Francesco Fontana and His Astronomical Telescope
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Placing World War I in the History of Mathematics David Aubin, Catherine Goldstein
Placing World War I in the History of Mathematics David Aubin, Catherine Goldstein To cite this version: David Aubin, Catherine Goldstein. Placing World War I in the History of Mathematics. 2013. hal- 00830121v1 HAL Id: hal-00830121 https://hal.sorbonne-universite.fr/hal-00830121v1 Preprint submitted on 4 Jun 2013 (v1), last revised 8 Jul 2014 (v2) 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. Placing World War I in the History of Mathematics David Aubin and Catherine Goldstein Abstract. In the historical literature, opposite conclusions were drawn about the impact of the First World War on mathematics. In this chapter, the case is made that the war was an important event for the history of mathematics. We show that although mathematicians' experience of the war was extremely varied, its impact was decisive on the life of a great number of them. We present an overview of some uses of mathematics in war and of the development of mathematics during the war. We conclude by arguing that the war also was a crucial factor in the institutional modernization of mathematics. Les vrais adversaires, dans la guerre d'aujourd'hui, ce sont les professeurs de math´ematiques`aleur table, les physiciens et les chimistes dans leur laboratoire. -
Thesis Yaxuedong Feb20141.Pdf
ABSTRACT The Water Vapor and Dust Plumes of Enceladus by Yaxue Dong Enceladus is the most active moon of Saturn. Its south polar plume, composed mostly of water vapor and ice grains, is one of the groundbreaking discoveries made by the Cassini spacecraft. During Cassini’s E2, E3, E5 and E7 encounters with Enceladus, the Ion and Neutral Mass Spectrometer (INMS) measured high neutral water vapor densities up to ~109 cm-3 (Waite et al., 2006; Teolis et al., 2010; Dong et al., 2011). We have constructed a physical model for the expected water vapor density in the plumes, based on supersonic radial outflow from one or more of the surface vents. We apply this model to possible surface sources of water vapor associated with the dust jets (Spitale and Porco, 2007; Hansen et al., 2008). Our model fits well with the E3, E5, and E7 INMS data. The fit is optimized by the 28 outflow velocity of ~ 550 – 750 m/s and the total source rate of ~ 1.5 − 3.5×10 H2O molecules/s (~ 450 – 1050 kg/s). The dust (ice grain) plumes of Enceladus have been observed by multiple Cassini instruments. We propose a composite ice grain size distribution covering a continuous size range from nanometer to micrometers, by combining the CAPS (Cassini Plasma Spectrometer), CDA (Cosmic Dust Analyzer), and RPWS (Radio and Plasma Wave Science) data (Hill et al., 2012; Kempf et al., 2008; Ye et al., 2012, 2013). We also study the grain charging process using the RPWS-LP (Langmuir Probe) data (Morooka et al., 2011). -
Argonaut #2 2019 Cover.Indd 1 1/23/20 1:18 PM the Argonaut Journal of the San Francisco Historical Society Publisher and Editor-In-Chief Charles A
1/23/20 1:18 PM Winter 2020 Winter Volume 30 No. 2 Volume JOURNAL OF THE SAN FRANCISCO HISTORICAL SOCIETY VOL. 30 NO. 2 Argonaut #2_2019_cover.indd 1 THE ARGONAUT Journal of the San Francisco Historical Society PUBLISHER AND EDITOR-IN-CHIEF Charles A. Fracchia EDITOR Lana Costantini PHOTO AND COPY EDITOR Lorri Ungaretti GRapHIC DESIGNER Romney Lange PUBLIcatIONS COMMIttEE Hudson Bell Lee Bruno Lana Costantini Charles Fracchia John Freeman Chris O’Sullivan David Parry Ken Sproul Lorri Ungaretti BOARD OF DIREctORS John Briscoe, President Tom Owens, 1st Vice President Mike Fitzgerald, 2nd Vice President Kevin Pursglove, Secretary Jack Lapidos,Treasurer Rodger Birt Edith L. Piness, Ph.D. Mary Duffy Darlene Plumtree Nolte Noah Griffin Chris O’Sullivan Richard S. E. Johns David Parry Brent Johnson Christopher Patz Robyn Lipsky Ken Sproul Bruce M. Lubarsky Paul J. Su James Marchetti John Tregenza Talbot Moore Diana Whitehead Charles A. Fracchia, Founder & President Emeritus of SFHS EXECUTIVE DIREctOR Lana Costantini The Argonaut is published by the San Francisco Historical Society, P.O. Box 420470, San Francisco, CA 94142-0470. Changes of address should be sent to the above address. Or, for more information call us at 415.537.1105. TABLE OF CONTENTS A SECOND TUNNEL FOR THE SUNSET by Vincent Ring .....................................................................................................................................6 THE LAST BASTION OF SAN FRANCISCO’S CALIFORNIOS: The Mission Dolores Settlement, 1834–1848 by Hudson Bell .....................................................................................................................................22 A TENDERLOIN DISTRIct HISTORY The Pioneers of St. Ann’s Valley: 1847–1860 by Peter M. Field ..................................................................................................................................42 Cover photo: On October 21, 1928, the Sunset Tunnel opened for the first time. -
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. -
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. -
General Index
General Index Italicized page numbers indicate figures and tables. Color plates are in- cussed; full listings of authors’ works as cited in this volume may be dicated as “pl.” Color plates 1– 40 are in part 1 and plates 41–80 are found in the bibliographical index. in part 2. Authors are listed only when their ideas or works are dis- Aa, Pieter van der (1659–1733), 1338 of military cartography, 971 934 –39; Genoa, 864 –65; Low Coun- Aa River, pl.61, 1523 of nautical charts, 1069, 1424 tries, 1257 Aachen, 1241 printing’s impact on, 607–8 of Dutch hamlets, 1264 Abate, Agostino, 857–58, 864 –65 role of sources in, 66 –67 ecclesiastical subdivisions in, 1090, 1091 Abbeys. See also Cartularies; Monasteries of Russian maps, 1873 of forests, 50 maps: property, 50–51; water system, 43 standards of, 7 German maps in context of, 1224, 1225 plans: juridical uses of, pl.61, 1523–24, studies of, 505–8, 1258 n.53 map consciousness in, 636, 661–62 1525; Wildmore Fen (in psalter), 43– 44 of surveys, 505–8, 708, 1435–36 maps in: cadastral (See Cadastral maps); Abbreviations, 1897, 1899 of town models, 489 central Italy, 909–15; characteristics of, Abreu, Lisuarte de, 1019 Acequia Imperial de Aragón, 507 874 –75, 880 –82; coloring of, 1499, Abruzzi River, 547, 570 Acerra, 951 1588; East-Central Europe, 1806, 1808; Absolutism, 831, 833, 835–36 Ackerman, James S., 427 n.2 England, 50 –51, 1595, 1599, 1603, See also Sovereigns and monarchs Aconcio, Jacopo (d. 1566), 1611 1615, 1629, 1720; France, 1497–1500, Abstraction Acosta, José de (1539–1600), 1235 1501; humanism linked to, 909–10; in- in bird’s-eye views, 688 Acquaviva, Andrea Matteo (d. -
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. -
224641234.Pdf
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Helsingin yliopiston digitaalinen arkisto ASTROBIOLOGY Volume 19, Number 3, 2019 Mary Ann Liebert, Inc. DOI: 10.1089/ast.2018.1870 A Low-Diversity Microbiota Inhabits Extreme Terrestrial Basaltic Terrains and Their Fumaroles: Implications for the Exploration of Mars Charles S. Cockell,1 Jesse P. Harrison,2,3 Adam H. Stevens,1 Samuel J. Payler,1 Scott S. Hughes,4 Shannon E. Kobs Nawotniak,4 Allyson L. Brady,5 R.C. Elphic,6 Christopher W. Haberle,7 Alexander Sehlke,6 Kara H. Beaton,8 Andrew F.J. Abercromby,9 Petra Schwendner,1 Jennifer Wadsworth,1 Hanna Landenmark,1 Rosie Cane,1 Andrew W. Dickinson,1 Natasha Nicholson,1 Liam Perera,1 and Darlene S.S. Lim6,10 Abstract A major objective in the exploration of Mars is to test the hypothesis that the planet hosted life. Even in the absence of life, the mapping of habitable and uninhabitable environments is an essential task in developing a complete understanding of the geological and aqueous history of Mars and, as a consequence, understanding what factors caused Earth to take a different trajectory of biological potential. We carried out the aseptic collection of samples and comparison of the bacterial and archaeal communities associated with basaltic fumaroles and rocks of varying weathering states in Hawai‘i to test four hypotheses concerning the diversity of life in these environments. Using high-throughput sequencing, we found that all these materials are inhabited by a low-diversity biota. Multivariate analyses of bacterial community data showed a clear separation between sites that have active fumaroles and other sites that comprised relict fumaroles, unaltered, and syn-emplacement basalts. -
Revised Final MASTERS THESIS
UNIVERSITY OF CALIFORNIA RIVERSIDE Carlo Fontana and the Origins of the Architectural Monograph A Thesis submitted in partial satisfaction of the requirements for the degree of Master of Arts in Art History by Juliann Rose Walker June 2016 Thesis Committee: Dr. Kristoffer Neville, Chairperson Dr. Jeanette Kohl Dr. Conrad Rudolph Copyright by Juliann Walker 2016 The Thesis of Juliann Rose Walker is approved: Committee Chairperson University of California, Riverside Acknowledgements I would first like to start by thanking my committee members. Thank you to my advisor, Kristoffer Neville, who has worked with me for almost four years now as both an undergrad and graduate student; this project was possible because of you. To Jeanette Kohl, who was integral in helping me to outline and finish my first chapter, which made the rest of my thesis writing much easier in comparison. Your constructive comments were instrumental to the clarity and depth of my research, so thank you. And thank you to Conrad Rudolph, for your stern, yet fair, critiques of my writing, which were an invaluable reminder that you can never proofread enough. A special thank you to Malcolm Baker, who offered so much of his time and energy to me in my undergraduate career, and for being a valuable and vast resource of knowledge on early modern European artwork as I researched possible thesis topics. And the warmest of thanks to Alesha Jeanette, who has always left her door open for me to come and talk about anything that was on my mind. I would also like to thank Leigh Gleason at the California Museum of Photography, for giving me the opportunity to intern in collections. -
Thermal Infrared Spectroscopy of Explosively Erupted Terrestrial Basalts: Potential Analogues for Surface Compositions on Mars. J
Lunar and Planetary Science XXXVI (2005) 1114.pdf THERMAL INFRARED SPECTROSCOPY OF EXPLOSIVELY ERUPTED TERRESTRIAL BASALTS: POTENTIAL ANALOGUES FOR SURFACE COMPOSITIONS ON MARS. J. B. Witter1, V. E. Hamilton1 and B. F. Houghton2, 1Hawai'i Institute of Geophysics and Planetology, 2Department of Geology and Geophysics, University of Hawai'i at Manoa, 1680 East West Road, Honolulu, HI 96822; [email protected]. Introduction: Basaltic pyroclastic ejecta from parameters derived from the deposit are: column terrestrial Plinian eruptions may be analogues for height of 50 km and mass eruption rate of ~5 x 108 Martian surface materials observed by the Thermal kg/s [20]. The San Judas Formation resulted from a Emission Spectrometer (TES). We have acquired smaller eruption column (18 km height) and a lower samples from the 122 B.C. Etna (Italy), 1886 Taraw- mass eruption rate (~3 x 107 kg/s) that deposited at era (New Zealand), and prehistoric Masaya (Nicara- least 1.2 km3 of basaltic tephra [20]. The mechanism gua) eruptions for spectral analysis and comparison for Plinian eruption at Masaya is suggested by [19] to to Martian infrared surface spectra. involve rapid ascent of volatile-rich basaltic magma Explosive Basaltic Volcanism on Mars: Nu- from a deep (~100 km) source. merous lines of evidence suggest that explosive ba- 122 B.C. eruption of Etna, Italy. Basaltic pyro- saltic volcanism likely has occurred on Mars clastic deposits at Etna have formed from at least 24 throughout the planet's history. Evidence for explo- sub-Plinian eruptions and one Plinian eruption in the sive activity includes: models of magma ascent and last 13 ka [21]. -
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 -
2019 Publication Year 2020-05-18T17:09:00Z Acceptance
Publication Year 2019 Acceptance in OA@INAF 2020-05-18T17:09:00Z Title Della Porta, Colonna e Fontana e le prime osservazioni astronomiche a Napoli Authors GARGANO, MAURO DOI 10.35948/9788869521188/c25 Handle http://hdl.handle.net/20.500.12386/24943 Della Porta, Colonna e Fontana e le prime osservazioni astronomiche a Napoli Mauro Gargano ‒ INAF ‒ Osservatorio Astronomico di Capodimonte ‒ [email protected] Abstract: Giovan Battista Della Porta is known for his idea of experimental science, Fabio Colonna is well-known for his botanical studies, and Fran- cesco Fontana for his powerful telescopes and the exact observations of the Moon and planets. All three interested in astronomy. But when and what was observed in Naples for the first time with a telescope? And by whom? This communication, based on the correspondence of the protagonists, wants to contribute to retrace the events of the first Neapolitan astronomical observations. Keywords: Astronomy, Telescopes, Observations, Giovanni Battista Della Porta, Fabio Colonna, Francesco Fontana. 1. Il cannocchiale di Galileo «El S.r Galileo de i Galiliegi, vero arecoltore delle smatemateghe, e slenzaore in lo Bo de Pava à gi scuelari della so prefission» è l’intestazione di una dedicatoria in dialetto pavano scritta nel marzo 1608 dal gioviale poeta e pittore padovano Giuseppe Gagliardi (Firenze, Biblioteca Nazionale Centrale (FBNC), Manoscritti Galileiani (Mss. Gal.), Gagliardi 1608, P. I, T. III, cc. 68-82). In quest’epoca il “Coltivatore” Galilei è senza dubbio un raffinato professore dell’Università di Padova e un eccellente costruttore di strumenti matematici. Lo scienziato di Pisa comincia a praticare l’astronomia con l’esplosione “de stella nova in pede serpentari” verso la fine dell’ottobre 1604.