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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 -
Well Construction at the Lake Amoret Well Site in Polk County, Florida
Well Construction at the Lake Amoret Well Site in Polk County, Florida Southwest Florida Water Management District Geohydrologic Data Section Revised March 2019 Cover Photo: Permanent monitor wells at the Lake Amoret well site in Polk County, Florida. In order from left to right: SURF AQ MONI- TOR, U FLDN AQ MONITOR. Photograph by Julia Zydek Well Construction at the Lake Amoret Well Site in Polk County, Florida By Julia Zydek Revised March 2018 Southwest Florida Water Management District Geohydrologic Data Section Southwest Florida Water Management District Operations, Lands and Resource Monitoring Division Ken Frink, P.E., Director Data Collection Bureau Sandie Will, P.G., Chief Geohydrologic Data Section M. Ted Gates, P.G., C.P.G., Manager Southwest Florida Water Management District 2379 Broad Street Brooksville, FL 34604-6899 For ordering information: World Wide Web: http://www.watermatters.org/documents Telephone: 1-800-423-1476 For more information on the Southwest Florida Water Management District and its mission to manage and protect water and related resources: World Wide Web: http://www.watermatters.org Telephone: 1-800-423-1476 The Southwest Florida Water Management District (District) does not discriminate on the basis of disability. This nondiscrimination policy involves every aspect of the District’s functions, includ- ing access to and participation in the District’s programs and activities. Anyone requiring reason- able accommodation as provided for in the Americans with Disabilities Act should contact the District’s Human Resources Office Chief, 2379 Broad St., Brooksville, FL 34604-6899; telephone (352) 796-7211 or 1-800-423-1476 (FL only), ext. -
The Favorability of Florida's Geology to Sinkhole
Appendix H: Sinkhole Report 2018 State Hazard Mitigation Plan _______________________________________________________________________________________ APPENDIX H: Sinkhole Report _______________________________________________________________________________________ Florida Division of Emergency Management THE FAVORABILITY OF FLORIDA’S GEOLOGY TO SINKHOLE FORMATION Prepared For: The Florida Division of Emergency Management, Mitigation Section Florida Department of Environmental Protection, Florida Geological Survey 3000 Commonwealth Boulevard, Suite 1, Tallahassee, Florida 32303 June 2017 Table of Contents EXECUTIVE SUMMARY ............................................................................................................ 4 INTRODUCTION .......................................................................................................................... 4 Background ................................................................................................................................. 5 Subsidence Incident Report Database ..................................................................................... 6 Purpose and Scope ...................................................................................................................... 7 Sinkhole Development ................................................................................................................ 7 Subsidence Sinkhole Formation .............................................................................................. 8 Collapse Sinkhole -
African Origins 200 Million Years of Calcium Carbonate Deposition
The Florida We are all So Familiar With is a relatively new phenomenon, geologically speaking. This distinctive peninsula of land we live on, and the gently sloping, sandy shorelines we’re drawn to for recreation and renewal, have not always existed as they appear today. In fact, Florida was a very different-looking place not so long ago, and over the past 500 million years it has had quite a unique and surprising geological history. African Origins Believe it or not, the deep bedrock that underlies Florida was originally a part of Africa. Florida’s oldest Scott, Means) rocks formed about 500 million years ago on the “megacontinent” Gondwana. They were wedged between other masses of rock that would eventually separate—through the activity of plate tectonics—into (Kosche, Bryan,(Kosche, the modern continents of Africa and South America. About 250 million years ago, Gondwana (containing the geologic beginnings of Florida) collided with another megacontinent called Laurasia (which contained the rest of future North America). The result was the supercontinent Pangea. When Pangea eventually broke up, about 230 million years ago, that special wedge of African bedrock that would be Florida, rifted apart from its tectonic plate of origin, and remained sutured instead to what we’ve come to know as the continent of North America. 200 Million Years of Calcium Carbonate Deposition It is upon these very old, African-born igneous and metamorphic basement rocks that the sedimentary rocks of the Florida Platform would start to accumulate. Thick layers of carbonate rock—predominantly limestones and dolostones composed of the mineral calcium carbonate— built up over the next 200 million years to create Florida’s flat-topped, “carbonate platform” structure. -
IC-25 Subsurface Geology of the Georgia Coastal Plain
IC 25 GEORGIA STATE DIVISION OF CONSERVATION DEPARTMENT OF MINES, MINING AND GEOLOGY GARLAND PEYTON, Director THE GEOLOGICAL SURVEY Information Circular 25 SUBSURFACE GEOLOGY OF THE GEORGIA COASTAL PLAIN by Stephen M. Herrick and Robert C. Vorhis United States Geological Survey ~ ......oi············· a./!.. z.., l:r '~~ ~= . ·>~ a··;·;;·;· .......... Prepared cooperatively by the Geological Survey, United States Department of the Interior, Washington, D. C. ATLANTA 1963 CONTENTS Page ABSTRACT .................................................. , . 1 INTRODUCTION . 1 Previous work . • • • • • • . • . • . • . • • . • . • • . • • • • . • . • . • 2 Mapping methods . • . • . • . • . • . • . • . • • . • • . • . • 7 Cooperation, administration, and acknowledgments . • . • . • . • • • • . • • • • . • 8 STRATIGRAPHY. 9 Quaternary and Tertiary Systems . • . • • . • • • . • . • . • . • . • . • • . • . • • . 10 Recent to Miocene Series . • . • • . • • • • • • . • . • • • . • . 10 Tertiary System . • • . • • • . • . • • • . • . • • . • . • . • . • • . 13 Oligocene Series • . • . • . • . • • • . • • . • • . • . • • . • . • • • . 13 Eocene Series • . • • • . • • • • . • . • • . • . • • • . • • • • . • . • . 18 Upper Eocene rocks . • • • . • . • • • . • . • • • . • • • • • . • . • . • 18 Middle Eocene rocks • . • • • . • . • • • • • . • • • • • • • . • • • • . • • . • 25 Lower Eocene rocks . • . • • • • . • • • • • . • • . • . 32 Paleocene Series . • . • . • • . • • • . • • . • • • • . • . • . • • . • • . • . 36 Cretaceous System . • . • . • • . • . • -
Tertiary Stratigraphy of South Carolina
Tertiary Stratigraphy of South Carolina GEOLOGICAL SURVEY PROFESSIONAL PAPER 243-B Tertiary Stratigraphy of South Carolina By C. WYTHE COOKE and F. STEARNS MAcNEIL SHORTER CONTRIBUTIONS TO GENERAL GEOLOGY, 1952, PAGES 19-29 GEOLOGICAL SURVEY PROFESSIONAL PAPER 243-B A revised classification of Tertiary formations of the Coastal Plain, based mainly on new stratigraphic and paleontologic information UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1952 UNITED STATES DEPARTMENT OF THE INTERIOR Oscar L. Chapman, Secretary v GEOLOGICAL SURVEY W. E. Wrather, Director For sale by the Superintendent of Documents, U. S. Government Printing Office Washington 25, D. C. - Price. 15 cents (paper cover) CONTENTS Page Page Abstract- ______ _____.. _________ 19 Paleocene (?) and Eocene series- -Continued Introduction ________._!________ 19 Deposits of Jackson age. 26 Paleocene (?) and Eocene series-. 19 Barnwell formation. _ _. 26 Deposits of Wilcox age _____ 20 Oligocene series______________ 27 Deposits of Claiborne age___ 21 Cooper marl._________ 27 Congaree formation____ 21 Miocene series_______________ 28 Warley Hill marl ______ 23 Hawthorn formation. _. 28 Me Bean formation___ 23 Santee limestone_____ 24 References. ____________l_-___. 28 Castle Hayne limestone- 25 ILLUSTRATION Figure 2. Correlation of Tertiary formations of South Carolina. 20 in 99308T—52 TERTIARY STRATIGRAPHY OF SOUTH CAROLINA By C. WYTHE COOKE AND F. STEARNS ABSTRACT bridges have been built, and places formerly inacces The following changes in the current classification of the sible are now within easy reach. The spoil bank of Tertiary formations of South Carolina are proposed: The Black the Santee-Cooper Diversion Canal, cut about 1940, Mingo formation, mainly of Wilcox age, may include some Paleo- has brought to the surface an abundance of fossils of cene deposits. -
A Revision of the Lithostratigraphic Units of the Coastal Plain of Georgia
A Revision of the Lithostratigraphic Units of the Coastal Plain of Georgia THE OLIGOCENE Paul F. Huddleston DEPARTMENT OF NATURAL RESOURCES ENVIRONMENTAL PROTECTION DIVISION GEORGIA GEOLOGIC SURVEY I BULLETIN 105 Cover photo: Seventy feet of Bridgeboro Limestone exposed at the the type locality in the southern-most pit of the Bridgeboro Lime and Stone Company, 6.5 miles west-southwest of the community of Bridgeboro, south of Georgia 112, Mitchell County. A Revision of the Lithostratigraphic Units of the Coastal Plain of Georgia THE OLIGOCENE Paul F. Huddlestun ·Georgia Department of Natural Resources Joe D. Tanner, Commissioner Environmental Protection Division Harold F. Reheis, Director Georgia Geologic Survey William H. McLemore, State Geologist Atlanta 1993 BULLETIN 105 TABLE OF CONTENTS Page LIST OF ILLUSTRATIONS ............................................................................................................................................... v ABSTRACT ........................................................................................................................................................................ 1 ACKN"OWLEIJGMENTS ................................................................................................................................................. 1 INTRODUCTION .............................................................................................................................. :.............................. 2 Methods ........................................... ,................................................................................................................... -
A Study of the Lithological and Petrographical Changes Across The
Florida State University Libraries Electronic Theses, Treatises and Dissertations The Graduate School 2015 A Study of the Lithological and Petrographical Changes Across the Eocene- Oligocene Transition of the Ocala and Suwannee Formations in Northern Florida and Southern Georiga Kayla Smith Follow this and additional works at the FSU Digital Library. For more information, please contact [email protected] FLORIDA STATE UNIVERSITY COLLEGE OF ARTS AND SCIENCES A STUDY OF THE LITHOLOGICAL AND PETROGRAPHICAL CHANGES ACROSS THE EOCENE-OLIGOCENE TRANSITION OF THE OCALA AND SUWANNEE FORMATIONS IN NORTHERN FLORIDA AND SOUTHERN GEORIGA By KAYLA SMITH A Thesis submitted to the Department of Earth, Ocean, & Atmospheric Science in partial fulfillment of the requirements for the degree of Master of Science 2015 Kayla Smith defended this thesis on June 24, 2015. The members of the supervisory committee were: William Parker Professor Directing Thesis Stephen Kish Committee Member James Tull Committee Member The Graduate School as has verified and approved the above-named committee members, and certifies that thesis has been approved with accordance with university requirements. ii I dedicate this thesis to my parents and friends. Without their encouragement, I would have never embarked on this journey. iii AKNOWLEDGMENTS I would like to thank my committee for all the help and support they gave on my endeavors. Dr. William Parker, my major professor, was invaluable in helping me obtain materials and funding for this project as well as giving me the proper guidance needed to complete my research. Without him I could not have finished this work. Dr. Stephen Kish was always willing to lend a helping hand and exceedingly patient with me. -
Geologic Features of Areas of Abnormal Radioactivity South of Ocala Marion County, Florida
Geologic Features of Areas of Abnormal Radioactivity South of Ocala Marion County, Florida GEOLOGICAL SURVEY BULLETIN 1046-J This report concerns work done on behalf of the U. S. Atomic Energy Commission and is published with permission of the Commission Geologic Features of Areas of Abnormal Radioactivity South of Ocala Marion County, Florida £y GILBERT H. ESPENSHADE CONTRIBUTIONS TO THE GEOLOGY OF URANIUM GEOLOGICAL SURVEY BULLETIN 1046-J This report concerns work done on behalf of the U. S. Atomic Energy Commission and is published with permission of the Commission UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1958 UNITED STATES DEPARTMENT OF THE INTERIOR FRED A. SEATON, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director For sale by the Superintendent of Documents, U. S. Government Printing Ofnce Washington 25, D. C. - Price $1.00 (paper cover) CONTENTS Page Abstract..____--_____-_-____-----_________________-_______-_-___ 205 Introduction______________________________________________________ 205 Radioactivity anomalies-___________________________________________ 206 Geology_______________________._.._________________ 206 Stratigraphy__________--______-_________-__-____-_--_-_-____ 206 Ocala limestone----_______-____________-___--______--_____- 206 Miocene sedimentary rocks.-..______________________________ 207 Pleistocene sediments.._____________________________________ 209 Structure_______________________________________ 210 Effects of weathering-.___-_____________________________________ 210 Drilling and sampling methods__________________________._____-____- -
Shorter Contributions to General Geology
DEPARTMENT OF THE INTERIOR FRANKLIN K. LANE, Secretary UNITED STATES GEOLOGICAL SURVEY GEORGE OTIS SMITH, Director Professional Paper 95 SHORTER CONTRIBUTIONS TO GENERAL GEOLOGY 1915 DAVID WHITE, CHIEF GEOLOGIST WASHINGTON GOVERNMENT PRJ;NTING OFFlCE 1916 THE AGE OF THE OCALA LIMESTONE. By CHARLES W jYTHE CooKE. INTRODUCTION. In 1881 Eugene A. Smith 1 announced the presenc~, underlying large areas in both west ern and peninsular Florida, of limestone which he correlated with the Vicksburg limestone of Mississippi and Alabama and designated by the term Vicksburg limestone. Among the local ities he mentioned specifically are Marianna, in Jackson County, and Ocala, in Marion County. In the following year Heilprin 2 described a species of Nummulites from fragments of rock found by Willcox in Hernando County, on the west coast of Florida, and two years later Willcox discovered the nummulitic limestone in place not far away. Heilprin believed the rock to be the equivalent, in part, of the "Nutnmulitic" of Europe and, on account of the association of the Nummulites with Orbitoides ephippium, considered it to be of Oligocene age. At the -meeting of the American Association for the Advancement of Science in 1887 Johnson 3 said that the rocks mentioned by H ilprin "may be remnants of the Nummulitic limestone, which is really a stratum overlying the Vicksburg rocks" near Levyville and is apparently conformable with the "Vicksburg stage" but evidently not identical with it. The term Ocala appears to have been first formally used by Dall, who described the forma tion under the heading "Nummulitic beds, Ocala limestone (Oligocene of Heilprin)." He says: 4 Among the rocks which until recently were not discriminated from the Orbitoides limestone and which appear in central Florida directly and conformably to overlie the latter, though no one has described their contact, is a yellowish friable rock containing many Foraminifera, conspicuous among which are two species of Nummulites, N. -
Florida Geological
Geologic Map of the State of Florida - Southern Peninsula by Thomas M. Scott, P. G. #99, Kenneth M. Campbell, Frank R. Rupert, Jonathan D. Arthur, Thomas M. Missimer, Jacqueline M. Lloyd, J. William Yon, and Joel G. Duncan Qh Quaternary TQsu Tc Qh Thp Thpb Holocene Qh Qu Qh Holocene sedimennts Qu TQsu Tha TQuc Qu Pleistocene/Holocene Qa Qbd Qal Alluvium Qu Qu Qbd Beach ridge and dune Thp Qu TQd Qh Qu Undifferentiated sediments TQsu Pleistocene Qh Qa Anastasia Formation TQsu Qu TQsu Qk Key Largo Limestone Qh Qm Miami Limestone Qtr Trail Ridge sands Qa Tertiary/Quaternary Tt Pliocene/Pleistocene TQsu Shelly sediments of Qu Plio-Pleistocene age TQsu TQu Undifferentiated sediments Qh TQsu TQd Dunes TQuc Reworked Cypresshead sediments Tertiary Pliocene Tt Tc Cypresshead Formation Qm Tci Citronelle Formaation Tmc Miccosukee Formmation Tic Intracoastal Formmation Tt Tamiami Formation Tjb Jackson Bluff Formation Qh Miocene/Pliocene Tt Thcc Hawthorn Group, Coosawhatchie Formation, Charlton Member Thp Hawthorn Group, Peace River Formation Qm Thpb Hawthorn Group, Peace River Formation, Bone Valley Member Miocene Trm Residuum on Miocene sediments Tab Alum Bluff Group Qh Qk Hawthorn Group Th Qh Thc Hawthorn Group, Coosawhatchie Formation Ths Hawthorn Group, Statenville Formation Tht Hawthorn Group, Torreya Formation Tch Chatahoochee FFormation Qk Tsmk St. Marks Formaation Oligocene/Miocene Tha Hawthorn Group, Arcadia Formation That Hawthorn Group, Arcadia Formation, Tampa Member Qk Oligocene Qm Qm Tro Residuum on Oligocene sediments Ts Suwannee Limesttone Suwannee Limesttone - Marianna Limestone undifferentiated Tsm David B. Struhs, Secretary Eocene Tre Residuum on Eocene sediments To Ocala Limestone Tap Avon Park Formation 20 0 20 40 60 80 Miles 20 0 20 40 60 80 Kilometerrs Scale 1:750,000 1:750 000 Walter Schmidt Albers Conic Equal-Area Projection State Geologist and Chief SOFIA - http://sofia.usgs.gov. -
Larger Foraminiferal Biostratigraphy, Systematics And
Florida International University FIU Digital Commons FIU Electronic Theses and Dissertations University Graduate School 8-27-2010 Larger Foraminiferal Biostratigraphy, Systematics And Paleoenvironments of The vonA Park Formation and Ocala Limestone, Highlands County, Florida Jacqueline Bowen Powell Florida International University, [email protected] DOI: 10.25148/etd.FI10120306 Follow this and additional works at: https://digitalcommons.fiu.edu/etd Recommended Citation Bowen Powell, Jacqueline, "Larger Foraminiferal Biostratigraphy, Systematics And Paleoenvironments of The vA on Park Formation and Ocala Limestone, Highlands County, Florida" (2010). FIU Electronic Theses and Dissertations. 288. https://digitalcommons.fiu.edu/etd/288 This work is brought to you for free and open access by the University Graduate School at FIU Digital Commons. It has been accepted for inclusion in FIU Electronic Theses and Dissertations by an authorized administrator of FIU Digital Commons. For more information, please contact [email protected]. FLORIDA INTERNATIONAL UNIVERSITY Miami, Florida LARGER FORAMINIFERAL BIOSTRATIGRAPHY, SYSTEMATICS AND PALEOENVIRONMENTS OF THE AVON PARK FORMATION AND OCALA LIMESTONE, HIGHLANDS COUNTY, FLORIDA A dissertation submitted in partial fulfillment of the requirements for the degree of DOCTOR OF PHILOSOPHY in GEOSCIENCES by Jacqueline Bowen Powell 2010 To: Dean Kenneth Furton College of Arts and Sciences This dissertation, written by Jacqueline Bowen Powell, and entitled Larger Foraminiferal Biostratigraphy, Systematics