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Ecoregions of New England Forested Land Cover, Nutrient-Poor Frigid and Cryic Soils (Mostly Spodosols), and Numerous High-Gradient Streams and Glacial Lakes
58. Northeastern Highlands The Northeastern Highlands ecoregion covers most of the northern and mountainous parts of New England as well as the Adirondacks in New York. It is a relatively sparsely populated region compared to adjacent regions, and is characterized by hills and mountains, a mostly Ecoregions of New England forested land cover, nutrient-poor frigid and cryic soils (mostly Spodosols), and numerous high-gradient streams and glacial lakes. Forest vegetation is somewhat transitional between the boreal regions to the north in Canada and the broadleaf deciduous forests to the south. Typical forest types include northern hardwoods (maple-beech-birch), northern hardwoods/spruce, and northeastern spruce-fir forests. Recreation, tourism, and forestry are primary land uses. Farm-to-forest conversion began in the 19th century and continues today. In spite of this trend, Ecoregions denote areas of general similarity in ecosystems and in the type, quality, and 5 level III ecoregions and 40 level IV ecoregions in the New England states and many Commission for Environmental Cooperation Working Group, 1997, Ecological regions of North America – toward a common perspective: Montreal, Commission for Environmental Cooperation, 71 p. alluvial valleys, glacial lake basins, and areas of limestone-derived soils are still farmed for dairy products, forage crops, apples, and potatoes. In addition to the timber industry, recreational homes and associated lodging and services sustain the forested regions economically, but quantity of environmental resources; they are designed to serve as a spatial framework for continue into ecologically similar parts of adjacent states or provinces. they also create development pressure that threatens to change the pastoral character of the region. -
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. -
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. -
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 -
GEOLOGIC RADON POTENTIAL of EPA REGION 1 Connecticut Maine Massachusetts New Hampshire Rhode Island Vermont
U.S. DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY GEOLOGIC RADON POTENTIAL OF EPA REGION 1 Connecticut Maine Massachusetts New Hampshire Rhode Island Vermont OPEN-FILE REPORT 93-292-A Prepared in Cooperation with the | U.S. Environmental Protection Agency 9'% 1993 U.S. DEPARTMENT OF THE INTERIOR U. S. GEOLOGICAL SURVEY GEOLOGIC RADON POTENTIAL OF EPA REGION 1 Connecticut, Maine, Massachusetts, New Hampshire, Rhode Island, and Vermont R. Randall Schumann EDITOR OPEN-FILE REPORT 93-292-A Prepared in cooperation with the U.S. Environmental Protection Agency 1993 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards or with the North American Stratigraphic Code. CONTENTS SECTION____________________________________PAGE 1. The USGS/EPA State Radon Potential Assessments: An Introduction 1 Linda C.S. Gundersen, R. Randall Schumann, and Sharon W. White Appendix A: Geologic Time Scale 19 Appendix B: Glossary of Terms 20 Appendix C: EPA Regional Offices, State Radon Contacts, 26 and State Geological Surveys 2. EPA Region 1 Geologic Radon Potential Summary 36 Linda C.S. Gundersen, R. Randall Schumann, and Sandra L. Szarzi 3. Preliminary Geologic Radon Potential Assessment of Connecticut 47 Linda C.S. Gundersen andR. Randall Schumann 4. Preliminary Geologic Radon Potential Assessment of Maine 83 Linda C.S. Gundersen andR. Randall Schumann 5. Preliminary Geologic Radon Potential Assessment of Massachusetts 123 R. Randall Schumann and Linda C.S. Gundersen 6. Preliminary Geologic Radon Potential Assessment of New Hampshire 157 Linda C.S. Gundersen andR. Randall Schumann 7. Preliminary Geologic Radon Potential Assessment of Rhode Island 191 Linda C.S. -
Web Edition Part 2 Public Co
From: [email protected] [mailto:[email protected]] Sent: Thursday, February 07, 2013 11:13 AM To: [email protected]; Launder, Kelly; [email protected]; [email protected]; Margolis, Anne; Markowitz, Deb; Governor Peter Shumlin; Darling, Scott; PSB - Clerk Subject: Lowell Mountain Reduced Production http://theenergycollective.com/willem-post/53258/examples-wind-power-learnAll, I am surprised GMP did not do a timely study of Lowell's impact on the NEK grid. As a result, the $10.5 million synchronous-condenser system for power factor correction (losses of up to 3%) will not be completed until about the end of 2013. There are many factors reducing ridge line IWT CFs. Here is an excerpt from http://theenergycollective.com/willem-post/169521/wind-turbine-energy-capacity-less-estimated Below are some numbers regarding the much less than expected results of the Maine ridge line IWTs for the past 12 months. http://www.coalitionforenergysolutions.org/maine_wind_thru_3q2012m1.pdf Mars Hill, 42 MW 0.353; uniquely favorable winds due to topography. Stetson I, 57 MW 0.254 Stetson II, 26 MW 0.227 Kibby Mtn 132 MW 0.238 Rollins, 60 MW 0.238 Record Hill, 50.5 MW 0.197 The Maine weighted average CF = (42 x 0.353 + 57 x 0.254 + 26 x 0.227 + 132 x 0.238 + 60 x 0.238 + 50.5 x 0.197)/(42 + 57 + 26 + 132 + 60 + 50.5) = 0.247; excluding Mars Hill, the CF would be 0.234. Note: CF reduction due to aging is not yet a major factor, as all these IWTs were installed in the past 5 years. -
Nonpoint Source Pollution Assessment for the Deerfield River Watershed
Nonpoint Source Pollution Assessment for the Deerfield River Watershed Section 604(b) Project Number 04-02/604 Prepared by the Franklin Regional Council of Governments Prepared for the Massachusetts Department of Environmental Protection Massachusetts Executive Office of Energy and Environmental Affairs Ian A. Bowles, Secretary Department of Environmental Protection Laurie Burt, Commissioner Bureau of Resource Protection Glenn Hass, Acting Assistant Commissioner Division of Municipal Services Steven J. McCurdy, Director June 2008 This project has been financed partially with Federal Funds from the Environmental Protection Agency (EPA) to the Massachusetts Department of Environmental Protection (the Department) under a s.604(b) Water Quality Management Planning Grant. The contents do not necessarily reflect the views and policies of EPA or of the Department, nor does the mention of trade names or commercial products constitute endorsement or recommendation for use. Nonpoint Source Pollution Assessment for the Deerfield River Watershed Prepared by the Franklin Regional Council of Governments Planning Department Peggy Sloan, Director of Planning and Development Kimberly Noake MacPhee, P.G., Natural Resources Program Manager Ryan Clary, Senior GIS Specialist Whitty Sanford, Assistant Planner Franklin Regional Council of Governments 425 Main Street, Greenfield, MA 01301 413-774-3167 www.frcog.org Table of Contents Executive Summary............................................................................................................... -
Busby Trail to Spruce Hill Savoy Mountain State Forest
Busby Trail to Spruce Hill Savoy Mountain State Forest SELF-GUIDED HIKING TOUR WELCOME to Savoy Mountain State Forest, 10,200 acres managed by the Massachusetts Department of Conservation and Recreation, and located in the towns of Savoy, Florida, Adams and North Adams. Savoy Mountain has many miles of wooded trails offering opportunities for year-round passive recrea- tion. Much of this state forest was acquired by Massachusetts beginning in1918, assembled from aban- doned farmland. Many farming residents, tired of poor conditions, had moved into valley towns of Ad- ams and North Adams to work in the woolen mills, or headed west for better farmland. The evidence of these farms remains with old orchards and stone fences and a cellar hole found along the Busby Trail. Please remember to carrycarry----in,in, carrycarry----outout all your belongings, including trash. Please leave no trace of you visit, and leave all that you find in its natural environment for all to enjoy. Thank you. THE BUSBY TRAIL to Spruce Hill is perhaps Hoosac Range the most popular hiking trail in the state forest. It Trail offers a great panoramic view. The trailhead is lo- SPRUCE HILL cated 3 miles from MA Route 2, at the intersection (2,570 ft. elev.) of Central Shaft Road and Old Florida Road (a il Tra Bu rocky dirt road), just beyond the state forest head- sby T nd rai o l P quarters at 260 Central Shaft Road, where you t s o may also pick up a Savoy Mountain State Forest L Blackburnian Lo Trail Map . -
The Green Mountain Anticlinorium in the Vicinity of Wilmington and Woodford Vermont
THE GREEN MOUNTAIN ANTICLINORIUM IN THE VICINITY OF WILMINGTON AND WOODFORD VERMONT By JAMES WILLIAM SKEHAN, S. J. VERMONT GEOLOGICAL SURVEY CHARLES G. DOLL, Stale Geologist Published by VERMONT DEVELOPMENT DEPARTMENT MONTPELIER, VERMONT BULLETIN NO. 17 1961 = 0 0. Looking northwest from centra' \Vhitingham, from a point near C in WHITINCHAM IPlate 1 Looking across Sadawga Pond Dome to Haystack Mountain-Searsburg Ridge in the background; Stratton and Glastenburv Mountains in the far distance. Davidson Cemetery in center foreground on Route 8 serves as point of reference. TABLE OF CONTENTS PAGE ABSTRACT 9 INTRODUCTION . . . . . . . . . . . . . . . . . . . . . 10 Location ........................ 10 Regional Geologic Setting . . . . . . . . . . . . . . . 13 Previous Geologic Work ................. 15 The Problem ...................... 16 Present Investigation ................... 18 Acknowledgments .................... 19 Topography . . . . . . . . . . . . . . . . . . . . . 19 Rock Exposure ..................... 20 Culture and Accessibility ................. 20 STRATIGRAPHY AND LITHOLOGY ............... 23 General Statement . . . . . . . . . . . . . . . . . . 23 Stratigraphic Nomenclature . . . . . . . . . . . . . . 25 Lithologic Nomenclature ................. 26 Pre-Cambrian Rocks . . . . . . . . . . . . . . . . . 27 General Statement . . . . . . . . . . . . . . . . . 27 Mount Holly Complex ................. 28 Stamford -
Mohawk Trail West Ch3 Natural Resources
CHAPTER 3 Natural Resources long the Mohawk Trail Scenic Byway lies a wealth of important natural resources. Among these resources are: the Deerfield and Hoosic Rivers, which contain important trout habitat; the Glacial Potholes in AShelburne Falls, one of the largest collection of such potholes in the country; the Natural Bridge in North Adams, the only bridge in North America created by the erosive forces of water; and miles of northern hardwood forests along the Byway corridor, including old growth forests in the Mohawk Trail State Forest. The Byway also includes other geologic, flora and fauna, water resources that help make the Mohawk Trail Scenic Byway experience unique. The corridor’s natural resources contribute to the dramatic scenery viewed from the Byway, and attract recreational tourists seeking to experience the corridor’s wildness. This chapter of the Corridor Management Plan provides a gen- eral inventory and overview of the Byway’s natural resources, in- cluding its geology, soils, water resources, and rare species habitat areas. The purpose is to highlight the Byway’s primary natural and environmental assets. The chapter also discusses potential issues that could affect the quality of these resources over time, especially if the Byway experiences an increase in tourist and vehicle traffic. The chapter closes with a series of recommendations for protect- ing, maintaining, and enhancing the Byway’s natural resources. ago, a period of mountain building Geologic Resources (also known as an orogeny) called the Taconic Orogeny created the Taconic Geologic History Hills of western Berkshire County. During this period, bedrock and sedi- The formation of the Byway landscape ment deposits of the warm sea were began approximately six-hundred mil- pushed westward and inland. -
North Adams Hazard Mitigation and Climate Adaptation Plan January 2021
North Adams Hazard Mitigation and Climate Adaptation Plan January 2021 Table of Contents CHAPTER 1: INTRODUCTION……………………………………………………………………………………………………………………………………………………………………..………… 2 CHAPTER 2: PLANNING PROCESS…………………………………………………………………………………………………………………………………………………………….…........... 4 CHAPTER 3: RISK ASSESSMENT…………………………………………………………………………………………………………………………………………………………….…………….. 11 Inland Flooding……………………………………………………………………………………………………………………………………………………………….…………. 22 Severe Winter Storms …………………………………………………………………………………………………………………………………………..………………….. 37 Droughts…………………………………………………………………………………………………………………………………………………………..………………………. 44 Change in Average Temperatures/Extreme Temperatures…………………………………………………………………………………..…………………… 50 Tornadoes/High Wind……………………………………………………………………………………………………………………………………………..……………….. 57 Landslides…………………………………………………………………………………………………………………………………………………………………………………. 61 Wildfires…………………………………………………………………………………………………………………………………………………………………..………………. 69 Hurricanes/Tropical Storms………………………………………………………………………………………………………………………………………………………. 76 Other Severe Weather………………………………………………………………………………………………………………………………………………..………… …. 82 Invasive Species…………………………………………………………………………………………………………….…………………………………………….……………. 88 Vector-Borne Disease………………………………………………………………………………………………………………………………………………….……………. 97 Earthquakes………………………………………………………………………………………………………………….………………………………………………………….100 Dam failure……………………………………………………………………………………………………………..………………………………………………………….…… 106 Cyber Security…………………………………………………………………………………………….……………..………………………………………………………….… -
Annual Report of the Greylock Commission
: Public Document No. 67 FIFTEENTH ANNUAL REPORT GRETLOCK COMMISSION, January, 1916. BOSTON WEIGHT & POTTER PRINTING CO., STATE PRINTERS^ 32 DERNE STREET. 1916. Approved by The State Boaed of Publication. ®l]e Cotnmonroealtfi of iHasBacliustttB. PiTTSFiELD, Mass., Jan. 1, 1916. To His Excellency the Governor of the Commonwealth and the Hon- orable Council. Gentlemen : — Enclosed please find the annual report of the Greylock Reservation Commission. Very respectfully yours^ FRANCIS W. ROCKWELL, Chairman. GREYLOCK RESERVATION COMMISSION. PiTTSFiELD, Mass., Jan. 1, 1916. To the Committee on Revision. Gentlemen : — The records kept by the secretaries of the Greylock Reservation Commission are very brief. In order to keep the public informed, and to make it easier for the gentlemen who may succeed the present com- mission, we place in the annual report facts and references which will give a better understanding of the work of the Commission. These references will enable all interested hereafter in the reservation to find what has been done and the methods employed in the general conduct of reservation matters. While the records in the State Auditor's, State Treasurer's and Attorney-General's offices will explain the expenditure of the funds appropriated by the Commonwealth, and while the annual reports of the treasurer of the Commis- sion to the Berkshire county commissioners will aid in the matter, it remains true that many matters of interest can be found only in the county press, — hence the references to the newspapers of Berkshire. Many inquiries pertaining to the history of the mountain and reservation are made of the Commission. These ques- tions can best be answered by the references given in the brief bibliography and references written for this report.