson Production Control: Sarah Plenty Cover Design: Kevin Lowry Marketing Executive: Colin Fenton Published by Institute of Physics Publishing, wholly owned by The Institute of Physics, London Institute of Physics Publishing, Dirac House, Temple Back, Bristol BS1 6BE, UK US Office: Institute of Physics Publishing, The Public Ledger Building, Suite 1035, 150 South Independence Mall West, Philadelphia, PA 19106, USA Printed in the UK by Bookcraft, Midsomer Norton, Somerset CONTENTS FOREWORD vii 1 THE SOLAR SYSTEM 1
    [Show full text]
  • Transactions of the Astronomical and Physical Society of Toronto 1894
    TRANSACTIONS OF THE F O R T H E Y E A R 1 8 9 4 , INCLUDING FIFTH ANNUAL REPORT. PRICE ONE DOLLAR. T O R O N T O : ROWSELL & HUTCHISON, Printers to the Society. 1895. CHARLES CARPMAEL, M. A. (CANTAB.) TRANSACTIONS OF THE F O R T H E Y E A R 1 8 9 4 , INCLUDING FIFTH ANNUAL REPORT. PRICE ONE DOLLAR. T O R O N T O : ROWSELL & HUTCHISON, Printers to the Society. 1895. CORRIGENDA. Transactions, 1890, page 29, line 8 from bottom, for “Jupiter” read “Neptune.” Transactions, 1891, page 5, line 11 from top, for “B.C. 380” read “B.C. 310.” Transactions, 1893, page 59, line 9 from top, for “7 p.m.” read “11.15 p.m.” Transactions, 1893, page 67, line 3 from bottom, value of comp. log n' should be “22132633.” Transactions, 1894, page 16, line 3 from top, for “1·500th” read “1-500th.” “ “ “ line 5, for “1·250th” read “1-250th.” Transactions, 1894, page 31, line 14 from top, for “two angles” read “three angles.” TABLE OF CONTENTS. PAGE. Officers. V Council . V Life Members . V Honourary Members . VI Corresponding Members . VI Active Members and their Addresses. VII Associate Members . X An Evening with Jupiter . Musson and others. 1 Force and Energy . Allen. 7 “ “ . Collins and others. 9 Aurora of February 23rd . Copland. 13 Colour . Hull. 17 Magnetic Stress . Collins. 25 Fallacies in Mathematics and Astronomy . Lindsay. 32 Earth Currents. Abbe. 33 Magnetic Disturbance . Carpmael. 34 Solar Parallax. Morrison. 38 Earth Currents . .Copland. 46 Meteorology . Elvins.
    [Show full text]