A Historical Account of How Continental Drift and Plate Tectonics Provided the Framework for Our Current Understanding of Palaeogeography
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The Geology of England – Critical Examples of Earth History – an Overview
The Geology of England – critical examples of Earth history – an overview Mark A. Woods*, Jonathan R. Lee British Geological Survey, Environmental Science Centre, Keyworth, Nottingham, NG12 5GG *Corresponding Author: Mark A. Woods, email: [email protected] Abstract Over the past one billion years, England has experienced a remarkable geological journey. At times it has formed part of ancient volcanic island arcs, mountain ranges and arid deserts; lain beneath deep oceans, shallow tropical seas, extensive coal swamps and vast ice sheets; been inhabited by the earliest complex life forms, dinosaurs, and finally, witnessed the evolution of humans to a level where they now utilise and change the natural environment to meet their societal and economic needs. Evidence of this journey is recorded in the landscape and the rocks and sediments beneath our feet, and this article provides an overview of these events and the themed contributions to this Special Issue of Proceedings of the Geologists’ Association, which focuses on ‘The Geology of England – critical examples of Earth History’. Rather than being a stratigraphic account of English geology, this paper and the Special Issue attempts to place the Geology of England within the broader context of key ‘shifts’ and ‘tipping points’ that have occurred during Earth History. 1. Introduction England, together with the wider British Isles, is blessed with huge diversity of geology, reflected by the variety of natural landscapes and abundant geological resources that have underpinned economic growth during and since the Industrial Revolution. Industrialisation provided a practical impetus for better understanding the nature and pattern of the geological record, reflected by the publication in 1815 of the first geological map of Britain by William Smith (Winchester, 2001), and in 1835 by the founding of a national geological survey. -
Dolerites of Svalbard, North-West Barents Sea Shelf: Age, Tectonic Setting and Significance for Geotectonic Interpretation of Th
RESEARCH/REVIEW ARTICLE Dolerites of Svalbard, north-west Barents Sea Shelf: age, tectonic setting and significance for geotectonic interpretation of the High-Arctic Large Igneous Province Krzysztof Nejbert1, Krzysztof P. Krajewski2, Elz˙bieta Dubin´ ska1 & Zolta´ nPe´ cskay3 1 Institute of Geochemistry, Mineralogy and Petrology, University of Warsaw, Al. Z˙ wirki i Wigury 93, PL-02089 Warsaw, Poland 2 Institute of Geological Sciences, Polish Academy of Sciences, Research Centre in Warsaw, ul. Twarda 51/55, PL-00818 Warsaw, Poland 3 Institute of Nuclear Research, Hungarian Academy of Sciences, Bem te´ r 18/c, HU-4026 Debrecen, Hungary Keywords Abstract Dolerite; geochemistry; petrogenesis; KÁAr whole rock ages; Svalbard; Cretaceous. The dolerites of Svalbard are mineralogically and geochemically homogeneous with geochemical features typical of continental within-plate tholeiites. Their Correspondence geochemistry is similar to tholeiites belonging to a bimodal suite defined as the Krzysztof P. Krajewski, Institute of Geologi- High-Arctic Large Igneous Province (HALIP). KÁAr dating of numerous cal Sciences, Polish Academy of Sciences, dolerites sampled from many locations across Svalbard define a narrow time Research Centre in Warsaw, ul. Twarda 51/ span of this magmatism from 125.593.6 to 78.392.6 Mya. Discrete peaks of 55, PL-00818 Warsaw, Poland. E-mail: [email protected] intensive activity occurred at 115.3, 100.8, 91.3 and 78.5 Mya corresponding to (1) breakup of the continental crust and formation of an initial rift as a result of mantle plume activity, located in the southern part of the Alpha Ridge; (2) magmatic activity related to spreading along the Alpha Ridge that led to the development of the initial oceanic crust and (3) continuation of spreading along the Alpha Ridge and termination of magmatic activity related to HALIP (last two peaks at 91.3 and 78.5 Mya). -
Hydrographic Development of the Aral Sea During the Last 2000 Years Based on a Quantitative Analysis of Dinoflagellate Cysts
Palaeogeography, Palaeoclimatology, Palaeoecology 234 (2006) 304–327 www.elsevier.com/locate/palaeo Hydrographic development of the Aral Sea during the last 2000 years based on a quantitative analysis of dinoflagellate cysts P. Sorrel a,b,*, S.-M. Popescu b, M.J. Head c,1, J.P. Suc b, S. Klotz b,d, H. Oberha¨nsli a a GeoForschungsZentrum, Telegraphenberg, D-14473 Potsdam, Germany b Laboratoire Pale´oEnvironnements et Pale´obioSphe`re (UMR CNRS 5125), Universite´ Claude Bernard—Lyon 1, 27-43, boulevard du 11 Novembre, 69622 Villeurbanne Cedex, France c Department of Geography, University of Cambridge, Downing Place, Cambridge CB2 3EN, UK d Institut fu¨r Geowissenschaften, Universita¨t Tu¨bingen, Sigwartstrasse 10, 72070 Tu¨bingen, Germany Received 30 June 2005; received in revised form 4 October 2005; accepted 13 October 2005 Abstract The Aral Sea Basin is a critical area for studying the influence of climate and anthropogenic impact on the development of hydrographic conditions in an endorheic basin. We present organic-walled dinoflagellate cyst analyses with a sampling resolution of 15 to 20 years from a core retrieved at Chernyshov Bay in the NW Large Aral Sea (Kazakhstan). Cysts are present throughout, but species richness is low (seven taxa). The dominant morphotypes are Lingulodinium machaerophorum with varied process length and Impagidinium caspienense, a species recently described from the Caspian Sea. Subordinate species are Caspidinium rugosum, Romanodinium areolatum, Spiniferites cruciformis, cysts of Pentapharsodinium dalei, and round brownish protoper- idiniacean cysts. The chlorococcalean algae Botryococcus and Pediastrum are taken to represent freshwater inflow into the Aral Sea. The data are used to reconstruct salinity as expressed in lake level changes during the past 2000 years. -
Nov07 NUCLEUS Aa4b
DED UN 18 O 98 F http://www.nesacs.org N Y O T R E I T H C E N O A E S S S L T A E A C R C I N S M S E E H C C TI N O CA February 2009 Vol. LXXXVII, No. 6 N • AMERI Monthly Meeting Professor Wilton L. Virgo of Wellesley College to Speak at Simmons College Tips for Job Seekers By Megan Driscoll Summer Scholar Report Identification of Genes Regulated by Transcriptional Regulator, p8 By Derek Kong This Month in Chemical History By Harold Goldwhite, California State University, Los Angeles February Historical Events in Chemistry by Leopold May, The Catholic University of America, Washington, DC February 1, 1905 methods for the determination of ing and used it against pellagra and Fifty years ago, Emilio Segré shared crystal structures, was born on this pursued the idea that diseases such the Nobel Prize in Physics (1959) day. as beriberi, scurvy, rickets and pella- with Owen Chamberlain for their gra were caused by lack of vital sub- discovery of the antiproton. He co- February 16, 1955 stances in the diet. discovered technetium with C. Per- F. P. Bundy, H. T. Hall, H. M. Strong rier in 1937, and astatine with D. R. and R. H. O. Wentoff announced the February 25, 1880 Corson and R. MacKenzie in 1940, synthesis of diamonds at General Arthur B. Lamb, who was the editor and demonstrated the existence of Electric Research Laboratories on of the Journal of the American the antiproton in 1955. -
Geology: Ordovician Paleogeography and the Evolution of the Iapetus Ocean
Ordovician paleogeography and the evolution of the Iapetus ocean Conall Mac Niocaill* Department of Geological Sciences, University of Michigan, 2534 C. C. Little Building, Ben A. van der Pluijm Ann Arbor, Michigan 48109-1063. Rob Van der Voo ABSTRACT thermore, we contend that the combined paleomagnetic and faunal data ar- Paleomagnetic data from northern Appalachian terranes identify gue against a shared Taconic history between North and South America. several arcs within the Iapetus ocean in the Early to Middle Ordovi- cian, including a peri-Laurentian arc at ~10°–20°S, a peri-Avalonian PALEOMAGNETIC DATA FROM IAPETAN TERRANES arc at ~50°–60°S, and an intra-oceanic arc (called the Exploits arc) at Displaced terranes occur along the extent of the Appalachian-Cale- ~30°S. The peri-Avalonian and Exploits arcs are characterized by Are- donian orogen, although reliable Ordovician paleomagnetic data from Ia- nigian to Llanvirnian Celtic fauna that are distinct from similarly aged petan terranes have only been obtained from the Central Mobile belt of the Toquima–Table Head fauna of the Laurentian margin, and peri- northern Appalachians (Table 1). The Central Mobile belt separates the Lau- Laurentian arc. The Precordillera terrane of Argentina is also charac- rentian and Avalonian margins of Iapetus and preserves remnants of the terized by an increasing proportion of Celtic fauna from Arenig to ocean, including arcs, ocean islands, and ophiolite slivers (e.g., Keppie, Llanvirn time, which implies (1) that it was in reproductive communi- 1989). Paleomagnetic results from Arenigian and Llanvirnian volcanic units cation with the peri-Avalonian and Exploits arcs, and (2) that it must of the Moreton’s Harbour Group and the Lawrence Head Formation in cen- have been separate from Laurentia and the peri-Laurentian arc well tral Newfoundland indicate paleolatitudes of 11°S (Table 1), placing them before it collided with Gondwana. -
General Guide to the Science and Cosmos Museum
General guide to the Science and Cosmos Museum 1 Background: “Tenerife monts” and “Pico” near of Plato crater in the Moon PLANTA TERRAZA Terrace Floor 5 i 2 1 4 6 3 ASCENSOR 4 RELOJ DE SOL ECUATORIAL Elevator Analemmatic sundial i INFORMACIÓN 5 BUSTO PARLANTE Information “AGUSTÍN DE BETANCOURT” Agustín de Betancourt 1 PLAZA “AGUSTÍN DE talking bust BETANCOURT” Agustín de Betancourt 6 ZONA WI-FI Square Wi-Fi zone 2 ANTENA DE RADIOASTRONOMÍA Radioastronomy antenna 3 TELESCOPIO Telescope PLANTA BAJA Ground Floor WC 10 9 8 11 7 1 6 5 4 12 2 3 ASCENSOR Cosmos Lab - Creative Elevator Laboratory 1 EXPOSICIÓN 7 PLANETARIO Exhibition Planetarium 2 TALLER DE DIDÁCTICA 8 SALIDA DE EMERGENCIA Didactic Workshop Emergency exit 3 EFECTOS ÓPTICOS 9 MICROCOSMOS Optical illusions 10 SALÓN DE ACTOS 4 SALA CROMA KEY Assembly hall Chroma Key room 11 EXPOSICIONES TEMPORALES 5 LABERINTO DE ESPEJOS Temporary exhibitions Mirror Labyrinth 12 ZONA DE DESCANSO 6 COSMOS LAB - LABORATORIO Rest zone CREATIVO CONTENIDOS Contents 7 LA TIERRA The Earth 23 EL SOL The Sun 33 EL UNIVERSO The Universe 45 CÓMO FUNCIONA How does it work 72 EL CUERPO HUMANO The human body 5 ¿POR QUÉ PIRÁMIDES? Why pyramids? 1 Sacred places have often been con- ceived of as elevated spaces that draw the believer closer to the divi- nity. For this reason, once architec- tural techniques became sufficiently refined, mosques or cathedrals rai- sed their vaults, minarets, towers and spires to the sky. However, for thousands of years, the formula fa- voured by almost every culture was the pyramid. -
2012-Ruiz-Martinez-Etal-EPSL.Pdf
Earth and Planetary Science Letters 331-332 (2012) 67–79 Contents lists available at SciVerse ScienceDirect Earth and Planetary Science Letters journal homepage: www.elsevier.com/locate/epsl Earth at 200 Ma: Global palaeogeography refined from CAMP palaeomagnetic data Vicente Carlos Ruiz-Martínez a,b,⁎, Trond H. Torsvik b,c,d,e, Douwe J.J. van Hinsbergen b,c, Carmen Gaina b,c a Departamento de Geofísica y Meteorología, Facultad de Física, Universidad Complutense de Madrid, Avda. Complutense s/n, 28040 Madrid, Spain b Center for Physics of Geological Processes, University of Oslo, 0316 Oslo, Norway c Center of Advanced Study, Norwegian Academy of Science and Letters, 0271 Oslo, Norway d Geodynamics, NGU, N-7491 Trondheim, Norway e School of Geosciences, University of the Witwatersrand, WITS, 2050, South Africa article info abstract Article history: The Central Atlantic Magmatic Province was formed approximately 200 Ma ago as a prelude to the breakup of Received 21 November 2011 Pangea, and may have been a cause of the Triassic–Jurassic mass extinction. Based on a combination of (i) a Received in revised form 26 January 2012 new palaeomagnetic pole from the CAMP related Argana lavas (Moroccan Meseta Block), (ii) a global compila- Accepted 2 March 2012 tion of 190–210 Ma poles, and (iii) a re-evaluation of relative fits between NW Africa, the Moroccan Meseta Available online xxxx Block and Iberia, we calculate a new global 200 Ma pole (latitude=70.1° S, longitude=56.7° E and A95 =2.7°; Editor: P. DeMenocal N=40 poles; NW Africa co-ordinates). We consider the palaeomagnetic database to be robust at 200±10 Ma, which allows us to craft precise reconstructions near the Triassic–Jurassic boundary: at this very important Keywords: time in Earth history, Pangea was near-equatorially centered, the western sector was dominated by plate conver- palaeomagnetism gence and subduction, while in the eastern sector, the Palaeotethys oceanic domain was almost consumed palaeogeography because of a widening Neothethys. -
A Christian Physicist Examines Noah's Flood and Plate Tectonics
A Christian Physicist Examines Noah’s Flood and Plate Tectonics by Steven Ball, Ph.D. September 2003 Dedication I dedicate this work to my friend and colleague Rodric White-Stevens, who delighted in discussing with me the geologic wonders of the Earth and their relevance to Biblical faith. Cover picture courtesy of the U.S. Geological Survey, copyright free 1 Introduction It seems that no subject stirs the passions of those intending to defend biblical truth more than Noah’s Flood. It is perhaps the one biblical account that appears to conflict with modern science more than any other. Many aspiring Christian apologists have chosen to use this account as a litmus test of whether one accepts the Bible or modern science as true. Before we examine this together, let me clarify that I accept the account of Noah’s Flood as completely true, just as I do the entirety of the Bible. The Bible demonstrates itself to be reliable and remarkably consistent, having numerous interesting participants in various stories through which is interwoven a continuous theme of God’s plan for man’s redemption. Noah’s Flood is one of those stories, revealing to us both God’s judgment of sin and God’s over-riding grace and mercy. It remains a timeless account, for it has much to teach us about a God who never changes. It is one of the most popular Bible stories for children, and the truth be known, for us adults as well. It is rather unfortunate that many dismiss the account as mythical, simply because it seems to be at odds with a scientific view of the earth. -
Glacial Geomorphology☆ John Menzies, Brock University, St
Glacial Geomorphology☆ John Menzies, Brock University, St. Catharines, ON, Canada © 2018 Elsevier Inc. All rights reserved. This is an update of H. French and J. Harbor, 8.1 The Development and History of Glacial and Periglacial Geomorphology, In Treatise on Geomorphology, edited by John F. Shroder, Academic Press, San Diego, 2013. Introduction 1 Glacial Landscapes 3 Advances and Paradigm Shifts 3 Glacial Erosion—Processes 7 Glacial Transport—Processes 10 Glacial Deposition—Processes 10 “Linkages” Within Glacial Geomorphology 10 Future Prospects 11 References 11 Further Reading 16 Introduction The scientific study of glacial processes and landforms formed in front of, beneath and along the margins of valley glaciers, ice sheets and other ice masses on the Earth’s surface, both on land and in ocean basins, constitutes glacial geomorphology. The processes include understanding how ice masses move, erode, transport and deposit sediment. The landforms, developed and shaped by glaciation, supply topographic, morphologic and sedimentologic knowledge regarding these glacial processes. Likewise, glacial geomorphology studies all aspects of the mapped and interpreted effects of glaciation both modern and past on the Earth’s landscapes. The influence of glaciations is only too visible in those landscapes of the world only recently glaciated in the recent past and during the Quaternary. The impact on people living and working in those once glaciated environments is enormous in terms, for example, of groundwater resources, building materials and agriculture. The cities of Glasgow and Boston, their distinctive street patterns and numerable small hills (drumlins) attest to the effect of Quaternary glaciations on urban development and planning. It is problematic to precisely determine when the concept of glaciation first developed. -
Wegener and His Theory of Continental Drift
GENERAL I ARTICLE Wegener and his Theory of Continental Drift Ramesh Chander Alfred Wegener, an astronomer by training and meteorologist by profession, visualised that there was once a single very large landmass on the surface of the earth. Gradually it broke up into smaller fragments which drifted away to form the present continents. In a few cases, the drifting fragments subsequently collided, coalesced and Ramesh Chander is a formed larger landmasses again. Wegener could thus Professor at the Universit}' explain in a simple way (i) similarities in shapes of of Rool'kee, engaged in diverse studies related to continental coast lines separated by wide oceans, (ii) natural earthquakes in the similarities in the rocks and fossils occurring on such Himalaya as well as coasts and in the fauna and flora inhabiting them, (ill) the modelling of reservoir formation of several major mountain ranges of the world, induced earthquakes in that region. and (iv) the evidence in rocks on past climates ofthe earth. Introduction Astronomers take immense delight in enumerating the various motions that we partake even as we are apparently stationary on the surface of the earth. Geophysicists, the people who apply the principles of physics to investigate the earth, gleefully add that the surface of the terra firma itself is not steady but responds pliantly to many causes in the earth's interior and on its surface as well as to a few causes in the solar system. Occasionally, we can feel the motion of the earth's surface directly for brief periods, as during a major earthquake or when a heavy object moves near us. -
THE RELATION of PHYSICIANS to EARLY AMERICAN GEOLOGY by WILLIAM BROWNING, Ph.B., M.D
THE RELATION OF PHYSICIANS TO EARLY AMERICAN GEOLOGY By WILLIAM BROWNING, Ph.B., M.D. BROOKLYN, N. Y. HE part taken by physicians but part of the larger one of medical in the genesis of the natural pioneering in the sciences. Medicine sciences has long been re- has been termed “Mother of the marked. Their share in the Sciences,” which fits in very well, as development of such lines inMaclure, this a non-medical Scot, is some- Tcountry is worthy of consideration. A times called the father of American similarity in primogenesis of the geology; though, if medico-socialistic sciences here and at large is the more not to say communistic upheavers natural as they were not simply progress, the juniors may become even transplanted but in varying degrees less proud of the old lady. further developed. Especially in geol- The instances so far found of this ogy the necessary application to indi- double form of professional training genous conditions and the rapid are, as follows, the names arranged advance of the subject at that period chronologically according to date of made its origin here comparable to birth. Of course these men did their that of a new science. geologic work years later. Many of the It is from the historic point of names are so well-known that only view, rather than from any special brief mention is necessary. More de- knowledge of geology, that the subject tails are hence given of those whose is here approached, though every sketches in biographic works are im- intelligent person can find interest in perfect or wanting, or whose relation some phase of the science. -
President's Report
KASSACHUSETTS INSTITUTE OF TECHNOLOGY. t PRESIDENT'S REPORT FOR THE Year ending" Sept. 30, 1875, BOSTON: PRESS Or A. A. KINGMAN, I8'/6. ~i~ 1~i i MASSACHUSETTS INSTITUTE OF TECHNOLOGY. PRESIDENT'S REPORT FOR THE Year ending Sept. 30~ 1875. BOSTON : PRESS OF A. A. KINGMAN. 1876. , , , ~ ', Extracts from Acts of the General Court of Jl,[assachusetts, in relation to he Massachusetts Institute of Technology. Act of Incorporation. "William B. Rogers [and others named], their associates and successors, are hereby made a body corporate, by the name of the M.~SSA- CHUSliTTS INSTITUTEOF T~CHNOLOGY, for the purpose of instituting and maintaining a Society of Arts, a Museum of Arts, and a School of Industrial Science, and aiding generally, by suitable means, the advancement, development, and practical appli- cation of sciences in connection with arts, agriculture, manufactures, and commerce." Chapter 183, Acts and ~e~oZves of 1861. Grant of Public Lands. "When the Massachusetts Institute of Technology shall have been duly organized, located, and established, ...... there shall be appropriated and paid to its treasurer, each year, on the warrant of the Governor, for ~i~ ~ its endowment, support, and maintenance, one third part of the annual interest or Income which may be received from the fund created under and by virtue of the 130th chapter of the Acts of the 37th Congress~ at the second session thereof, approved July 2, 1862 [giving Public Lands to the States in aid of instruction in Agriculture, the Mechanic Arts, and Military Science and Tactics] ...... Said Institute of Technology, in addition to the objects set forth in its Act of Incorporation [as above quoted], shall provide for instruction in military tactics." Chapter 186, Acts and _Resolvesof 1863.