GROUND-WATER RESOURCES of FLAGLER COUNTY, FLORIDA by A.S
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Exhibit Specimen List FLORIDA SUBMERGED the Cretaceous, Paleocene, and Eocene (145 to 34 Million Years Ago) PARADISE ISLAND
Exhibit Specimen List FLORIDA SUBMERGED The Cretaceous, Paleocene, and Eocene (145 to 34 million years ago) FLORIDA FORMATIONS Avon Park Formation, Dolostone from Eocene time; Citrus County, Florida; with echinoid sand dollar fossil (Periarchus lyelli); specimen from Florida Geological Survey Avon Park Formation, Limestone from Eocene time; Citrus County, Florida; with organic layers containing seagrass remains from formation in shallow marine environment; specimen from Florida Geological Survey Ocala Limestone (Upper), Limestone from Eocene time; Jackson County, Florida; with foraminifera; specimen from Florida Geological Survey Ocala Limestone (Lower), Limestone from Eocene time; Citrus County, Florida; specimens from Tanner Collection OTHER Anhydrite, Evaporite from early Cenozoic time; Unknown location, Florida; from subsurface core, showing evaporite sequence, older than Avon Park Formation; specimen from Florida Geological Survey FOSSILS Tethyan Gastropod Fossil, (Velates floridanus); In Ocala Limestone from Eocene time; Barge Canal spoil island, Levy County, Florida; specimen from Tanner Collection Echinoid Sea Biscuit Fossils, (Eupatagus antillarum); In Ocala Limestone from Eocene time; Barge Canal spoil island, Levy County, Florida; specimens from Tanner Collection Echinoid Sea Biscuit Fossils, (Eupatagus antillarum); In Ocala Limestone from Eocene time; Mouth of Withlacoochee River, Levy County, Florida; specimens from John Sacha Collection PARADISE ISLAND The Oligocene (34 to 23 million years ago) FLORIDA FORMATIONS Suwannee -
Lacustrine Coquinas and Hybrid Deposits from Rift Phase Pre-Salt
Journal of South American Earth Sciences 95 (2019) 102254 Contents lists available at ScienceDirect Journal of South American Earth Sciences journal homepage: www.elsevier.com/locate/jsames Lacustrine coquinas and hybrid deposits from rift phase: Pre-Salt, lower T Cretaceous, Campos Basin, Brazil Vinicius Carbone Bernardes de Oliveiraa,b,*, Carlos Manuel de Assis Silvaa, Leonardo Fonseca Borghib, Ismar de Souza Carvalhob a Petrobras Research and Development Center (CENPES), Avenida Horacio de Macedo, 950, Ilha do Fundao – Cidade Universitaria, Rio de Janeiro, RJ, 21949-915, Brazil b Universidade Federal do Rio de Janeiro, Centro de Ciencias Matematicas e da Natureza, Instituto de Geociencias, Departamento de Geologia, Programa de Pos-graduacao em Geologia, Av. Athos da Silveira Ramos, 274, Bloco F, Ilha do Fundao – Cidade Universitaria, Rio de Janeiro, RJ, 21949-900, Brazil ARTICLE INFO ABSTRACT Keywords: This study presents a facies characterization, facies succession and conceptual depositional model of the Pre-salt Coqueiros Formation, Lower Cretaceous of Campos Basin, based on core analyses of two wells. WELL-1 is a Rift sedimentation shallow water drilling located at south of Campos Basin within the Badejo structural high, and WELL-2 is an ultra Coquinas deep water drilling located at north, over the “External High”. Ten carbonate facies, three siliciclastic facies, two Hybrid deposits magnesium clay mineral rich facies and two hybrid facies were identified. The carbonate facies were defined as Lower cretaceous rudstone, grainstone, packstone and mud supported carbonate rock, composed of bivalves, ostracods, and rare gastropods. Bivalve shells, mostly disarticulated with distinct degrees of fragmentation, characterized the main components of the ten carbonate facies. -
How Pumping Sands on NC Beaches
The Risks of Renourishment: North Carolina Coastal Federation How pumping sand on North Carolina’s beaches can affect Sea Turtles, Mole Crabs and other Critters April 2002 Who We Are The North Carolina Coastal Federation (NCCF) is the state’s largest non-profit organization working to restore and protect the coast. NCCF headquarters are at 3609 Highway 24 in Ocean between Morehead City and Swansboro and are open Monday through Friday. The headquarters houses NCCF’s main offices, a nature shop, library, and information area. NCCF also operates a field office at 3806-B Park Avenue in Wilmington. For more information call 252-393-8185 or visit our website at www.nccoast.org. This report was written by Ted Wilgis, the Federation’s Cape Fear Coastkeeper, and edited by Frank Tursi, the Cape Lookout Coastkeeper, and Jim Stephenson, Program Analyst. All are closely monitoring beach renourishment projects in North Carolina during the time covered in this report. Wilgis and Tursi also took all of the photographs. Cover Photo Bulldozers work the new sand being pumped onto the beach at Fort Macon State Park in Carteret County. 2 Index Executive Summary.................................................4 Recommendations....................................................5 Background..............................................................6 Sea Turtles ........................................................ 7-11 Mole Crabs and Other Critters...............................12 Other Effects ..........................................................13 -
Upper Ordovician and Silurian Stratigraphy in Sequatchie Valley and Parts of the Adjacent Valley and Ridge, Tennessee
Upper Ordovician and Silurian Stratigraphy in Sequatchie Valley and Parts of the Adjacent Valley and Ridge, Tennessee GEOLOGICAL SURVEY PROFESSIONAL PAPER 996 Prepared in cooperation with the Tennessee Division of Geology Upper Ordovician and Silurian Stratigraphy in Sequatchie Valley and Parts of the Adjacent Valley and Ridge, Tennessee By ROBERT C. MILICI and HELMUTH WEDOW, JR. GEOLOGICAL SURVEY PROFESSIONAL PAPER 996 Prepared in cooperation with the Tennessee Division of Geology UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON 1977 UNITED STATES DEPARTMENT OF THE INTERIOR CECIL D. ANDRUS, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress Cataloging in Publication Data Milici, Robert C 1931- Upper Ordovician and Silurian stratigraphy in Sequatchie Valley and parts of the adjacent valley and ridge, Tennessee. (Geological Survey professional paper; 996) Bibliography: p. Supt. of Docs. no.: I 19.16:996 1. Geology, Stratigraphic--Ordovician. 2. Geology, Stratigraphic--Silurian. 3. Geology--Tennessee--Sequatchie Valley. 4. Geology--Tennessee--Chattanooga region. I. Wedow, Helmuth, 1917- joint author. II: Title. Upper Ordovician and Silurian stratigraphy in Sequatchie Valley .... III. Series: United States. Geological Survey. Professional paper; 996. QE660.M54 551.7'310976877 76-608170 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 Stock Number 024-001-03002·1 CONTENTS Page Abstract 1 Introduction ----------------------------------------------------------------------------- -
Seismic Facies/Geometries of the Pre-Salt Limestone Units and Newly-Identified Exploration Trends Within the Santos and Campos Basins, Brazil
Seismic facies/geometries of the pre-salt limestone units and newly-identified exploration trends within the Santos and Campos basins, Brazil Senira Kattah *, PGS Petroleum Geo-Services Yermek Balabekov, PGS Petroleum Geo-Services Copyright 2015, SBGf - Sociedade Brasileira de Geofísica exploration targets in the pre-salt succession of Campos and Santos basins, proven by successful performance This paper was prepared for presentation during the 14th International Congress of the Brazilian Geophysical Society held in Rio de Janeiro, Brazil, August 3-6, 2015. tests on Búzios and Libra discoveries. Contents of this paper were reviewed by the Technical Committee of the 14th The pre-salt hydrocarbon play fairway extends from the International Congress of the Brazilian Geophysical Society and do not necessarily represent any position of the SBGf, its officers or members. Electronic reproduction or Santos basin in the south through the Campos basin to storage of any part of this paper for commercial purposes without the written consent the north, possibly reaching the Espirito Santo Basin. It is of the Brazilian Geophysical Society is prohibited. ____________________________________________________________________ approximately 800 km from SW to NE and 200 km from NW to SE, extending into water depths exceeding 2,000 Abstract m. The NE trend approximates to the crustal extension of Based on preliminary seismic/geological the Early Cretaceous rift fabric, whereas the NW trend interpretation of nearly 36,000 sq. km of 3D PSDM reflects transfer/accomodation zones with transpression surveys and analogies with the pre-salt hydrocarbon and/or transtension regimes, mostly active during late commercial and sub-commercial discoveries, this phases of the rift development. -
Geology of Florida Local Abundance of Quartz Sand
28390_00_cover.qxd 1/16/09 4:03 PM Page 1 Summary of Content The geologic past of Florida is mostly out of sight with its maximum elevation at only ~105 m (in the panhandle) and much of south Florida is virtually flat. The surface of Florida is dominated by subtle shorelines from previous sea-level high-stands, karst-generated lakes, and small river drainage basins What we see are modern geologic (and biologic) environments, some that are world famous such as the Everglades, the coral reefs, and the beaches. But, where did all of this come from? Does Florida have a geologic history other than the usual mantra about having been “derived from the sea”? If so, what events of the geologic past converged to produce the Florida we see today? Toanswer these questions, this module has two objectives: (1) to provide a rapid transit through geologic time to describe the key events of Florida’s past emphasizing processes, and (2) to present the high-profile modern geologic features in Florida that have made the State a world-class destination for visitors. About the Author Albert C. Hine is the Associate Dean and Professor in the College of Marine Science at the University of South Florida. He earned his A.B. from Dartmouth College; M.S. from the University of Massachusetts, Amherst; and Ph.D. from the University of South Carolina, Columbia—all in the geological sciences. Dr. Hine is a broadly-trained geological oceanographer who has addressed sedimentary geology and stratigraphy problems from the estuarine system out to the base of slope. -
BISCAYNE NATIONAL PARK the Florida Keys Begin with Soldier Key in the Northern Section of the Park and Continue to the South and West
CHAPTER TWO: BACKGROUND HISTORY GEOLOGY AND PHYSICAL GEOGRAPHY OF BISCAYNE NATIONAL PARK The Florida Keys begin with Soldier Key in the northern section of the Park and continue to the south and west. The upper Florida Keys (from Soldier to Big Pine Key) are the remains of a shallow coral patch reef that thrived one hundred thousand or more years ago, during the Pleistocene epoch. The ocean level subsided during the following glacial period, exposing the coral to die in the air and sunlight. The coral was transformed into a stone often called coral rock, but more correctly termed Key Largo limestone. The other limestones of the Florida peninsula are related to the Key Largo; all are basically soft limestones, but with different bases. The nearby Miami oolitic limestone, for example, was formed by the precipitation of calcium carbonate from seawater into tiny oval particles (oolites),2 while farther north along the Florida east coast the coquina of the Anastasia formation was formed around the shells of Pleistocene sea creatures. When the first aboriginal peoples arrived in South Florida approximately 10,000 years ago, Biscayne Bay was a freshwater marsh or lake that extended from the rocky hills of the present- day keys to the ridge that forms the current Florida coast. The retreat of the glaciers brought about a gradual rise in global sea levels and resulted in the inundation of the basin by seawater some 4,000 years ago. Two thousand years later, the rising waters levelled off, leaving the Florida Keys, mainland, and Biscayne Bay with something similar to their current appearance.3 The keys change. -
Biscayne Aquifer of Dade and Broward Counties, Florida
Biscayne aquifer in Dade and Broward Counties, Florida Item Type monograph Authors Schroeder, Melvin C.; Klein, Howard; Hoy, Nevin D. Publisher Florida Geological Survey Download date 07/10/2021 07:06:01 Link to Item http://hdl.handle.net/1834/19701 STATE OF FLORIDA STATE BOARD OF CONSERVATION Ernest Mitts, Director FLORIDA GEOLOGICAL SURVEY Herman Gunter, Director REPORT OF INVESTIGATIONS NO. 17 BISCAYNE AQUIFER OF DADE AND BROWARD COUNTIES, FLORIDA By Melvin C. Schroeder, Howard Klein, and Nevin D. Hoy U. S. Geological Survey Prepared by the UNITED STATES GEOLOGICAL SURVEY in cooperation with the FLORIDA GEOLOGICAL SURVEY CENTRAL AND SOUTHERN FLORIDA FLOOD CONTROL DISTRICT DADE COUNTY CITIES OF MIAMI, MIAMI BEACH and FORT LAUDERDALE TALLAHASSEE, FLORIDA 1958 c-,3 .,r' to,/7 FLORIDA STATE BOARD OF CONSERVATION LEROY COLLINS Governor R. A. GRAY RICHARD ERVIN Secretary of State Attorney General J. EDWIN LARSON RAY E. GREEN Treasurer Comptroller THOMAS D. BAILEY NATHAN MAYO Superintendentof Public Instruction Commissioner of Agriculture ERNEST MITTS Director of Conservation ii LETTER OF TRANSMITTAL Tallahassee December 5, 1957 Mr. Ernest Mitts, Director Florida State Board of Conservation Tallahassee, Florida Dear Mr. Mitts: I am forwarding to you a report entitled, BISCAYNE AQUIFER OF DADE AND BROWARD COUNTIES, FLORIDA, which was pre- pared by Melvin C. Schroeder, Howard Klein, and Nevin D. Hoy, Geologists of the United States Geological Survey. The report was sub- mitted for publication March 15, 1956, and it is recommended that it be published as Report of Investigations No. 17. The Biscayne Aquifer is the principal source of water for the heavily populated area in the vicinity of West Palm Beach and Miami. -
Morphology and Histology of Acanthodian Fin Spines from the Late Silurian Ramsasa E Locality, Skane, Sweden Anna Jerve, Oskar Bremer, Sophie Sanchez, Per E
Morphology and histology of acanthodian fin spines from the late Silurian Ramsasa E locality, Skane, Sweden Anna Jerve, Oskar Bremer, Sophie Sanchez, Per E. Ahlberg To cite this version: Anna Jerve, Oskar Bremer, Sophie Sanchez, Per E. Ahlberg. Morphology and histology of acanthodian fin spines from the late Silurian Ramsasa E locality, Skane, Sweden. Palaeontologia Electronica, Coquina Press, 2017, 20 (3), pp.20.3.56A-1-20.3.56A-19. 10.26879/749. hal-02976007 HAL Id: hal-02976007 https://hal.archives-ouvertes.fr/hal-02976007 Submitted on 23 Oct 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. Palaeontologia Electronica palaeo-electronica.org Morphology and histology of acanthodian fin spines from the late Silurian Ramsåsa E locality, Skåne, Sweden Anna Jerve, Oskar Bremer, Sophie Sanchez, and Per E. Ahlberg ABSTRACT Comparisons of acanthodians to extant gnathostomes are often hampered by the paucity of mineralized structures in their endoskeleton, which limits the potential pres- ervation of phylogenetically informative traits. Fin spines, mineralized dermal struc- tures that sit anterior to fins, are found on both stem- and crown-group gnathostomes, and represent an additional potential source of comparative data for studying acantho- dian relationships with the other groups of early gnathostomes. -
Florida's Rocks and Minerals
FLORIDA’S ROCKS KEY LARGO LIMESTONE: The Key Largo red sandy clay formations of the central peninsula Limestone is a hard, white to light gray rock which and northwestern part of the state. No commercial CHERT: Chert is also known as flint or flint rock and contains numerous fossil corals. The Key Largo use is made of Florida sandstone, though it has been is a deposit of microcrystalline silica. Florida’s cherts Limestone extends on the surface from Soldier Key on used on a very limited scale as a building stone. are generally gray in color, though some are bright the north to the New Harbor Keys just south of Big Pine shades of blue, red, yellow and orange. It is Key. FLORIDA'S MINERALS characterized by its extreme hardness and is found in association with some of the limestone formations, MIAMI LIMESTONE: The Miami Limestone is a ANHYDRITE: The mineral anhydrite is an especially the Ocala. Florida’s Native Americans used soft to hard, recrystallized limestone. Near the east coast, anhydrous calcium sulfate. It is closely related to the chert in the manufacturing of axes, spear heads and it is composed mainly of ooliths with some quartz sand mineral gypsum but has a marble-like texture and arrow points. and fossils. Inland, it is a fossiliferous limestone with usually shows no crystal form. Anhydrite has a some sand. Ooliths are small rounded grains that look white, gray or brown color and a white streak. It is COMMON CLAY: Another sedimentary rock found like fish eggs and are composed of layers of calcite harder than calcite and does not effervesce in throughout Florida, common clay is sticky and is deposited around sand grains or fossil fragments. -
Turkey Point Units 6 & 7 COLA
Turkey Point Units 6 & 7 COL Application Part 2 — FSAR SUBSECTION 2.5.1: BASIC GEOLOGIC AND SEISMIC INFORMATION TABLE OF CONTENTS 2.5.1 BASIC GEOLOGIC AND SEISMIC INFORMATION .............................2.5.1-1 2.5.1.1 Regional Geology .....................................................................2.5.1-1 2.5.1.2 Site Geology ...........................................................................2.5.1-56 2.5.1.3 References .............................................................................2.5.1-69 2.5.1-i Revision 1 Turkey Point Units 6 & 7 COL Application Part 2 — FSAR SUBSECTION 2.5.1 LIST OF FIGURES Number Title 2.5.1-201 Site Region Geologic Map (Sheet 1 of 2) 2.5.1-201 Site Region Geologic Map Legend, Florida Geology (Sheet 2 of 2) 2.5.1-202 Coastal Plain Physiographic Region: Florida 2.5.1-203 Paleozoic — Mesozoic Stratigraphy 2.5.1-204 Simplified North-South Profile of Mesozoic-Age Rocks in Florida 2.5.1-205 Regional Cenozoic Stratigraphy 2.5.1-206 North-South Geologic Cross Section of Upper Mesozoic and Lower Cenozoic Rocks in Southern Florida 2.5.1-207 Simplified North-South Geologic Profile of Florida 2.5.1-208 East-West Geologic Cross Section of Upper Cenozoic-Age Rocks in Southern Florida 2.5.1-209 East-West Geologic Cross Section of Eocene through Pliocene-Age Rocks in Southern Florida 2.5.1-210 East-West Geologic Cross Section of Miocene through Pleistocene-Age Rocks in Miami-Dade County Florida 2.5.1-211 Great Bahama Bank Geologic Environment 2.5.1-212 Miocene-Pliocene Siliciclastic Transport Pathways -
STATE of FLORIDA STATE BOARD of CONSERVATION Ernest Mitts, Director
Interim report on geology and ground-water resources of Indian River County, Florida Item Type monograph Authors Bermes, B. J. Publisher Florida Geological Survey Download date 01/10/2021 23:12:53 Link to Item http://hdl.handle.net/1834/19401 STATE OF FLORIDA STATE BOARD OF CONSERVATION Ernest Mitts, Director FLORIDA GEOLOGICAL SURVEY Robert O. Vernon, Director INFORMATION CIRCULAR NO. 18 INTERIM REPORT ON GEOLOGY AND GROUND-WATER RESOURCES OF INDIAN RIVER COUNTY, FLORIDA By Boris J. Bermes, Geologist U. S. Geological Survey Prepared by U. S. Geological Survey in cooperation with the Florida Geological Survey and the Central and Southern Florida Flood Control District Tallahassee, Florida 1958 TABLE OF CONTENTS Page Abstract ..................................... 1 Introduction ................................ 2 Purpose and scope of investigation ........... 2 Acknowledgments .......................... 3 Geography .................................... 3 Location and general features of the county.... 3 Climate ..... ........................... 6 Agriculture and industry .................... 6 Topography.............. ................ 6 Drainage ................. ........ ...... 7 Geology...................................... 8 Eocene series ...................... ..... 8 Lake City limestone....................... 8 Avon Park limestone .................... 12 Ocala group ............................ 13 Williston and Inglis formations ......... 13 Crystal River formation ................ 14 Oligocene series ............................. 14