Geology of the Coastal Plain of South Carolina
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Alexander the Great's Tombolos at Tyre and Alexandria, Eastern Mediterranean ⁎ N
Available online at www.sciencedirect.com Geomorphology 100 (2008) 377–400 www.elsevier.com/locate/geomorph Alexander the Great's tombolos at Tyre and Alexandria, eastern Mediterranean ⁎ N. Marriner a, , J.P. Goiran b, C. Morhange a a CNRS CEREGE UMR 6635, Université Aix-Marseille, Europôle de l'Arbois, BP 80, 13545 Aix-en-Provence cedex 04, France b CNRS MOM Archéorient UMR 5133, 5/7 rue Raulin, 69365 Lyon cedex 07, France Received 25 July 2007; received in revised form 10 January 2008; accepted 11 January 2008 Available online 2 February 2008 Abstract Tyre and Alexandria's coastlines are today characterised by wave-dominated tombolos, peculiar sand isthmuses that link former islands to the adjacent continent. Paradoxically, despite a long history of inquiry into spit and barrier formation, understanding of the dynamics and sedimentary history of tombolos over the Holocene timescale is poor. At Tyre and Alexandria we demonstrate that these rare coastal features are the heritage of a long history of natural morphodynamic forcing and human impacts. In 332 BC, following a protracted seven-month siege of the city, Alexander the Great's engineers cleverly exploited a shallow sublittoral sand bank to seize the island fortress; Tyre's causeway served as a prototype for Alexandria's Heptastadium built a few months later. We report stratigraphic and geomorphological data from the two sand spits, proposing a chronostratigraphic model of tombolo evolution. © 2008 Elsevier B.V. All rights reserved. Keywords: Tombolo; Spit; Tyre; Alexandria; Mediterranean; Holocene 1. Introduction Courtaud, 2000; Browder and McNinch, 2006); (2) establishing a typology of shoreline salients and tombolos (Zenkovich, 1967; The term tombolo is used to define a spit of sand or shingle Sanderson and Eliot, 1996); and (3) modelling the geometrical linking an island to the adjacent coast. -
1 Paleobotanical Proxies for Early Eocene Climates and Ecosystems in Northern North 2 America from Mid to High Latitudes 3 4 Christopher K
https://doi.org/10.5194/cp-2020-32 Preprint. Discussion started: 24 March 2020 c Author(s) 2020. CC BY 4.0 License. 1 Paleobotanical proxies for early Eocene climates and ecosystems in northern North 2 America from mid to high latitudes 3 4 Christopher K. West1, David R. Greenwood2, Tammo Reichgelt3, Alexander J. Lowe4, Janelle M. 5 Vachon2, and James F. Basinger1. 6 1 Dept. of Geological Sciences, University of Saskatchewan, 114 Science Place, Saskatoon, 7 Saskatchewan, S7N 5E2, Canada. 8 2 Dept. of Biology, Brandon University, 270-18th Street, Brandon, Manitoba R7A 6A9, Canada. 9 3 Department of Geosciences, University of Connecticut, Beach Hall, 354 Mansfield Rd #207, 10 Storrs, CT 06269, U.S.A. 11 4 Dept. of Biology, University of Washington, Seattle, WA 98195-1800, U.S.A. 12 13 Correspondence to: C.K West ([email protected]) 14 15 Abstract. Early Eocene climates were globally warm, with ice-free conditions at both poles. Early 16 Eocene polar landmasses supported extensive forest ecosystems of a primarily temperate biota, 17 but also with abundant thermophilic elements such as crocodilians, and mesothermic taxodioid 18 conifers and angiosperms. The globally warm early Eocene was punctuated by geologically brief 19 hyperthermals such as the Paleocene-Eocene Thermal Maximum (PETM), culminating in the 20 Early Eocene Climatic Optimum (EECO), during which the range of thermophilic plants such as 21 palms extended into the Arctic. Climate models have struggled to reproduce early Eocene Arctic 22 warm winters and high precipitation, with models invoking a variety of mechanisms, from 23 atmospheric CO2 levels that are unsupported by proxy evidence, to the role of an enhanced 24 hydrological cycle to reproduce winters that experienced no direct solar energy input yet remained 25 wet and above freezing. -
Geology of the Charleston Phosphate Area, South Carolina
Geology of the Charleston Phosphate Area, South Carolina GEOLOGICAL SURVEY BULLETIN 1079 Geology of the Charleston Phosphate Area, South Carolina By HAROLD E. MALDE GEOLOGICAL SURVEY BULLETIN 1079 A detailed study of the area from which phosphate rock was first produced in this country UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1959 UNITED STATES DEPARTMENT OF THE INTERIOR FRED A. SEATON, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director The U.S. Geographical Survey Library has cataloged! this publication as follows: Malde, Harold Edwin, 1923- Geology of the Charleston phosphate area, South Carolina; a detailed study of the area from which phosphate rock was first produced in this country. Washington, U.S. Govt. Print. Off., 1959. v, 105 p. illus., maps, diagrs., profile, tables. 25 cm. (U. S. Geological Survey. Bulletin 1079) Part of illustrative matter folded in pocket. Bibliography: p. 96-101. 1. Geology South Carolina Charleston area. 2. Phosphates South Carolina. i. Title: Charleston phosphate area, South Caro lina. (Series) [QET5.B9 no. 1079] G S 59-214 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington 25, D.C. - Price $1.75 (paper cover) CONTENTS Page Abstract.___-_-----_--_----___-__-___---_-__-_--____----_-_----__ 1 Introduction______________________________________________________ 2 Stratigraphy. ____-_---_--_-_-___-_-_____-_-__----_-_-__-__-____-_- 5 General features_-_____--__________-_-_-__-__-_-___-____-___- 5 Oligocene series_______-_-__--_____-_-_-__--__-_----__________- 7 Cooper marl_______________________________________________ 7 Name_ ______________________________________________ 7 Distribution._________________________________________ 7 Structural attitude________.___-__----_-__-_--_-______- 8 Thickness. -
HORSE in TRAINING, Consigned by Kingstone Warren Stables (H
HORSE IN TRAINING, consigned by Kingstone Warren Stables (H. Candy) the Property of a Partnership Will Stand at Park Paddocks, Highflyer Paddock DD, Box 750 Danehill Dancer Danehill (USA) 2182 (WITH VAT) (IRE) Mira Adonde (USA) Monsieur Bond (IRE) Song MADELEINE BOND Musical Essence (GB) Effervescence II (2014) Pivotal (GB) Captain Rio (GB) A Chesnut Mare Spin A Wish (GB) Beloved Visitor (USA) (2008) Be My Chief (USA) Be My Wish (GB) Spinner MADELEINE BOND (GB): won 3 races at 3 years and £22,479 and placed 6 times. Highest BHA rating 86 (Flat) Latest BHA rating 71 (Flat) (prior to compilation) TURF 17 runs 3 wins 5 pl £21,216 G - S 7f - 1m ALL WEATHER 5 runs 1 pl £1,262 1st Dam SPIN A WISH (GB), won 1 race at 4 years and placed 3 times; dam of two winners from 3 runners and 3 foals of racing age viz- MADELEINE BOND (GB) (2014 f. by Monsieur Bond (IRE)), see above. STONEY LANE (GB) (2015 g. by Mayson (GB)), won 1 race at 4 years, 2019, placed 4 times. Samantha James (GB) (2016 f. by Kuroshio (AUS)), placed once at 2 years, 2018. She also has a 2018 filly by Charming Thought (GB). 2nd Dam BE MY WISH (GB), won 2 races at 3 and 5 years and £14,884 and placed 11 times; dam of three winners from 6 runners and 6 foals of racing age including- BUTCH AND SUNDANCE (GB), won 1 race at 2 years and placed twice. 3rd Dam SPINNER, won 1 race at 3 years and placed 4 times; dam of eight winners from 11 runners and 12 foals of racing age including- Seigneurial (GB), won 7 races at 2, 4 and 5 years at home and in U.S.A., placed third in Timeform Harry Rosebery Trophy, Ayr, L., Radar Ahead Handicap, Hollywood Park, L. -
Wec01's SSSS Fossils Test 2019
wec01’s SSSS Fossils Test 2019 Team Name: _________________KEY________________ Team Number: ___KEY___ Team Members: ____________KEY____________, ____________KEY____________ This test consists of 18 stations with a total of 200 points. Each answer is worth one point except where specified otherwise. You are only given 2 ½ minutes with the specimens at each station, however you can work on any station’s questions at any time. Scoring Station 1: ___10___ / 10 Station 10: ___12___ / 12 Station 2: ___10___ / 10 Station 11: ____9___ / 9 Station 3: ___11___ / 11 Station 12: ___11___ / 11 Station 4: ___10___ / 10 Station 13: ___10___ / 10 Station 5: ___10___ / 10 Station 14: ___10___ / 10 Station 6: ____9___ / 9 Station 15: ___12___ / 12 Station 7: ____9___ / 9 Station 16: ____9___ / 9 Station 8: ___10___ / 10 Station 17: ___10___ / 10 Station 9: ____9___ / 9 Station 18: ___29___ / 29 Total: __200___ / 200 Team Number: _KEY_ Station 1: Dinosaurs (10 pt) 1. Identify the genus of specimen A Tyrannosaurus (1 pt) 2. Identify the genus of specimen B Stegosaurus (1 pt) 3. Identify the genus of specimen C Allosaurus (1 pt) 4. Which specimen(s) (A, B, or C) are A, C (1 pt) Saurischians? 5. Which two specimens (A, B, or C) lived at B, C (1 pt) the same time? 6. Identify the genus of specimen D Velociraptor (1 pt) 7. Identify the genus of specimen E Coelophysis (1 pt) 8. Which specimen (D or E) is commonly E (1 pt) found in Ghost Ranch, New Mexico? 9. Which specimen (A, B, C, D, or E) would D (1 pt) specimen F have been found on? 10. -
Temperature Variability in the Bay of Biscay During the Past 40 Years, from an in Situ Analysis and a 3D Global Simulation
ARTICLE IN PRESS Continental Shelf Research 29 (2009) 1070–1087 Contents lists available at ScienceDirect Continental Shelf Research journal homepage: www.elsevier.com/locate/csr Temperature variability in the Bay of Biscay during the past 40 years, from an in situ analysis and a 3D global simulation S. Michel a,Ã, A.-M. Treguier b, F. Vandermeirsch a a Dynamiques de l’Environnement Coˆtier/Physique Hydrodynamique et Se´dimentaire, IFREMER, BP 70, 29280 Plouzane´, France b Laboratoire de Physique des Oce´ans, CNRS-IFREMER-IRD-UBO, BP 70, 29280 Plouzane´, France article info abstract Article history: A global in situ analysis and a global ocean simulation are used jointly to study interannual to decadal Received 21 June 2008 variability of temperature in the Bay of Biscay, from 1965 to 2003. A strong cooling is obtained at all Received in revised form depths until the mid-1970’s, followed by a sustained warming over 30 years. Strong interannual 21 November 2008 fluctuations are superimposed on this slow evolution. The fluctuations are intensified at the surface and Accepted 27 November 2008 are weakest at 500 m. A good agreement is found between the observed and simulated temperatures, Available online 6 February 2009 in terms of mean values, interannual variability and time correlations. Only the decadal trend is Keywords: significantly underestimated in the simulation. A comparison to satellite sea surface temperature (SST) Bay of Biscay data over the last 20 years is also presented. The first mode of interannual variability exhibits a quasi- Interannual temperature variability uniform structure and is related to the inverse winter North Atlantic Oscillation (NAO) index. -
The Mississippi River Delta Basin and Why We Are Failing to Save Its Wetlands
University of New Orleans ScholarWorks@UNO University of New Orleans Theses and Dissertations Dissertations and Theses 8-8-2007 The Mississippi River Delta Basin and Why We are Failing to Save its Wetlands Lon Boudreaux Jr. University of New Orleans Follow this and additional works at: https://scholarworks.uno.edu/td Recommended Citation Boudreaux, Lon Jr., "The Mississippi River Delta Basin and Why We are Failing to Save its Wetlands" (2007). University of New Orleans Theses and Dissertations. 564. https://scholarworks.uno.edu/td/564 This Thesis is protected by copyright and/or related rights. It has been brought to you by ScholarWorks@UNO with permission from the rights-holder(s). You are free to use this Thesis in any way that is permitted by the copyright and related rights legislation that applies to your use. For other uses you need to obtain permission from the rights- holder(s) directly, unless additional rights are indicated by a Creative Commons license in the record and/or on the work itself. This Thesis has been accepted for inclusion in University of New Orleans Theses and Dissertations by an authorized administrator of ScholarWorks@UNO. For more information, please contact [email protected]. The Mississippi River Delta Basin and Why We Are Failing to Save Its Wetlands A Thesis Submitted to the Graduate Faculty of the University of New Orleans in partial fulfillment of the requirements for the degree of Master of Science in Urban Studies By Lon J. Boudreaux Jr. B.S. Our Lady of Holy Cross College, 1992 M.S. University of New Orleans, 2007 August, 2007 Table of Contents Abstract............................................................................................................................. -
Kentucky Derby, Flamingo Stakes, Florida Derby, Blue Grass Stakes, Preakness, Queen’S Plate 3RD Belmont Stakes
Northern Dancer 90th May 2, 1964 THE WINNER’S PEDIGREE AND CAREER HIGHLIGHTS Pharos Nearco Nogara Nearctic *Lady Angela Hyperion NORTHERN DANCER Sister Sarah Polynesian Bay Colt Native Dancer Geisha Natalma Almahmoud *Mahmoud Arbitrator YEAR AGE STS. 1ST 2ND 3RD EARNINGS 1963 2 9 7 2 0 $ 90,635 1964 3 9 7 0 2 $490,012 TOTALS 18 14 2 2 $580,647 At 2 Years WON Summer Stakes, Coronation Futurity, Carleton Stakes, Remsen Stakes 2ND Vandal Stakes, Cup and Saucer Stakes At 3 Years WON Kentucky Derby, Flamingo Stakes, Florida Derby, Blue Grass Stakes, Preakness, Queen’s Plate 3RD Belmont Stakes Horse Eq. Wt. PP 1/4 1/2 3/4 MILE STR. FIN. Jockey Owner Odds To $1 Northern Dancer b 126 7 7 2-1/2 6 hd 6 2 1 hd 1 2 1 nk W. Hartack Windfields Farm 3.40 Hill Rise 126 11 6 1-1/2 7 2-1/2 8 hd 4 hd 2 1-1/2 2 3-1/4 W. Shoemaker El Peco Ranch 1.40 The Scoundrel b 126 6 3 1/2 4 hd 3 1 2 1 3 2 3 no M. Ycaza R. C. Ellsworth 6.00 Roman Brother 126 12 9 2 9 1/2 9 2 6 2 4 1/2 4 nk W. Chambers Harbor View Farm 30.60 Quadrangle b 126 2 5 1 5 1-1/2 4 hd 5 1-1/2 5 1 5 3 R. Ussery Rokeby Stables 5.30 Mr. Brick 126 1 2 3 1 1/2 1 1/2 3 1 6 3 6 3/4 I. -
Functional Morphology of the Vertebral Column in Remingtonocetus (Mammalia, Cetacea) and the Evolution of Aquatic Locomotion in Early Archaeocetes
Functional Morphology of the Vertebral Column in Remingtonocetus (Mammalia, Cetacea) and the Evolution of Aquatic Locomotion in Early Archaeocetes by Ryan Matthew Bebej A dissertation submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy (Ecology and Evolutionary Biology) in The University of Michigan 2011 Doctoral Committee: Professor Philip D. Gingerich, Co-Chair Professor Philip Myers, Co-Chair Professor Daniel C. Fisher Professor Paul W. Webb © Ryan Matthew Bebej 2011 To my wonderful wife Melissa, for her infinite love and support ii Acknowledgments First, I would like to thank each of my committee members. I will be forever grateful to my primary mentor, Philip D. Gingerich, for providing me the opportunity of a lifetime, studying the very organisms that sparked my interest in evolution and paleontology in the first place. His encouragement, patience, instruction, and advice have been instrumental in my development as a scholar, and his dedication to his craft has instilled in me the importance of doing careful and solid research. I am extremely grateful to Philip Myers, who graciously consented to be my co-advisor and co-chair early in my career and guided me through some of the most stressful aspects of life as a Ph.D. student (e.g., preliminary examinations). I also thank Paul W. Webb, for his novel thoughts about living in and moving through water, and Daniel C. Fisher, for his insights into functional morphology, 3D modeling, and mammalian paleobiology. My research was almost entirely predicated on cetacean fossils collected through a collaboration of the University of Michigan and the Geological Survey of Pakistan before my arrival in Ann Arbor. -
A Review of Ethnographic and Historically Recorded Dentaliurn Source Locations
FISHINGFOR IVORYWORMS: A REVIEWOF ETHNOGRAPHICAND HISTORICALLY RECORDEDDENTALIUM SOURCE LOCATIONS Andrew John Barton B.A., Simon Fraser University, 1979 THESIS SUBMITTED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF ARTS IN THE DEPARTMENT OF ARCHAEOLOGY Q Andrew John Barton 1994 SIMON FRASER UNIVERSITY Burnaby October, 1994 All rights reserved. This work may not be reproduced in whole or in part, by photocopy or other means without permission of the author. Name: Andrew John Barton Degree: Master of Arts (Archaeology) Title of Thesis: Fishing for Ivory Worms: A Review of Ethnographic and Historically Recorded Dentaliurn Source Locations Examining Committee: Chairperson: Jack D. Nance - -, David V. Burley Senior Supervisor Associate Professor Richard Inglis External Examiner Department of Aboriginal Affairs Government of British Columbia PARTIAL COPYRIGHT LICENSE I hereby grant to Simon Fraser University the right to lend my thesis or dissertation (the title of which is shown below) to users of the Simon Fraser University Library, and to make partial or single copies only for such users or in response to a request from the library of any other university, or other educational institution, on its own behalf or for one of its users. I further agree that permission for multiple copying of this thesis for scholarly purposes may be granted by me or the Dean of Graduate Studies. It is understood that copying or publication of this thesis for financial gain shall not be allowed without my written permission. Title of ThesisIDissertation: Fishing for Ivory Worms: A Review of Ethnographic and Historically Recorded Dentalium Source Locations Author: Andrew John Barton Name October 14, 1994 Date This study reviews and examines historic and ethnographic written documents that identify locations where Dentaliurn shells were procured by west coast Native North Americans. -
Jutland, Denmark
Contr. Tert. Geol. 7 fig'., 4 tab., 3 pis. Leiden, September 1990 Quatern. 27(2-3) 3981 A Late Oligocene (Chattian B) molluscan fauna from the coastal cliff at Mogenstrup, North of Skive, Jutland, Denmark K.I. Schnetler LANGA, DENMARK and C. Beyer STAVANGER, NORWAY Schnetler, K.I., & C. Beyer. A Late Oligocene (Chattian B) molluscan fauna from the coastal cliff at Mogenstrup, North of Skive, Jutland, Denmark. — Contr. Tert. Quatern. Geol., 27(2-3): 39-82, 7 figs, 3 tabs, 3 pis. Leiden, September 1990. rich Late molluscan fauna from coastal cliff North of Skive, was studied. A very Oligocene a at Mogenstrup, Jutland, Denmark, A of the Late in NW is the and the section are des- summary Palaeogene sedimentary sequence Jutland given, locality exposed cribed. Lithostratigraphical, magnetostratigraphical and biostratigraphical correlations are suggested. A list of the molluscan species is given, comparisons with other Danish and German Late Oligocene localities are made, and palaeoecological interpreta- the Andersondrillia is introduced within the Microdrillia. tions are suggested. In the systematic part subgenus subgen. nov. genus Several taxa are discussed and the followingnew species and subspecies are described: Limopsis (Pectunculina) lamellata chattica subsp. vonderhochti Collonia troelsi nov., Limopsis (Pectunculina) sp. nov., (Collonia) sp. nov., Lepetella helgae sp. nov., Lepetellajytteae sp. nov., Laiocochlis Tubiola subangulata sp. nov., Cerithiopsis (s. lat.) antonjansei sp. nov., (Laiocochlis) supraoligocaenica sp. nov., Triforis (Trituba) Cirsotrema Searlesia ravni brueckneri danica Clavatula sorgenfreii sp. nov., (Opaliopsis) subglabrum sp. nov., sp. nov., Angistoma subsp. nov., Microdrillia Pleurotomella mogenstrupensis sp. nov., Microdrillia (Microdrillia) ingerae sp. nov., (Andersondrillia) brejningensis sp. nov., rasmusseni and ? nov. -
Major Geographic Regions and Popula on of the United States of America
Major geographic regions and populaon of the United States of America Major geographic regions and populaon of the United States of America Lesson plan (Polish) Lesson plan (English) Major geographic regions and populaon of the United States of America Link to the lesson Before you start you should know that the United Stated is an economically developed country; that the United States is an immigrant country founded mainly by immigrants from Europe and slaves brought from Africa; that a region’s natural environment influences its economic development. You will learn to show the great regions on a map of the United States; to name the major population groups inhabiting the United States; to name the reasons for the decline of the Native American culture. Nagranie dostępne na portalu epodreczniki.pl Nagranie dźwiękowe abstraktu Major geographic regions of the United States of America The United States of America is the fourth largest country in the world, with a surface area of 9,526,5 thousand sq. km, and the third most populous one, with 322 million inhabitants in 2010. This vast country is made up of continental states that lie in the central part of the North American continent, between the 25th parallel north and the 49th parallel north. Two more states, Alaska in the northwest extremity of North America and Hawaii in the Pacific Ocean, are located outside the main part of the United States. One of the crucial features of the natural environment of the United States is the meridional layout of its major geographic regions, which differ in altitude above sea level and landscape.