Download Guidebook As .Pdf
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Silicified Eocene Molluscs from the Lower Murchison District, Southern Carnarvon Basin, Western Australia
[<ecords o{ the Western A uslralian Museum 24: 217--246 (2008). Silicified Eocene molluscs from the Lower Murchison district, Southern Carnarvon Basin, Western Australia Thomas A. Darragh1 and George W. Kendrick2.3 I Department of Invertebrate Palaeontology, Museum Victoria, 1'.0. Box 666, Melbourne, Victoria 3001, Australia. Email: tdarragh(il.Illuseum.vic.gov.au :' Department of Earth and Planetary Sciences, Western Australian Museum, Locked Bag 49, Welshpool D.C., Western Australia 6986, Australia. 1 School of Earth and Ceographical Sciences, The University of Western Australia, 35 Stirling Highway, Crawlev, Western Australia 6009, Australia. Abstract - Silicified Middle to Late Eocene shallow water sandstones outcropping in the Lower Murchison District near Kalbarri township contain a silicified fossil fauna including foraminifera, sponges, bryozoans, solitary corals, brachiopods, echinoids and molluscs. The known molluscan fauna consists of 51 species, comprising 2 cephalopods, 14 bivalves, 1 scaphopod and 34 gastropods. Of these taxa three are newly described, Cerithium lvilya, Zeacolpus bartol1i, and Lyria lamellatoplicata. 25 of these molluscs are identical to or closely comparable with taxa from the southern Australian Eocene. The occurrence of this fauna extends the Southeast Australian Province during the Eocene from southwest Western Australia along the west coast north to at least 27° present day south latitude; consequently the province is here renamed the Southern Australian Province. Keywords: siliceous fossils, Eocene, Kalbarri, molluscs, new taxa, Carnarvon Basin, biogeography, Southern Australian Province. INTRODUCTION The source deposit, a pallid to ferruginous silicified Eocene marine molluscan assemblages from sandstone, forms a weakly defined, low breakaway coastal sedimentary basins in southern Australia trending N-S and sloping gently westward. -
Spouse Puts New Value in Rocks Can Leverage Both Richmond and Columbia Counties’ Current by LAURA LEVERING to Someone’S Face,” Allissa Said
LOOK INSIDE: St. Patrick’s Day Shuffle - Page 7 Friday, March 17, 2017 | Vol. 3, No. 11 Published for the Department of Defense and the Fort Gordon community FORTGORDONGLOBE.COM CRAFTSMAN’S PASSION Poor credit can lead to big problems BY LAURA LEVERING “There could be something Fort Gordon Public Affairs Office on the report that doesn’t be- long to you, so reviewing it Financial readiness is a lot gives you a chance to check it like driving an automobile. before applying and potentially If you don’t perform regular being turned down for a credit preventative maintenance, it’s card or loan,” explained Bar- bound to cause problems. bara Brown, personal financial In the case of finances, check- readiness specialist, Financial ing one’s credit report is pre- Readiness Program, Army ventative maintenance. Community Service. Credit reports and credit Credit reports are a detailed re- scores are different but di- port of a person’s debt history, in- rectly affect one another. By quiries about credit applications, law, individuals have an op- personal address and places of portunity to review their credit employment. In most cases, debt report three times a year. It’s seven years and older disappears the first thing a person should from credit reports and gets sent do before applying for a credit to a third party collections agen- card or taking out a loan for cy, which then tries to collect large items such as a car or the debt on behalf of company. house. Other cases may take longer and Consumers can request a free require action to disappear. -
CSRA REGIONAL PLAN 2035 Regional Assessment Stakeholder Involvement Program
CSRA REGIONAL PLAN 2035 Regional Assessment Stakeholder Involvement Program CSRA Regional Plan 2035 Table of Contents A. Regional Assessment 1. Introduction…………………………………………………………………………………………….…..4 2. Potential Regional Issues and Opportunities………………………………………………..……….8 2.1 Population…….……………………………………………………………………………….....8 2.2 Housing…………………………………………………………………………………………...9 2.3 Economic Development………………………………………………………………….……9 2.4 Land Use………………………………………………………………………………………..10 2.5 Transportation and Community Facilities……………………………………………….11 2.6 Natural and Environmental Resources……………………………………………………12 2.7 Intergovernmental Coordination…………………………………………………………..12 3. Regional Development Patterns………………………………………………………………………14 3.1 Projected Development Patterns…………………………………………………………..15 3.2 Analysis…………………………………………………………………………………………17 3.3 Areas Requiring Special Attention………………………………………………………...17 4. Supporting Data………………………………………………………………………………………….21 4.1 Population………………………………………………………………………………………21 4.2 Housing………………………………………………………………………………………....25 4.3 Economic Development………………………………………………………………………27 4.4 Land Use………………………………………………………………………………………...50 4.5 Transportation and Community Facilities………………………………………………..52 4.6 Natural and Environmental Resources……………………………………………………58 B. Stakeholder Involvement Program………………………………………..…………………………74 C. Regional Agenda (pending) Appendix: Analysis of Quality Community Objectives……………………………………………..79 Regional Assessment and Stakeholder Involvement Program | CSRA Regional Commission | 1 CSRA Regional Plan -
South Carolina State Water Assessment, 2Nd Ed., Chapter 1
SOUTH Carolina IN PERSPECTIVE SOCIOECONOMIC ENVironment influx of capital and population advanced the economy from an agricultural base to a 21st-century economy that Geography has played an important role in South is dominated by manufacturing and is well diversified by Carolina’s history and development. Archaeological agriculture and tourism. evidence shows us that early Indian inhabitants found the land and climate well suited for hunting and gathering Population and later for agriculture. Spanish, French, and English explorers discovered that South Carolina’s harbors and South Carolina’s population increased from rivers provided ingress to the New World and its vast about 250,000 in 1790 to more than 4 million in 2005 resources. The settlers who followed on the heels of (Figure 1-1). The nearly one-million person increase exploration exploited the land and streams of the lower between 1980 and 2005 accounted for 27 percent of the Coastal Plain, and for almost 200 years they enjoyed a state’s growth during the past two centuries. Population predominantly agricultural economy based first on indigo growth is above the national average and is expected to and rice and later on cotton, tobacco, and timber. Abundant continue at an above-average rate owing to factors such as land, water, and labor and a mild climate attracted the state’s mild climate, natural attractions, favorable tax national and international investment and a migration to and labor laws, and relatively low cost of living. the State during the middle and late 20th century. That 6,000 5,000 4,000 3,000 opulation, in thousands P 2,000 1,000 0 0 1790 1800 1810 1820 1830 1840 1850 1860 1870 1880 1890 1900 1910 1920 1930 1940 1950 1960 1970 1980 1990 200 2010 2020 2030 Year Figure 1-1. -
Augusta Regional Transportation Study
AUGUSTA REGIONAL TRANSPORTATION STUDY y w H E e d ll i g v e e it f i y n e a l w r d G H H ld a O w i y b m u l Old Evans Rd o C Edgefield d §20 Line Rd T ¨ y ubm s R Trolle an Rd Mcmanu y R d r u a d e y H Richland Av AIKEN d d M R R a r i h s o a c W l n e a ot P s B h N k i n S w Wagener Rd g N ud H y t e lo o w i n v t i L c Rd F ak h F 520 e R c ¨§ o u d r W c C y k h s arl F es P to e n H r k r w y w y R y o a Co d lumbi Jefferson Davis Hwy a Rd Pkw ch y R at i W rw NORTH BURNETTOWN c ive h h R d a i R H r s a u d k W t e ashi AUGUSTA s b s ngton u e o y R r n d g R E Au C s Palmetto Pkwy d M l a L 20 a ¨§ a y k r ti e n R R to w d d n AUGUSTA R d ¨§20 Broad St Walton Way Wrig ht d sboro R R Aiken 11th St f d f Wrightsboro Rd u 520 l ¨§ B Columbia Sa r nd A e t B o ilv a m d r S i R F c e R h rry rc d u R S h to C d rm ll P e i B n ra B e n ch e GROVETOWN L Rd im Go y o h rdo w g Gordon Hwy n H C R d Main St ¨§520 W illis ton NEW Rd ELLENTON A to m ic d R R d e g d ri B ns ea D d R g n i r FORT p Tobacco Rd S r Doug Barnard Pkwy o GORDON s d n i W Mi k e Will d P is For nR a e ma d g e tt H w y Highway 88 HEPHZIBAH d idge R Deans Br BLYTHE Peach Orchard Rd Richmond S t o r e y M i l l R d TRANSPORTATION IMPROVEMENT PROGRAM FY 2015 – 2018 AMENDED – MARCH 3, 2016 SEPTEMBER 2, 2015 Prepared By: Augusta Planning & Development Department In Cooperation With: Aiken County Planning And Development Department Lower Savannah Council of Governments Georgia Department Of Transportation South Carolina Department Of Transportation AUGUSTA REGIONAL -
Aperçus D'un Écosystème Marin Et De Ses Abords Au Maastrichtien
Aperçus d’un écosystème marin et de ses abords au Maastrichtien supérieur: le site nigérien d’In Daman et la mer épicontinentale du bassin des Iullemmeden Marc Michaut To cite this version: Marc Michaut. Aperçus d’un écosystème marin et de ses abords au Maastrichtien supérieur: le site nigérien d’In Daman et la mer épicontinentale du bassin des Iullemmeden. 2013. hal-00797424 HAL Id: hal-00797424 https://hal.archives-ouvertes.fr/hal-00797424 Preprint submitted on 6 Mar 2013 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. Aperçus d’un écosystème marin et de ses abords au Maastrichtien supérieur : le site nigérien d’In Daman et la mer épicontinentale du bassin des Iullemmeden Marc Michaut Institut préparatoire aux études scientifiques et techniques, Université de Tunis, La Marsa, Tunisie 5 mars 2013 Abstract Many studies were performed for several decades about Nigerian maastrichtian sites and other fossiliferous sites of the same epoch in their vicinity, which allow us to reconstruct the marine epicontinental ecosystem and associated coastal ecosystems with a fair amount of accuracy. We begin with a detailed compilation of the re- sults obtained about biotope and taphocenose. -
B-127 Lithostratigraphic Framework Of
&A 'NlOO,G-3 &i flo, 12 7 g l F£i&f THE LITHOSTRATIGRAPHIC FRAMEWORK OF \;\ .-t "- THE UPPERMOST CRETACEOUS AND LOWER TERTIARY OF EASTERN BURKE COUNTY, GEORGIA Paul F. Huddlestun and Joseph H. Summerour Work Performed in Cooperation with United States Geological Survey (Cooperative Agreement Number 1434-92-A-0959) and U. S. Department of Energy (Cooperative Agreement Number DE-FG-09-92SR12868) GEORGIA DEPARTMENT OF NATURAL RESOURCES ENVIRONMENTAL PROTECTION DIVISION GEORGIA GEOLOGIC SURVEY Atlanta 1996 Bulletin 127 THE LITHOSTRATIGRAPHIC FRAMEWORK OF THE UPPERMOST CRETACEOUS AND LOWER TERTIARY OF EASTERN BURKE COUNTY, GEORGIA Paul F. Huddlestun and Joseph H. Summerour GEORGIA DEPARTMENT OF NATURAL RESOURCES Lonice C. Barrett, Commissioner ENVIRONMENTAL PROTECTION DIVISION Harold F. Reheis, Director GEORGIA GEOLOGIC SURVEY William H. McLemore, State Geologist Atlanta 1996 Bulletin 127 ABSTRACT One new formation, two new members, and a redefinition of an established lithostratigraphic unit are formally introduced here. The Oconee Group is formally recognized in the Savannah River area and four South Carolina Formations not previously used in Georgia by the Georgia Geologic Survey are recognized in eastern Burke County. The Still Branch Sand is a new formation and the two new members are the Bennock Millpond Sand Member of the Still Branch Sand and the Blue Bluff Member of the Lisbon Formation. The four South Carolina formations recognized in eastern Burke CountY include the Steel Creek Formation and Snapp Formation of the Oconee Group, the Black Mingo Formation (undifferentiated), and the Congaree Formation. The Congaree Formation and Still Branch Sand are considered to be lithostratigraphic components of the Claiborne Group. -
Geologic Resources Inventory Map Document for Congaree National Park
U.S. Department of the Interior National Park Service Natural Resource Stewardship and Science Directorate Geologic Resources Division Congaree National Park GRI Ancillary Map Information Document Produced to accompany the Geologic Resources Inventory (GRI) Digital Geologic Data for Congaree National Park cong_geology.pdf Version: 1/27/2014 I Congaree National Park Geologic Resources Inventory Map Document for Congaree National Park Table of Contents Geolog.i.c. .R...e..s.o..u..r.c..e..s.. .I.n..v.e..n..t.o..r..y. .M...a..p.. .D..o..c..u..m...e..n..t....................................................................... 1 About th..e.. .N...P..S.. .G...e..o..l.o..g..i.c. .R...e..s.o..u..r.c..e..s.. .I.n..v.e..n..t.o..r..y. .P...r.o..g..r.a..m........................................................... 2 GRI Dig.i.t.a..l. .M...a..p.. .a..n..d.. .S..o..u..r.c..e.. .M...a..p.. .C..i.t.a..t.i.o..n..s............................................................................. 4 Map Un.i.t. .L..i.s..t.......................................................................................................................... 5 Map Un.i.t. .D..e..s..c..r.i.p..t.i.o..n..s............................................................................................................. 7 Qme - M...o..v..e..d.. .e..a..r.t.h.. .(..H..o..l.o..c..e..n..e..).................................................................................................................................... 7 Qfw - F..r..e..s..h..w...a..t.e..r. .m...a..r.s..h.. .a..n..d.. .s..w....a..m..p.. .d..e..p..o..s..i.t.s.. .(.H...o..lo..c..e..n..e..)........................................................................................ 7 Qslk - S..a..n..d..h..i.l.ls. -
Stratigraphy and Depositional Environments of Sediments from Five Cores from Screven and Burke Counties, Georgia by W
U.S. Department of the Interior U.S. Geological Survey Stratigraphy and Depositional Environments of Sediments from Five Cores from Screven and Burke Counties, Georgia By W. Fred Falls and David C. Prowell U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1603-A Prepared in cooperation with the U.S. Department of Energy and the Georgia Geologic Survey GEOLOGY AND PALEONTOLOGY OF FIVE CORES FROM SCREVEN AND BURKE COUNTIES, EASTERN GEORGIA Edited by Lucy E. Edwards CONTENTS Abstract Al Introduction . 1 Test Hole and Core Information 2 Previous Work 4 Acknowledgments 4 Stratigraphic Framework................................................................................................. 4 Cretaceous Stratigraphy 7 Cape Fear Formation 9 Middendorf Formation 10 Black Creek Group 10 Steel Creek Formation 11 Tertiary Stratigraphy 12 Ellenton Formation 12 Snapp Formation 13 Fourmile Branch/CongareelWarley Hill Unit 13 Santee Limestone 14 Barnwell Unit -............................................................................................. 16 Summary 17 References Cited 17 FIGURES 1. Index map showing the Savannah River Site and the location of stratigraphic test holes in the study area A2 2. Correlation diagram showing a generalized comparison of Cretaceous and Tertiary geologic units in the Southeastern United States 3 3-5. Gamma-ray, single-point resistance, and lithologic logs and geologic units of the- 3. Millhaven test hole in Screven County, Ga............................................................................................................ -
Synoptic Taxonomy of Major Fossil Groups
APPENDIX Synoptic Taxonomy of Major Fossil Groups Important fossil taxa are listed down to the lowest practical taxonomic level; in most cases, this will be the ordinal or subordinallevel. Abbreviated stratigraphic units in parentheses (e.g., UCamb-Ree) indicate maximum range known for the group; units followed by question marks are isolated occurrences followed generally by an interval with no known representatives. Taxa with ranges to "Ree" are extant. Data are extracted principally from Harland et al. (1967), Moore et al. (1956 et seq.), Sepkoski (1982), Romer (1966), Colbert (1980), Moy-Thomas and Miles (1971), Taylor (1981), and Brasier (1980). KINGDOM MONERA Class Ciliata (cont.) Order Spirotrichia (Tintinnida) (UOrd-Rec) DIVISION CYANOPHYTA ?Class [mertae sedis Order Chitinozoa (Proterozoic?, LOrd-UDev) Class Cyanophyceae Class Actinopoda Order Chroococcales (Archean-Rec) Subclass Radiolaria Order Nostocales (Archean-Ree) Order Polycystina Order Spongiostromales (Archean-Ree) Suborder Spumellaria (MCamb-Rec) Order Stigonematales (LDev-Rec) Suborder Nasselaria (Dev-Ree) Three minor orders KINGDOM ANIMALIA KINGDOM PROTISTA PHYLUM PORIFERA PHYLUM PROTOZOA Class Hexactinellida Order Amphidiscophora (Miss-Ree) Class Rhizopodea Order Hexactinosida (MTrias-Rec) Order Foraminiferida* Order Lyssacinosida (LCamb-Rec) Suborder Allogromiina (UCamb-Ree) Order Lychniscosida (UTrias-Rec) Suborder Textulariina (LCamb-Ree) Class Demospongia Suborder Fusulinina (Ord-Perm) Order Monaxonida (MCamb-Ree) Suborder Miliolina (Sil-Ree) Order Lithistida -
U.S. Geological Survey Professional Paper 1603-H
Chap H-front.fm Page I Tuesday, July 11, 2000 9:25 AM U.S. Department of the Interior U.S. Geological Survey Pollen Biostratigraphy of Lower Tertiary Sediments from Five Cores from Screven and Burke Counties, Georgia By Norman O. Frederiksen U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1603–H Prepared in cooperation with the U.S. Department of Energy and the Georgia Geologic Survey GEOLOGY AND PALEONTOLOGY OF FIVE CORES FROM SCREVEN AND BURKE COUNTIES, EASTERN GEORGIA Edited by Lucy E. Edwards Chap-H-contents.fm Page III Tuesday, July 11, 2000 9:28 AM CONTENTS Abstract .......................................................................................................................... H1 Introduction ....................................................................................................................1 Acknowledgments .................................................................................................. 2 Material and Methods .................................................................................................... 2 Correlations and Age Determinations ............................................................................ 2 Millhaven Test Hole........................................................................................................ 2 Ellenton Formation ................................................................................................. 2 Snapp Formation .................................................................................................... 6 Congaree Formation -
235416771.Pdf
W&M ScholarWorks Undergraduate Honors Theses Theses, Dissertations, & Master Projects 5-2009 Phylogenetic relationships and morphological changes in Venericardia on the Gulf Coastal Plain during the Paleogene Kate McClure College of William and Mary Follow this and additional works at: https://scholarworks.wm.edu/honorstheses Recommended Citation McClure, Kate, "Phylogenetic relationships and morphological changes in Venericardia on the Gulf Coastal Plain during the Paleogene" (2009). Undergraduate Honors Theses. Paper 297. https://scholarworks.wm.edu/honorstheses/297 This Honors Thesis is brought to you for free and open access by the Theses, Dissertations, & Master Projects at W&M ScholarWorks. It has been accepted for inclusion in Undergraduate Honors Theses by an authorized administrator of W&M ScholarWorks. For more information, please contact [email protected]. Table of Contents List of Figures……………………………………………………………………………...3 List of Tables.……………………………………………………………………………...4 Abstract………………………………………………………………………………….…5 Introduction………………………………………………………… ………………….….6 Background Venericard Biology ………………………………………… ……………………..7 Taxonomic Classification ………………………………………………………...13 Paleogene Molluscan Fauna on the U.S. Gulf Coastal Plain ………… ………...17 Paleogene Climate ……………………………………….……… ……………....18 Geologic Setting on the U.S. Gulf Coastal Plain …………………… …………..21 Methods Species and Specimen Selection ………………………………………… …….…25 Phylogenetic Data Collection ………………………………………… …………28 Phylogenetic Analysis ………………………………………….... ………………29 Landmark