Geologic Framework and Petroleum Potential of the Atlantic Coastal Plain and Continental Shelf
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Ecoregions of New England Forested Land Cover, Nutrient-Poor Frigid and Cryic Soils (Mostly Spodosols), and Numerous High-Gradient Streams and Glacial Lakes
58. Northeastern Highlands The Northeastern Highlands ecoregion covers most of the northern and mountainous parts of New England as well as the Adirondacks in New York. It is a relatively sparsely populated region compared to adjacent regions, and is characterized by hills and mountains, a mostly Ecoregions of New England forested land cover, nutrient-poor frigid and cryic soils (mostly Spodosols), and numerous high-gradient streams and glacial lakes. Forest vegetation is somewhat transitional between the boreal regions to the north in Canada and the broadleaf deciduous forests to the south. Typical forest types include northern hardwoods (maple-beech-birch), northern hardwoods/spruce, and northeastern spruce-fir forests. Recreation, tourism, and forestry are primary land uses. Farm-to-forest conversion began in the 19th century and continues today. In spite of this trend, Ecoregions denote areas of general similarity in ecosystems and in the type, quality, and 5 level III ecoregions and 40 level IV ecoregions in the New England states and many Commission for Environmental Cooperation Working Group, 1997, Ecological regions of North America – toward a common perspective: Montreal, Commission for Environmental Cooperation, 71 p. alluvial valleys, glacial lake basins, and areas of limestone-derived soils are still farmed for dairy products, forage crops, apples, and potatoes. In addition to the timber industry, recreational homes and associated lodging and services sustain the forested regions economically, but quantity of environmental resources; they are designed to serve as a spatial framework for continue into ecologically similar parts of adjacent states or provinces. they also create development pressure that threatens to change the pastoral character of the region. -
Southeastern Coastal Plains-Caribbean Region Report
Southeastern Coastal Plains-Caribbean Region Report U.S. Shorebird Conservation Plan April 10, 2000 (Revised September 30, 2002) Written by: William C. (Chuck) Hunter U.S. Fish and Wildlife Service 1875 Century Boulevard Atlanta, Georgia 30345 404/679-7130 (FAX 7285) [email protected] along with Jaime Collazo, North Carolina State University, Raleigh, NC Bob Noffsinger, U.S. Fish and Wildlife Service, Manteo, NC Brad Winn, Georgia DNR Wildlife Resources Division, Brunswick, GA David Allen, North Carolina Wildlife Resources Commission, Trenton, NC Brian Harrington, Manomet Center for Conservation Sciences, Manomet, MA Marc Epstein, U.S. Fish and Wildlife Service, Merritt Island NWR, FL Jorge Saliva, U.S. Fish and Wildlife Service, Boqueron, PR Executive Summary This report articulates what is needed in the Southeastern Coastal Plains and Caribbean Region to advance shorebird conservation. A separate Caribbean Shorebird Plan is under development and will be based in part on principles outlined in this plan. We identify priority species, outline potential and present threats to shorebirds and their habitats, report gaps in knowledge relevant to shorebird conservation, and make recommendations for addressing identified problems. This document should serve as a template for a regional strategic management plan, with step-down objectives, local allocations and priority needs outlined. The Southeastern Coastal Plains and Caribbean region is important for breeding shorebirds as well as for supporting transient species during both northbound -
The Sedimentology of Cay Sal Bank - an Incipiently Drowned Carbonate Platform
Nova Southeastern University NSUWorks HCNSO Student Theses and Dissertations HCNSO Student Work 4-30-2019 The edimeS ntology of Cay Sal Bank - an Incipiently Drowned Carbonate Platform Luis Ramirez [email protected] Follow this and additional works at: https://nsuworks.nova.edu/occ_stuetd Part of the Geology Commons, Marine Biology Commons, and the Oceanography and Atmospheric Sciences and Meteorology Commons Share Feedback About This Item NSUWorks Citation Luis Ramirez. 2019. The Sedimentology of Cay Sal Bank - an Incipiently Drowned Carbonate Platform. Master's thesis. Nova Southeastern University. Retrieved from NSUWorks, . (503) https://nsuworks.nova.edu/occ_stuetd/503. This Thesis is brought to you by the HCNSO Student Work at NSUWorks. It has been accepted for inclusion in HCNSO Student Theses and Dissertations by an authorized administrator of NSUWorks. For more information, please contact [email protected]. Thesis of Luis Ramirez Submitted in Partial Fulfillment of the Requirements for the Degree of Master of Science M.S. Marine Environmental Sciences Nova Southeastern University Halmos College of Natural Sciences and Oceanography April 2019 Approved: Thesis Committee Major Professor: Sam Purkis, Ph.D Committee Member: Bernhard Riegl, Ph.D Committee Member: Robert Madden, Ph.D This thesis is available at NSUWorks: https://nsuworks.nova.edu/occ_stuetd/503 HALMOS COLLEGE OF NATURAL SCIENCES AND OCEANOGRAPHY The Sedimentology of Cay Sal Bank, an Incipiently Drowned Carbonate Platform By Luis F. Ramirez Submitted to the Faculty of Halmos College of Natural Sciences and Oceanography in partial fulfillment of the requirements for the degree of Master of Science with a specialty in: Marine Environmental Science Nova Southeastern University May 2019 Submitted in Partial Fulfillment of the Requirements for the Degree of Masters of Science: Marine Environmental Science Luis F. -
Partners in Flight: Mid-Atlantic Coastal Plain Bird Conservation Plan (Physiographic Area #44)
W&M ScholarWorks CCB Technical Reports Center for Conservation Biology (CCB) 1999 Partners in Flight: Mid-Atlantic Coastal Plain Bird Conservation Plan (Physiographic Area #44) B. D. Watts The Center for Conservation Biology, [email protected] Follow this and additional works at: https://scholarworks.wm.edu/ccb_reports Recommended Citation Watts, B. D., "Partners in Flight: Mid-Atlantic Coastal Plain Bird Conservation Plan (Physiographic Area #44)" (1999). CCB Technical Reports. 454. https://scholarworks.wm.edu/ccb_reports/454 This Report is brought to you for free and open access by the Center for Conservation Biology (CCB) at W&M ScholarWorks. It has been accepted for inclusion in CCB Technical Reports by an authorized administrator of W&M ScholarWorks. For more information, please contact [email protected]. Partners in Flight: Mid-Atlantic Coastal Plain Bird Conservation Plan (Physiographic Area #44) April 1999 Center for Conservation Biology College of William and Mary & Virginia Commonwealth University Partners in Flight: Mid-Atlantic Coastal Plain Bird Conservation Plan (Physiographic Area #44) April 1999 Bryan D. Watts, PhD Center for Conservation Biology College of William and Mary & Virginia Commonwealth University Address comments to: Bryan D. Watts Center for Conservation Biology College of William and Mary Williamsburg, VA 23187-8795 (757) 221-2247 [email protected] Recommended Citation: Watts, B. D. 1999. Partners in Flight: Mid-Atlantic Coastal Plain Bird Conservation Plan (Physiographic Area #44). Center for Conservation Biology Technical Report Series, CCBTR-99-08. College of William and Mary & Virginia Commonwealth University, Williamsburg, VA. 84 pp. The Center for Conservation Biology is an organization dedicated to discovering innovative solutions to environmental problems that are both scientifically sound and practical within today’s social context. -
Structural and Stratigraphic Framework, and Spatial Distribution of Permeability of the Atlantic Coastal Plain, North Carolina to New York
Structural and Stratigraphic Framework, and Spatial Distribution of Permeability of the Atlantic Coastal Plain, North Carolina to New York GEOLOGICAL SURVEY PROFESSIONAL PAPER 796 Structural and Stratigraphic Framework, and Spatial Distribution of Permeability of the Atlantic Coastal Plain, North Carolina to New York By PHILIP M. BROWN, JAMES A. MILLER, and FREDERICK M. SWAIN GEOLOGICAL SURVEY PROFESSIONAL PAPER 796 UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1972 UNITED STATES DEPARTMENT OF THE INTERIOR ROGERS C. B. MORTON, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress catalog-card No. 72-600285 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 Stock Number 2401-00243 CONTENTS Page Abstract.___________________________________________ 1 Stratigraphic framework Continued Introduction. __ _____________________---____----_-____ 2 Lithostratigraphic description and biostratigraphic Location of area.____________________________________ 3 discussion Continued Acknowledgments. __________________________________ 3 Cenozoic Era__ ____________-_-___--__-------_ 45 Previous work_______________________________________ 5 Tertiary System. _______.-_______----__-_ 45 Purpose of this report. ________________________________ 6 Paleocene Series _ ___________________ 45 Structural architecture._______________________________ 6 Midway Stage Rocks of Midway Introduction, __ ________________________________ 6 Age_ ___----__-____--_------__ 45 General discussion________________________ -
JAMES E. ANDREWS Department of Oceanography, University of Hawaii, Honolulu, Hawaii 96822 FRANCIS P
JAMES E. ANDREWS Department of Oceanography, University of Hawaii, Honolulu, Hawaii 96822 FRANCIS P. SHEPARD Geological Research Division, University of California, Scripps Institution of Oceanography, La Jolla, California 92037 ROBERT J. HURLEY Institute of Marine and Atmospheric Sciences, University of Miami, Miami, Florida Great Bahama Canyon ABSTRACT Recent surveys and sampling of the V-shaped rock, rounded cobbles, and boulders along their canyon that cuts into parts of the broad troughs axes, as well as ripple-marked sand to indicate the separating the Bahama Banks have given a greatly importance of currents moving along the canyon improved picture of this gigantic valley and the floor. Further evidence that erosion has at least processes operating to shape it. The canyon has kept the valleys open as the Bahama Banks grew two major branches, one following Northwest comes from the winding courses and the numerous Providence Channel and the other the Tongue of tributaries that descend the walls from the shallow the Ocean, which join 15 mi north of New Provi- Banks, particularly on the south side of Northwest dence Island, and continue seaward as a submarine Branch. The possibility that limestone solution has canyon with walls almost 3 mi high. These, so lar been important comes from the finding of more as we know, are the world's highest canyon walls depressions along Northwest Branch than in other (either submarine or subaenal), and the canyon submarine canyons of the world, and the discovery length, including the branch in Northwest Provi- ol caverns along the walls by observers during deep dence Channel, is at least 150 mi, exceeded only by dives into Tongue Branch in the Alvin and two submarine canyons in the Bering Sea. -
Delaware Pennsylvania
Comparing and Contrasting Delaware and Pennsylvania Name: _________________________ Delaware Delaware, one of America’s original 13 colonies, became America’s first state on December 7, 1787. Hence, its nickname is simply the First State. It became the first state when it ratified, or accepted, the United States Constitution. Delaware is located in the Mid-Atlantic region of the United States, entirely within the Atlantic Coastal Plain. Its capital is Dover and its largest city is Wilmington. Delaware’s land is mostly flat. Its east coast has many wetlands and popular beaches. Delaware is the second smallest state in America in terms of area, and fifth smallest in terms of population. There are less than a million people who live in Delaware. It borders three states: Maryland, Pennsylvania, and New Jersey. Delaware and New Jersey are separated by the wide Delaware River. Pennsylvania Pennsylvania, one of the original 13 colonies, became America’s second state on December 12, 1787. At the time, Philadelphia, Pennsylvania, was the capital of the United States. Millions of people flock to Philadelphia every year to see Independence Hall and the Liberty Bell. Independence Hall was the site of the drafting of both the Declaration of independence and the United States Constitution, two of the most important documents in American history. Gettysburg National Park, located in southern Pennsylvania, was the site of the largest battle ever fought on American soil. The majority of Pennsylvania is covered by the Appalachian Mountains and foothills. Pennsylvania is the only state in the Mid-Atlantic region without beaches. It borders five states: New York, New Jersey, Maryland, West Virginia, and Ohio. -
The Mid-Atlantic Coastal Plain (Physiographic Area 44)
Partners in Flight Bird Conservation Plan for The Mid-Atlantic Coastal Plain (Physiographic Area 44) Partners in Flight: Mid-Atlantic Coastal Plain Bird Conservation Plan (Physiographic Area #44) VERSION 1.0 April 1999 Address comments to: Bryan D. Watts Center for Conservation Biology College of William and Mary Williamsburg, VA 23187-8795 (757) 221-2247 [email protected] *********************************************** Front cover illustration from ‘All the Birds of North America’ by Jack Griggs, courtesy of HarperCollins publishers. PIF Bird Conservation Plan -- Mid-Atlantic Coastal Plain 2 ACKNOWLEDGMENTS This draft plan was produced with funds provided by the Northern Neck Audubon Society, the Tennessee Conservation League, and the Center for Conservation Biology at the College of William and Mary. I thank Bob Ford and Ken Rosenberg for guidance throughout the planning process. Dana Bradshaw, Mike Wilson, and Marian Watts provided assistance with information and literature. PIF Bird Conservation Plan -- Mid-Atlantic Coastal Plain 3 MID-ATLANTIC COASTAL PLAIN BIRD CONSERVATION PLAN EXECUTIVE SUMMARY The mid-Atlantic Coastal Plain was the site of the first successful European settlement in North America and its landscape has been subject to influence by European culture for nearly four centuries. Currently, the urban crescent from Baltimore south to Richmond and east to Norfolk is experiencing one of the fastest human growth rates in North America. Managing this population growth while maintaining functional natural ecosystems is the greatest conservation challenge faced by land managers within the region. Despite these important management challenges, the potential for successful conservation of priority bird populations remains optimistic. This optimism stems from 1) the fact that a large number of lands critical to priority bird populations are currently protected or held by PIF partners, and 2) many priority species remain relatively abundant and widespread within the region. -
Transport, Potential Vorticity, and Current/Temperature Structure Across Northwest Providence and Santaren Channels and the Florida Current Off Cay Sal Bank
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 100, NO. C5, PAGES 8561-8569, MAY 15, 1995 Transport, potential vorticity, and current/temperature structure across Northwest Providence and Santaren Channels and the Florida Current off Cay Sal Bank Kevin D. Leaman,' PeterS. Vertes, 1 Larry P. Atkinson,2 Thomas N. Lee,' Peter Hamilton,3 and Evans WaddelP Abstract. Currents and temperatures were measured using Pegasus current profilers across Northwest Providence and Santaren Channels and across the Florida Current off Cay Sal Bank during four cruises from November 1990 to September 1991. On average, Northwest Providence (1.2 Sv) and Santaren (1.8 Sv) contribute about 3 Sv to the total Florida Current transport farther north (e.g., 27°N). Partitioning of transport into temperature layers shows that about one-half of this transport is of" 18°C" water (17°C-19.SOC); this can account for all of the "excess" 18°C water observed in previous experiments. This excess is thought to be injected into the 18°C layer in its region of formation in the northwestern North Atlantic Ocean. Due to its large thickness, potential vorticities in this layer in its area of formation are very low. In our data, lowest potential vorticities in this layer are found on the northern end of Northwest Providence Channel and are comparable to those observed on the eastern side of the Florida Current at 27°N. On average a low-potential-vorticity l8°C layer was not found in the Florida Current off Cay Sal Bank. 1. Introduction the Florida Current/Gulf Stream cross-stream structure was carried out using Pegasus profiler data at 27°N as well as at Because of its importance to the overall general circula 29°N and off Cape Hatteras [Leaman et al., 1989]. -
Deep-Water Biogenic Sediment Off the Coast of Florida
Deep-Water Biogenic Sediment off the Coast of Florida by Claudio L. Zuccarelli 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, FL May 2017 Copyright 2017 by Claudio L. Zuccarelli ii Abstract Author: Claudio L. Zuccarelli Title: Deep-Water Biogenic Sediment off the Coast of Florida Institution: Florida Atlantic University Thesis Advisor: Dr. Anton Oleinik Degree: Master of Science Year: 2017 Biogenic “oozes” are pelagic sediments that are composed of > 30% carbonate microfossils and are estimated to cover about 50% of the ocean floor, which accounts for about 67% of calcium carbonate in oceanic surface sediments worldwide. These deposits exhibit diverse assemblages of planktonic microfossils and contribute significantly to the overall sediment supply and function of Florida’s deep-water regions. However, the composition and distribution of biogenic sediment deposits along these regions remains poorly documented. Seafloor surface sediments have been collected in situ via Johnson- Sea-Link I submersible along four of Florida’s deep-water regions during a joint research cruise between Harbor Branch Oceanographic Institute (HBOI) and Florida Atlantic University (FAU). Sedimentological analyses of the taxonomy, species diversity, and sedimentation dynamics reveal a complex interconnected development system of Florida’s deep-water habitats. Results disclose characteristic microfossil assemblages of planktonic foraminiferal ooze off the South West Florida Shelf, a foraminiferal-pteropod ooze through the Straits iv of Florida, and pteropod ooze deposits off Florida’s east coast. The distribution of the biogenic ooze deposits is attributed to factors such as oceanographic surface production, surface and bottom currents, off-bank transport, and deep-water sediment drifts. -
Shallow Structure
IBRARY CO Atlantic Continental Shelf and Slope of the United States Shallow Structure GEOLOGICAL SURVEY PROFESSIONAL PAPER 529·1 Atlantic Continental . r.. Shelf and Slope of The United States- Shallow Structure By ELAZAR UCHUPI GEOLOGICAL SURVEY PROFESSIONAL PAPER 529-I Description of the subsurface morphology of the shelf and slop~ (continental terrace) ·and some speculations on the evolution of the sedimentary framework of the terrace UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON 1970 • UNITED STATES DEPARTMENT OF THE INTERIOR WALTER J. HICKEL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 - Price $1 (paper cover) CONTENTS P11ge Pllge Abstract------------------------------------------- 11 Continental shelf from Cape lioa to Virginia___________ 113 Introduction---------------------~----------------- 1 Continental slope from· Georges Bank to Cape Hatteras_ 15 Acknowledgments _____________________________ _ 2 Continental shelf from Cape Hatteras to Cape Romain___ 19 Topographic setting ___________________ --- _____ ---- __ 2 Blake Plateau area__________________________________ 19 Methods of study __________________________________ _ 2 Straits of Florida ___________ :... _______________ :._______ 30 Scotian Shelf area _________________________________ _ 5 Geologic maP-------------------------------------- 31 5 Isopach maps_ _ _ _ _ __ _ _ _ _ __ __ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ 33 Gulf of Maine and Bay of -
Federal Register/Vol. 72, No. 27/Friday, February 9, 2007/Rules
Federal Register / Vol. 72, No. 27 / Friday, February 9, 2007 / Rules and Regulations 6165 all provisions in §§ 1.181–1T through SUMMARY: This Treasury decision purchase. Establishment of a viticultural 1.181–5T to the productions. establishes the Outer Coastal Plain area is neither an approval nor an (c) Special rules for returns filed for viticultural area in southeastern New endorsement by TTB of the wine prior taxable years. If before March 12, Jersey. The viticultural area consists of produced in that area. 2007, an owner of a film or television approximately 2,255,400 acres and Requirements production began principal photography includes all of Cumberland, Cape May, (or ‘‘in-between’’ animation) for the Atlantic, and Ocean Counties and Section 4.25(e)(2) of the TTB production after October 22, 2004, and portions of Salem, Gloucester, Camden, regulations outlines the procedure for filed its original Federal income tax Burlington, and Monmouth Counties. proposing an American viticultural area return for the year such costs were first We designate viticultural areas to allow and provides that any interested party paid or incurred without making an bottlers to better describe the origin of may petition TTB to establish a grape- election under section 181 for the costs their wines and to allow consumers to growing region as a viticultural area. of the production, and if the taxpayer better identify the wines they may Section 9.3(b) of the TTB regulations wants to make an election under section purchase. requires the petition to include— • 181 for such taxable year, see § 1.181– DATES: Effective Date: March 12, 2007.