Smithsonian Miscellaneous Collections
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Special Presentation by Wassim Jabi, Quentin Jones, Katia
Special Presentation by Wassim Jabi, Quentin Jones, Katia Passerini, Cristian Borcea, and Theodore Hall, “Fostering Creativity in Ubiquitous Social Computing through Casual and Formal Interactions in Interdisciplinary Design Studios”, Tables 1 This project aims to foster "CreativeIT": using information technology to enhance creativity in design, and applying creative design processes employed in disciplines such as architecture to enhance information technology. One aspect of this project is an interactive touch-screen poster display that enables two-way communication between designers, other team members, and the general public. Poster authors prepare their presentations in the form of web pages and submit the URIs to the display manager. The URIs are placed in an XML poster database on a networked server. The display kiosk software updates its poster list from the XML file periodically, displays the posters in sequence, and places thumbnails in a selection area. Viewers can give feedback on any poster that interests them through graffiti-style interaction with the touch-sensitive display, and e-mail the marked-up poster back to the author. This free-form feedback is a vital part of the creative process. Ikemefuna Chukwuemeka Agbanusi, Senior Student in Mathematics, “Dissecting the Phase Response Curve of a Bursting Neuron”, (advised by Amitabha Bose, advisors Amitabha Bose, Farzan Nadim and Jorge Golowasch), Table 52 We define and analyze the Phase Response Curve (PRC) of an endogenous neuronal oscillator. The PRC measures how an oscillator responds to the timing of stimulus. We utilize a Morris-Leccar type model to reproduce some of the phenomena observed in laboratory experiments on the PD neuron in the Stomatogastric Ganglion of the crab, Cancer borealis. -
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. -
Martian Crater Morphology
ANALYSIS OF THE DEPTH-DIAMETER RELATIONSHIP OF MARTIAN CRATERS A Capstone Experience Thesis Presented by Jared Howenstine Completion Date: May 2006 Approved By: Professor M. Darby Dyar, Astronomy Professor Christopher Condit, Geology Professor Judith Young, Astronomy Abstract Title: Analysis of the Depth-Diameter Relationship of Martian Craters Author: Jared Howenstine, Astronomy Approved By: Judith Young, Astronomy Approved By: M. Darby Dyar, Astronomy Approved By: Christopher Condit, Geology CE Type: Departmental Honors Project Using a gridded version of maritan topography with the computer program Gridview, this project studied the depth-diameter relationship of martian impact craters. The work encompasses 361 profiles of impacts with diameters larger than 15 kilometers and is a continuation of work that was started at the Lunar and Planetary Institute in Houston, Texas under the guidance of Dr. Walter S. Keifer. Using the most ‘pristine,’ or deepest craters in the data a depth-diameter relationship was determined: d = 0.610D 0.327 , where d is the depth of the crater and D is the diameter of the crater, both in kilometers. This relationship can then be used to estimate the theoretical depth of any impact radius, and therefore can be used to estimate the pristine shape of the crater. With a depth-diameter ratio for a particular crater, the measured depth can then be compared to this theoretical value and an estimate of the amount of material within the crater, or fill, can then be calculated. The data includes 140 named impact craters, 3 basins, and 218 other impacts. The named data encompasses all named impact structures of greater than 100 kilometers in diameter. -
Annual Report, Fiscal Year 1965
1965 TECHNICAL HIGHLIGHTS OF THE NATIONAL BUREAU OF STANDARDS Annual Report for: INSTITUTE FOR BASIC STANDARDS INSTITUTE FOR MATERIALS RESEARCH INSTITUTE FOR APPLIED TECHNOLOGY CENTRAL RADIO PROPAGATION LABORATORY n UNITED STATES DEPARTMENT OF COMMERCE John T. Connor, Secretary J. Herbert Hollomon, Assistant Secretary for Science and Technology NATIONAL BUREAU OF STANDARDS A. V. Astin, Director 1965 Technical Highlights of the National Bureau of Standards Annual Report, Fiscal Year 1965 May 1966 Miscellaneous Publication 279 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D. C, 20402 — Price 65 cents Library of Congress Catalog Card Number: 6-23979 CONTENTS THE DIRECTOR'S STATEMENT _ 1 NBS—An Evolving Institution 1 Management Progress 3 NBS As a Scientific Laboratory 5 INSTITUTE FOR BASIC STANDARDS 11 Physical Quantities, Constants, and Calibration Services 12 International Base L nits 13 Length. Mass. Frequency and Time. Temperature. Luminous Intensity. Electric Current. Mechanical Quantities 19 Force. Pressure. Vacuum. Electrical Quantities—DC 24 Resistance Ratios. Voltage. Current Ratio Standards. New Compensated Current Comparator. Absolute Electrical Meas- urements. AC-DC Transfer Standards. Voltage Ratio Detector for Millivolt Signals. Electrical Quantities—Radio 25 Low-Frequency Calibration. High-Frequency Electrical Stand- ards. High-Frequency Impedance Standards. High-Frequency Calibrations. Microwave Standards. Microwave Calibrations. Photometric and Radiometric Quantities 30 Ionizing Radiations 32 Engineering Measurement and Standards 36 Phyical Properties 39 National Standard Reference Data System 40 Nuclear Data. Atomic and Molecular Data. Solid State Data. Thermodynamics and Transport Data. Chemical Kinetics. Col- loid and Surface Properties. Information Services. Measurement 48 Nuclear Properties. Atomic and Molecular Properties. Solid State Properties. -
Planetary Science : a Lunar Perspective
APPENDICES APPENDIX I Reference Abbreviations AJS: American Journal of Science Ancient Sun: The Ancient Sun: Fossil Record in the Earth, Moon and Meteorites (Eds. R. 0.Pepin, et al.), Pergamon Press (1980) Geochim. Cosmochim. Acta Suppl. 13 Ap. J.: Astrophysical Journal Apollo 15: The Apollo 1.5 Lunar Samples, Lunar Science Insti- tute, Houston, Texas (1972) Apollo 16 Workshop: Workshop on Apollo 16, LPI Technical Report 81- 01, Lunar and Planetary Institute, Houston (1981) Basaltic Volcanism: Basaltic Volcanism on the Terrestrial Planets, Per- gamon Press (1981) Bull. GSA: Bulletin of the Geological Society of America EOS: EOS, Transactions of the American Geophysical Union EPSL: Earth and Planetary Science Letters GCA: Geochimica et Cosmochimica Acta GRL: Geophysical Research Letters Impact Cratering: Impact and Explosion Cratering (Eds. D. J. Roddy, et al.), 1301 pp., Pergamon Press (1977) JGR: Journal of Geophysical Research LS 111: Lunar Science III (Lunar Science Institute) see extended abstract of Lunar Science Conferences Appendix I1 LS IV: Lunar Science IV (Lunar Science Institute) LS V: Lunar Science V (Lunar Science Institute) LS VI: Lunar Science VI (Lunar Science Institute) LS VII: Lunar Science VII (Lunar Science Institute) LS VIII: Lunar Science VIII (Lunar Science Institute LPS IX: Lunar and Planetary Science IX (Lunar and Plane- tary Institute LPS X: Lunar and Planetary Science X (Lunar and Plane- tary Institute) LPS XI: Lunar and Planetary Science XI (Lunar and Plane- tary Institute) LPS XII: Lunar and Planetary Science XII (Lunar and Planetary Institute) 444 Appendix I Lunar Highlands Crust: Proceedings of the Conference in the Lunar High- lands Crust, 505 pp., Pergamon Press (1980) Geo- chim. -
Dust Coatings on Basaltic Rocks and Implications for Thermal Infrared Spectroscopy of Mars Jeffrey R
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 107, NO. E6, 10.1029/2000JE001405, 2002 Dust coatings on basaltic rocks and implications for thermal infrared spectroscopy of Mars Jeffrey R. Johnson Branch of Astrogeology, U.S. Geological Survey, Flagstaff, Arizona, USA Philip R. Christensen Department of Geology, Arizona State University, Tempe, Arizona, USA Paul G. Lucey Hawaii Institute for Geology and Planetology, University of Hawaii at Manoa, Honolulu, Hawaii, USA Received 2 October 2000; revised 6 July 2001; accepted 12 October 2001; published 5 June 2002. [1] Thin coatings of atmospherically deposited dust can mask the spectral characteristics of underlying surfaces on Mars from the visible to thermal infrared wavelengths, making identification of substrate and coating mineralogy difficult from lander and orbiter spectrometer data. To study the spectral effects of dust coatings, we acquired thermal emission and hemispherical reflectance spectra (5–25 mm; 2000–400 cmÀ1) of basaltic andesite coated with different thicknesses of air fall-deposited palagonitic soils, fine-grained ceramic clay powders, and terrestrial loess. The results show that thin coatings (10–20 mm) reduce the spectral contrast of the rock substrate substantially, consistent with previous work. This contrast reduction continues linearly with increasing coating thickness until a ‘‘saturation thickness’’ is reached, after which little further change is observed. The saturation thickness of the spectrally flat palagonite coatings is 100–120 mm, whereas that for coatings with higher spectral contrast is only 50–75 mm. Spectral differences among coated and uncoated samples correlate with measured coating thicknesses in a quadratic manner, whereas correlations with estimated surface area coverage are better fit by linear functions. -
DMAAC – February 1973
LUNAR TOPOGRAPHIC ORTHOPHOTOMAP (LTO) AND LUNAR ORTHOPHOTMAP (LO) SERIES (Published by DMATC) Lunar Topographic Orthophotmaps and Lunar Orthophotomaps Scale: 1:250,000 Projection: Transverse Mercator Sheet Size: 25.5”x 26.5” The Lunar Topographic Orthophotmaps and Lunar Orthophotomaps Series are the first comprehensive and continuous mapping to be accomplished from Apollo Mission 15-17 mapping photographs. This series is also the first major effort to apply recent advances in orthophotography to lunar mapping. Presently developed maps of this series were designed to support initial lunar scientific investigations primarily employing results of Apollo Mission 15-17 data. Individual maps of this series cover 4 degrees of lunar latitude and 5 degrees of lunar longitude consisting of 1/16 of the area of a 1:1,000,000 scale Lunar Astronautical Chart (LAC) (Section 4.2.1). Their apha-numeric identification (example – LTO38B1) consists of the designator LTO for topographic orthophoto editions or LO for orthophoto editions followed by the LAC number in which they fall, followed by an A, B, C or D designator defining the pertinent LAC quadrant and a 1, 2, 3, or 4 designator defining the specific sub-quadrant actually covered. The following designation (250) identifies the sheets as being at 1:250,000 scale. The LTO editions display 100-meter contours, 50-meter supplemental contours and spot elevations in a red overprint to the base, which is lithographed in black and white. LO editions are identical except that all relief information is omitted and selenographic graticule is restricted to border ticks, presenting an umencumbered view of lunar features imaged by the photographic base. -
INDEX to 1915-1919 Obituaries in the Canton Repository
INDEX To 1915-1919 Obituaries in the Canton Repository Published by the Stark County District Library of Canton, Ohio 2005 Index to 1915-1919 Obituaries in the Canton Repository The following is an alphabetical listing, by the deceased’s surname, of obituaries that appeared in the Canton, Ohio newspaper, The Repository. It was compiled by the library staff during the course of the year in the hope that it would be a useful tool to genealogy, as well as other researchers. To use this index, simply locate the name of the person whose obituary you wish to find. The entries will appear as follows: Miller William A. (Estella M.) Mrs. 1924 Jan. 13 30 The first column is the name of the deceased. The second gives the date on which the item appeared. And the third tells the page number containing the obituary. You may find one name with multiple listings showing different dates and locations in the paper. This indicates consecutive listings for that individual. I encourage you to view each for additional information. Index to 1915-1919 Obituaries in the Canton Repository Surname Given Name Maiden Title Year Mth Day Pg ? Mary 1918 Apr. 18 15 Aaron Benjamin 1918 Nov. 27 2 Abbott Lawrence C. 1919 Mar. 14 24 Abels infant 1919 July 16 6 Abherve Minnie Jacobs Mrs. 1918 Dec. 13 33 Abrams Leo 1917 Apr. 24 2 Abt Leo 1918 Apr. 27 1 Abvrezis Macone 1917 Sept. 17 2 Acker L. E. 1918 Jan. 13 26 Acker Leonard E. 1918 Jan. 12 5 Acker Sarah Mrs. -
Global Spectral Classification of Martian Low-Albedo Regions with Mars Global Surveyor Thermal Emission Spectrometer (MGS-TES) Data A
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 112, E02004, doi:10.1029/2006JE002726, 2007 Global spectral classification of Martian low-albedo regions with Mars Global Surveyor Thermal Emission Spectrometer (MGS-TES) data A. Deanne Rogers,1 Joshua L. Bandfield,2 and Philip R. Christensen2 Received 4 April 2006; revised 12 August 2006; accepted 13 September 2006; published 14 February 2007. [1] Martian low-albedo surfaces (defined here as surfaces with Mars Global Surveyor Thermal Emission Spectrometer (MGS-TES) albedo values 0.15) were reexamined for regional variations in spectral response. Low-albedo regions exhibit spatially coherent variations in spectral character, which in this work are grouped into 11 representative spectral shapes. The use of these spectral shapes in modeling global surface emissivity results in refined distributions of previously determined global spectral unit types (Surface Types 1 and 2). Pure Type 2 surfaces are less extensive than previously thought, and are mostly confined to the northern lowlands. Regional-scale spectral variations are present within areas previously mapped as Surface Type 1 or as a mixture of the two surface types, suggesting variations in mineral abundance among basaltic units. For example, Syrtis Major, which was the Surface Type 1 type locality, is spectrally distinct from terrains that were also previously mapped as Type 1. A spectral difference also exists between southern and northern Acidalia Planitia, which may be due in part to a small amount of dust cover in southern Acidalia. Groups of these spectral shapes can be averaged to produce spectra that are similar to Surface Types 1 and 2, indicating that the originally derived surface types are representative of the average of all low-albedo regions. -
Water on the Moon, III. Volatiles & Activity
Water on The Moon, III. Volatiles & Activity Arlin Crotts (Columbia University) For centuries some scientists have argued that there is activity on the Moon (or water, as recounted in Parts I & II), while others have thought the Moon is simply a dead, inactive world. [1] The question comes in several forms: is there a detectable atmosphere? Does the surface of the Moon change? What causes interior seismic activity? From a more modern viewpoint, we now know that as much carbon monoxide as water was excavated during the LCROSS impact, as detailed in Part I, and a comparable amount of other volatiles were found. At one time the Moon outgassed prodigious amounts of water and hydrogen in volcanic fire fountains, but released similar amounts of volatile sulfur (or SO2), and presumably large amounts of carbon dioxide or monoxide, if theory is to be believed. So water on the Moon is associated with other gases. Astronomers have agreed for centuries that there is no firm evidence for “weather” on the Moon visible from Earth, and little evidence of thick atmosphere. [2] How would one detect the Moon’s atmosphere from Earth? An obvious means is atmospheric refraction. As you watch the Sun set, its image is displaced by Earth’s atmospheric refraction at the horizon from the position it would have if there were no atmosphere, by roughly 0.6 degree (a bit more than the Sun’s angular diameter). On the Moon, any atmosphere would cause an analogous effect for a star passing behind the Moon during an occultation (multiplied by two since the light travels both into and out of the lunar atmosphere). -
Glossary of Lunar Terminology
Glossary of Lunar Terminology albedo A measure of the reflectivity of the Moon's gabbro A coarse crystalline rock, often found in the visible surface. The Moon's albedo averages 0.07, which lunar highlands, containing plagioclase and pyroxene. means that its surface reflects, on average, 7% of the Anorthositic gabbros contain 65-78% calcium feldspar. light falling on it. gardening The process by which the Moon's surface is anorthosite A coarse-grained rock, largely composed of mixed with deeper layers, mainly as a result of meteor calcium feldspar, common on the Moon. itic bombardment. basalt A type of fine-grained volcanic rock containing ghost crater (ruined crater) The faint outline that remains the minerals pyroxene and plagioclase (calcium of a lunar crater that has been largely erased by some feldspar). Mare basalts are rich in iron and titanium, later action, usually lava flooding. while highland basalts are high in aluminum. glacis A gently sloping bank; an old term for the outer breccia A rock composed of a matrix oflarger, angular slope of a crater's walls. stony fragments and a finer, binding component. graben A sunken area between faults. caldera A type of volcanic crater formed primarily by a highlands The Moon's lighter-colored regions, which sinking of its floor rather than by the ejection of lava. are higher than their surroundings and thus not central peak A mountainous landform at or near the covered by dark lavas. Most highland features are the center of certain lunar craters, possibly formed by an rims or central peaks of impact sites. -
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