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Show Program
Mystic Valley Hunt Club, Inc, Dressage Show Saturday - Sunday May 1 – 2, 2021 Show Personnel Managers: Sally Hinkle Russell Secretary: Sue McKeown Technical Delegate: Ray Denis, r Judges Susanne Hamilton (ME), S Willette Brown (NJ), S Sue Mandas (OH), S Rita Brown (MA), R Adam Cropper (NH), r Vet: EMT: Farrier: Anderson Vet Services Ed Quinlan Chip Rankin 860-639-6927 860-334-4994 Show Committee Sue McKeown Sally Hinkle Russell Michelle Ugartechea Announcers Eleanor Gaumer Photography Moments in Time Brenda Cataldo [email protected] http://moments-in-time.smugmug.com/ Volunteers Thank you to all of our volunteers. Our show would not be successful without their generosity of time and effort. Cover Image Designed By Claire Bornstein MVHC May 2021 Schedule of Classes Saturday, May 1, 2021 Ring 1 8:30 AM FEI Prix St. Georges - Stakes Sue Mandas at E; Willette Brown at C 8:57 AM FEI Test of Choice 9:51 AM FEI Junior Team Test 2019 NAYC Qualifying 10:18 AM FEI Young Rider Team Test 2019 NAYC Qualifying 10:27 AM FEI Intermediate II - Brentina's Cup 10:45 AM - Break - 11:05 AM FEI Children Team Test Sue Mandas at E; Willette Brown at C; Susanne Hamilton at M 11:14 AM FEI Pony Team Test 2016 11:30 AM FEI Grand Prix - USEF Qualifier 11:39 AM Young Horse TOC Willette/Susanne/Sue Brown/Hamilton/Mandas at C 11:59 AM USDF Freestyle TOC Sue Mandas at E; Willette Brown at C; Susanne Hamilton at M 12:08 PM - Lunch Break - 12:57 PM Training Level Test 1 Willette Brown at C 1:32 PM Second Level Test 3 2:36 PM Fourth Level Test 1 3:08 PM - Break - 3:28 PM -
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 -
No. 40. the System of Lunar Craters, Quadrant Ii Alice P
NO. 40. THE SYSTEM OF LUNAR CRATERS, QUADRANT II by D. W. G. ARTHUR, ALICE P. AGNIERAY, RUTH A. HORVATH ,tl l C.A. WOOD AND C. R. CHAPMAN \_9 (_ /_) March 14, 1964 ABSTRACT The designation, diameter, position, central-peak information, and state of completeness arc listed for each discernible crater in the second lunar quadrant with a diameter exceeding 3.5 km. The catalog contains more than 2,000 items and is illustrated by a map in 11 sections. his Communication is the second part of The However, since we also have suppressed many Greek System of Lunar Craters, which is a catalog in letters used by these authorities, there was need for four parts of all craters recognizable with reasonable some care in the incorporation of new letters to certainty on photographs and having diameters avoid confusion. Accordingly, the Greek letters greater than 3.5 kilometers. Thus it is a continua- added by us are always different from those that tion of Comm. LPL No. 30 of September 1963. The have been suppressed. Observers who wish may use format is the same except for some minor changes the omitted symbols of Blagg and Miiller without to improve clarity and legibility. The information in fear of ambiguity. the text of Comm. LPL No. 30 therefore applies to The photographic coverage of the second quad- this Communication also. rant is by no means uniform in quality, and certain Some of the minor changes mentioned above phases are not well represented. Thus for small cra- have been introduced because of the particular ters in certain longitudes there are no good determi- nature of the second lunar quadrant, most of which nations of the diameters, and our values are little is covered by the dark areas Mare Imbrium and better than rough estimates. -
Commonwealth of Australia Gazette ASIC 16/02, Tuesday, 9 April 2002
= = `çããçåïÉ~äíÜ=çÑ=^ìëíê~äá~= = Commonwealth of Australia Gazette No. ASIC 16/02, Tuesday, 9 April 2002 Published by ASIC ^^ppff``==dd~~òòÉÉííííÉÉ== Contents Notices under the Corporations Act 2001 00/2496 01/1681 01/1682 02/0391 02/0392 02/0393 02/0394 02/0395 02/0396 02/0397 02/0398 02/0399 02/0400 02/0401 02/0402 02/0403 02/0404 02/0405 02/0406 02/0408 02/0409 Company deregistrations Page 43 Change of company status Page 404 Company reinstatements Page 405 ISSN 1445-6060 Available from www.asic.gov.au © Commonwealth of Australia, 2001 Email [email protected] This work is copyright. Apart from any use permitted under the Copyright Act 1968, all rights are reserved. Requests for authorisation to reproduce, publish or communicate this work should be made to: Gazette Publisher, Australian Securities and Investment Commission, GPO Box 5179AA, Melbourne Vic 3001 Commonwealth of Australia Gazette ASIC Gazette ASIC 16/02, Tuesday, 9 April 2002 Company deregistrations Page 43= = CORPORATIONS ACT 2001 Section 601CL(5) Notice is hereby given that the names of the foreign companies mentioned below have been struck off the register. Dated this nineteenth day of March 2002 Brendan Morgan DELEGATE OF THE AUSTRALIAN SECURITIES AND INVESTMENTS COMMISSION Name of Company ARBN ABBOTT WINES LIMITED 091 394 204 ADERO INTERNATIONAL,INC. 094 918 886 AEROSPATIALE SOCIETE NATIONALE INDUSTRIELLE 083 792 072 AGGREKO UK LIMITED 052 895 922 ANZEX RESOURCES LTD 088 458 637 ASIAN TITLE LIMITED 083 755 828 AXENT TECHNOLOGIES I, INC. 094 401 617 BANQUE WORMS 082 172 307 BLACKWELL'S BOOK SERVICES LIMITED 093 501 252 BLUE OCEAN INT'L LIMITED 086 028 391 BRIGGS OF BURTON PLC 094 599 372 CANAUSTRA RESOURCES INC. -
Glossary Glossary
Glossary Glossary Albedo A measure of an object’s reflectivity. A pure white reflecting surface has an albedo of 1.0 (100%). A pitch-black, nonreflecting surface has an albedo of 0.0. The Moon is a fairly dark object with a combined albedo of 0.07 (reflecting 7% of the sunlight that falls upon it). The albedo range of the lunar maria is between 0.05 and 0.08. The brighter highlands have an albedo range from 0.09 to 0.15. Anorthosite Rocks rich in the mineral feldspar, making up much of the Moon’s bright highland regions. Aperture The diameter of a telescope’s objective lens or primary mirror. Apogee The point in the Moon’s orbit where it is furthest from the Earth. At apogee, the Moon can reach a maximum distance of 406,700 km from the Earth. Apollo The manned lunar program of the United States. Between July 1969 and December 1972, six Apollo missions landed on the Moon, allowing a total of 12 astronauts to explore its surface. Asteroid A minor planet. A large solid body of rock in orbit around the Sun. Banded crater A crater that displays dusky linear tracts on its inner walls and/or floor. 250 Basalt A dark, fine-grained volcanic rock, low in silicon, with a low viscosity. Basaltic material fills many of the Moon’s major basins, especially on the near side. Glossary Basin A very large circular impact structure (usually comprising multiple concentric rings) that usually displays some degree of flooding with lava. The largest and most conspicuous lava- flooded basins on the Moon are found on the near side, and most are filled to their outer edges with mare basalts. -
Planetary Surfaces
Chapter 4 PLANETARY SURFACES 4.1 The Absence of Bedrock A striking and obvious observation is that at full Moon, the lunar surface is bright from limb to limb, with only limited darkening toward the edges. Since this effect is not consistent with the intensity of light reflected from a smooth sphere, pre-Apollo observers concluded that the upper surface was porous on a centimeter scale and had the properties of dust. The thickness of the dust layer was a critical question for landing on the surface. The general view was that a layer a few meters thick of rubble and dust from the meteorite bombardment covered the surface. Alternative views called for kilometer thicknesses of fine dust, filling the maria. The unmanned missions, notably Surveyor, resolved questions about the nature and bearing strength of the surface. However, a somewhat surprising feature of the lunar surface was the completeness of the mantle or blanket of debris. Bedrock exposures are extremely rare, the occurrence in the wall of Hadley Rille (Fig. 6.6) being the only one which was observed closely during the Apollo missions. Fragments of rock excavated during meteorite impact are, of course, common, and provided both samples and evidence of co,mpetent rock layers at shallow levels in the mare basins. Freshly exposed surface material (e.g., bright rays from craters such as Tycho) darken with time due mainly to the production of glass during micro- meteorite impacts. Since some magnetic anomalies correlate with unusually bright regions, the solar wind bombardment (which is strongly deflected by the magnetic anomalies) may also be responsible for darkening the surface [I]. -
2021 Transpacific Yacht Race Event Program
TRANSPACTHE FIFTY-FIRST RACE FROM LOS ANGELES 2021 TO HONOLULU 2 0 21 JULY 13-30, 2021 Comanche: © Sharon Green / Ultimate Sailing COMANCHE Taxi Dancer: © Ronnie Simpson / Ultimate Sailing • Hamachi: © Team Hamachi HAMACHI 2019 FIRST TO FINISH Official race guide - $5.00 2019 OVERALL CORRECTED TIME WINNER P: 808.845.6465 [email protected] F: 808.841.6610 OFFICIAL HANDBOOK OF THE 51ST TRANSPACIFIC YACHT RACE The Transpac 2021 Official Race Handbook is published for the Honolulu Committee of the Transpacific Yacht Club by Roth Communications, 2040 Alewa Drive, Honolulu, HI 96817 USA (808) 595-4124 [email protected] Publisher .............................................Michael J. Roth Roth Communications Editor .............................................. Ray Pendleton, Kim Ickler Contributing Writers .................... Dobbs Davis, Stan Honey, Ray Pendleton Contributing Photographers ...... Sharon Green/ultimatesailingcom, Ronnie Simpson/ultimatesailing.com, Todd Rasmussen, Betsy Crowfoot Senescu/ultimatesailing.com, Walter Cooper/ ultimatesailing.com, Lauren Easley - Leialoha Creative, Joyce Riley, Geri Conser, Emma Deardorff, Rachel Rosales, Phil Uhl, David Livingston, Pam Davis, Brian Farr Designer ........................................ Leslie Johnson Design On the Cover: CONTENTS Taxi Dancer R/P 70 Yabsley/Compton 2019 1st Div. 2 Sleds ET: 8:06:43:22 CT: 08:23:09:26 Schedule of Events . 3 Photo: Ronnie Simpson / ultimatesailing.com Welcome from the Governor of Hawaii . 8 Inset left: Welcome from the Mayor of Honolulu . 9 Comanche Verdier/VPLP 100 Jim Cooney & Samantha Grant Welcome from the Mayor of Long Beach . 9 2019 Barndoor Winner - First to Finish Overall: ET: 5:11:14:05 Welcome from the Transpacific Yacht Club Commodore . 10 Photo: Sharon Green / ultimatesailingcom Welcome from the Honolulu Committee Chair . 10 Inset right: Welcome from the Sponsoring Yacht Clubs . -
The Osgood Family of Andover
fb.e OSGOOD FAllILY of Andover. Line of Chrlstopeeri GtflstoPher O~good of st. Mary'.,Marlboro,England, married April 21, 1632, vary Everard. She died shortly and was buried April 21, 1633. A daughter, Mary (2), born 1633 was baptized there on Maroh 17,1633. Christopher mar1""\ ried second, also at St. MarY'a, Marlboro, July 28, 1633, Var jory, daughter ~ Philip Fowler and his wit. Mary Winsley, who was bapt. at Marlboro in Wiltshirel Kay 25,1615. These all C~e with . sailing from Lon.on in the "Var~ and JOhn",Mar.24 1634. Fowler to Amerioa,/( The Fowler DOOK claIms tliat Uhrls£opher Ia o/alls-A bury, Wiltshire. It places him aa brother to VIm. and John Osgood, but th8t is not so at all.) Christopher died at Ipswioh,Mass. 1650. Marjory took for her second husband, Thomas Rowell of Salisbury, about a year atter Christopher's death and oame with him and children and grand children to Andover, where they- the Fowlers and Rowell, started the first fUlling mill. Rowell, who was one of the original proprietors of S.lisbury, ~/'--., 1639, died here in Andover. She married third, Thomas Coleman, who was recorded in NantuokeD, June 8, 1678, and rented a house in Andover to a son,Chr1stopher Oagood,for 12 years • He was to pay 15 ~bs. to his brother Tom of Andover and to have )he house, later. Her fourth husband was Thomas Osborne of Nantucket. Marjory died Nov. 20, 1701 aged about 8'7. Sefore her departure for .Nantucket, ahe le~t a feather bed with her son-in-law John Lovejoy, which he waa to give to her son,uacob Rowell. -
JPL to Map the Moon on India Mission
I n s i d e May 19, 2006 Volume 36 Number 10 News Briefs ............... 2 Griffin Visits Lab ............ 3 Special Events Calendar ...... 2 Passings, Letters ........... 4 Spitzer Sees Comet Breakup... 2 Retirees, Classifieds ......... 4 Jet Propulsion Laborator y A JPL state-of-the-art imaging spectrometer that will provide the first high-resolution spectral map of the JPL to entire lunar surface successfully completed its critical design review this week. The Moon Mineralogy Mapper, also known as “M3,” is one of two in- materials across the surface at high spatial resolution. This data map the struments that NASA is contributing to India’s first mission to the moon, will provide a much-needed long-term baseline for future exploration scheduled to launch in late 2007 or early 2008. By mapping the mineral activities. composition of the lunar surface, the mission will both provide clues to The mission’s observations will address several important scientific moon the early development of the solar system and guide future astronauts to issues, including early evolution of the solar system; fundamental stores of precious resources. processes acting on planets that shape their character; assessment of on India Chandrayaan-1 is India’s first deep-space mission as well as its first potential impact hazards to Earth; and assessment of space resources. lunar mission. “The entire M3 team feels honored to be able to partici- From its vantage point in orbit around the moon, the spacecraft will mission pate,” said Project Manager Tom Glavich of JPL. measure the sunlight reflected by all of the rocks and soil over which The instrument is well on its way to being delivered to the Chandray- it passes. -
Testing Hypotheses for the Origin of Steep Slope of Lunar Size-Frequency Distribution for Small Craters
CORE Metadata, citation and similar papers at core.ac.uk Provided by Springer - Publisher Connector Earth Planets Space, 55, 39–51, 2003 Testing hypotheses for the origin of steep slope of lunar size-frequency distribution for small craters Noriyuki Namiki1 and Chikatoshi Honda2 1Department of Earth and Planetary Sciences, Kyushu University, Hakozaki 6-10-1, Higashi-ku, Fukuoka 812-8581, Japan 2The Institute of Space and Astronautical Science, Yoshinodai 3-1-1, Sagamihara 229-8510, Japan (Received June 13, 2001; Revised June 24, 2002; Accepted January 6, 2003) The crater size-frequency distribution of lunar maria is characterized by the change in slope of the population between 0.3 and 4 km in crater diameter. The origin of the steep segment in the distribution is not well understood. Nonetheless, craters smaller than a few km in diameter are widely used to estimate the crater retention age for areas so small that the number of larger craters is statistically insufficient. Future missions to the moon, which will obtain high resolution images, will provide a new, large data set of small craters. Thus it is important to review current hypotheses for their distributions before future missions are launched. We examine previous and new arguments and data bearing on the admixture of endogenic and secondary craters, horizontal heterogeneity of the substratum, and the size-frequency distribution of the primary production function. The endogenic crater and heterogeneous substratum hypotheses are seen to have little evidence in their favor, and can be eliminated. The primary production hypothesis fails to explain a wide variation of the size-frequency distribution of Apollo panoramic photographs. -
Tracing the Seepage of Subsurface Sinkhole Vent Waters Into Lake Huron Using Radium and Stable Isotopes of Oxygen and Hydrogen
Aquat Geochem (2016) 22:349–374 DOI 10.1007/s10498-015-9286-7 ORIGINAL PAPER Tracing the Seepage of Subsurface Sinkhole Vent Waters into Lake Huron Using Radium and Stable Isotopes of Oxygen and Hydrogen 1 1 1 2 M. Baskaran • T. Novell • K. Nash • S. A. Ruberg • 3 2 4 5 T. Johengen • N. Hawley • J. V. Klump • B. A. Biddanda Received: 28 April 2015 / Accepted: 31 December 2015 / Published online: 12 January 2016 Ó Springer Science+Business Media Dordrecht 2016 Abstract Exchange of water between groundwater and surface water could alter water quality of the surface waters and thereby impact its ecosystem. Discharges of anoxic groundwater, with high concentrations of sulfate and chloride and low concentrations of nitrate and oxygen, from three sinkhole vents (El Cajon, Middle Island and Isolated) in Lake Huron have been recently documented. In this investigation, we collected and ana- lyzed a suite of water samples from these three sinkhole vents and lake water samples from Lake Huron for Ra, radon-222, stable isotopes of oxygen and hydrogen, and other ancillary parameters. These measurements are among the first of their kind in this unique envi- ronment. The activities of Ra are found to be one to two orders of magnitude higher than that of the lake water. Isotopic signatures of some of the bottom lake water samples indicate evidences for micro-seeps at distances farther from these three vents. A plot of dD versus d18O indicates that there are deviations from the Global Meteoric Line that can be attributed to mixing of different water masses and/or due to some subsurface chemical reactions. -
Compositional and Mineralogical Characteristics of Archimedes Crater Region Using Chandrayaan – 1 M3 Data
50th Lunar and Planetary Science Conference 2019 (LPI Contrib. No. 2132) 1040.pdf COMPOSITIONAL AND MINERALOGICAL CHARACTERISTICS OF ARCHIMEDES CRATER REGION USING CHANDRAYAAN – 1 M3 DATA. P. R. Kumaresan1 and J. Saravanavel2, 1Research Scholar, 2Assistant Professor, Department of Remote Sensing, Bharathidasan University, Tiruchirappalli-23, Tamil Nadu, India, email: [email protected], [email protected] Introduction: The Earth’s natural satellite the tometry corrected reflectance data captured during the moon is nearest celestial body appears brightest object OP1B optical period. in our night sky. Moon surfaces are composed of dark and light areas. The dark areas are called Maria which is made up of basaltic terrain and light areas are high- lands mostly made up of Anorthositic rocks. The moon surface is littered with craters, which are formed when meteors hit its surface. To understand the evolution, geological process of the moon it is important to study the surface composition and minerals present in crustal surface. In this regard, in our study, we have attempted to map the minerals and surface composition of Archi- medes crater region. Study area: Archimedes crater is a large impact crater located on the eastern edges of the Mare Imbri- um of near side moon (29.7° N, 4.0° W). The diameter of the crater is 83 km with smooth floor flooded (1) with mare basalt and lack of a central peak. The rim (2) has a significant outer rampart brightened with ejecta (3) and the some portion of a terraced inner wall. Ar- chimedes Crater is named for the Greek mathematician Archimedes, who made many mathematical discoveries in the 200 B.C [1, 2].