Analysis of Coastal Erosion on Martha's Vineyard, Massachusetts: a Paraglacial Island Denise M

Total Page:16

File Type:pdf, Size:1020Kb

Analysis of Coastal Erosion on Martha's Vineyard, Massachusetts: a Paraglacial Island Denise M University of Massachusetts Amherst ScholarWorks@UMass Amherst Masters Theses 1911 - February 2014 January 2008 Analysis of Coastal Erosion on Martha's Vineyard, Massachusetts: a Paraglacial Island Denise M. Brouillette-jacobson University of Massachusetts Amherst Follow this and additional works at: https://scholarworks.umass.edu/theses Brouillette-jacobson, Denise M., "Analysis of Coastal Erosion on Martha's Vineyard, Massachusetts: a aP raglacial Island" (2008). Masters Theses 1911 - February 2014. 176. Retrieved from https://scholarworks.umass.edu/theses/176 This thesis is brought to you for free and open access by ScholarWorks@UMass Amherst. It has been accepted for inclusion in Masters Theses 1911 - February 2014 by an authorized administrator of ScholarWorks@UMass Amherst. For more information, please contact [email protected]. ANALYSIS OF COASTAL EROSION ON MARTHA’S VINEYARD, MASSACHUSETTS: A PARAGLACIAL ISLAND A Thesis Presented by DENISE BROUILLETTE-JACOBSON Submitted to the Graduate School of the University of Massachusetts Amherst in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE September 2008 Natural Resources Conservation © Copyright by Denise Brouillette-Jacobson 2008 All Rights Reserved ANALYSIS OF COASTAL EROSION ON MARTHA’S VINEYARD, MASSACHUSETTS: A PARAGLACIAL ISLAND A Thesis Presented by DENISE BROUILLETTE-JACOBSON Approved as to style and content by: ____________________________________ John T. Finn, Chair ____________________________________ Robin Harrington, Member ____________________________________ John Gerber, Member __________________________________________ Paul Fisette, Department Head, Department of Natural Resources Conservation DEDICATION All I can think about as I write this dedication to my loved ones is the song by The Shirelles called “Dedicated to the One I Love.” Only in this case there is more than one love. First, I’d like to acknowledge a few good friends who have waited patiently for me to finish my thesis and without whose emotional support this work would have been difficult. They constantly rooted for me and kept me going. I am thankful to my family members, in particular to my brother, Butch, and his wonderful daughters, Brandy and Niki, for allowing me to be an absentee sister and aunt, yet they continued to offer words of encouragement throughout the years. In addition, I wish that my parents were here to see this moment because they always knew my persistence usually worked in my favor. They would have been proud to see their first family member receive a graduate degree. As a mother, you think of yourself as a role model for your children, but little did Seth, Michael, and Jaclyn know that they were my role models. Their faith in me inspired me to continue this thesis to completion. I raised them to never give up on something while they were in the middle of it and to finish what they started. Those words came back to me from my children more than I can count. My children were selfless on many, many occasions when I felt that I was needed, yet they imparted their own inner strengths and pushed me to continue my work, allowing me to keep my dream alive. I’d like to thank my dear daughter-in-law, Joyce, who was always there with her smiling face and constantly cheer me on. Now as new parents, Seth and Joyce have a son, Zachary, who I hope to inspire one day to become a steward of the environment. When I began my thesis, we had one fish (Fluffy), two birds (Mine and Yours), two cats (Percy and Cookie), and three dogs (Calvin, Lillie, and Lucy). As I finished my thesis, only one cat and three dogs remained. I want to acknowledge the pets that could not hang in for me to finish, but especially to our fluffy kitty, Percy, who died two months ago. He provided never-ending companionship while he sat on my lap as I did my research and wrote my thesis, keeping constant vigilance on my comings and goings. Next, to Calvin, Lillie, Lucy, and Cookie who followed me around every day as if we were in a parade. Even though I was quite boring, all of them were by my side, day in and day out, not asking for anything but an occasional pat or treat. They were the consummate friends. In spite of support from colleagues, friends, children, and pets, I would never have even started this thesis without the understanding and generosity from my loving husband, Allan. Besides being an established scientist, he was always inspirational, supportive, funny, an excellent cook, a fantastic editor and a true friend. Not only did he see the value of my work for my own personal growth, but he understands what this research means to the scientific community and to the people who will be affected by global sea level rise in the near future. I dedicate my thesis to Allan because he always believed in me and never let me down. ACKNOWLEDGMENTS This thesis could not have been completed without the help of numerous individuals who played crucial inspirational and supporting roles. My first inspiration came from Donna Williams during our years together as members of the League of Women Voters. Her passion and professionalism for protecting and enhancing the environment is a model which all of us should live by. Her husband, Ted Williams, an environmental writer who challenges all of us to think critically, was always on the other end of cyber space to offer words of encouragement and to provide an endless supply of jokes, when needed. When I went back to college in 2001, Dr. John Gerber was my sponsor, my professor, and an advocate for my education. He has continued his support by willingly accepting my request to become a member of my thesis committee. He has provided stability for me during my ups and downs at the University of Massachusetts. Dr. Robin Harrington was not only a member of my committee, but she became a friend and a mentor for me throughout my graduate school years. I will always be grateful to her for excellent lectures, her open door policy, and her warm hugs when either one of us needed one. She was truly an inspiration to me, particularly as a woman scientist. Last, but certainly not least, my thesis advisor, Dr. Jack Finn, took me on as his graduate student in 2005, without even a moment of hesitation on his part. Jack is a very humble person, but the wealth of knowledge he has about the oceans, coastal areas, ecology, spatial data modeling, and more specifically, mathematics, always astounded me. Between his knowledge, working style, views on life, sense of humor, and devotion to the vi sciences, I never wanted to finish. If it wasn’t for deadlines set by the University, I would still be working away. I am also indebted to several researchers and organizations for their investigative work and historical data collections. Data from “The Massachusetts Shoreline Change Projected,” led by Dr. Robert Thieler of the United States Geological Survey (USGS), was invaluable to me and established the underlying structure of my thesis. All this data was made readily available to me by the Massachusetts Office of Coastal Zone Management (MA CZM). The work of a USGS geologist, Robert N. Oldale, whose book I purchased in the mid-1990s (Cape Cod and the Islands, the Geologic Story) led me to become when of his favorite followers. The Office of Geographic and Environmental Information (MassGIS), the USGS, the National Oceanic and Atmospheric Administration (NOAA), the Permanent Service for Mean Sea Level (PSMSL) in the United Kingdom, the United States Department of Agriculture (USDA), and the Natural Resources Conservation Service (NRCS) all provided data relevant to my research. vii ABSTRACT ANALYSIS OF COASTAL EROSION ON MARTHA’S VINEYARD, MASSACHUSETTS: A PARAGLACIAL ISLAND SEPTEMBER 2008 DENISE BROUILLETTE-JACOBSON, B.A., UNIVERSITY OF MASSACHUSETTS AMHERST M.S., UNIVERSITY OF MASSACHUSETTS AMHERST Directed by: Professor John T. Finn As the sea rises in response to global climate changes, small islands will lose a significant portion of their land through ensuing erosion processes. The particular vulnerability of small island systems led me to choose Martha’s Vineyard (MV), a 248 km2 paraglacial island, 8 km off the south shore of Cape Cod, Massachusetts, as a model system with which to analyze the interrelated problems of sea level rise (SLR) and coastal erosion. Historical data documented ongoing SLR (~3mm/yr) in the vicinity of MV. Three study sites differing in geomorphological and climatological properties, on the island’s south (SS), northwest (NW), and northeastern (NE) coasts, were selected for further study. Mathematical models and spatial data analysis, as well as data on shoreline erosion from almost 1500 transects, were employed to evaluate the roles of geology, surficial geology, wetlands, land use, soils, percent of sand, slope, erodible land, wind, waves, and compass direction in the erosion processes at each site. These analyses indicated that: 1) the three sites manifested different rates of erosion and accretion, from a loss of approximately 0.1 m/yr at the NE and NW sites to over 1.7 m/yr at the SS site; 2) the NE and NW sites fit the ratio predicted by Bruun for the rate of erosion vs. SLR, viii but the SS site exceeded that ratio more than fivefold; 3) the shoreline erosion patterns for all three sites are dominated by short-range effects, not long-range stable effects; 4) geological components play key roles in erosion on MV, a possibility consistent with the island’s paraglacial nature; and 5) the south side of MV is the segment of the coastline that is particularly vulnerable to significant erosion over the next 100 years. These conclusions were not evident from simple statistical analyses.
Recommended publications
  • University Microfilms, Inc., Ann Arbor, Michigan GEOLOGY of the SCOTT GLACIER and WISCONSIN RANGE AREAS, CENTRAL TRANSANTARCTIC MOUNTAINS, ANTARCTICA
    This dissertation has been /»OOAOO m icrofilm ed exactly as received MINSHEW, Jr., Velon Haywood, 1939- GEOLOGY OF THE SCOTT GLACIER AND WISCONSIN RANGE AREAS, CENTRAL TRANSANTARCTIC MOUNTAINS, ANTARCTICA. The Ohio State University, Ph.D., 1967 Geology University Microfilms, Inc., Ann Arbor, Michigan GEOLOGY OF THE SCOTT GLACIER AND WISCONSIN RANGE AREAS, CENTRAL TRANSANTARCTIC MOUNTAINS, ANTARCTICA DISSERTATION Presented in Partial Fulfillment of the Requirements for the Degree Doctor of Philosophy in the Graduate School of The Ohio State University by Velon Haywood Minshew, Jr. B.S., M.S, The Ohio State University 1967 Approved by -Adviser Department of Geology ACKNOWLEDGMENTS This report covers two field seasons in the central Trans- antarctic Mountains, During this time, the Mt, Weaver field party consisted of: George Doumani, leader and paleontologist; Larry Lackey, field assistant; Courtney Skinner, field assistant. The Wisconsin Range party was composed of: Gunter Faure, leader and geochronologist; John Mercer, glacial geologist; John Murtaugh, igneous petrclogist; James Teller, field assistant; Courtney Skinner, field assistant; Harry Gair, visiting strati- grapher. The author served as a stratigrapher with both expedi­ tions . Various members of the staff of the Department of Geology, The Ohio State University, as well as some specialists from the outside were consulted in the laboratory studies for the pre­ paration of this report. Dr. George E. Moore supervised the petrographic work and critically reviewed the manuscript. Dr. J. M. Schopf examined the coal and plant fossils, and provided information concerning their age and environmental significance. Drs. Richard P. Goldthwait and Colin B. B. Bull spent time with the author discussing the late Paleozoic glacial deposits, and reviewed portions of the manuscript.
    [Show full text]
  • Directional Dependency and Coastal Framework Geology: Implications for Barrier Island Resilience
    Earth Surf. Dynam., 6, 1139–1153, 2018 https://doi.org/10.5194/esurf-6-1139-2018 © Author(s) 2018. This work is distributed under the Creative Commons Attribution 4.0 License. Directional dependency and coastal framework geology: implications for barrier island resilience Phillipe A. Wernette1,2,a, Chris Houser1, Bradley A. Weymer3, Mark E. Everett4, Michael P. Bishop2, and Bobby Reece4 1Department of Earth and Environmental Sciences, University of Windsor, Windsor, Ontario, N9B 3P4, Canada 2Department of Geography, Texas A&M University, College Station, Texas, 77843, USA 3GEOMAR Helmholtz Centre for Ocean Research Kiel, 24148 Kiel, Germany 4Department of Geology and Geophysics, Texas A&M University, College Station, Texas, 77843, USA anow at: Department of Earth and Environmental Sciences, University of Windsor, 401 Sunset Ave., Windsor, Ontario, N9B 3P4, Canada Correspondence: Phillipe A. Wernette ([email protected]) Received: 9 May 2018 – Discussion started: 15 June 2018 Revised: 18 October 2018 – Accepted: 6 November 2018 – Published: 27 November 2018 Abstract. Barrier island transgression is influenced by the alongshore variation in beach and dune morphol- ogy, which determines the amount of sediment moved landward through wash-over. While several studies have demonstrated how variations in dune morphology affect island response to storms, the reasons for that vari- ation and the implications for island management remain unclear. This paper builds on previous research by demonstrating that paleo-channels in the irregular framework geology can have a directional influence on along- shore beach and dune morphology. The influence of relict paleo-channels on beach and dune morphology on Padre Island National Seashore, Texas, was quantified by isolating the long-range dependence (LRD) parame- ter in autoregressive fractionally integrated moving average (ARFIMA) models, originally developed for stock market economic forecasting.
    [Show full text]
  • Introduction to Geological Process in Illinois Glacial
    INTRODUCTION TO GEOLOGICAL PROCESS IN ILLINOIS GLACIAL PROCESSES AND LANDSCAPES GLACIERS A glacier is a flowing mass of ice. This simple definition covers many possibilities. Glaciers are large, but they can range in size from continent covering (like that occupying Antarctica) to barely covering the head of a mountain valley (like those found in the Grand Tetons and Glacier National Park). No glaciers are found in Illinois; however, they had a profound effect shaping our landscape. More on glaciers: http://www.physicalgeography.net/fundamentals/10ad.html Formation and Movement of Glacial Ice When placed under the appropriate conditions of pressure and temperature, ice will flow. In a glacier, this occurs when the ice is at least 20-50 meters (60 to 150 feet) thick. The buildup results from the accumulation of snow over the course of many years and requires that at least some of each winter’s snowfall does not melt over the following summer. The portion of the glacier where there is a net accumulation of ice and snow from year to year is called the zone of accumulation. The normal rate of glacial movement is a few feet per day, although some glaciers can surge at tens of feet per day. The ice moves by flowing and basal slip. Flow occurs through “plastic deformation” in which the solid ice deforms without melting or breaking. Plastic deformation is much like the slow flow of Silly Putty and can only occur when the ice is under pressure from above. The accumulation of meltwater underneath the glacier can act as a lubricant which allows the ice to slide on its base.
    [Show full text]
  • The Perfect Planet Trailer
    Top Tips: 1. Read the questions carefully. 2. Use a highlighter or your pencil to underline the relevant information from the text. 3. Answer the questions in full sentences unless you need to copy individual words. The Perfect Planet Trailer This is a perfect planet. Life flourishes here thanks to powerful natural forces. Light from the sun reaches us in just eight minutes, powering our living world and its daily and yearly rhythms shape the lives of every creature on Earth. Volcanoes are powerful and uncontrollable forces, but they are the architects of the planet, creating over 80 of the Earth's surface. Life could not exist without them. Our oceans are in constant motion. They're linked by a network of powerful currents that carry nutrients around the globe. Every drop of sea water rides these currents taking a thousand years to complete a single circuit. And where there are currents there is life. From mighty storms to freezing winds, weather is vital to life. Rain clouds form and powerful winds carry this fresh water around the globe revitalizing the land. Annual weather patterns have been stable for thousands of years and it's this reliability on which life depends. Together these forces have shaped our perfect planet. But it's a fragile system. Today there is a new force one so powerful it threatens life on Earth. Human activity is now so dominant that it's disrupting the forces of nature and the vital habitats life needs to survive on Earth. To preserve our planet, we need to act now.
    [Show full text]
  • Free Land Attracted Many Colonists to Texas in 1840S 3-29-92 “No Quitting Sense” We Claim Is Typically Texas
    “Between the Creeks” Gwen Pettit This is a compilation of weekly newspaper columns on local history written by Gwen Pettit during 1986-1992 for the Allen Leader and the Allen American in Allen, Texas. Most of these articles were initially written and published, then run again later with changes and additions made. I compiled these articles from the Allen American on microfilm at the Allen Public Library and from the Allen Leader newspapers provided by Mike Williams. Then, I typed them into the computer and indexed them in 2006-07. Lois Curtis and then Rick Mann, Managing Editor of the Allen American gave permission for them to be reprinted on April 30, 2007, [email protected]. Please, contact me to obtain a free copy on a CD. I have given a copy of this to the Allen Public Library, the Harrington Library in Plano, the McKinney Library, the Allen Independent School District and the Lovejoy School District. Tom Keener of the Allen Heritage Guild has better copies of all these photographs and is currently working on an Allen history book. Keener offices at the Allen Public Library. Gwen was a longtime Allen resident with an avid interest in this area’s history. Some of her sources were: Pioneering in North Texas by Capt. Roy and Helen Hall, The History of Collin County by Stambaugh & Stambaugh, The Brown Papers by George Pearis Brown, The Peters Colony of Texas by Seymour V. Conner, Collin County census & tax records and verbal history from local long-time residents of the county. She does not document all of her sources.
    [Show full text]
  • The Light-Houses, Beacons, and Floating Lights, of the United
    £& @EC I TUE L I G H 'r -H O U S E S , BEACONS, .AND FLOATING LIGHTS, OF THE UNI'rED ST ATES, FOR 1838. PREPARED BY ORDER OF S TEPHEN PLEASONTON, FIFTH AUDITOR AND ACTING COMMISSIONER OF THE REVENUE, WASHINGTON : PRINTEa BY BLAlR AND RlVES. 1838. INDEX. l' No. Page. No. Page. V A. E. ssalea~ue Island . 145 8 Edgartown - 63 4 htabu a.Beacon . 172 10 Eaton's Neck 85 6 B. F. Baker's Island, ~aine) 16 2 Franklin Island - 4 2 Baker's island, ( ass.) - 32 2 Faulkner Island - 76 4 Boston - 30 2 Five Mil« Point - 80 6 Billingsgate Island 41 2 Fayerweather Island 82 6 Brown's Head - 21 2 Fire Island Inlet - 88 6 Burnt Island - 9 2 Fort Tompkins - 91 6 Boon Island - 26 2 Four Mile P oint 93 6 Bird Island . 59 4 Franks Island - 174 10 Block IR.land - 72 4 Fort Gratiot - - 192 12 Bu.ffalo - - 100 6 Federal Point . 147 8 Bombay Hook - 121 8 Fort P oint 25 2 Bodkin Island - 126 8 Back River Point. - 144 8 G. Bald Head . - 146 8 Be~s on Wolf's Island - 160 10 Goat Island, (Maine) . 23 2 Ba ou St. John's - • - 173 10 Gloucester P oint - - 44 4 Bois Blanc - - • - 195 12 Gayhead - - • 48 4 Barnegat Shoals - 115 6 Goat Island, (R. I.(: • 68 4 - Great Captains' Is and - 84 6 C. Grand River - - • . 163 10 Galloo Island . 103 6 Cape Elizabeth 17 2 Genesee - 105 6 Cape Cod • 34 2 Clark's Point 49 4 H.
    [Show full text]
  • Future of Public Service Media: Open University Response Summary
    Ofcom – Future of Public Service Media: Open University Response Summary 1. Education is a crucial part of the Public Service Broadcasting (PSB) requirements. Several of the statutory requirements set out in Section 264 of the Communications Act 2003 relate to educational objectives. There are opportunities to strengthen these requirements as part of the new Public Service Media (PSM) offer. 2. The Open University (OU) plays a key role in supporting the delivery of PSB requirements around education through its partnership with the BBC. The partnership co-produces high-quality factual content across several channels and platforms, which is developed in collaboration with academic experts and closely linked to related educational materials hosted by the OU. A key objective of the partnership is to encourage people to embark on learning journeys from the informal, factual content produced with the BBC, through online and printed educational resources which enhance and enrich their broadcast/digital experience, to taking up formal learning opportunites inspired by watching, listening to and engaging with the content produced as part of the partnership. 3. In 2019/20: • A total of 257 hours of content produced via the OU/BBC partnership was broadcast by the BBC. • This resulted in a combined total of 308 million viewing/listening “events” and digital engagement interactions. • The three most popular television programmes broadcast – A Perfect Planet, Springwatch and Hospital (Series 5) all saw viewing figures in excess of 22 million. • There were 765,000 unique visitors to the online educational content related to the OU/BBC partnership hosted on the OU’s free online learning platform, OpenLearn.
    [Show full text]
  • Massachusetts Estuaries Project
    Massachusetts Estuaries Project Linked Watershed-Embayment Model to Determine Critical Nitrogen Loading Threshold for the Menemsha-Squibnocket Pond Embayment System, Wampanoag Tribe, the Towns of Chilmark & Aquinnah, MA University of Massachusetts Dartmouth Massachusetts Department of School of Marine Science and Technology Environmental Protection DRAFT REPORT – JUNE 2017 Massachusetts Estuaries Project Linked Watershed-Embayment Model to Determine Critical Nitrogen Loading Threshold for the Menemsha-Squibnocket Pond Embayment System, Wampanoag Tribe, the Towns of Chilmark & Aquinnah, MA DRAFT REPORT – JUNE 2017 Brian Howes Roland Samimy David Schlezinger Ed Eichner Trey Ruthven John Ramsey Contributors: US Geological Survey Don Walters and John Masterson Applied Coastal Research and Engineering, Inc. Elizabeth Hunt and Sean Kelley Massachusetts Department of Environmental Protection Charles Costello and Brian Dudley (DEP project manager) SMAST Coastal Systems Program Jennifer Benson, Michael Bartlett, and Sara Sampieri Martha's Vineyard Commission Chris Seidel and Sheri Caseau ACKNOWLEDGMENTS The Massachusetts Estuaries Project Technical Team would like to acknowledge the contributions of the many individuals who have worked tirelessly for the restoration and protection of the critical coastal resources of the Menemsha-Squibnocket Pond Embayment and supported the application of the Linked Watershed-Embayment Model to Determine the Critical Nitrogen Loading Threshold for this estuarine system. Without these stewards and their efforts, this project would not have been possible. First and foremost we would like to recognize and applaud the significant time and effort in data collection and discussion spent by members of the Martha's Vineyard Commission. These individuals gave of their time to develop a consistent and sound baseline of nutrient related water quality for this system, without which the present analysis would not have been possible.
    [Show full text]
  • Glacial Morphology of the Cary Age Deposits in a Portion of Central Iowa John David Foster Iowa State University
    Iowa State University Capstones, Theses and Retrospective Theses and Dissertations Dissertations 1-1-1969 Glacial morphology of the Cary age deposits in a portion of central Iowa John David Foster Iowa State University Follow this and additional works at: https://lib.dr.iastate.edu/rtd Recommended Citation Foster, John David, "Glacial morphology of the Cary age deposits in a portion of central Iowa" (1969). Retrospective Theses and Dissertations. 17570. https://lib.dr.iastate.edu/rtd/17570 This Thesis is brought to you for free and open access by the Iowa State University Capstones, Theses and Dissertations at Iowa State University Digital Repository. It has been accepted for inclusion in Retrospective Theses and Dissertations by an authorized administrator of Iowa State University Digital Repository. For more information, please contact [email protected]. GLACIAL MORPHOLOGY OF THE CARY AGE DEPOSITS IN A PORTION OF CENTRAL IOWA by John David Foster A Thesis Submitted to the . • Graduate Faculty in Partial Fulfillment of The Requirements for the Degree of MASTER OF SCIENCE Major Subject: Geology Approved: Signatures have been redacted for privacy rs ity Ames, Iowa 1969 !/Y-J ii &EW TABLE OF CONTENTS Page ABSTRACT vii INTRODUCTION Location 2 Drainage 3 Geologic Description 3 Preglacial Topography 6 Pleistocene Stratigraphy 12 Acknowledgments . 16 GLACIAL GEOLOGY 18 General Description 18 Glacial Geology of the Study Area 18 Till Petrofabric Investigation 72 DISCUSSION 82 Introduction 82 Hypothetical Regime of the Cary Glacier 82 Review
    [Show full text]
  • Commonwealth of Massachusetts Energy Facilities Siting Board
    COMMONWEALTH OF MASSACHUSETTS ENERGY FACILITIES SITING BOARD ) Petition of Vineyard Wind LLC Pursuant to G.L. c. ) 164, § 69J for Approval to Construct, Operate, and ) Maintain Transmission Facilities in Massachusetts ) for the Delivery of Energy from an Offshore Wind ) EFSB 20-01 Energy Facility Located in Federal Waters to an ) NSTAR Electric (d/b/a Eversource Energy) ) Substation Located in the Town of Barnstable, ) Massachusetts. ) ) ) Petition of Vineyard Wind LLC Pursuant to G.L. c. ) 40A, § 3 for Exemptions from the Operation of the ) Zoning Ordinance of the Town of Barnstable for ) the Construction and Operation of New Transmission Facilities for the Delivery of Energy ) D.P.U. 20-56 from an Offshore Wind Energy Facility Located in ) Federal Waters to an NSTAR Electric (d/b/a. ) Eversource Energy) Substation Located in the ) Town of Barnstable, Massachusetts. ) ) ) Petition of Vineyard Wind LLC Pursuant to G.L. c. ) 164, § 72 for Approval to Construct, Operate, and ) Maintain Transmission Lines in Massachusetts for ) the Delivery of Energy from an Offshore Wind ) D.P.U 20-57 Energy Facility Located in Federal Waters to an ) NSTAR Electric (d/b/a Eversource Energy) ) Substation Located in the Town of Barnstable, ) Massachusetts. ) ) AFFIDAVIT OF AARON LANG I, Aaron Lang, Esq., do depose and state as follows: 1. I make this affidavit of my own personal knowledge. 2. I am an attorney at Foley Hoag LLP, counsel for Vineyard Wind LLC (“Vineyard Wind”) in this proceeding before the Energy Facilities Siting Board. 3. On September 16, 2020, the Presiding Officer issued a letter to Vineyard Wind containing translation, publication, posting, and service requirements for the Notice of Adjudication and Public Comment Hearing (“Notice”) and the Notice of Public Comment Hearing Please Read Document (“Please Read Document”) in the above-captioned proceeding.
    [Show full text]
  • Flora of the Carolinas, Virginia, and Georgia, Working Draft of 17 March 2004 -- ERICACEAE
    Flora of the Carolinas, Virginia, and Georgia, Working Draft of 17 March 2004 -- ERICACEAE ERICACEAE (Heath Family) A family of about 107 genera and 3400 species, primarily shrubs, small trees, and subshrubs, nearly cosmopolitan. The Ericaceae is very important in our area, with a great diversity of genera and species, many of them rather narrowly endemic. Our area is one of the north temperate centers of diversity for the Ericaceae. Along with Quercus and Pinus, various members of this family are dominant in much of our landscape. References: Kron et al. (2002); Wood (1961); Judd & Kron (1993); Kron & Chase (1993); Luteyn et al. (1996)=L; Dorr & Barrie (1993); Cullings & Hileman (1997). Main Key, for use with flowering or fruiting material 1 Plant an herb, subshrub, or sprawling shrub, not clonal by underground rhizomes (except Gaultheria procumbens and Epigaea repens), rarely more than 3 dm tall; plants mycotrophic or hemi-mycotrophic (except Epigaea, Gaultheria, and Arctostaphylos). 2 Plants without chlorophyll (fully mycotrophic); stems fleshy; leaves represented by bract-like scales, white or variously colored, but not green; pollen grains single; [subfamily Monotropoideae; section Monotropeae]. 3 Petals united; fruit nodding, a berry; flower and fruit several per stem . Monotropsis 3 Petals separate; fruit erect, a capsule; flower and fruit 1-several per stem. 4 Flowers few to many, racemose; stem pubescent, at least in the inflorescence; plant yellow, orange, or red when fresh, aging or drying dark brown ...............................................Hypopitys 4 Flower solitary; stem glabrous; plant white (rarely pink) when fresh, aging or drying black . Monotropa 2 Plants with chlorophyll (hemi-mycotrophic or autotrophic); stems woody; leaves present and well-developed, green; pollen grains in tetrads (single in Orthilia).
    [Show full text]
  • Part 629 – Glossary of Landform and Geologic Terms
    Title 430 – National Soil Survey Handbook Part 629 – Glossary of Landform and Geologic Terms Subpart A – General Information 629.0 Definition and Purpose This glossary provides the NCSS soil survey program, soil scientists, and natural resource specialists with landform, geologic, and related terms and their definitions to— (1) Improve soil landscape description with a standard, single source landform and geologic glossary. (2) Enhance geomorphic content and clarity of soil map unit descriptions by use of accurate, defined terms. (3) Establish consistent geomorphic term usage in soil science and the National Cooperative Soil Survey (NCSS). (4) Provide standard geomorphic definitions for databases and soil survey technical publications. (5) Train soil scientists and related professionals in soils as landscape and geomorphic entities. 629.1 Responsibilities This glossary serves as the official NCSS reference for landform, geologic, and related terms. The staff of the National Soil Survey Center, located in Lincoln, NE, is responsible for maintaining and updating this glossary. Soil Science Division staff and NCSS participants are encouraged to propose additions and changes to the glossary for use in pedon descriptions, soil map unit descriptions, and soil survey publications. The Glossary of Geology (GG, 2005) serves as a major source for many glossary terms. The American Geologic Institute (AGI) granted the USDA Natural Resources Conservation Service (formerly the Soil Conservation Service) permission (in letters dated September 11, 1985, and September 22, 1993) to use existing definitions. Sources of, and modifications to, original definitions are explained immediately below. 629.2 Definitions A. Reference Codes Sources from which definitions were taken, whole or in part, are identified by a code (e.g., GG) following each definition.
    [Show full text]