Singletracks #165 Winter 2021
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Stony Brook University
SSStttooonnnyyy BBBrrrooooookkk UUUnnniiivvveeerrrsssiiitttyyy The official electronic file of this thesis or dissertation is maintained by the University Libraries on behalf of The Graduate School at Stony Brook University. ©©© AAAllllll RRRiiiggghhhtttsss RRReeessseeerrrvvveeeddd bbbyyy AAAuuuttthhhooorrr... Exploratory Steatite Source Characterization in the Long Island Sound Watershed A Thesis Presented by Mark Stephenson Tweedie to The Graduate School in Partial Fulfillment of the Requirements for the Degree of Master of Arts in Anthropology (Archaeology) Stony Brook University December 2014 Stony Brook University The Graduate School Mark Stephenson Tweedie We, the thesis committee for the above candidate for the Master of Arts degree, hereby recommend acceptance of this thesis. John J. Shea, PhD. - Advisor Associate Professor, Anthropological Sciences E. Troy Rasbury, PhD. - Second Reader Associate Professor, Geosciences Nina M. Versaggi, PhD. - Outside Reader Associate Professor, Binghamton University This thesis is accepted by the Graduate School Charles Taber Dean of the Graduate School ii Abstract of the Thesis Exploratory Steatite Source Characterization in the Long Island Sound Watershed by Mark Stephenson Tweedie Master of Arts in Anthropology (Archaeology) Stony Brook University 2014 For as long as humans have incorporated stone into their material culture, they have used cooperative strategies (i.e., exchange networks) to mitigate the uneven distribution of available resources on the landscape. The procurement, transport, and selective distribution of lithic materials are thus uniquely human social institutions. One of the few ways to examine the limited evidence for this behavior in the archaeological record is through the geochemical characterization of artifacts and their potential source areas. Steatite cooking vessels recovered on the outer coastal plain of Long Island, New York, are unique in that their acquisition required water-borne transportation from quarries in Connecticut, Massachusetts, or Rhode Island. -
Preserve Cape Cod to Association
Association to Preserve Cape Cod Association to Preserve Cape Cod, Inc. 2011 Annual Report P.O. Box 398, 3010 Main Street Barnstable, MA 02630 Never Forgotten & Still Making a Difference Maggie Geist retired as executive director of the Association to Preserve Cape Cod in 2011. For a dozen years, Maggie steered our organization over many challenges and established her reputation as both a passionate environmentalist and a creative businesswoman. Capewind, county government reform, the Cape Cod Water Resources Restoration Project, the Upper Cape Water Supply Reserve on 15,000 acres of the Massachusetts Military Reservation, the No Discharge Area designation for Cape Cod Bay and, most of all, clean water were all positively impacted by her proactive style. She is still working with APCC developing a regional wastewater plan. Maggie led APCC and lives her life by the creed instilled upon her by her mom: “Leave the world a better place than you found it.” In her honor, the board of directors established the Geist Internship. The Geist Internship is intended to be a perpetual fund established to permit APCC to help train the next generation of environmental scientists, planners, engineers and creative thinkers. Each summer APCC will hire a promising college student to work on a project to help preserve Cape Cod. The fund is over one third the way toward being a self-perpetuating dedicated fund for this purpose. Member generosity, especially from current and past board members, made this possible. Programs & Projects Marine Invasive Species Monitoring: Over the past decade, many non-native marine plants and animals have arrived in coastal waters, often out- competing local species. -
Processes Influencing the Transport and Fate of Contaminated Sediments in the Coastal Ocean-Boston Harbor and Massachusetts
26 Section 4: Oceanographic Setting By Bradford Butman, Richard P. Signell, John C. Warner, and P. Soupy Alexander The ocean currents in Massachusetts Bay mix and time because of the complex bathymetry and coastal transport water and material in the bay, and exchange geometry, and because of the multiple processes (for water with the adjacent Gulf of Maine. The currents example wind, river runoff, and currents in the Gulf of can conceptually be separated into tidal currents (which Maine) that drive the flow and change seasonally. fluctuate 1–2 times each day), low-frequency currents The oceanography of Massachusetts Bay may caused by winds and river runoff (which typically be conceptually separated into four seasonal intervals fluctuate with a period of a few days), and a residual (following Geyer and others, 1992) based on the wind current (steady over a few weeks). Field observations and surface waves (fig. 4.1); the temperature and thermal (Butman, 1976; Geyer and others, 1992; Butman and stratification of the water column (fig. 4.2); the salinity, others, 2004a; Butman and others, 2006) and simulations salinity stratification, and horizontal salinity gradients of the currents by numerical hydrodynamic models (for caused by river discharge (fig. 4.3); and the density example Signell and others, 1996; Signell and others, 2000) provide descriptions of the flow pattern, strength, stratification, which results from the temperature and and variability of the currents. Field observations salinity distribution (fig. 4.4). From November through provide measurements of the currents at selected March (winter), the water column is vertically well- locations during specific periods of time, whereas model mixed, and the wind and surface waves are the largest of simulations provide a high-resolution view of the often the year. -
January 2012 #119
January 2012 #119 www.nemba.org SSingleingleTTrackS NEMBA, the New England Mountain Bike January 2012, Number 119 Association, is a non-profit 501 (c) (3) organi- zation dedicated to promoting trail access, maintaining trails open for mountain bicyclists, and educating mountain bicyclists to use these trails sensitively and responsibly. Cape Cod, Exit 7 SingleTracks is published six times a year by the Are your trails snowbound? Maybe it’s time for a New England Mountain Bike Association for road trip to Cape Cod. Willow Street, AKA, Exit 7 is the trail community. one of the best rides on the Cape. By Bill Boles. ©SingleTracks Editor & Publisher: Philip Keyes Contributing Writers: Bill Boles, Jeff Cutler, Thom Parsons 10 Cartoonist: Philippe Guillerm Copy Editor: Nanyee Keyes Executive Director: Philip Keyes [email protected] NEMBA 8 PO Box 2221 Acton MA 01720 Board of Directors Harold Green, President Adam Glick, Vice-President The Ultimate Road Trip Matt Schulde, Vice-President Anne Shepard, Treasurer Glenn and Paula’s excellent adventure took them on great sin- Tom Grimble, Secretary gletracks across the US of A, from Michigan to Park City. Read all about them! By Glenn Vernes and Paula Burton Rob Adair, White Mountains NEMBA Brian Alexander, CeMeNEMBA John Anders, Midcoast Maine NEMBA John Barley, White Mountains NEMBA Matt Bowser, Central NH NEMBA Eammon Carleton, BV NEMBA Matt Caron, Southern NH NEMBA SingleTracks Hey, get creative! We wel- Steve Cobble, SE MA NEMBA come submissions, photos and artwork. This is Leo Corrigan, RI NEMBA Peter DeSantis, Southern NH NEMBA your forum and your magazine. Be nice, and Adam Glick, Greater Boston NEMBA Paper Trail share! David Hughes, Carrabassett Region NEMBA On the Cover: Todd Swinton mountain biking Steve LaFlame, Central NH NEMBA Frank Lane, NS NEMBA Letters — 6 in the Fore River Sanctuary, Portland Maine. -
Boston Harbor South Watersheds 2004 Assessment Report
Boston Harbor South Watersheds 2004 Assessment Report June 30, 2004 Prepared for: Massachusetts Executive Office of Environmental Affairs Prepared by: Neponset River Watershed Association University of Massachusetts, Urban Harbors Institute Boston Harbor Association Fore River Watershed Association Weir River Watershed Association Contents How rapidly is open space being lost?.......................................................35 Introduction ix What % of the shoreline is publicly accessible?........................................35 References for Boston Inner Harbor Watershed........................................37 Common Assessment for All Watersheds 1 Does bacterial pollution limit fishing or recreation? ...................................1 Neponset River Watershed 41 Does nutrient pollution pose a threat to aquatic life? ..................................1 Does bacterial pollution limit fishing or recreational use? ......................46 Do dissolved oxygen levels support aquatic life?........................................5 Does nutrient pollution pose a threat to aquatic life or other uses?...........48 Are there other water quality problems? ....................................................6 Do dissolved oxygen (DO) levels support aquatic life? ..........................51 Do water supply or wastewater management impact instream flows?........7 Are there other indicators that limit use of the watershed? .....................53 Roughly what percentage of the watersheds is impervious? .....................8 Do water supply, -
Draft Report
IPSWICH BASIN WATER MANAGEMENT ACT PLANNING GRANT FY17 DRAFT REPORT 20173509.001A JUNE 19, 2017 This project has been financed partially with State Capital Funds from the Massachusetts Department of Environmental Protection (the Department) under a Sustainable Water Management Initiative Grant. The contents do not necessarily reflect the views and policies of the Department, nor does the mention of trade names or commercial products constitute endorsement or recommendation for use. TOWN OF DANVERS TOWN OF MIDDLETON TOWN OF HAMILTON LYNNFIELD CENTER WATER DISTRICT TOWN OF TOPSFIELD TOWN OF WENHAM WMA Grant Ipswich Basin Report © 2017 Kleinfelder THIS PAGE INTENTIONALLY BLANK WMA Grant Ipswich Basin Report © 2017 Kleinfelder A Report Prepared for: The Town of Danvers, MA In partnership with: Town of Middleton, MA Town of Hamilton, MA Lynnfield Center Water District Town of Topsfield, MA Town of Wenham, MA IPSWICH BASIN WATER MANAGEMENT ACT PLANNING GRANT FY17 DRAFT REPORT Prepared by: Kirsten N. Ryan, P.G.(NH) Project Manager; Principal Hydrogeologist Reviewed by: Elizabeth C. Frederick Principal Planner KLEINFELDER 215 First Street, Suite 320 Cambridge, MA 02142 Phone: 617.497.7800 Fax: 617.498.4630 June 19, 2017 20173509.001A WMA Grant Ipswich Basin Report Page i of v DRAFT June 19, 2017 © 2017 Kleinfelder ACKNOWLEDGEMENTS to be added WMA Grant Ipswich Basin Report Page ii of v DRAFT June 19, 2017 © 2017 Kleinfelder TABLE OF CONTENTS ____________________________________________________________________________ Section Page 0 EXECUTIVE -
A. Geology, Soils and Topography Geology and Topography Glacial Deposits Formed the Shape of Cape Cod
Section IV: Environmental Inventory and Analysis A. Geology, Soils and Topography Geology and Topography Glacial deposits formed the shape of Cape Cod. Approximately 25,000 years ago the Canadian Ice Sheet reached its southernmost point at Martha’s Vineyard and Nantucket. Three lobes of ice covered Cape Cod: the Cape Cod Bay Lobe, the South Channel Lobe, and the Buzzards Bay Lobe. About 15,500 years ago the sheets of ice began retreating, depositing rock debris, known as drift, as they receded. Drift ranges from till, an unstratified mixture of fine to coarse material, to deposits sorted by the flow of water and spread across the landscape. The drift deposited by the ice created the major landscape forms found in Falmouth and the Cape: moraines, outwash plains, kames (knobs), and kettle holes. Moraines are terminal ridges that represent the edge of a glacier. As the glacier retreated, drift was churned up and deposited in a ridge. The Buzzards Bay Moraine runs northeast from the Elizabeth Islands through Woods Hole to Sandwich. Outwash plains slope gradually away Map 4-1: Geologic Map of Cape Cod from the Buzzards Bay Moraine to the sea (Figure 4- 1). They are formed by sand Lake deposits and gravel deposits left by water streaming out of the Younger ice-contact deposits melting glacial lobes. Kames and kettles are known as ice Younger outwash deposits contact features. Kames are knobs of drift deposits left by Moraine deposits debris once embedded in ice. Kettles are holes in the ground Older outwash deposits formed by large ice blocks. -
Existing Connections
INTRODUCTION HUMAN CONNECTIONS NATURAL CONNECTIONS Chapter 3: Existing Connections Human landscape features like roads, rails, trails, and sidewalks create human connections. Natural landscape features like waterways, forests, and meadows create connections for the animals, birds, and fish living in our shared world. Roads Roadsides Public Transit Page 26 Page 28 Page 30 Bikeways Sidewalks Natural Connections Page 32 Page 34 Page 36 SOUTH SHORE GREENWAY PROJECT CONWAY SCHOOL OF LANDSCAPE DESIGN, WINTER 2008 23 Road Ecology Roads Roads Affect Ecological and Human Health The nearly five million-mile American road network slices The South Shore is rich in roads. Nearly 600 miles of roads across the land, moving humans, food, and goods, but connect people and places in the 136-square mile South Roads have important implications for human and fragmenting the landscape and disrupting natural processes. Shore study area. Road density (~8 miles of road/square ecological health on the South Shore. With roads comes mile) is twice as high as the state average (4 miles/square traffic and the air, water, and noise pollution it produces. Take a walk along a busy highway if you dare. If you can mile). Of the five towns Hull has the highest road density Studies have shown that humans living near major roadways ignore the noisy roar, stinking exhaust, and hot air blasts (23 miles/square mile) and Norwell the lowest (6 miles/ are at increased risk for death from heart and lung disease. from the rushing traffic, you may notice that almost nothing square mile). grows or lives along the edge of the road. -
Massachusetts
Geology and Ground-Water Conditions in the Wilmington-Reading Are? Massachusetts By JOHN A. BAKER, HENRY G. HEALY, and O. M. HACKETT GEOLOGICAL SURVEY WAT E R-S U P.PLY PAPER 1694 Prepared in cooperation with the Commonwealth of Massachusetts, Department of Public ff^orks UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1964 IOT mIOR ^Ucrtlon appears after the The CONTENTS Page Abstract-...________.-_---_----_-_________________________-______-_ 1 Introduction._____________________________________________________ 2 Location and description of the area____-__-i________-___________ 2 Purpose and scope of the report.________________________________ 3 Acknowledgments.__-----_-___-________-___--___-_---____----_ 4 Previous investigations._-_-_--_______________-___-_----____-___ 5 Methods of investigation_______________________________________ 5 General features of the area.________________________________________ 6 Climate_ ________--_-__---_-_________-___-________-_-__-____-_ 6 Topography and drainage______________________________________ 8 Soils and land cover.__________________________________________ 9 Summary of general hydrology and water supply ______________________ 10 Geologic units and the occurrence of ground water_____________________ 13 Bedrock._____________________________________________________ 15 Tin consolidated deposits. -__-_-_____-__--____-_____._______----_ 21 Till-__-_-___-_--------_---______-----_----_-__----------_ 23 Ice-contact deposits..._____________________________________ 26 Outwash.________________________________________________ -
Franklin County by Foot and Paddle Doug Dunlap
Franklin County by Foot and Paddle Doug Dunlap Progress Report September 15, 2020 For walks and hikes; and travel by kayak and canoe, August 31-September 15, 2020 Discoveries: The United Way and the 2-1-1 phone number, Six Months into the Pandemic Over the past two weeks I have learned much about 2-1-1, a major, indispensable service to people of Franklin County, and throughout Maine, led by the United Way. The United Way of the Tri-Valley continues to serve as a vital safety net for Franklin County residents. The 2-1-1 project is an indispensable service. This is a 24/7 service, staffed by call specialists who take calls from people seeking help of many kinds: food, clothing, shelter, heat; access to mental health services, help with caring for a sick or incapacitated family member, financial burdens of many kinds. United Ways throughout Maine fund this service, in cooperation with the State of Maine. There is always someone to take the call, always available to help guide the calling person to someone who may speak to the very specific need expressed. 2-1-1 was available prior to the COVID-19 pandemic, and widely used by thousands of callers each year. I am informed by United Way leadership that in 2020, Maine 2-1- 1 has received 36,000 pandemic related calls since the month of March. That amounts to 6000 calls per month for six months, an average of 200 calls per day. That is an astonishing figure. It costs money to provide the service. -
Alpine Soils on Mount Mansfield, Vermont
Alpine Soils on Mount Mansfi eld, Vermont, USA: Pedology, History, and Intraregional Comparison Jeffrey S. Munroe* The highest summits in the northeastern United States rise above the tree line and support Geology Dep. unique islands of alpine tundra. Little is known about the properties and history of these soils Middlebury College and it is unclear how soils compare between the separate, isolated alpine areas. As a step toward Middlebury, VT 05753 addressing this oversight, the physical and chemical properties of alpine soils were investigated on Mt. Mansfi eld, the highest mountain in Vermont. Soil thickness was determined through probing, while profi le development and horizon properties were investigated in 31 excava- tions. Soil covers ∼85% of the study area, with profi les averaging 18 cm thick (maximum of 58 cm). Most profi les demonstrate a variation on the sequence Oi, Oa and/or A, Bw or Bs (rare), AC, and Cr horizons. The Oa horizons contain signifi cantly more C, Ca, K, and Mg than A horizons, and have higher cation exchange capacity and base saturation, and lower pH values. Almost one-third of the profi les were classifi ed as Histosols, while nearly twice as many were classifi ed as Entisols. Only two profi les contained cambic horizons and were classifi ed as Inceptisols. Histosols contained signifi cantly more K and organic matter than Entisols. A buried Sphagnum layer, radiocarbon dated to approximately 1000 yr ago, suggests a wetter climate at that time. Mount Mansfi eld soils are generally thinner than those described from nearby alpine environments and contain more organic matter with higher C/N ratios. -
Outdoor Recreation Recreation Outdoor Massachusetts the Wildlife
Photos by MassWildlife by Photos Photo © Kindra Clineff massvacation.com mass.gov/massgrown Office of Fishing & Boating Access * = Access to coastal waters A = General Access: Boats and trailer parking B = Fisherman Access: Smaller boats and trailers C = Cartop Access: Small boats, canoes, kayaks D = River Access: Canoes and kayaks Other Massachusetts Outdoor Information Outdoor Massachusetts Other E = Sportfishing Pier: Barrier free fishing area F = Shorefishing Area: Onshore fishing access mass.gov/eea/agencies/dfg/fba/ Western Massachusetts boundaries and access points. mass.gov/dfw/pond-maps points. access and boundaries BOAT ACCESS SITE TOWN SITE ACCESS then head outdoors with your friends and family! and friends your with outdoors head then publicly accessible ponds providing approximate depths, depths, approximate providing ponds accessible publicly ID# TYPE Conservation & Recreation websites. Make a plan and and plan a Make websites. Recreation & Conservation Ashmere Lake Hinsdale 202 B Pond Maps – Suitable for printing, this is a list of maps to to maps of list a is this printing, for Suitable – Maps Pond Benedict Pond Monterey 15 B Department of Fish & Game and the Department of of Department the and Game & Fish of Department Big Pond Otis 125 B properties and recreational activities, visit the the visit activities, recreational and properties customize and print maps. mass.gov/dfw/wildlife-lands maps. print and customize Center Pond Becket 147 C For interactive maps and information on other other on information and maps interactive For Cheshire Lake Cheshire 210 B displays all MassWildlife properties and allows you to to you allows and properties MassWildlife all displays Cheshire Lake-Farnams Causeway Cheshire 273 F Wildlife Lands Maps – The MassWildlife Lands Viewer Viewer Lands MassWildlife The – Maps Lands Wildlife Cranberry Pond West Stockbridge 233 C Commonwealth’s properties and recreation activities.