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Space Administration
https://ntrs.nasa.gov/search.jsp?R=19700024651 2020-03-23T18:20:34+00:00Z TO THE CONGRESSOF THE UNITEDSTATES : Transmitted herewith is the Twenty-first Semiannual Repol* of the National Aeronautics and Space Administration. Twen~-first SEMIANNUAL REPORT TO CONGRESS JANUARY 1 - JUNE 30, 1969 NATIONAL AERONAUTICS AND SPACE ADMINISTRATION WASHINGTON, D. C. 20546 Editors: G. B. DeGennaro, H. H. Milton, W. E. Boardman, Office of Public Affairs; Art work: A. Jordan, T. L. Lindsey, Office of Organiza- tion and Management. For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402-Price $1.25 THE PRESIDENT May 27,1970 The White House I submit this Twenty-First Semiannual Report of the National Aeronautics and Space Aldministration to you for transmitttal to Congress in accordance with section 206(a) of the National Aero- nautics and Space Act of 1958. It reports on aotivities which took place betiween January 1 and June 30, 1969. During this time, the Nation's space program moved forward on schedule. ApolIo 9 and 10 demonstrated the ability of ;the man- ned Lunar Module to operate in earth and lunar orbit and its 'eadi- ness to attempt the lunar landing. Unmanned observatory and ex- plorer class satellites carried on scientific studies of the regions surrounding the Earth, the Moon, and the Sun; a Biosatellite oarwing complex biological science experiment was orbited; and sophisticated weather satellites and advanced commercial com- munications spacecraft became operational. Advanced research projects expanded knowledge of space flighk and spacecraft engi- neering as well as of aeronautics. -
Problems of Planetology, Cosmochemistry and Meteoritica Alexeev V.A., Ustinova G.K
Problems of Planetology… Problems of Planetology, Cosmochemistry and Meteoritica Alexeev V.A., Ustinova G.K. Meteoritic evidence radionuclides before the meteorite fall onto the Earth. The investigation of radionuclides with different T1/2 in the on peculiarities of the contemporary solar cycles chondrites with various dates of fall, which have various V.I. Vernadsky Institute of Geochemistry and Analytical Chemistry extension and inclination of orbits, provides us with such RAS, Moscow long sequences of homogeneous data on variation of the Abstract. The meteorite data on monitoring of the intensity and GCR intensity and integral gradients (E >100 MeV) in the gradient of the galactic cosmic rays (GCR) in the heliosphere 3D heliosphere [Lavrukhina,Ustinova,1990]. The long during 5 solar cycles are used for the correlative analysis with the sequences of homogeneous data on the GCR intensity in variations of the solar activity (SA), strength of the interplanetary magnetic field (IMF) and tilt angle of the heliospheric current the stratosphere [Stozhkov et al., 2009] are used for sheet (HCS). The dependence of the GCR modulation depth in the evaluation of the gradients. Nowadays, such a sequence of 11-year solar cycles on the character of the solar magnetic field certain homogeneous data on the GCR intensity and (SMF) inversions in the heliosphere at the change of the 22-year gradients in the inner heliosphere covers ~5 solar cycles magnetic cycles is revealed. (see figure 1) [Alexeev, Ustinova, 2006]. This smoothes, Key words: galactic cosmic rays, solar modulation, solar cycles, to a considerable extent, both the temporal and spatial inversion of magnetic field, solar dynamo, climate. -
Lost Lake by Robert Verish
Meteorite-Times Magazine Contents by Editor Like Sign Up to see what your friends like. Featured Monthly Articles Accretion Desk by Martin Horejsi Jim’s Fragments by Jim Tobin Meteorite Market Trends by Michael Blood Bob’s Findings by Robert Verish IMCA Insights by The IMCA Team Micro Visions by John Kashuba Galactic Lore by Mike Gilmer Meteorite Calendar by Anne Black Meteorite of the Month by Michael Johnson Tektite of the Month by Editor Terms Of Use Materials contained in and linked to from this website do not necessarily reflect the views or opinions of The Meteorite Exchange, Inc., nor those of any person connected therewith. In no event shall The Meteorite Exchange, Inc. be responsible for, nor liable for, exposure to any such material in any form by any person or persons, whether written, graphic, audio or otherwise, presented on this or by any other website, web page or other cyber location linked to from this website. The Meteorite Exchange, Inc. does not endorse, edit nor hold any copyright interest in any material found on any website, web page or other cyber location linked to from this website. The Meteorite Exchange, Inc. shall not be held liable for any misinformation by any author, dealer and or seller. In no event will The Meteorite Exchange, Inc. be liable for any damages, including any loss of profits, lost savings, or any other commercial damage, including but not limited to special, consequential, or other damages arising out of this service. © Copyright 2002–2010 The Meteorite Exchange, Inc. All rights reserved. No reproduction of copyrighted material is allowed by any means without prior written permission of the copyright owner. -
Orbital Debris: a Chronology
NASA/TP-1999-208856 January 1999 Orbital Debris: A Chronology David S. F. Portree Houston, Texas Joseph P. Loftus, Jr Lwldon B. Johnson Space Center Houston, Texas David S. F. Portree is a freelance writer working in Houston_ Texas Contents List of Figures ................................................................................................................ iv Preface ........................................................................................................................... v Acknowledgments ......................................................................................................... vii Acronyms and Abbreviations ........................................................................................ ix The Chronology ............................................................................................................. 1 1961 ......................................................................................................................... 4 1962 ......................................................................................................................... 5 963 ......................................................................................................................... 5 964 ......................................................................................................................... 6 965 ......................................................................................................................... 6 966 ........................................................................................................................ -
USBC Approved Bowling Balls
USBC Approved Bowling Balls (See rulebook, Chapter VII, "USBC Equipment Specifications" for any balls manufactured prior to January 1991.) ** Bowling balls manufactured only under 13 pounds. 5/17/2011 Brand Ball Name Date Approved 900 Global Awakening Jul-08 900 Global BAM Aug-07 900 Global Bank Jun-10 900 Global Bank Pearl Jan-11 900 Global Bounty Oct-08 900 Global Bounty Hunter Jun-09 900 Global Bounty Hunter Black Jan-10 900 Global Bounty Hunter Black/Purple Feb-10 900 Global Bounty Hunter Pearl Oct-09 900 Global Break Out Dec-09 900 Global Break Pearl Jan-08 900 Global Break Point Feb-09 900 Global Break Point Pearl Jun-09 900 Global Creature Aug-07 900 Global Creature Pearl Feb-08 900 Global Day Break Jun-09 900 Global DVA Open Aug-07 900 Global Earth Ball Aug-07 900 Global Favorite May-10 900 Global Head Hunter Jul-09 900 Global Hook Dark Blue/Light Blue Feb-11 900 Global Hook Purple/Orange Pearl Feb-11 900 Global Hook Red/Yellow Solid Feb-11 900 Global Integral Break Black Nov-10 900 Global Integral Break Rose/Orange Nov-10 900 Global Integral Break Rose/Silver Nov-10 900 Global Link Jul-08 900 Global Link Black/Red Feb-09 900 Global Link Purple/Blue Pearl Dec-08 900 Global Link Rose/White Feb-09 900 Global Longshot Jul-10 900 Global Lunatic Jun-09 900 Global Mach One Blackberry Pearl Sep-10 900 Global Mach One Rose/Purple Pearl Sep-10 900 Global Maniac Oct-08 900 Global Mark Roth Ball Jan-10 900 Global Missing Link Black/Red Jul-10 900 Global Missing Link Blackberry/Silver Jul-10 900 Global Missing Link Blue/White Jul-10 900 Global -
Pallasites: Olivine-Metal Textures, Phosphoran Olivine, and Origin
Pallasites: olivine-metal textures, phosphoranolivine, and origin Ed Scott University of Hawai’i, Honolulu, HI 96822. [email protected] Four questions: 3. Origin of the four FeO-rich MG pallasites 1. Why do some pallasites have rounded olivines? 2. Why is phosphoran olivine only found in five main-group pallasites? 3. Why do four main group pallasites with rounded olivines contain abnormally Fe-rich olivine? 4. Where did main group and Eagle Station group pallasites form? a 1. Origin of rounded olivine Did cm-sized rounded olivines form before angular olivines [9], or were olivines rounded after Fig. 5. Zaisho, Springwater, Rawlinna, and Phillips Co. fragmentation of olivine [2.3,7]? Constraints: contain anomalously Fe-rich olivine, Ni-rich metal, and • Uniform size distribution of rounded olivines in farringtonite Mg3(PO4)2 [20] suggesting Fe was oxidized. Fig.1c is unlike that of angular olivine pallasites Fig. 3. Ir vs. Ni showing metal in main group pallasites and IIIAB irons. Arrows show Data from [2]. which may contain dunite fragments several cm solid and liquid Fe-Ni paths during fractional crystallization. MG pallasites were b in width (Fig. 1a.). mostly formed by mixing of residual metallic liquid from a IIIAB-like core after 75- Springwater contains 4 • Angular olivine pallasites may contain pieces of 80% crystallization [1,2]. Pavlodar (Pa) has rounded olivines and plots near the vol.% farringtonite (center) rounded olivine texture (Fig. 1b). initial melt composition showing that rounding preceded metal crystallization. enclosing olivine. Slice ~12 • Pavlodar metal matches that expected for initial Marjalahti (Ma), Huckitta (Hu) and Seymchan (Se) have angular olivines and cm wide. -
Meteor- Scatter
Catch a Falling Star A beginner’s guide to meteor-scatter communication— just in time for “stormy” weather! By Kirk Kleinschmidt, NT0Z Newcomers to Amateur Radio usually have a few misconceptions about VHF propagation. The worst—which is often “propagated” by more experienced hams who should know better—suggests that VHF signals travel exclusively along line-of-sight paths and peter out after about 30 miles. That’s far from true, but if your VHF operation is limited to 2-meter FM it’s somehow practical, especially if you’re using a hand-held radio and a rubber ducky antenna. Once you cross the “30-mile barrier,” however, there are many exciting and interesting ways to propagate your VHF signal hundreds or even thousands of kilometers. Articles in the ARRL Operating Manual and QST detail E- and F-layer skip, tropospheric ducting and transequatorial field-aligned irregularities, moon-bounce, auroral propagation and others. These modes aren’t always casual. That is, many require robust stations, high power and more than a little patience. Meteor- scatter work—bouncing radio signals off the ionized trails produced by meteors burning through the ionosphere—doesn’t require an extraordinary station, but some patience is usually necessary unless you know exactly when conditions may be favorable! That’s precisely the case with the November Leonids meteor showers for the next few years. (Meteor showers are named for the constellations from which they seem to appear. Meteors produced during the recurring November 17 shower seem to “pour” from the constellation Leo.) As an added bonus, on one or more of those November days the short-duration, high-intensity Leonids have the potential to produce the best meteor-scatter propagation since November 1966 (and a spectacular light show if you’re on the night side of the planet!). -
ELEMENTAL ABUNDANCES in the SILICATE PHASE of PALLASITIC METEORITES Redacted for Privacy Abstract Approved: Roman A
AN ABSTRACT OF THE THESIS OF THURMAN DALE COOPER for theMASTER OF SCIENCE (Name) (Degree) in CHEMISTRY presented on June 1, 1973 (Major) (Date) Title: ELEMENTAL ABUNDANCES IN THE SILICATE PHASE OF PALLASITIC METEORITES Redacted for privacy Abstract approved: Roman A. Schmitt The silicate phases of 11 pallasites were analyzed instrumen- tally to determine the concentrations of some major, minor, and trace elements.The silicate phases were found to contain about 98% olivine with 1 to 2% accessory minerals such as lawrencite, schreibersite, troilite, chromite, and farringtonite present.The trace element concentrations, except Sc and Mn, were found to be extremely low and were found primarily in the accessory phases rather than in the pure olivine.An unusual bimodal Mn distribution was noted in the pallasites, and Eagle Station had a chondritic nor- malized REE pattern enrichedin the heavy REE. The silicate phases of pallasites and mesosiderites were shown to be sufficiently diverse in origin such that separate classifications are entirely justified. APPROVED: Redacted for privacy Professor of Chemistry in charge of major Redacted for privacy Chairman of Department of Chemistry Redacted for privacy Dean of Graduate School Date thesis is presented June 1,1973 Typed by Opal Grossnicklaus for Thurman Dale Cooper Elemental Abundances in the Silicate Phase of Pallasitic Meteorites by Thurman Dale Cooper A THESIS submitted to Oregon State University in partial fulfillment of the requirements for the degree of Master of Science June 1974 ACKNOWLEDGMENTS The author wishes to express his gratitude to Prof. Roman A. Schmitt for his guidance, suggestions, discussions, and thoughtful- ness which have served as an inspiration. -
N Arieuican%Mllsellm
n ARieuican%Mllsellm PUBLISHED BY THE AMERICAN MUSEUM OF NATURAL HISTORY CENTRAL PARK WEST AT 79TH STREET, NEW YORK 24, N.Y. NUMBER 2I63 DECEMBER I9, I963 The Pallasites BY BRIAN MASON' INTRODUCTION The pallasites are a comparatively rare type of meteorite, but are remarkable in several respects. Historically, it was a pallasite for which an extraterrestrial origin was first postulated because of its unique compositional and structural features. The Krasnoyarsk pallasite was discovered in 1749 about 150 miles south of Krasnoyarsk, and seen by P. S. Pallas in 1772, who recognized these unique features and arranged for its removal to the Academy of Sciences in St. Petersburg. Chladni (1794) examined it and concluded it must have come from beyond the earth, at a time when the scientific community did not accept the reality of stones falling from the sky. Compositionally, the combination of olivine and nickel-iron in subequal amounts clearly distinguishes the pallasites from all other groups of meteorites, and the remarkable juxtaposition of a comparatively light silicate mineral and heavy metal poses a nice problem of origin. Several theories of the internal structure of the earth have postulated the presence of a pallasitic layer to account for the geophysical data. No apology is therefore required for an attempt to provide a comprehensive account of this remarkable group of meteorites. Some 40 pallasites are known, of which only two, Marjalahti and Zaisho, were seen to fall (table 1). Of these, some may be portions of a single meteorite. It has been suggested that the pallasite found in Indian mounds at Anderson, Ohio, may be fragments of the Brenham meteorite, I Chairman, Department of Mineralogy, the American Museum of Natural History. -
Meteorite Collections: Sample List
Meteorite Collections: Sample List Institute of Meteoritics Department of Earth and Planetary Sciences University of New Mexico October 01, 2021 Institute of Meteoritics Meteorite Collection The IOM meteorite collection includes samples from approximately 600 different meteorites, representative of most meteorite types. The last printed copy of the collection's Catalog was published in 1990. We will no longer publish a printed catalog, but instead have produced this web-based Online Catalog, which presents the current catalog in searchable and downloadable forms. The database will be updated periodically. The date on the front page of this version of the catalog is the date that it was downloaded from the worldwide web. The catalog website is: Although we have made every effort to avoid inaccuracies, the database may still contain errors. Please contact the collection's Curator, Dr. Rhian Jones, ([email protected]) if you have any questions or comments. Cover photos: Top left: Thin section photomicrograph of the martian shergottite, Zagami (crossed nicols). Brightly colored crystals are pyroxene; black material is maskelynite (a form of plagioclase feldspar that has been rendered amorphous by high shock pressures). Photo is 1.5 mm across. (Photo by R. Jones.) Top right: The Pasamonte, New Mexico, eucrite (basalt). This individual stone is covered with shiny black fusion crust that formed as the stone fell through the earth's atmosphere. Photo is 8 cm across. (Photo by K. Nicols.) Bottom left: The Dora, New Mexico, pallasite. Orange crystals of olivine are set in a matrix of iron, nickel metal. Photo is 10 cm across. (Photo by K. -
Desind Finding
NATIONAL AIR AND SPACE ARCHIVES Herbert Stephen Desind Collection Accession No. 1997-0014 NASM 9A00657 National Air and Space Museum Smithsonian Institution Washington, DC Brian D. Nicklas © Smithsonian Institution, 2003 NASM Archives Desind Collection 1997-0014 Herbert Stephen Desind Collection 109 Cubic Feet, 305 Boxes Biographical Note Herbert Stephen Desind was a Washington, DC area native born on January 15, 1945, raised in Silver Spring, Maryland and educated at the University of Maryland. He obtained his BA degree in Communications at Maryland in 1967, and began working in the local public schools as a science teacher. At the time of his death, in October 1992, he was a high school teacher and a freelance writer/lecturer on spaceflight. Desind also was an avid model rocketeer, specializing in using the Estes Cineroc, a model rocket with an 8mm movie camera mounted in the nose. To many members of the National Association of Rocketry (NAR), he was known as “Mr. Cineroc.” His extensive requests worldwide for information and photographs of rocketry programs even led to a visit from FBI agents who asked him about the nature of his activities. Mr. Desind used the collection to support his writings in NAR publications, and his building scale model rockets for NAR competitions. Desind also used the material in the classroom, and in promoting model rocket clubs to foster an interest in spaceflight among his students. Desind entered the NASA Teacher in Space program in 1985, but it is not clear how far along his submission rose in the selection process. He was not a semi-finalist, although he had a strong application. -
To Watch the Perseids 2014! Experts Dr
Web Chat: Stay ‘Up All Night’ to Watch the Perseids 2014! Experts Dr. Bill Cooke, Danielle Moser and Rhiannon Blaauw August 12-13, 2014 _____________________________________________________________________________________ Brooke_Moderator: Hi everyone, and welcome to the chat. Our experts are finalizing their prep and will start taking questions in about 10 minutes. Thanks for being here tonight! Brooke_Moderator: Just a few more moments, everyone, and our chat will get started. We're seeing a good number of meteors in our Ustream feed -- we may get a very nice show tonight! Brooke_Moderator: And...here we go. Our experts are ready for your questions. Let's talk Perseids! Eow: When you say local time is it local time of Huntsville, Alabama ? or Pacific time ? The time mentioned is so misleading ! I hope you dont keep people all nigh up at wrong time zones !!! Rhiannon_Blaauw: Local time means that it is that time, no matter what time zone you are in. For example, if you are in NYC, 3-5 a.m. local time means 3-5 a.m. EST. If you are in Chicago, 3-5 a.m. local time means 3-5 a.m. CST. Polarest: Is this where there will be pictures of the meteor shower? Rhiannon_Blaauw: The feed below is showing a 21x15 degree field of view from one of the Meteoroid Environment Office's meteor cameras. We have already seen at least 8 meteors in it in the last hour. Bava: When can I see the Meteor shower? I am going out and watching sky every now and then Rhiannon_Blaauw: You can see the meteor shower any time after 10 p.m.