Geophysical Abstracts 163 October- December 1955
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Timeline of Natural History
Timeline of natural history This timeline of natural history summarizes significant geological and Life timeline Ice Ages biological events from the formation of the 0 — Primates Quater nary Flowers ←Earliest apes Earth to the arrival of modern humans. P Birds h Mammals – Plants Dinosaurs Times are listed in millions of years, or Karo o a n ← Andean Tetrapoda megaanni (Ma). -50 0 — e Arthropods Molluscs r ←Cambrian explosion o ← Cryoge nian Ediacara biota – z ←Earliest animals o ←Earliest plants i Multicellular -1000 — c Contents life ←Sexual reproduction Dating of the Geologic record – P r The earliest Solar System -1500 — o t Precambrian Supereon – e r Eukaryotes Hadean Eon o -2000 — z o Archean Eon i Huron ian – c Eoarchean Era ←Oxygen crisis Paleoarchean Era -2500 — ←Atmospheric oxygen Mesoarchean Era – Photosynthesis Neoarchean Era Pong ola Proterozoic Eon -3000 — A r Paleoproterozoic Era c – h Siderian Period e a Rhyacian Period -3500 — n ←Earliest oxygen Orosirian Period Single-celled – life Statherian Period -4000 — ←Earliest life Mesoproterozoic Era H Calymmian Period a water – d e Ectasian Period a ←Earliest water Stenian Period -4500 — n ←Earth (−4540) (million years ago) Clickable Neoproterozoic Era ( Tonian Period Cryogenian Period Ediacaran Period Phanerozoic Eon Paleozoic Era Cambrian Period Ordovician Period Silurian Period Devonian Period Carboniferous Period Permian Period Mesozoic Era Triassic Period Jurassic Period Cretaceous Period Cenozoic Era Paleogene Period Neogene Period Quaternary Period Etymology of period names References See also External links Dating of the Geologic record The Geologic record is the strata (layers) of rock in the planet's crust and the science of geology is much concerned with the age and origin of all rocks to determine the history and formation of Earth and to understand the forces that have acted upon it. -
UC Irvine UC Irvine Previously Published Works
UC Irvine UC Irvine Previously Published Works Title Astrophysics in 2006 Permalink https://escholarship.org/uc/item/5760h9v8 Journal Space Science Reviews, 132(1) ISSN 0038-6308 Authors Trimble, V Aschwanden, MJ Hansen, CJ Publication Date 2007-09-01 DOI 10.1007/s11214-007-9224-0 License https://creativecommons.org/licenses/by/4.0/ 4.0 Peer reviewed eScholarship.org Powered by the California Digital Library University of California Space Sci Rev (2007) 132: 1–182 DOI 10.1007/s11214-007-9224-0 Astrophysics in 2006 Virginia Trimble · Markus J. Aschwanden · Carl J. Hansen Received: 11 May 2007 / Accepted: 24 May 2007 / Published online: 23 October 2007 © Springer Science+Business Media B.V. 2007 Abstract The fastest pulsar and the slowest nova; the oldest galaxies and the youngest stars; the weirdest life forms and the commonest dwarfs; the highest energy particles and the lowest energy photons. These were some of the extremes of Astrophysics 2006. We attempt also to bring you updates on things of which there is currently only one (habitable planets, the Sun, and the Universe) and others of which there are always many, like meteors and molecules, black holes and binaries. Keywords Cosmology: general · Galaxies: general · ISM: general · Stars: general · Sun: general · Planets and satellites: general · Astrobiology · Star clusters · Binary stars · Clusters of galaxies · Gamma-ray bursts · Milky Way · Earth · Active galaxies · Supernovae 1 Introduction Astrophysics in 2006 modifies a long tradition by moving to a new journal, which you hold in your (real or virtual) hands. The fifteen previous articles in the series are referenced oc- casionally as Ap91 to Ap05 below and appeared in volumes 104–118 of Publications of V. -
Voyageurs National Park Geologic Resource Evaluation Report
National Park Service U.S. Department of the Interior Natural Resource Program Center Voyageurs National Park Geologic Resource Evaluation Report Natural Resource Report NPS/NRPC/GRD/NRR—2007/007 THIS PAGE: A geologist highlights a geologic contact during a Geologic Resource Evaluation scoping field trip at Voyageurs NP, MN ON THE COVER: Aerial view of Voyageurs NP, MN NPS Photos Voyageurs National Park Geologic Resource Evaluation Report Natural Resource Report NPS/NRPC/GRD/NRR—2007/007 Geologic Resources Division Natural Resource Program Center P.O. Box 25287 Denver, Colorado 80225 June 2007 U.S. Department of the Interior Washington, D.C. The Natural Resource Publication series addresses natural resource topics that are of interest and applicability to a broad readership in the National Park Service and to others in the management of natural resources, including the scientific community, the public, and the NPS conservation and environmental constituencies. Manuscripts are peer- reviewed to ensure that the information is scientifically credible, technically accurate, appropriately written for the intended audience, and is designed and published in a professional manner. Natural Resource Reports are the designated medium for disseminating high priority, current natural resource management information with managerial application. The series targets a general, diverse audience, and may contain NPS policy considerations or address sensitive issues of management applicability. Examples of the diverse array of reports published in this series include vital signs monitoring plans; "how to" resource management papers; proceedings of resource management workshops or conferences; annual reports of resource programs or divisions of the Natural Resource Program Center; resource action plans; fact sheets; and regularly- published newsletters. -
Crystal Size Distribution of Saganaga Tonalite, MN
Crystal Size Distribution of Saganaga Tonalite, MN ALEXANDER REIMERS PETROLOGY PROJECT 2018 Regional Setting Saganaga Tonalite is situated to the north plex of the Duluth com within the Archean Superior Craton Named aer Saganaga Lake Archean in Age: ~2700 ± 50 m.y.a ◦ Rb-‐Sr, K-‐Ar, and U-‐Pb dang methods were used Originated from the Algoman Orogeny (Kenoran Orogeny in Canada) before the Mid-‐conNnental ri Saganaga Tonalite Map of!8chean terranes of Minnesota Map: usgeologymorphology.com Saganaga Tonalite Extent (USA) Algoman Orogeny Repeate. episo.es of Late Archean conNnental collisions, compressions, an. sub.ucNons Saganaga Tonalite Homogenous, composite Intrusive bo.y Intru.es Greenstone an. Northern Light Gneiss an. overlain by metase.imentary rocks of Knife Lake Group PHanson,1962) Composion ◦ Felsic ◦ 20I60Y Zuartz ◦ 50I90Y Plagioclase POligoclase or An.esine) ◦ <10Y Alkali Fel.spar Mineral Approximation Sample Plagioclase PY) KIspar PY) Zuartz PY) Other PY) 55 5 35 5 ACR1_ I 1 Saganaga Tonalite 65 5 25 5 ACR1_ I 2 65 0 30 5 ACR1_ I 3 61.67 3.33 30.00 5.00 Average • Mineral Appro6imaons were made via petrographic microscope for three .iaerent thin secons. • Average mineral percentage for the bulk rock sample is shown. Guiding Question 2etermine if the cooling rate of the Saganaga Tonalite can be esNmate. base. on 2I2 crystal size .istribuNon of Plagioclase Methods Pro.uce. 3 thin secNons Analyze. general mineral composiNon an. i.enNbe. Plagioclase crystals Import image, taken on 2r. Tackecds microscope, of thin secNons into an image analysis so;ware PDigimizer) for crystal size .istribuNon analysis Photo courtesy of Eidukat 2r. -
Geology and Petrology of the Logan Intrusives of the Hungry Jack Lake Quadrangle, Cook County, Minnesota
Geology and petrology of the Logan intrusives of the Hungry Jack Lake Quadrangle, Cook County, Minnesota Item Type text; Thesis-Reproduction (electronic); maps Authors Mathez, Edmond Albigese, 1946- Publisher The University of Arizona. Rights Copyright © is held by the author. Digital access to this material is made possible by the University Libraries, University of Arizona. Further transmission, reproduction or presentation (such as public display or performance) of protected items is prohibited except with permission of the author. Download date 04/10/2021 03:37:21 Link to Item http://hdl.handle.net/10150/557306 GEOLOGY AND PETROLOGY OF THE LOGAN INTRUSIVES OF THE HUNGRY JACK LAKE QUADRANGLE COOK COUNTY, MINNESOTA by Edmond Albigese Mathez A Thesis Submitted to the Faculty of the DEPARTMENT OF GEOSCIENCES In Partial Fulfillment of the Requirements For the Degree of MASTER OF SCIENCE WITH A MAJOR IN GEOLOGY In the Graduate College THE UNIVERSITY OF ARIZONA 19 7 1 STATEMENT BY AUTHOR This thesis has been submitted in partial fulfillment of re quirements for an advanced degree at The University of Arizona and is deposited in the University Library to be made available to borrowers under rules of the Library. Brief quotations from this thesis are allowable without special permission, provided that accurate acknowledgment of source is made. Requests for permission for extended quotation from or reproduction of this manuscript in whole or in part may be granted by the head of the major department or the Dean of the Graduate College when in his judg ment the proposed use of the material is in the interests of scholar ship. -
The Bullard, Everett and Smith Reconstruction of the Circum-Atlantic Continents
1 GENESIS OF A GEOPHYSICAL ICON: THE BULLARD, EVERETT AND SMITH RECONSTRUCTION OF THE CIRCUM-ATLANTIC CONTINENTS J. E. EVERETT Faculty of Economics and Commerce The University of Western Australia, Nedlands, Western Australia 6009 [email protected] A. G. SMITH Department of Earth Sciences, Sedgwick Museum, Downing Street, Cambridge CB2 3EQ, U.K. [email protected] ABSTRACT The first computer fit of the continents had its origins in a controversy over Warren Carey’s visual fit between South America and Africa. Sir Harold Jeffreys denied that there was a fit, but Sir Edward Bullard considered the fit to be impressive. Bullard suggested quantifying the fit to Jim Everett, a graduate student at the time. Everett did so, developing his own method from his mathematical background, and computed the fit for the South Atlantic. Alan Smith, then a research assistant, used his geological knowledge and worked with Everett to fit together all the circum-Atlantic continents. Thus Bullard had the idea of quantifying the fit, and Everett and Smith implemented it. Then Smith extended the method to fits beyond the Earth Sciences History Atlantic. The outcome owed much to Bullard’s leadership, and to the lively v. 27, no. 1, 2008 and open discussions that prevailed during coffee and tea at Madingley pp. Rise, which housed the Department of Geodesy and Geophysics of the University of Cambridge at that time. 1. INTRODUCTION Bullard, Everett and Smith’s (1965) computer fit of the circum-Atlantic continents has become something of a geophysical icon. It gave rise to new ideas and set new approaches in motion, whose consequences are still being worked out today. -
The Historical Background
01 orestes part 1 10/24/01 3:40 PM Page 1 Part I The Historical Background The idea that continents move was first seriously considered in the early 20th century, but it took scientists 40 years to decide that it was true. Part I describes the historical background to this question: how scientists first pondered the question of crustal mobility, why they rejected the idea the first time around, and how they ultimately came back to it with new evidence, new ideas, and a global model of how it works. 01 orestes part 1 10/24/01 3:40 PM Page 2 01 orestes part 1 10/24/01 3:40 PM Page 3 Chapter 1 From Continental Drift to Plate Tectonics Naomi Oreskes Since the 16th century, cartographers have noticed the jigsaw-puzzle fit of the continental edges.1 Since the 19th century, geol- ogists have known that some fossil plants and animals are extraordinar- ily similar across the globe, and some sequences of rock formations in distant continents are also strikingly alike. At the turn of the 20th cen- tury, Austrian geologist Eduard Suess proposed the theory of Gond- wanaland to account for these similarities: that a giant supercontinent had once covered much or all of Earth’s surface before breaking apart to form continents and ocean basins. A few years later, German meteo- rologist Alfred Wegener suggested an alternative explanation: conti- nental drift. The paleontological patterns and jigsaw-puzzle fit could be explained if the continents had migrated across the earth’s surface, sometimes joining together, sometimes breaking apart. -
Lunar Impact Basins Revealed by Gravity Recovery and Interior
Lunar impact basins revealed by Gravity Recovery and Interior Laboratory measurements Gregory Neumann, Maria Zuber, Mark Wieczorek, James Head, David Baker, Sean Solomon, David Smith, Frank Lemoine, Erwan Mazarico, Terence Sabaka, et al. To cite this version: Gregory Neumann, Maria Zuber, Mark Wieczorek, James Head, David Baker, et al.. Lunar im- pact basins revealed by Gravity Recovery and Interior Laboratory measurements. Science Advances , American Association for the Advancement of Science (AAAS), 2015, 1 (9), pp.e1500852. 10.1126/sci- adv.1500852. hal-02458613 HAL Id: hal-02458613 https://hal.archives-ouvertes.fr/hal-02458613 Submitted on 26 Jun 2020 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. RESEARCH ARTICLE PLANETARY SCIENCE 2015 © The Authors, some rights reserved; exclusive licensee American Association for the Advancement of Science. Distributed Lunar impact basins revealed by Gravity under a Creative Commons Attribution NonCommercial License 4.0 (CC BY-NC). Recovery and Interior Laboratory measurements 10.1126/sciadv.1500852 Gregory A. Neumann,1* Maria T. Zuber,2 Mark A. Wieczorek,3 James W. Head,4 David M. H. Baker,4 Sean C. Solomon,5,6 David E. Smith,2 Frank G. -
Affairs of the Sea
AFFAIRS OF THE SEA Walter H. Munk Institute ofGeophysics and Planetary Physics Scripps Institution ofOceanography University ofCalifornia at San Diego La Jolla, California 92093 The following pages are taken from an introductory chapter was published did I realize that I had failed to even chapter written at the request of the Editors of the Annual mention the ill-fated MOHOLE project (perhaps because I Review ofEarth and Planetary Sciences,' This chapter was writ have been trying to forget it for twenty years). This omission ten on a skiing vacation at San Vigilio di Marebbe; it pro is now remedied. There are several other modifications, and vided a ready excuse for coming off the mountain in the the account is brought up-to-date." early afternoon, before it got cold and icy, Only after the I associate most ofmy boyhood prior to coming to America with life at the Eggelgut, in Altaussee, a village about 45 minutes out ofSalzburg. My grandfa ther converted and enlarged a 17th century peasant house to the Eggelgut. located on a steep meadow between the forest and a brook. Life was centered around the lake, and around the tennis courts. I lOok tennis very seriously and once made it to the Austrian semi-semi ./inals for junior doubles. in winter we would ski on the Loser which started right behind the house. .vter the war Mother sold the house and most ofthe land, but we still visit there occasion ally. 'Reproduced, wnn permission, from the Annual Review of "References to papers in which I am an author are numbered Earth and Planetary Sciences, Volume 8, © 1980 by Annual in accordance with the Bibliography in this volume. -
Pipestone National Monument Geologic Resources Inventory Report
National Park Service U.S. Department of the Interior Natural Resource Stewardship and Science Pipestone National Monument Geologic Resources Inventory Report Natural Resource Report NPS/NRSS/GRD/NRR—2017/1512 George Catlin wrote of his journey to Pipestone: “For many miles we had the Coteau in view in the distance before us, which looked like a blue cloud settling down in the horizon . On the very top of this mound or ridge, we found the far-famed quarry or fountain of the Red Pipe, which is truly an anomaly in nature. The principal and most striking feature of this place, is a perpendicular wall of close-grained, compact quartz, of twenty-five and thirty feet in elevation, running nearly North and South with its face to the West, exhibiting a front of nearly two miles in length, when it disappears at both ends by running under the prairie . At the base of this wall there is a level prairie, of half a mile in width, running parallel to it; in any and all parts of which, the Indians procure the red stone for their pipes, by digging through the soil and several slaty layers of the red stone, to the depth of four or five feet. From the very numerous marks of ancient and modern diggings or excavations, it would appear that this place has been for many centuries resorted to for the red stone; and from the great number of graves and remains of ancient fortifications in its vicinity, it would seem, as well as from their actual traditions, that the Indian tribes have long held this place in high superstitious estimation; and also that it has been the resort of different tribes, who have made their regular pilgrimages here to renew their pipes.” (Quote from the Smithsonian website below, citing Truettner 1979 and Gurney and Heyman 2002) ON THE COVER George Catlin’s 1836 painting Pipestone Quarry on the Coteau des Prairies. -
Modeling Polarimetric Radar Scattering from the Lunar Surface: Study on the Effect of Physical Properties of the Regolith Layer Wenzhe Fa, Mark Wieczorek, Essam Heggy
Modeling polarimetric radar scattering from the lunar surface: Study on the effect of physical properties of the regolith layer Wenzhe Fa, Mark Wieczorek, Essam Heggy To cite this version: Wenzhe Fa, Mark Wieczorek, Essam Heggy. Modeling polarimetric radar scattering from the lunar sur- face: Study on the effect of physical properties of the regolith layer. Journal of Geophysical Research. Planets, Wiley-Blackwell, 2011, 116 (E3), pp.E03005. 10.1029/2010JE003649. hal-02458568 HAL Id: hal-02458568 https://hal.archives-ouvertes.fr/hal-02458568 Submitted on 26 Jun 2020 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. JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 116, E03005, doi:10.1029/2010JE003649, 2011 Modeling polarimetric radar scattering from the lunar surface: Study on the effect of physical properties of the regolith layer Wenzhe Fa,1 Mark A. Wieczorek,1 and Essam Heggy1,2 Received 10 May 2010; revised 21 November 2010; accepted 15 December 2010; published 5 March 2011. [1] A theoretical model for radar scattering from the lunar regolith using the vector radiative transfer theory for random media has been developed in order to aid in the interpretation of Mini‐SAR data from the Chandrayaan‐1 and Lunar Reconnaissance Orbiter missions. -
Monday Morning, October 19, 2015 Atom Probe Tomography Focus Topic Complex Device Such As Solar Cells and Batteries Is the Need of the Hour
Monday Morning, October 19, 2015 Atom Probe Tomography Focus Topic complex device such as solar cells and batteries is the need of the hour. Here we report on laser assisted atom probe tomography of energy storage Room: 230A - Session AP+AS+MC+MI+NS-MoM and conversion devices to identify the spatial distribution of the elements comprising the various layers and materials. Recent progress and significant Atom Probe Tomography of Nanomaterials challenges for preparation and study of perovskite solar cells and battery materials using laser assisted atom probe tomography will be discussed. Moderator: Daniel Perea, Pacific Northwest National This opens up new avenues to understand complex mutli-layer systems at Laboratory the atomic scale and provide a nanoscopic view into the intricate workings of energy materials. 8:20am AP+AS+MC+MI+NS-MoM1 Correlative Multi-scale Analysis of Nd-Fe-B Permanent Magnet, Taisuke Sasaki, T. Ohkubo, K. Hono, 10:00am AP+AS+MC+MI+NS-MoM6 Atom Probe Tomography of Pt- National Institute for Materials Science (NIMS), Japan INVITED based Nanoparticles, Katja Eder, P.J. Felfer, J.M. Cairney, The (Nd,Dy)–Fe–B based sintered magnets are currently used for traction University of Sydney, Australia motors and generators of (hybrid) electric vehicles because of their Pt nanoparticles are commonly used as catalysts in fuel cells. There are a lot excellent combination of maximum energy product and coercivity. of factors which influence the activity of a catalyst, including the surface However, there is a strong demand to achieve high coercivity without using structure and geometry [1], d-band vacancy of the metal catalyst [2], the Dy due to its scarce natural resources and high cost.