Archaeological and Historic Resources He Mohawk Trail Area Is Steeped in Regional and Local His Tory

Total Page:16

File Type:pdf, Size:1020Kb

Archaeological and Historic Resources He Mohawk Trail Area Is Steeped in Regional and Local His Tory CHAPTER 5 Archaeological and Historic Resources he Mohawk Trail area is steeped in regional and local his tory. Native Americans occupied the area since the re treat of the last glacial ice sheets approximately 12,000 years ago. The Mohawk Trail Scenic Byway follows the Teast-west route used for approximately 10,000 to 12,000 years by the Native Americans to hunt, trade, and conduct war campaigns between the Hudson River and Connecticut River Valleys. In subsequent years, the European settlers used the trail for the same purposes, and eventu- ally upgraded it to support the use of horse and cart. As the automo- bile increased in popularity the road was improved to better serve its use. The existing road, though officially opened as a modern highway in 1914, has only been maintained as a year round highway since the State assumed winter upkeep in the mid 1930’s. Prior to that time the road was shoveled by hand and often remained closed for long periods of time during inclement weather. The history of the Mohawk Trail Scenic Byway region is a signifi- cant component of the corridor management plan. The region’s his- tory plays an important role in understanding the unique resources of the area and preserving these assets for future residents and visitors. This chapter of the report provides insight into the development of the area prior to, during and after the construction of the Byway. This in- formation is intended to help to tell the story of the Byway. The residents of the area during the Archaeological Paleo-Indian Period were hunters of Resources larger game such as caribou, using weap- ons mounted with a fluted spearpoint. Native American Only a few artifacts of this era have been found due to the wide distribution of Use of Area people. There are only four known sites Post-glacial effects, which produced the for this period in Western Massachu- agriculturally productive floodplain areas setts. The closest one to the Byway is of the Connecticut and Hudson River located in Deerfield. Most of the early Valleys, are also responsible for the more sites are located in lowland regions along spartan or severe conditions of the up- rivers and floodplains where food lands that lie between them. Beginning sources were close at hand. Evidence of approximately 12,000 years ago the ice the upland sites from this period are few retreated, leaving immediately behind it a due to the more limited resources of the vista reminiscent of today’s tundra condi- areas at this time; however, travel tions, including low shrubs. The result through the area was probable. was an area utilized by widely distributed, More productive soils evolved natu- thinly dispersed, and highly mobile rally, and allowed for an increase in the groups of hunter/gatherers. This period is number and diversity of the flora and classified as Paleo-Indian and lasted from fauna of the region. From the dominant, 12,000 to around 9,000 years ago. boreal type forest with little diversity, the 64 MOHAWK TRAIL SCENIC BYWAY landscape gradually took the shape of a period, is seen more toward the end of the more mature temperate forest with an in- Late Archaic and is also considered to creasing preponderance of nut producing predominate the other two. With its in- trees including oak, chestnut, and beech, troduction, the beginnings of a horticul- providing food for many species of wild- tural society emerge. All three cultures life including deer, bear, squirrels, etc. The are found in the region, however the more diverse herbaceous level increased Susquehanna was very common in the the foraging prospects for both animals Mahican-Mohawk Trail area. and humans. These changes initiated the Many prehistoric sites have been expansion of foraging societies into the documented along the Byway, though upland areas. The number of prehistoric not all have complete information. Ar- sites increased proportionately in re- tifacts for several of the sites have been sponse to the greater availability of food lost and/or the period of occupation is resources. not known. In order to protect the The period from 9,000 to 7,000 years sites, only general descriptions and lo- ago, the Early Archaic, is typified by a cations are included in this report. dramatic increase in the production of There are four prehistoric sites located nut bearing trees, with oak production in Shelburne. One of the sites has been tripling to about 30 percent over the dated to the Early Woodland period, previous period. The larger rivers sup- around 2,500 years ago. This site pro- ported a variety of fish and other duced several quartzite flakes (used to aquatic species that were important make other tools) and 1 quartzite core food sources, particularly shad, which from which flakes had been struck. predictably ascend the river each spring. Also recovered from this site were 11 The Middle Archaic lasted from about grit-tempered potsherds (pottery frag- 7,000 to 5,000 years ago, with the area ments) and 5 fire-cracked rocks, indi- following the general trend found in cating a prolonged habitation during Southern New England as to the num- this period. Another site, located in a ber of prehistoric sites found. rock-shelter, produced both quartzite The most sites have been found from and quartz flakes. Two other sites do the Late Archaic period of 6,000 to 3,000 not have the artifacts recorded years ago. The number of artifact styles (Mulholland). associated with this period increases and There are seven sites in Charlemont, is complicated by the fact that there were including one that served as a second- three distinct cultural traditions present ary, stone-tool production and mainte- (Laurentian, Small Stem, and Susque– nance site. Artifacts found at this site hanna) during that time. The types of ar- include 3 each of siltstone and quartzite tifacts differentiate these cultural flakes, and one each of chalcedony and traditions as well as the socio-cultural tra- quartz flakes, as well as 10 fire-cracked ditions. It is thought that the Laurentian rocks. Another site produced a projec- cultural traditions may represent a spe- tile point but no style was recorded. cialized adaptation by small, mobile bands Four other sites are documented with to exploit the interior resources without artifacts not reported or lost. The last semiannual relocations for food sources. site is “The Mohawk Trail”, placed on The Small Stem cultural traditions, which the National Register of Historic Places may have been handed down from the in 1972. It is a significant trail noted as a Middle Archaic, most likely exploited re- pathway connecting the Hudson and sources on a more seasonal basis by sum- Connecticut River Valleys. mering near the coast and wintering in Crossing into the Berkshire Segment the interior. The Susquehanna cultural in Florida, three more sites are cata- tradition, also considered a transitional logued. While the date of occupation for CHAPTER 5: Archaeological and Historic Resources 65 these sites is not known, the artifacts communities along the Byway, and from one of the sites are stored at a identifies important locations and nearby museum. Another of the sites has properties within these towns. Tables already been destroyed. North Adams with the significant historic areas and contains another three sites, the first lo- properties in each town are included in cated near the ‘hairpin’ turn (actually in the appendices. Clarksburg). No date of occupation is Properties listed in this chapter and given for this site, however four projectile the appendix will be designated ac- points were discovered. Another site, cording to the definitions in the State near the location of Fort Massachusetts, Register of Historic Places 2001, was determined to be occupied some which are defined as follows: 3,000 years ago. Artifacts included a NRIND: National Register of Individual Wayland Notch projectile point. The last Property site is actually south of Blackinton and NRDIS: National Register District produced one vein quartz flake. The date NRMRA: National Register Multiple of the occupation is unknown. Resource Area (Refers to a community- There are four sites located in the wide or area-wide designation that in- town of Williamstown. One site reports cludes nomination of both individual artifacts found as “many indian relics”. and district properties.) Another site produced several flakes of grey chert, the residue of stone tool making. No date of occupation is known for either site. The other two sites both Franklin County produced Susquehanna Broad projectile points made from chert and both are Greenfield dated to around 3,500 years ago. The Mohawk Trail Scenic Byway be- These prehistoric sites along the By- gins or ends, depending on travel di- way, represent a significant historical rection, at the rotary located at the segment. Many of the known sites have intersections of Route 2, Route 2A not yet been fully examined; therefore and Interstate 91 in Greenfield. His- the possibility remains for more exten- torically, the town of Greenfield has sive results. Also, as the Byway was the played an important role as a regional connecting crossroad for several differ- economic center due to its location at ent cultures, further exploration may the junction between Northampton provide additional information concern- and Vermont, the Berkshires and Bos- ing their interactions. This is a significant ton. This role has meant that the part of the history of the Byway. It in- events of Greenfield’s history are cludes more than 10,000 years, and strongly reflective of the development should be protected as such. occurring throughout the Byway. Be- cause the early history of Greenfield History of the Communities reflects the Mohawk Trail’s history it is along the Scenic Byway: important to understand this history.
Recommended publications
  • DEERFIELD RIVER WATERSHED Assessment Report
    DEERFIELD RIVER WATERSHED Assessment Report 2004-2008 Downstream of Fife Brook Dam The Commonwealth of Massachusetts Executive Office of Environmental Affairs The Commonwealth of Massachusetts Executive Office of Environmental Affairs 251 Causeway Street, Suite 900 Boston, MA 02114-2119 Mitt Romney GOVERNOR Kerry Healey LIEUTENANT GOVERNOR Tel: (617) 626-1000 Fax: (617) 626-1181 Ellen Roy Herzfelder or (617) 626-1180 SECRETARY http://www.state.ma.us/envir November 19, 2004 Dear Friends of the Deerfield River Watershed: It is with great pleasure that I present you with the Assessment Report for the Deerfield River Watershed. The report helped formulate the 5-year watershed action plan that will guide local and state environmental efforts within the Deerfield River Watershed over the next five years. The report expresses some of the overall goals of the Executive Office of Environmental Affairs, such as improving water quality, restoring natural flows to rivers, protecting and restoring biodiversity and habitats, improving public access and balanced resource use, improving local capacity, and promoting a shared responsibility for watershed protection and management. The Deerfield River Watershed Assessment Report was developed with input from the Deerfield River Watershed Team and multiple stakeholders including watershed groups, state and federal agencies, Regional Planning Agencies and, of course, the general public from across the Watershed. We appreciate the opportunity to engage such a wide group of expertise and experience as it allows the state to focus on the issues and challenges that might otherwise not be easily characterized. From your input we have identified the following priority issues: • Water Quantity • Water Quality • Fish Communities • Wildlife and Terrestrial Habitat • Open Space • Recreation I commend everyone involved in this endeavor.
    [Show full text]
  • Native Americans Ol'
    Native Americans ol' Clarendon, Vermont *This is only a report of my early findings. This is subject to charge as new evidence and facts arise. I\rly research has led me to cliscover two groups of Native Americiurs that could have resided in Clarendon and one other that may have simply passed through time to time. The tribe of Native l[mericans that has the highest likelihood of being in Clarendon isi the Mahican, specifically the subdivision Mahican proper. Their territory extended from Poughkeepsie, New York to Deerfield, I\4assachusetts, and extended flrttrest north in Rutland. It is important to mention that tlhey are not to be mistaken with the Mohegan tribes of Connecticut; however, they do have lineage witkr one another. As a side note, the Mahicans have lineage with the Lenape and ['equot. Other names for the Mahicans is as follows: Akochakanen (koquois name that means "Those who,speak a strangertongue"), Canoe Indians (Given by colonists), Hikanagi/Nhilcana (Given by the Shawnee), Laups (Given by the French), Orunges (,Given by a school textbook author, Chauvignerie, who rvas referring to a specific Mahican tribe in 1736), River Indians (Given by the Dutch), and Uragees (Again given by an author, Colden, in reference to a specific tribe of the.Mahicans 1747). Mahicans were hunters of southwestem and western Vermont. lheir langrllge belonged to the linguistic family of the Algonquian, spoken with an r-dialect. Sieldom did they settle anywhere in Vermont to stay due to the fact that they were typically hLunters, hotvever, it is not irnprobable that they had permanent selllements in Clarendon.r Historic territory of the |tdahicans l Swanton, John R., The lndion Tribes of North America,1953 pg.
    [Show full text]
  • 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.
    [Show full text]
  • Town of Shrewsbury, Vermont Local Hazard Mitigation Plan
    Town of Shrewsbury, Vermont Local Hazard Mitigation Plan Date of Adoption Prepared by the Town of Shrewsbury With the assistance of The Rutland Regional Planning Commission Table of Contents 1. Introduction……………………………………………………………………………………..……...2 2. Purpose……………………………………………………………………………………………..…..3 3. Community Background……………………………………………………………………………….3 4. Planning Process…………………..……………………………………………………………….…..6 4.1. Plan Changes……………………………………………………………………………………...7 5. Community Hazard Inventory and Risk Assessment…………………………………………………10 5.1. Low Risk Hazards………………………………………………………………………………..11 Aircraft Crashes……………………………………………………………………………….….11 Continuity of Government/Record Retention…………………………………………………….11 Hazardous Materials, Radiological and Chemical/Biological Incidents…………………………11 Drought…………………………………………………………………………………………...12 Earthquakes……………………………………………………………………………………….12 Structure Fires…………………………………………………………………………………….13 Temperature Extremes…………………………………………………………………………....13 Terrorism………………………………………………………………………………………….13 Water Supply Contamination………………………………………………………………….....13 Winter Storms, Ice Storms, and Power Outages………………………………………………....14 Wildfires and Forest Fires………………………………………………………………………..14 5.2. Medium Risk Hazards…………………………………………………………………………...14 Climate Change………………………………………………………………………………….14 Dam Failure……………………………………………………………………………………...14 5.3. High Risk Hazards……………………………………………………………………………….15 Floods, Fluvial Erosion, and Ice Jams…………………………………………………………...15 Highway and Railroad Accidents………………………………………………………………..17
    [Show full text]
  • Tall Pines Trail
    Tall Pines Trail Location: Mohawk Trail State Forest. Updated 7-29-2019 County: Franklin Township: Charlemont Start and End of Trail Network: Lat 42.638425 N, Long 72.936285 W Trail length (complete loop plus spur): 3.0 miles Introduction Mohawk Trail State Forest (MTSF) was one of the first state forests to be established as part of the Massachusetts system of Forests and Parks. Today the property covers approximately 6,700 acres and is split by State Route #2, named the Mohawk Trail in recognition of the ancient Indian path that ran from the waters of the Hudson to the Connecticut River. MTSF is mountainous, possessing some of the most rugged topography in the Commonwealth. The Cold River and Deerfield River gorges reach depths of 1,000 feet in Mohawk, and elevations vary from 600 to almost 2100 feet within the property. Mohawk has many outstanding features, including: (1) its wealth of old growth forests (nearly half of the total for Massachusetts), (2) record-breaking tall, second-growth white pines, (3) a section of the original Mohawk Indian Trail, (4) section of the old Shunpike, (5) site of an old Indian encampment, and (6) the gravesite of Revolutionary War veteran John and his wife Susannah Wheeler. The State Forest is part of the 9th Forest Reserve, which is maintained in pristine condition. The Park area is located on the north side of Route #2, and includes the Headquarters, picnic area, campground (for RVs and tents), cabin area (six rental cabins), the Old Cold River Road, and the upper and lower meadows.
    [Show full text]
  • The Mohawk Trail Region the Official Visitors Mohawk Guide 2018 - 2019 Trail Region Eugene Michalenko Tourist Information
    The Mohawk Trail REGION The Official Visitors Mohawk Guide 2018 - 2019 Trail www.mohawktrail.com REGION Explore The Trail Region 4-6 Ride off the beaten path ....33 Historic and literary figures Savoy .............................33 travelled The Trail ............7 Rowe ..............................33 Traffic on The Trail Annual Events for millenniums ................7 along The Trail ..........34-35 Tourist Information ... 8-10 map of the Ice Cream along The Trail ...11 mohawk trail find a place to region ...............36-37 enjoy yourself Charlemont ...................38 in the mohawk Shelburne Falls .............43 trail region Colrain ...........................46 The Arts & Culture .........12 Shelburne ......................46 Places to Eat & Drink .12-13 Greenfield .....................48 Places to Stay ..................13 Cultural Districts ..............49 Places to Shop .................14 Deerfield .......................49 Services ...........................15 South Deerfield .............51 www.mohawk trail.com How to Get Here .............15 Turners Falls .................51 Distances from Bernardston ..................52 BIENVENIDO | BIENVENUE North Adams to ? ...........15 Northfield .....................54 Camping, State Parks & Gill .................................54 WILLKOMMEN | BENVENUTO Outdoor Recreation .......16 Athol .............................55 欢迎 Sights to See .................17 Phillipston ....................55 ようこそ | cities & towns Westminster .................55 in the trail Farmers’ Markets ...56-57
    [Show full text]
  • Progress Report on River Basin Water Quality Management Planning During 2010
    PROGRESS REPORT ON RIVER BASIN WATER QUALITY MANAGEMENT PLANNING DURING 2010 A REPORT FOR: HOUSE & SENATE COMMITTEE ON AGRICULTURE HOUSE & SENATE COMMITTEE ON NATURAL RESOURCES AND ENERGY JANUARY 2011 PREPARED BY: VERMONT AGENCY OF NATURAL RESOURCES DEPARTMENT OF ENVIRONMENTAL CONSERVATION WATER QUALITY DIVISION 103 SOUTH MAIN STREET WATERBURY, VT 05671 www.vtwaterquality.org Introduction..........................................................................................................................................................3 Section 1) Statewide Surface Water Management Strategy - a Framework for Statewide Efforts to Guide Surface Water Management.................................................................................................................................5 Protecting & Improving Surface Waters by Managing Stressors ....................................................................5 What are the 10 Major Stressors affecting Vermont’s surface waters? ...........................................................6 Using the Stressor Approach to Evaluate Program Effectiveness ...................................................................6 Tactical Basin Planning: Managing waters along a gradient of condition.......................................................6 WQD Ambient Surface Water Monitoring & Assessment Strategy................................................................6 Public Input......................................................................................................................................................6
    [Show full text]
  • Stol. 12 NO. 2
    •‘j \ " - y E ^ tf -jj ^ ^ p j | %A .~.,.. ,.<•;: ,.0v -^~., v:-,’-' ' •'... : .......... ■l:"'-"4.< «S ife.,.. .1 { ‘. , ‘ 'M* m m m m m m m ...y m ;y StoL.W 12 NO. 2 V"-' . :.... .,.■... '..'/.'iff? ' ' kC'"^ ' BIRD OBSERVER OF EASTERN MASSACHUSETTS APRIL 1984 VOL. 12 NO. 2 President Editorial Board Robert H. Stymeist H. Christian Floyd Treasurer Harriet Hoffman Theodore H. Atkinson Wayne R. Petersen Editor Leif J. Robinson Dorothy R. Arvidson Bruce A. Sorrie Martha Vaughan Production Manager Soheil Zendeh Janet L. Heywood Production Subscription Manager James Bird David E. Lange Denise Braunhardt Records Committee Herman H. D’Entremont Ruth P. Emery, Statistician Barbara Phillips Richard A. Forster, Consultant Shirley Young George W. Gove Field Studies Committee Robert H. Stymeist John W. Andrews, Chairman Lee E. Taylor Bird Observer of Eastern Massachusetts (USPS 369-850) A bi-monthly publication Volume 12, No. 2 March-April 1984 $8.50 per calendar year, January - December Articles, photographs, letters-to-the-editor and short field notes are welcomed. All material submitted will be reviewed by the editorial board. Correspondence should be sent to: Bird Observer > 462 Trapelo Road POSTMASTER: Send address changes to: Belmont, MA 02178 All field records for any given month should be sent promptly and not later than the eighth of the following month to Ruth Emery, 225 Belmont Street, Wollaston, MA 02170. Second class postage is paid at Boston, MA. ALL RIGHTS RESERVED. Subscription to BIRD OBSERVER is based on a calendar year, from January to December, at $8.50 per year. Back issues are available at $7.50 per year or $1.50 per issue.
    [Show full text]
  • Hoosac Stores 1 & 2 / Hoosac Stores 3
    Form No. 10-306 (Rev. 10-74) UNITED STATtS DEPARTMENT OF THH INTERIOR NATIONAL PARK SERVICE NATIONAL REGISTER OF HISTORIC PLACES INVENTORY - NOMINATION FORM 14 FOR FEDERAL PROPERTIES SEE INSTRUCTIONS IN HOWTO COMPLETE NATIONAL REGISTER FORMS ____________TYPE ALL ENTRIES - COMPLETE APPLICABLE SECTIONS______ | NAME HISTORIC Hoosac Stores 1 & 2; Hoosac Stores 3 AND/OR COMMON same [LOCATION STREETS, NUMBER 25 (3) and 115 (1 & 2) Water Street (Constitution Road) and Railroad Right-of-way between them. _NOT FOR PUBLICATION CITY. TOWN CONGRESSIONAL DISTRICT L^StOWn $LA VICINITY OF 8th STATE CODE COUNTY CODE MA 02129 025 Suffolk 025 HCLASSIFICATION CATEGORY OWNERSHIP STATUS PRESENT USE ^.DISTRICT —PUBLIC —OCCUPIED _ AGRICULTURE —MUSEUM _ BUILDING(S) —PRIVATE —UNOCCUPIED —COMMERCIAL —PARK —STRUCTURE X.BOTH —WORK IN PROGRESS —EDUCATIONAL —PRIVATE RESIDENCE —SITE PUBLIC ACQUISITION ACCESSIBLE —ENTERTAINMENT —RELIGIOUS —OBJECT _IN PROCESS n/a ?LYES: RESTRICTED ;<XGOVERNMENT 1& —SCIENTIFIC —BEING CONSIDERED — YES: UNRESTRICTED —INDUSTRIAL —TRANSPORTATION _NO _ MILITARY X-OTHER: vacant AGENCY REGIONAL HEADQUARTERS: (If applicable) North Atlantic Regional Office (see continuation sheet) STREETS NUMBER 15 State Street CITY. TOWN STATE Boston VICINITY OF MA LOCATION OF LEGAL DESCRIPTION COURTHOUSE. REGISTRY OF DEEDS, ETC Registry of Deeds, Suffolk County Courthouse STREET & NUMBER CITY. TOWN STATE Boston, MA I REPRESENTATION IN EXISTING SURVEYS TITLE n/a DATE —FEDERAL —STATE —COUNTY —LOCAL DEPOSITORY FOR SURVEY RECORDS CITY. TOWN STATE DESCRIPTION CONDITION CHECK ONE CHECK ONE -EXCELLENT «, a ^.DETERIORATED XjJNALTERED X_ORIGINALSITE _GOOD _RUiNS _ALTERED __MOVED DATE_ _UNEXPOSED DESCRIBETHE PRESENT AND ORIGINAL^ KNOWN) PHYSICAL APPEARANCE Hoosac Stores 1 & 2, 115 Water Street (1895) Hoosac Stores 1 & 2, built in 1895, is a six-story warehouse structure of red brick laid in common bond.
    [Show full text]
  • WATERS THAT DRAIN VERMONT the Connecticut River Drains South
    WATERS THAT DRAIN VERMONT The Connecticut River drains south. Flowing into it are: Deerfield River, Greenfield, Massachusetts o Green River, Greenfield, Massachusetts o Glastenbury River, Somerset Fall River, Greenfield, Massachusetts Whetstone Brook, Brattleboro, Vermont West River, Brattleboro o Rock River, Newfane o Wardsboro Brook, Jamaica o Winhall River, Londonderry o Utley Brook, Londonderry Saxtons River, Westminster Williams River, Rockingham o Middle Branch Williams River, Chester Black River, Springfield Mill Brook, Windsor Ottauquechee River, Hartland o Barnard Brook, Woodstock o Broad Brook, Bridgewater o North Branch Ottauquechee River, Bridgewater White River, White River Junction o First Branch White River, South Royalton o Second Branch White River, North Royalton o Third Branch White River, Bethel o Tweed River, Stockbridge o West Branch White River, Rochester Ompompanoosuc River, Norwich o West Branch Ompompanoosuc River, Thetford Waits River, Bradford o South Branch Waits River, Bradford Wells River, Wells River Stevens River, Barnet Passumpsic River, Barnet o Joes Brook, Barnet o Sleepers River, St. Johnsbury o Moose River, St. Johnsbury o Miller Run, Lyndonville o Sutton River, West Burke Paul Stream, Brunswick Nulhegan River, Bloomfield Leach Creek, Canaan Halls Stream, Beecher Falls 1 Lake Champlain Lake Champlain drains into the Richelieu River in Québec, thence into the Saint Lawrence River, and into the Gulf of Saint Lawrence. Pike River, Venise-en-Quebec, Québec Rock River, Highgate Missisquoi
    [Show full text]
  • Lanesborough Report
    Town of Lanesborough, Massachusetts Community Resilience Building Workshop Summary of Findings JUNE 30, 2018 TABLE OF CONTENTS Community Background 2 Community Resilience-Building Process Overview and Workshop 4 Top Hazards and Vulnerable Areas of Concern 5 Current Concerns and Challenges Presented by Hazards 6 Specific Categories of Concerns & Challenges 6 Current Strengths and Assets 8 Top Recommendations to Improve Resilience 8 Post-Workshop Implementation 13 Workshop Participants 14 Citation 15 Acknowledgements 15 Appendices 16 1 Town of Lanesborough Community Resilience Building Workshop Summary of Findings June 30, 2018 Community Background The need for municipalities to increase resilience and adapt to extreme weather events and natural hazards is becoming more evident among the communities of Berkshire County, Massachusetts, the western-most county in the Commonwealth. In general, the region is separated from the Pioneer Valley and the rest of the state by the Berkshire Highlands and the Hoosac Range that serve as its eastern boundary and by the Taconic Mountains that serve as its western boundary with upper New York State. Lanesborough is located in north-central Berkshire County and is bordered to north by New Ashford, to the east by Cheshire and Dalton, to the south by Pittsfield and to the west by Hancock. The town is 18,764 acres in size, which is approximately 30 square miles. Lanesborough is situated at the headwaters of the two major river watersheds in the county: the Housatonic River, which flows southward through Connecticut to Long Island Sound, and the Hoosic River, which flows northward into the Hudson River, which ultimately flows into the Atlantic Ocean.
    [Show full text]
  • 7 the Geology of the Bennington Area
    I S; 5, •-' -"•L - THE GEOLOGY OF THE BENNINGTON AREIA, VERMONT By ItV £ JOHN A MACFAD\ EN, JR t "I VERMON I GEOLOGIC \L SURVEY :• CHARLiS G. DOLL Stale Geologist Published by S S VERMON'! DEVELOPMEf\ t COMMISSION •• MONTPELIER VE! MONT S S S S S • BiLETIN NO. 7 - 1956 S ' S S - THE GEOLOGY OF THE BENNINGTON ARF A, VERMONT By JOHN A. MACFAD\ 1N, JR £ I VERMON I GEOLOGIC 'LL SURVEY CHARLCS G. DOLL State Geologist 4 / • •• • . • • Published by VERMONT DEVELOPMEr''1' COMMISSION MONTPELIER VERIONT I • .BPLLETIN NO. • • • 1956 • •• •. •• eBr.4.n TABLE OF CONI1NTS / ' I PAGE 1 / ABSTRACT ......................... 7 i oRatlsn4 1 INTRODUCTION ........................ 8 0 Location. ......................... PWtney 8 Physiogiaphy and Glaciation ................. 9 Purpose of Study ....................... 11 I / I, Method of Study ...................... 11 I 0.> Regional Geologic Setting .................. 11 Vt. ) N.H. Previous Work ....................... 13 Acknowledgments . I ( 14 I I STRATIGRAPHY ........................ 15 I oManshular 1 General Statement .................... is I' Pre-Cambrian Sequence ......... ' .....16 / Mount Holly Gneiss ..................... 16 So.s.tqa 3r- I. I I Stamford Granite Gneiss................. 17 Lower Cambrian Sequence .................. 17 41 Mendon Formation ................... 17 I • —4 ( Cheshire Quartzite ................... 20 •• #3 Dunham Dolomite ..................... 21 'S Monkton Quartzite .................. 22 ------\-------- Winooski Dolomite ................... 23
    [Show full text]