Soil Survey of Pinellas County, Florida
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WS-32, Hydrogeologic Investigation of the Floridan Aquifer System at The
SOUTH FLORIDA WATER MANAGEMENT DISTRICT Hydrogeologic Investigation of the Floridan Aquifer System at the S-65C Site (Well OKF-105) Okeechobee County, Florida Technical Publication WS-32 R. Simon A. Sunderland, P.G., Brian Collins, and Steve Anderson, P.G. South Florida Water Management District 3301 Gun Club Road West Palm Beach, Florida 33406 July 2011 AAcckknnoowwlleeddggeemmeennttss The authors would like to thank the Everglades Restoration Planning Department of the South Florida Water Management District (SFWMD) for providing the project funding for Phase II and Phase III of this project. We would also like to thank Sue Farland and Frances Johnson in the Water Quality Analysis Division of the SFWMD’s Environmental Resource Assessment Department for organizing and providing water quality sampling kits. Thanks and appreciation to Craig Wilson, Mike Curley, and Houston Tripp in the SFWMD’s Everglades Construction Department for their expertise and help with construction contract issues during this project. The SFWMD’s Okeechobee Field Station deserves recognition for their support of the project and for cooperating with our contractors during this project. Hydrogeologic Investigation of the Floridan Aquifer System at the S-65C Site (Well OKF-105) | i ii | Acknowledgements EExxeeccuuttiivvee SSuummmmaarryy The South Florida Water Management District (SFWMD) oversaw the construction and testing of a Floridan aquifer exploratory well (OKF-105) in Okeechobee County, Florida. The well is located on the west side of the Kissimmee River, adjacent to structure S-65C, approximately 20 miles northwest of the City of Okeechobee. Construction and testing of OKF-105 took place in three phases over three years. -
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 -
Sequence Stratigraphy of the Arcadia Formation, Southeast
SEQUENCE STRATIGRAPHY OF THE ARCADIA FORMATION, SOUTHEAST FLORIDA: AN INTEGRATED APPROACH by Caroline M. Wright A Thesis Submitted to the Faculty of the Charles E. Schmidt College of Science in Partial Fulfillment of the Requirements for the Degree of Master of Science Florida Atlantic University Boca Raton, Florida August 2014 ACKNOWLEDGEMENTS I would like to thank my committee and the professionals at the USGS for their support and patience. Dr. Kevin Cunningham‟s expertise on Oligocene/Miocene ichnotaxa and carbonate microfacies analysis was invaluable. Ron Reese‟s guidance and help on lithologic, geophysical, and sequence analysis was instrumental and much appreciated. A special thanks to the entire staff at the USGS Florida Water Science Center for their support and help in obtaining the material and equipment for the study. Dr. Root and Dr. Comas were helpful in reviewing the manuscript and providing useful geophysical and hydrogeologic advice. To my family, friends, and all those who encouraged me to continue, thank you. Finally, I would like to thank my major professor Dr. Anton Oleinik for his unwavering support, guidance and patience as well his helpful expertise on sedimentology and stratigraphy; the completion of this study would not have been possible without his continued dedication. iii ABSTRACT Author: Caroline M. Wright Title: Sequence Stratigraphy of the Arcadia Formation, Southeast Florida: An Integrated Approach Institution: Florida Atlantic University Thesis Advisor: Dr. Anton Oleinik Degree: Master of Science Year: 2014 The Arcadia Formation is a mixed carbonate-siliciclastic rock unit that existed as a shallow carbonate ramp to platform environment during the Late Oligocene to Early Miocene Epoch. -
Paleogene-Early Neogene Palynomorphs from the Eastern Equatorial Atlantic and Southeastern Florida, USA: Biostratigraphy and Paleoenvironmental Implications
Scholars' Mine Doctoral Dissertations Student Theses and Dissertations Spring 2018 Paleogene-Early Neogene palynomorphs from the Eastern Equatorial Atlantic and Southeastern Florida, USA: Biostratigraphy and paleoenvironmental implications Walaa K. Awad Follow this and additional works at: https://scholarsmine.mst.edu/doctoral_dissertations Part of the Geology Commons, and the Geophysics and Seismology Commons Department: Geosciences and Geological and Petroleum Engineering Recommended Citation Awad, Walaa K., "Paleogene-Early Neogene palynomorphs from the Eastern Equatorial Atlantic and Southeastern Florida, USA: Biostratigraphy and paleoenvironmental implications" (2018). Doctoral Dissertations. 2665. https://scholarsmine.mst.edu/doctoral_dissertations/2665 This thesis is brought to you by Scholars' Mine, a service of the Missouri S&T Library and Learning Resources. This work is protected by U. S. Copyright Law. Unauthorized use including reproduction for redistribution requires the permission of the copyright holder. For more information, please contact [email protected]. i PALEOGENE-EARLY NEOGENE PALYNOMORPHS FROM THE EASTERN EQUATORIAL ATLANTIC AND SOUTHEASTERN FLORIDA, USA: BIOSTRATIGRAPHY AND PALEOENVIRONMENTAL IMPLICATIONS by WALAA KAMALELDEEN AWAD A DISSERTATION Presented to the Faculty of the Graduate School of the MISSOURI UNIVERSITY OF SCIENCE AND TECHNOLOGY In Partial Fulfillment of the Requirements for the Degree DOCTOR OF PHILOSOPHY in GEOLOGY and GEOPHYSICS 2018 Approved by Francisca Oboh-Ikuenobe, Advisor John Hogan David Wronkiewicz Wan Yang Lucy Edwards ii © 2018 Walaa Kamaleldeen Awad All Rights Reserved iii To my daughters, Hala and Sara iv PUBLICATION DISSERTATION OPTION This dissertation consists of the following five articles which have been submitted for publication, or will be submitted for publication as follows: Paper I, pages 3-71 have been accepted by JOURNAL OF AFRICAN EARTH SCIENCES. -
A New Machairodont from the Palmetto Fauna (Early Pliocene) of Florida, with Comments on the Origin of the Smilodontini (Mammalia, Carnivora, Felidae)
A New Machairodont from the Palmetto Fauna (Early Pliocene) of Florida, with Comments on the Origin of the Smilodontini (Mammalia, Carnivora, Felidae) Steven C. Wallace1*, Richard C. Hulbert Jr.2 1 Department of Geosciences, Don Sundquist Center of Excellence in Paleontology, East Tennessee State University, Johnson City, Tennessee, United States of America, 2 Florida Museum of Natural History, University of Florida, Gainesville, Florida, United States of America Abstract South-central Florida’s latest Hemphillian Palmetto Fauna includes two machairodontine felids, the lion-sized Machairodus coloradensis and a smaller, jaguar-sized species, initially referred to Megantereon hesperus based on a single, relatively incomplete mandible. This made the latter the oldest record of Megantereon, suggesting a New World origin of the genus. Subsequent workers variously accepted or rejected this identification and biogeographic scenario. Fortunately, new material, which preserves previously unknown characters, is now known for the smaller taxon. The most parsimonious results of a phylogenetic analysis using 37 cranio-mandibular characters from 13 taxa place it in the Smilodontini, like the original study; however, as the sister-taxon to Megantereon and Smilodon. Accordingly, we formally describe Rhizosmilodon fiteae gen. et sp. nov. Rhizosmilodon, Megantereon, and Smilodon ( = Smilodontini) share synapomorphies relative to their sister-taxon Machairodontini: serrations smaller and restricted to canines; offset of P3 with P4 and p4 with m1; complete verticalization of mandibular symphysis; m1 shortened and robust with widest point anterior to notch; and extreme posterior ‘‘lean’’ to p3/p4. Rhizosmilodon has small anterior and posterior accessory cusps on p4, a relatively large lower canine, and small, non-procumbent lower incisors; all more primitive states than in Megantereon and Smilodon. -
Pinellas County Community Health Assessment
PINELLAS COUNTY COMMUNITY HEALTH ASSESSMENT 2012 Pinellas County | Community Health Assessment 0 PINELLAS COUNTY COMMUNITY HEALTH ASSESSMENT REPORT 2012 Produced by: Pinellas County Health Department Report and Supplemental Materials Available at: www.pinellashealth.com To Provide Feedback or Request Additional Information: contact the Pinellas County Health Department, Office of Performance and Quality Improvement at (727)820-4214 Acknowledgments: The community health improvement planning process has been a collaborative and community driven approach for Pinellas County. Many individuals and organizations participated in and contributed valuable information to the community health assessment. This collaborative approach was essential in the development of a quality community health assessment report. 1 Pinellas County | Community Health Assessment 1. Introduction.............................................................................................................3 1.1. Acknowledgements.......................................................................................7 2. Pinellas County Overview....................................................................................8 3. Community Themes & Strengths Assessment.............................................10 3.1. Collaborative Engagement.........................................................................11 3.2. Community Survey.......................................................................................18 4. Local Public Health System Performance Assessment............................25 -
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 -
Honeymoon Island Beach Nourishment Field Trip, 2015, 37 P
Honeymoon Island Beach Nourishment Field Trip Southeastern Geological Society Guidebook No. 64 June 12-13, 2015 A Field Guide to Honeymoon Island Beach Nourishment Southeastern Geological Society Guidebook No. 64 Field Trip June 12-13, 2015 2015 SEGS OFFICERS President – Greg Mudd Vice President – Bryan Carrick Secretary – Samantha Andrews Treasurer – Harley Means Past President - John Herbert Guidebook Compiled and Edited by: Bryan Carrick, P.G., 2015 Published by: THE SOUTHEASTERN GEOLOGICAL SOCIETY P.O. Box 1636 Tallahassee, Florida 32302 Southeastern Geological Society Guidebook No. 64 June 12-13, 2015 TABLE OF CONTENTS INTRODUCTION AND ACKNOWLEDGMENTS by: Bryan Carrick, P.G. …............................................................................................... 2 HONEYMOON ISLAND BEACH RESTORATION PROJECT by: Brett D. Moore, P.E., Humiston & Moore Engineers .................................................. 3 ROSS/OSSI (ROSSI): A COASTAL MANAGEMENT TOOL FOR OFFSHORE SAND SOURCES by:Jennifer L. Coor1, Candace Beauvais2, Jase D. Ousley3................................................ 9 SEDIMENT ENGINEERING THRU DREDGING AND WITH NATURE (SETDWN) – FATE OF FINES IN THE DREDGING AND PLACEMENT PROCESS by:Coraggio K. Maglio1, Jase D. Ousley2, Jennifer L.Coor3.…..…………......................16 MODERN AND HISTORICAL MORPHODYNAMICS OF THE JOHN’S PASS - BLIND PASS DUAL-INLET SYSTEM, PINELLAS COUNTY, FLORIDA by: Mark H. Horwitz, University of South Florida........................................................... 23 INVERTEBRATE PALEONTOLOGY -
Miocene Paleontology and Stratigraphy of the Suwannee River Basin of North Florida and South Georgia
MIOCENE PALEONTOLOGY AND STRATIGRAPHY OF THE SUWANNEE RIVER BASIN OF NORTH FLORIDA AND SOUTH GEORGIA SOUTHEASTERN GEOLOGICAL SOCIETY Guidebook Number 30 October 7, 1989 MIOCENE PALEONTOLOGY AND STRATIGRAPHY OF THE SUWANNEE RIVER BASIN OF NORTH FLORIDA AND SOUTH GEORGIA Compiled and edit e d by GARY S . MORGAN GUIDEBOOK NUMBER 30 A Guidebook for the Annual Field Trip of the Southeastern Geological Society October 7, 1989 Published by the Southeastern Geological Society P. 0 . Box 1634 Tallahassee, Florida 32303 TABLE OF CONTENTS Map of field trip area ...... ... ................................... 1 Road log . ....................................... ..... ..... ... .... 2 Preface . .................. ....................................... 4 The lithostratigraphy of the sediments exposed along the Suwannee River in the vicinity of White Springs by Thomas M. scott ........................................... 6 Fossil invertebrates from the banks of the Suwannee River at White Springs, Florida by Roger W. Portell ...... ......................... ......... 14 Miocene vertebrate faunas from the Suwannee River Basin of North Florida and South Georgia by Gary s. Morgan .................................. ........ 2 6 Fossil sirenians from the Suwannee River, Florida and Georgia by Daryl P. Damning . .................................... .... 54 1 HAMIL TON CO. MAP OF FIELD TRIP AREA 2 ROAD LOG Total Mileage from Reference Points Mileage Last Point 0.0 0.0 Begin at Holiday Inn, Lake City, intersection of I-75 and US 90. 7.3 7.3 Pass under I-10. 12 . 6 5.3 Turn right (east) on SR 136. 15.8 3 . 2 SR 136 Bridge over Suwannee River. 16.0 0.2 Turn left (west) on us 41. 19 . 5 3 . 5 Turn right (northeast) on CR 137. 23.1 3.6 On right-main office of Occidental Chemical Corporation. -
Traffic Counts 2018
Average Annual Daily Traffic 2018 Counts in Pinellas County Pasco County Pinellas County Dunedin Cswy 3600 7500 15500 49500 29000 22000 Curlew Rd Trinity Blvd CURLEW RD 4300 9800 14200 22500 DEMARET DR OAK CREE K JONES DR 3300 22500 HAGEN AVE PalmPALM BLVDBlvd BRADY DR 1900 17100 15200 14000 5900 MichiganMICHIGAN Blvd BLVD Tarpon Ave 14000 CR 1 34500 Keystone Rd ALT US 19 | BAYSHORE BLVD Tarpon 16300 39500 Bayshore Blvd 3500 77500 GARRISONRD Springs 19800MIRA VISTA DR 4600 3300 SOLON AVE 6300 SAN JOSE DR RD PINEHURST Pinehurst RdPinehurst 20000 SAN SALVADOR DR 10500 Klosterman Rd 3000DR PALOMA 4800 950 8100 5900 SAN CHRISTOPHER DR 17000 20500 72000 31500 BASS BLVD Main St 2000 17600 SR 580 | MAIN ST 17800 Rd Lake East 10800 Pinellas County 28000 Skinner Blvd NEW YORK AVE YORK NEW 8000 LAKE HAVEN RD HAVEN LAKE 18500 County Hillsborough 2100 MAIN ST INDIGO DR INDIGO VIRGINIAVirginia3400 ST St 14800 US19 | BROADWAY ALT 25000 4100 DOUGLAS AVE DOUGLAS 9100 8200 Alderman Rd 4100 AR LYNDHURST ST LYNDHURST ST HIGHLAND W AVE 4800 Palm 14500 20500 11400 63500 GREENBRI BELTREES ST Edgewater Dr 1400 VIRGINIA AVE S Harbor 2300 AVE PATRICIA MILWAUKEE AVE MILWAUKEE 250 7500 Douglas Ave 83500 21500 16000 15500 Patricia Ave BROADWAY 3800 8900 Keene Rd Keene 6900 ALT US 19 | EDGEWATER DR Oldsmar UNION ST Union St 26000 24000 4700 17300 Tampa Rd 39500 KEENERD MONTCLAIR Y ES AVE ES LAND AVE LAND LN UL GH 35500 HW 13500 20500 Area 4400 Dunedin 23000 23500 Palmetto St 49500 Memorial Causeway 19000 74500 890089008900 25500 35500 Curlew Rd 58500 Betty Ln 119001190011900 -
Chapter 3. Origin and Evolution of Tampa Bay 37
Chapter 3. Origin and Evolution of Tampa Bay 37 Chapter 3. Origin and Evolution of Tampa Bay By Gerold Morrison (AMEC-BCI) and Kimberly K. Yates (U.S. Geological Survey–St. Petersburg, Florida) TAMPA BAY HAS AN UNUSUAL geologic history when compared to many other estuaries in the eastern U.S. (Brooks and Doyle, 1998; Hine and others, 2009). It lies near the center of the carbonate Florida Platform (fig. 3–1), and is associated with a buried “shelf valley system” (including a paleo-channel feature located beneath the modern Egmont Channel) that formed in the early Miocene, about 20 million years ago (Ma) (Hine, 1997; Donahue and others, 2003; Duncan and others, 2003). Since that time the area has been subject to substantial fluctuations in sea level and alternating periods of sediment deposition and removal. These events have produced a complex distribution of siliciclastic and carbonate-based sediments within the bay, its associated barrier islands, and the inner Florida shelf (Brooks and Doyle, 1998; Brooks and others, 2003; Duncan and others, 2003; Ferguson and Davis, 2003). Sinkholes and other karst features in the underlying carbonate strata, which are common throughout the west-central Florida region, have been important factors underlying the development of both Tampa Bay (Brooks and Doyle, 1998; Donahue and others, 2003) and Charlotte Harbor, a geologically similar estuary located about 100 mi to the south (Hine and others, 2009). In the case of Tampa Bay, the underlying shelf valley system consists of multiple karst controlled subbasins (separated by bedrock highs) that have been filled by sediments, some of which were deposited fluvially (Hine and others, 2009). -
Ginsburg IAS Volume
05/02/2007/1420hrs Karst Subbasins and Their Relation to the Transport of Tertiary Siliciclastic Sediments on the Florida Platform Running Title: Karst Subbasins on the Florida Platform ALBERT C. HINE1, *BEAU SUTHARD1, STANLEY D. LOCKER1, KEVIN J. CUNNINGHAM2, DAVID S. DUNCAN3, MARK EVANS4, AND ROBERT A. MORTON5 1 College of Marine Science, University of South Florida, St. Petersburg, FL 33701, [email protected] 2 U.S. Geological Survey,3110 SW 9th Ave, Ft. Lauderdale, FL 33315 3 Department of Marine Science, Eckerd College, 4200 54th Ave So., St. Petersburg, FL 33711 4 Division of Health Assessment and Consultation, NCEH/ATSDR, Mail Stop E-32, 1600 Clifton Rd., Atlanta, GA 30333 5 U.S. Geological Survey, 600 4th St. So., St. Petersburg, FL 33701 *Present Address Coastal Planning and Engineering 2481 NW Boca Raton Blvd Boca Raton, FL 33431 [email protected] 1 ABSTRACT Multiple, spatially-restricted, partly-enclosed karst subbasins with as much as 100 m of relief occur on a mid-carbonate platform setting beneath the modern estuaries of Tampa Bay and Charlotte Harbor located along the west-central Florida coastline. A relatively high-amplitude seismic basement consists of the mostly carbonate, upper Oligocene to middle Miocene Arcadia Formation, which has been significantly deformed into folds, sags, warps and sinkholes. Presumably, this deformation was caused during a mid-to-late Miocene sea-level lowstand by deep-seated dissolution of carbonates, evaporates or both, resulting in collapse of the overlying stratigraphy, thus creating paleotopographic depressions. Seismic sequences containing prograding clinoforms filled approximately 90% of the accommodation space of these western Florida subbasins.