Geology and Tectonic History of the Lower Cape Fear River Valley, Southeastern North Carolina

Total Page:16

File Type:pdf, Size:1020Kb

Geology and Tectonic History of the Lower Cape Fear River Valley, Southeastern North Carolina Geology and Tectonic History of the Lower Cape Fear River Valley, Southeastern North Carolina U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1466 - A Geology and Tectonic History of the Lower Cape Fear River Valley, Southeastern North Carolina By DAVID R. SOLLER SURFACE AND SHALLOW SUBSURFACE GEOLOGIC STUDIES OF THE CAROLINA COASTAL PLAINS U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1466-A A study of a major river valley on the outer Atlantic Coastal Plain including mineralogic analysis of the deposits and geomorphic evidence for tectonic uplift UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON: 1988 DEPARTMENT OF THE INTERIOR DONALD PAUL MODEL, Secretary U.S. GEOLOGICAL SURVEY Dallas L. Peck, Director Any use of trade names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Geological Survey Library of Congress Cataloging in Publication Data Seller, D.R. (David R.) Geology and tectonic history of the lower Cape Fear River valley, southeastern North Carolina. (U.S. Geological Survey professional paper ; 1466A) Bibliography: p. 1. Geology North Carolina Cape Fear River valley. 2. Cape Fear River valley (N.C.) I. Title. II. Series. QE148.C35S65 1988 557.3 s [557.56'2] 86-600245 For sale by the Books and Open-File Reports Section, U.S. Geological Survey Federal Center, Box 25425, Denver, CO 80225 CONTENTS Page Page Abstract........................................................................................................ Al Mineralogy of the fluvial and upland deposits Continued Introduction.................................................................................................... 1 Clay-sized fraction............................................................................A25 Acknowledgments........................................................................................ 2 Weathering processes and patterns ...................................................... 33 Geographic setting........................................................................................ 2 Weathering of the upland deposits................................................ 39 Geologic setting ............................................................................................ 3 Weathering of the fluvial deposits ................................................ 39 Previous investigations................................................................................ 6 Weathering of the dune deposits.................................................... 40 General stratigraphy .................................................................................. 8 An estimate of the ages of dunes and Carolina bays ........................ 41 Study approach.............................................................................................. 9 Geomorphic evidence for uplift of the Cape Fear River valley...... 42 Sample localities .......................................................................................... 9 Longitudinal profiling...................................................................... 43 Methods of analysis...................................................................................... 9 Local uplift of the Cape Fear River valley.................................. 46 Radiocarbon data........................................................................................ 11 Cause of the elevated shorelines...................................................... 50 Pollen data.................................................................................................... 11 Comparison of the Cape Fear and Pee Dee River valleys .............. 52 Identification and correlation of terraces............................................ 12 Upland drainage patterns and regional tectonics .................... 53 Gross lithology and thickness of the fluvial deposits........................ 15 Summary...................................................................................................... 54 Mineralogy of the fluvial and upland deposits .................................. 18 References .................................................................................................... 56 "Heavy" sand-sized fraction ............................................................ 18 Appendix: Drill-site locations.................................................................. 59 "Light" sand-sized fraction.............................................................. 19 ILLUSTRATIONS Page PLATE 1. Geologic map of the Cape Fear River valley and surrounding upland areas.................................................. In pocket Page FIGURE 1. Map showing location of the study area .............................................................................................. ........ A2 2. Landsat image of the study area........................................................................................................................... ..3 3. Aerial photograph of the lower Cape Fear River valley showing Carolina bays and sand dunes..................................4 4. Maps presenting geologic evidence for the Cape Fear arch................................................................. ............. .5 5. Map showing location of drill sites within the study area ................................................................................ .. 10 6. Cross sections of the Cape Fear River valley along four auger hole transects......................... 13 7. Aerial photograph of the Cape Fear River valley and uplands near Garland, N.C. .................................................. 14 8. Aerial photograph of the Cape Fear River valley showing diversion of Colly Creek by migrating dunes .................. 16 9. Aerial photograph of the lower reaches of the Cape Fear River valley showing the Socastee and Wando terraces. .. .. ..............................................................................................._^ 10,11. Diagrams comparing lithology and sand mineralogy of auger hole samples of: 10. Upland deposits.......................................................................................................................................... 20 11. Valley deposits ...................................................................................................................... ..... 22 12-17. Maps of the Cape Fear River valley showing variations in: 12. Hornblende abundance in the fluvial sediments............................................................... ... ..... 29 13. Epidote abundance in the fluvial sediments......................................................................... ...... .... 29 14. Hornblende abundance in the dune sands ......................................................................... .. .. .. 30 15. Epidote abundance in the dune sands..................... ...................... ... ... 30 16. Feldspar abundance in the fluvial sediments .............................................. 31 17. Feldspar abundance in the dune sands................................................................. 31 18,19. X-ray diffraction traces of the untreated clay-sized fraction in samples of: 18. Upland deposits................................................................................................................................... 32 19. Valley deposits ............................................................................................................................... 34 20. Graph showing the rate at which the Cape Fear River has migrated to the southwest............... 43 in IV CONTENTS Page FIGURE 21-26. Diagrams showing: 21. Longitudinal profiles of fluvial terrace upper surfaces in the Cape Fear River valley................................ A44 22. Hypothetical profiles of a graded river along a stable continental margin .................................................. 45 23. Hypothetical profiles along a tectonically active continental margin............................................................ 45 24. Uplift of the Cape Fear River valley as measured by a best fit procedure on longitudinal profiles................ 46 25. Profile reconstruction used to assess the accuracy of the best fit procedure for profiling.............................. 47 26. Reconstructed profiles for all intervals of deposition since Waccamaw time (early Pleistocene).................... 48 27. Diagram comparing southeastern Atlantic Coastal Plain deposits with major interglacial oxygen isotope stages .............................................................................................................................................................. 51 28. Generalized location map showing major drainage and cities between the Pee Dee and Cape Fear Rivers, South Carolina and North Carolina ........................................................................................ ............. .... 52 TABLES Page TABLE Generalized late Cenozoic stratigraphy for the outer Coastal Plain of parts of North Carolina and South Carolina ................................................................................................................................................................................................. A9 Radiocarbon data for peat and macerated wood samples ........................................................................-..........-...--.--.....-.~~ 11 Pollen data...................................................................................................................................................................................................
Recommended publications
  • Environmental Assessment of the Lower Cape Fear River System, 2013
    Environmental Assessment of the Lower Cape Fear River System, 2013 By Michael A. Mallin, Matthew R. McIver and James F. Merritt August 2014 CMS Report No. 14-02 Center for Marine Science University of North Carolina Wilmington Wilmington, N.C. 28409 Executive Summary Multiparameter water sampling for the Lower Cape Fear River Program (LCFRP) has been ongoing since June 1995. Scientists from the University of North Carolina Wilmington’s (UNCW) Aquatic Ecology Laboratory perform the sampling effort. The LCFRP currently encompasses 33 water sampling stations throughout the lower Cape Fear, Black, and Northeast Cape Fear River watersheds. The LCFRP sampling program includes physical, chemical, and biological water quality measurements and analyses of the benthic and epibenthic macroinvertebrate communities, and has in the past included assessment of the fish communities. Principal conclusions of the UNCW researchers conducting these analyses are presented below, with emphasis on water quality of the period January - December 2013. The opinions expressed are those of UNCW scientists and do not necessarily reflect viewpoints of individual contributors to the Lower Cape Fear River Program. The mainstem lower Cape Fear River is a 6th order stream characterized by periodically turbid water containing moderate to high levels of inorganic nutrients. It is fed by two large 5th order blackwater rivers (the Black and Northeast Cape Fear Rivers) that have low levels of turbidity, but highly colored water with less inorganic nutrient content than the mainstem. While nutrients are reasonably high in the river channels, major algal blooms have until recently been rare because light is attenuated by water color or turbidity, and flushing is usually high (Ensign et al.
    [Show full text]
  • Suspended Sediment and Nutrients in the Upper Cape Fear River Basin, North Carolina, 2002–04, with an Analysis of Temporal Changes, 1976–2004
    Prepared in cooperation with the Upper Cape Fear River Basin Association Suspended Sediment and Nutrients in the Upper Cape Fear River Basin, North Carolina, 2002–04, with an Analysis of Temporal Changes, 1976–2004 Scientific Investigations Report 2005–5271 U.S. Department of the Interior U.S. Geological Survey Cover. Deep River spillway upstream from the U.S. highway 1 bridge in Chatham County, North Carolina (photograph by Ryan B. Rasmussen, U.S. Geological Survey). Suspended Sediment and Nutrients in the Upper Cape Fear River Basin, North Carolina, 2002–04, with an Analysis of Temporal Changes, 1976–2004 By Timothy B. Spruill, Phillip S. Jen, and Ryan B. Rasmussen Prepared in cooperation with the Upper Cape Fear River Basin Association Scientific Investigations Report 2005–5271 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior Gale A. Norton, Secretary U.S. Geological Survey P. Patrick Leahy, Acting Director U.S. Geological Survey, Reston, Virginia: 2006 For product and ordering information: World Wide Web: http://www.usgs.gov/pubprod Telephone: 1-888-ASK-USGS For more information on the USGS--the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment: World Wide Web: http://www.usgs.gov Telephone: 1-888-ASK-USGS Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted materials contained within this report.
    [Show full text]
  • Regional and County Population Change in North Carolina
    Regional and County Population Change in North Carolina A Summary of Trends from April 1, 2010 through July 1, 2016 North Carolina Office of State Budget and Management December 2017 Introduction The following document summarizes population trends for North Carolina using the certified county population estimates produced by the North Carolina Office of State Budget and Management (OSBM) released in September of 2017. These certified population estimates are as of July 1, 2016.1 Additional population tables that include statistics for all 100 counties can be obtained from https://www.osbm.nc.gov/demog/county‐estimates.2 Highlights: North Carolina grew by 620,254 people between April 1, 2010 and July 1, 2016, a 6.5% increase; Three of every four people added in this period were living in central North Carolina3; 95% of all growth occurred within metropolitan counties4; Among regional planning areas, only the Upper Coastal Plain Council of Governments experienced population decline; The fastest growing metropolitan statistical areas (MSAs) since April 1, 2010 were the North Carolina portion of the Myrtle Beach‐Conway‐North Myrtle Beach MSA, the Raleigh MSA, the North Carolina portion of the Charlotte‐Concord‐Gastonia MSA, and the Wilmington MSA. Only the Rocky Mount MSA experienced population decline since the last census, losing 4,460 people (a 2.9% decline); The Charlotte‐Concord‐Gastonia MSA remains the largest metropolitan area in the state (at 2.1 million people); Mecklenburg (1.1 million) and Wake (1.0 million) Counties remain
    [Show full text]
  • A Case Study of Carolina Bays and Ditched Streams at Risk Under the Proposed WOTUS Definition
    CAPE FEAR RIVER WATERSHED: A Case Study of Carolina Bays and Ditched Streams at Risk under the Proposed WOTUS Definition The Cape Fear River. Photo by Kemp Burdette The Cape Fear River Basin is North Carolina’s largest watershed, with an area of over 9,000 square miles. Major tributaries include the Deep River, the Haw River, the Northeast Cape Fear River, the Black River, and the South River. These rivers converge to form a thirty-mile-long estuary before flowing into the Atlantic Ocean at Cape Fear.1 The Cape Fear supplies water to some of the fastest ​ growing counties in the United States;2 roughly one in five North Carolinians gets their drinking ​ water from the Cape Fear, including residents of Greensboro, Fayetteville, and Wilmington.3 ​ The Cape Fear Basin is a popular watershed for a variety of recreation activities. State parks along the river include Haw River State Park, Raven Rock State Park, and Carolina Beach State Park. The faster-flowing water of the upper basin is popular with paddlers, as are the slow meandering blackwater rivers and streams of the lower Cape Fear and estuary. Fishing is very popular; the Cape Fear supports a number of freshwater species, saltwater species, and even anadromous (migratory) species like the endangered sturgeon, striped bass, and shad. Cape Fear River Watershed: Case Study Page 2 of 8 The Cape Fear is North Carolina’s most ecologically diverse watershed; the Lower Cape Fear is notable because it is part of a biodiversity “hotspot,” recording the largest degree of biodiversity on the eastern seaboard of the United States.
    [Show full text]
  • Cape Fear River Blueprint
    Lower Cape Fear River Blueprint Since 1982, the North Carolina Coastal Federation has worked with residents and visitors of North Carolina to protect and restore the coast, including participating in many issues and projects within the Cape Fear region. The Lower Cape Fear River provides critical coastal and riverine habitat, storm and flood protection and commercial and recreational fishery resources. It is also a popular recreational destination and an economic driver for the state’s southeastern region, and it embodies a rich historic and cultural heritage. The river also serves as an important source of drinking water for many coastal communities, including the City of Wilmington. Today, the lower river needs improved environmental safeguards, a clear vision for compatible and sustainable economic development. Further, effective leadership is needed to address existing issues of pollution and habitat loss and prevent projects that threaten the health of the community and the river. The Lower Cape Fear River is continually affected by both local and upstream actions. The continued degradation of these essential functions threatens the well-being of all within the community. The Coastal Federation continues to address these issues by actively engaging with local governments, state and federal agencies and other entities. Our board of directors recognizes these needs and adopted the following goals as part of a three-year, organizationwide initiative: Advocate for compatible industrial development in the coastal zone; Restore coastal habitats and protect water quality; Improve our economy through coastal restoration. The Lower Cape Fear River Blueprint (The Blueprint) is a collaborative effort to focus on the river’s estuarine and riverine natural resources.
    [Show full text]
  • Environmental Assessment of the Lower Cape Fear River System, 2015
    Environmental Assessment of the Lower Cape Fear River System, 2015 By Michael A. Mallin, Matthew R. McIver and James F. Merritt November 2016 CMS Report No. 16-02 Center for Marine Science University of North Carolina Wilmington Wilmington, N.C. 28409 Executive Summary Multiparameter water sampling for the Lower Cape Fear River Program (LCFRP) http://www.uncw.edu/cms/aelab/LCFRP/index.htm, has been ongoing since June 1995. Scientists from the University of North Carolina Wilmington’s (UNCW) Aquatic Ecology Laboratory perform the sampling effort. The LCFRP currently encompasses 33 water sampling stations throughout the lower Cape Fear, Black, and Northeast Cape Fear River watersheds. The LCFRP sampling program includes physical, chemical, and biological water quality measurements and analyses of the benthic and epibenthic macroinvertebrate communities, and has in the past included assessment of the fish communities. Principal conclusions of the UNCW researchers conducting these analyses are presented below, with emphasis on water quality of the period January - December 2015. The opinions expressed are those of UNCW scientists and do not necessarily reflect viewpoints of individual contributors to the Lower Cape Fear River Program. The mainstem lower Cape Fear River is a 6th order stream characterized by periodically turbid water containing moderate to high levels of inorganic nutrients. It is fed by two large 5th order blackwater rivers (the Black and Northeast Cape Fear Rivers) that have low levels of turbidity, but highly colored water with less inorganic nutrient content than the mainstem. While nutrients are reasonably high in the river channels, major algal blooms have until recently been rare because light is attenuated by water color or turbidity, and flushing is usually high (Ensign et al.
    [Show full text]
  • Spotlight on Wilmington
    SPOTLIGHT ON WILMINGTON WELCOME TO WILMINGTON, NORTH CAROLINA The city has been declared “The Next Big Thing” by national media as one of the best places to live in North Carolina. Nestled between the Cape Fear River and Atlantic Ocean, Wilmington strikes an enviable balance between a casual lifestyle and global business opportunities and makes an ideal destination for moving to North Carolina. Entrepreneurial zeal permeates every facet of the community, giving it the vibrancy of a city much larger in size, with the ease of living found in a small town. Contents Climate and Geography 02 Cost of Living and Transportation 03 Sports and Outdoor Activities 04 Shopping and Dining 05 Schools and Education 06 GLOBAL MOBILITY SOLUTIONS l SPOTLIGHT ON WILMINGTON l 01 SPOTLIGHT ON WILMINGTON CLIMATE Wilmington, NC Climate Graph Wilmington has a humid subtropical climate, characterized by hot, usually humid summers and mild to cold winters. People in Wilmington breathe easily because the air quality for Wilmington is rated 21% better than the national average and the pollution index is 16% better than the national average. Average High/Low Temperatures Low / High January 36oF / 56oF July 73oF / 90oF Average Precipitation Rain 58 in. Snow 1 in. GEOGRAPHY Wilmington is in a part of North Carolina known as the Tidewater or Coastal Plain. This area is characterized by thick forests of pines and other evergreens; due to the sandy soils it is difficult for many deciduous trees to grow. This portion of the state contains the Outer Banks, sandy islands that do not have coral reefs to attach to and thus are constantly shifting their locations.
    [Show full text]
  • Native Americans in the Cape Fear, by Dr. Jan Davidson
    Native Americans in the Cape Fear, By Dr. Jan Davidson Archaeologists believe that Native Americans have lived in what is now the state of North Carolina for more than 13,000 years. These first inhabitants, now called Paleo-Indians by experts, were likely descended from people who came over a then-existing land bridge from Asia.1 Evidence had been found at Town Creek Mound that suggests Indians lived there as early as 11000 B.C.E. Work at another major North Carolinian Paleo-Indian where Indian artifacts have been found in layers of the soil, puts Native Americans on that land before 8000 B.C.E. That site, in North Carolina’s Uwharrie Mountains, near Badin, became an important source of stone that Paleo and Archaic period Indians made into tools such as spears.2 It is harder to know when the first people arrived in the lower Cape Fear. The coastal archaeological record is not as rich as it is in some other regions. In the Paleo-Indian period around 12000 B.C.E., the coast was about 60 miles further out to sea than it is today. So land where Indians might have lived is buried under water. Furthermore, the coastal Cape Fear region’s sandy soils don’t provide a lot of stone for making tools, and stone implements are one of the major ways that archeologists have to trace and track where and when Indians lived before 2000 B.C.E.3 These challenges may help explain why no one has yet found any definitive evidence that Indians were in New Hanover County before 8000 B.C.E.4 We may never know if there were indigenous people here before the Archaic period began in approximately 8000 B.C.E.
    [Show full text]
  • NORTH CAROLINA 2020 DRAFT 303(D) LIST Upper Broad Broad River Basin
    NORTH CAROLINA 2020 DRAFT 303(D) LIST Upper Broad Broad River Basin AU Name AU Number Classification AU_LengthArea AU_Units AU ID Description Broad River Basin 03050105 Upper Broad BROAD RIVER 9-(22)a C 1.8 FW Miles 12499 From Carolina Mountain Power Company to US 64/74 Benthos (Nar, AL, FW) 5 Exceeding Criteria Fair, Poor or Severe Bioclassification 2008 BROAD RIVER 9-(22)b1 C 6.3 FW Miles 13396 From US 64/74 to Cove Creek Benthos (Nar, AL, FW) 5 Exceeding Criteria Fair, Poor or Severe Bioclassification 2008 Cleghorn Creek 9-26-(0.75) C 1.5 FW Miles 13295 From 90 meters south of Baber Road to the Broad River Benthos (Nar, AL, FW) 5 Exceeding Criteria Fair, Poor or Severe Bioclassification 2008 Catheys Creek 9-41-13-(6)b C 1.9 FW Miles 12701 From confluence with Hollands Creek to S. Broad R. Fish Community (Nar, AL, FW) 5 Exceeding Criteria Fair, Poor or Severe Bioclassification 1998 Mill Creek 9-41-13-3 WS-V 4.5 FW Miles 12705 From source to Catheys Creek Benthos (Nar, AL, FW) 5 Exceeding Criteria Fair, Poor or Severe Bioclassification 2008 Hollands Creek 9-41-13-7-(3) C 2.2 FW Miles 12709 From Case Branch to Catheys Creek Fish Community (Nar, AL, FW) 5 Exceeding Criteria Fair, Poor or Severe Bioclassification 1998 Sandy Run Creek 9-46-(1) WS-IV 10.4 FW Miles 13221 From source to a point approximately 0.7 mile upstream of SR 1168 Fish Community (Nar, AL, FW) 5 Exceeding Criteria Fair, Poor or Severe Bioclassification 2018 Hinton Creek 9-50-15 C 13.2 FW Miles 12777 From source to First Broad River Benthos (Nar, AL, FW) 5 Exceeding Criteria
    [Show full text]
  • Emerging Per- and Polyfluoroalkyl Substances: the North Carolina Experience
    Emerging Per- and Polyfluoroalkyl Substances: The North Carolina Experience Zack Moore, MD, MPH State Epidemiologist Division of Public Health, N.C. DHHS Outline • Timeline of GenX response and scope of issue • Public health responses • Challenges and data gaps • Ongoing and future activities Wilmington, North Carolina Timeline of Response to GenX in Drinking Water • June 2017 −News coverage brings GenX to the forefront −N.C. DHHS contacted by local health departments 4 What is GenX? • Replacement chemical for PFOA • Perfluoroalkyl Ether Carboxylic Acid (PFECA) • Manufactured since 2009 • Byproduct of other manufacturing processes since ~1980 Scope of Problem – Surface water sourced public water • Hundreds of thousands public water customers affected by GenX and other PFAS in Cape Fear River Sun et al 2016 Timeline of Response to GenX in Drinking Water • June 2017 • August 2017 −News coverage brings GenX to −GenX detected in monitoring the forefront wells on-site −N.C. DHHS contacted by local • September 2017 health departments −Private well sampling near the −N.C. DHHS issues initial drinking facility begins water assessment −Chemours stops discharge of GenX to Cape Fear River • July 2017 −N.C. DHHS updates assessment and issues a provisional health goal of 140 ng/L (ppt) Scope of Problem – Groundwater sourced private wells • Hundreds of parcels with private wells near the facility potentially impacted by GenX and other PFAS • Phase 1 & 2 GenX results −Blue: ND −Green: 11-100 ng/L −Yellow: 101-140 ng/L −Orange: 141-420 ng/L −Red: >420 ng/L N.C. DEQ Scope of Problem – Groundwater sourced private wells • Sampling will continue until full extent of contamination is determined −Dark blue: phase 1 −Orange: phase 2 −Light blue/yellow: phase 3 −Fuchsia: phase 4 N.C.
    [Show full text]
  • Genx, Environmental Justice, and North Carolina's Legacy of Pollution
    GenX, Environmental Justice, and North Carolina’s Legacy of Pollution Christine Billings Nicholas Krebs Jatu F. Nugrohorukmi Cameron Smith Mackenzie Todd December 8, 2017 Department of Public and International Affairs Leutze Hall, University of North Carolina Wilmington Wilmington, NC 28403 GenX, Environmental Justice, and North Carolina’s Legacy of Pollution Final Project Fall Semester 2017 Prepared For Dr. Weinkle’s MCOP 595 Prepared By University of North Carolina at Wilmington Coastal and Ocean Policy Program The cover page pictures were provided by the EPA and StarNews Online. Maps throughout this paper were created using ArcGIS software by Esri. ArcGIS and ArcMap are the intellectual property of Esri and are used herein under license. Copyright © Esri. All Rights Reserved. For more information about Esri software, please visit www.esri.com. Acknowledgements The authors would like to thank Dr. Rob Hart of UNC Wilmington Department of History, Dr. Larry Cahoon of UNC Wilmington Department of Marine Biology, and Kemp Burdette of Cape Fear River Watch. i Table of Contents Acknowledgements ........................................................................................................................ i Introduction ................................................................................................................................... 1 Literature Review ......................................................................................................................... 4 Methods .........................................................................................................................................
    [Show full text]
  • Coastal Resilience Assessment of the Cape Fear Watershed
    PILOT: Coastal Resilience Assessment of the Cape Fear Watershed i IMPORTANT INFORMATION/DISCLAIMER: This report represents a Regional Coastal Resilience Assessment that can be used to identify places on the landscape for resilience-building efforts and conservation actions through understanding coastal flood threats, the exposure of populations and infrastructure have to those threats, and the presence of suitable fish and wildlife habitat. As with all remotely sensed or publicly available data, all features should be verified with a site visit, as the locations of suitable landscapes or areas containing flood hazards and community assets are approximate. The data, maps, and analysis provided should be used only as a screening-level resource to support management decisions. This report should be used strictly as a planning reference tool and not for permitting or other legal purposes. The scientific results and conclusions, as well as any views or opinions expressed herein, are those of the authors and should not be interpreted as representing the opinions or policies of the U.S. Government, or the National Fish and Wildlife Foundation’s partners. Mention of trade names or commercial products does not constitute their endorsement by the U.S. Government or the National Fish and Wildlife Foundation or its funding sources. NATIONAL OCEANIC AND ATMOSPHERIC ADMINISTRATION DISCLAIMER: The scientific results and conclusions, as well as any views or opinions expressed herein, are those of the author(s) and do not necessarily reflect those of NOAA or the Department of Commerce. U.S. ARMY CORPS OF ENGINEERS DISCLAIMER: NFWF’s assessment methodology focuses on identifying and ranking Resilience Hubs, or undeveloped areas of open space.
    [Show full text]