Contents SECTION 3 - COMMUNITY SETTING
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Stream-Aquifer Relations and Yield of Stratified-Drift Aquifers in the Nashua River Basin, Massachusetts
STREAM-AQUIFER RELATIONS AND YIELD OF STRATIFIED-DRIFT AQUIFERS IN THE NASHUA RIVER BASIN, MASSACHUSETTS by Virginia de Lima U.S. GEOLOGICAL SURVEY Water-Resources Investigations Report 88-4147 Prepared in cooperation with the MASSACHUSETTS DEPARTMENT OF ENVIRONMENTAL MANAGEMENT, DIVISION OF WATER RESOURCES Boston, Massachusetts 1991 U.S. DEPARTMENT OF THE INTERIOR MANUEL LUJAN, JR., Secretary U.S. GEOLOGICAL SURVEY Dallas L. Peck, Director For additional information, write to: Copies of this report can be purchased from: District Chief U.S. Geological Survey U.S. Geological Survey Books and Open-File Reports Section 10 Causeway Street, Suite 926 Box 25425, Federal Center, Bldg. 810 Boston, MA 02222-1040 Denver, CO 80225 CONTENTS Page Abstract..................................................................... 1 Introduction ................................................................. 1 Purpose and scope .......................................................... 2 Previous investigations ...................................................... 2 Acknowledgments .......................................................... 2 Description of the study area .................................................... 4 Geographic setting ......................................................... 4 Hydrogeologic setting ....................................................... 4 Sources of potential ground-water withdrawals .................................. 4 Stream-aquifer relations in stratified-drift aquifers ................................. 5 Methods -
Hydrologic Assessment Report
CDM DEM-Office of Water Resources EOEA - Nashua River Basin Team Hydrologic Assessment Nashua River Watershed March 2002 2.5 2.0 1.5 1.0 0.5 0.0 JAN FEB MAR APR MAY JUN JUL AUG SEP OCT NOV DEC 60 50 Wastewater Flow Existing Flow 40 Virgin Flow 30 20 10 0 River River Brook RIVER River 2 NORTH Stillwater Stillwater Reservoir Nissitissit Nissitissit NASHUA Wachusett Wachusett Quinapoxet James Brook James Mulpus Brook Mulpus Catacoonamug Catacoonamug Contents Introduction 1.1 General ...................................................................................................................... 1-1 1.2 Watershed Description............................................................................................ 1-1 1.3 Overview of Assessment......................................................................................... 1-2 Background Information 2.1 General ...................................................................................................................... 2-1 2.2 Community Land Areas ......................................................................................... 2-1 2.3 Surficial Geology and Aquifer Delineations ........................................................ 2-1 2.4 Water Supplies ......................................................................................................... 2-4 2.5 Wastewater Discharges......................................................................................... 2-26 2.6 Population.............................................................................................................. -
1 Cook Conservation Area Photo by MRPC Section 4. Environmental
Cook Conservation Area Photo by MRPC Section 4. Environmental Inventory & Analysis 4.A. Geology, Soils and Topography See Map 4: “Soils and Geologic Features” in the Appendix. Lancaster is located along the eastern margin of the Central Upgrade Region of Massachusetts, a region of moderate relief characterized by numerous, irregularly shaped granite hills, plains, and glacial features known as Monadnocks. Where the North Nashua and South Nashua Rivers join in south Lancaster at “The Meeting of the Waters”, the main stem of the Nashua flows northward at an elevation of 220’ above mean sea level. To the north and west, rolling hills reach elevations of more than 550 feet; this area is highly conducive to rapid runoff from rain events and melting snow cover. Throughout the region, geology, soils, and topography historically determined where and how forests were interspersed with wetlands, ponds, lakes, rivers, and streams. Bedrock Lancaster’s bedrock is made primarily of low-grade, metamorphic rock of the Nashua belt and Worcester formations. Much of the underlying bedrock is exposed on hillsides and summits of the area and is oriented north to south. 1 Legacies of the Ice Age The Wisconsin Glacier of the Pleistocene epoch, which ended approximately 12,000 years ago, was the last major advance in North America of the Laurentide ice sheet which radically changed New England’s landscape. Two miles thick in places, the Wisconsin carved out the Nashua River Valley through intense scouring action as it advanced southward, and created drumlins by riding over loose bedrock. As it melted, the glacier dumped boulders, stones and soils along its southerly receding face; known as glacial till, this heterogeneous material covers much of the landscape in Worcester County and approximately 30% of Lancaster. -
THE PHYSICAL FEATURES of CENTRAL MASSACHUSETTS. By
THE PHYSICAL FEATURES OF CENTRAL MASSACHUSETTS. By WILLIAM C. AIDEN. INTRODUCTION. The area described in this paper lies mainly in central Massachu setts and comprises about two-thirds of the plateau extending from the eastern part of the Connecticut Valley on the west to the low lands of Middlesex County on the east (fig. 1). The area is about FIQDBE 1. Map showing location of the Holyoke, Ware, and Quinslgamond quadrangles, central Massachusetts. 52 miles in exstent from east to west and 35 miles from north to south and includes approximately 1,835 square miles. It lies between parallels 42° N. and 42° 30' N. and meridians 71° 30' W. and 72° 30' W. and thus includes on the south a strip of northern Rhode Island about half a mile to a mile wide and a strip of northeastern Connecticut about 2 to 2£ miles wide. In the years 1885-1887 a topographic survey of the Belchertown, Barre, Worcester, Marlboro, Palmer, Brookfield, Webster, and Black- stone 15-minute quadrangles was made by the United States Geologi- 92818° 25 2 13 14 COJSTTEIBUT10NS TO GEOGRAPHY OF UNITED STATES, 1923-1924. cal Survey, and maps of these quadrangles were published on a scale of 1:62,500, or approximately 1 mile to the inch, with a 20-foot con tour interval. In 1908 these maps were combined into two covering the same area on a scale of 1:125,000, or approximately 2 miles to the inch, with a contour interval of 40 feet. The two 30-minute quad rangles thus mapped were designated the Ware and Quinsigamond quadrangles. -
A Citizen's Guide
A Citizen’s Guide to Wildlife Habitat and Natural Resource Inventories in the Nashua River Watershed Written and compiled by James DeNormandie Table of Contents ACKNOWLEDGMENTS...............................................................................................................................................4 SECTION 1 - INTRODUCTION ..................................................................................................................................5 SECTION 1.1 - WHY INVENTORY HABITAT AND NATURAL RESOURCES?.......................................................................5 SECTION 1.2 - WHAT IS A WILDLIFE HABITAT OR NATURAL RESOURCE INVENTORY? ..................................................8 SECTION 1.3 - HOW CAN INVENTORIES BE USED?........................................................................................................12 SECTION 1.4 - INTENDED AUDIENCE ............................................................................................................................17 SECTION 1.5 - FORMAT OF THE GUIDE..........................................................................................................................17 SECTION 2 - DEFINING AND INITIATING THE INVENTORY .....................................................................20 SECTION 2.1 - REASONS TO UNDERTAKE LOCAL INVENTORIES ...................................................................................20 SECTION 2.2 - DEFINE THE GOAL OF THE PROJECT.......................................................................................................21 -
4-1 Photo by Shawn Winsor Frog in Pond Section 4. Environmental
Photo by Shawn Winsor Frog in Pond Section 4. Environmental Inventory & Analysis 4. A. Geology, Soils, and Topography Lancaster is located along the eastern margin of the Central Upgrade region of Massachusetts, a region of moderate relief characterized by numerous, irregularly shaped granite hills, plains, and glacial features known as monadnocks. Throughout the region, forests are interspersed with wetlands, ponds, lakes, rivers, and streams. Where the North Nashua and South Nashua Rivers join in Lancaster at “The Meeting of the Waters”, the main stem of the Nashua flows northward at an elevation of 220’ above mean sea level. To the north and west, rolling hills reach elevations of more than 550 feet. This area is highly conducive to rapid runoff. The Wisconsin Glacier of the Pleistocene epoch, which ended approximately 12,000 years ago, was the last major advance in North America of the Laurentide ice sheet which radically changed the landscape. Two miles thick in places, it caused drumlins to be formed by riding over loose bedrock and, as it melted and by dumping boulders, stones and soils along its southerly receding face. Called glacial till, this heterogeneous material covers much of the landscape in Worcester County. Glacial outwash was formed by melt water from the receding glacier picking up glacial till, sorting it by size and water velocity, and redepositing it downstream. The region surrounding the Nashua River Valley is an example of this outwash plain. Alluvium, made up of sand, silt, or clay, was deposited upon the land by streams. Areas of glacial till generally range from gently sloping to strongly sloping. -
DESIGNATION of the CENTRAL NASHUA RIVER VALLEY AREA OF
DESIGNATION of the CENTRAL NASHUA RIVER VALLEY AREA OF CRITICAL ENVIRONMENTAL CONCERN located in portions of the MUNICIPALITIES OF BOLTON, HARVARD, LANCASTER and LEOMINSTER WITH SUPPORTING FINDINGS Following an extensive formal review required by the regulations of the Executive Office of Environmental Affairs (301 CMR 12.00) including nomination, review, on-site visits, research, public information meetings, a public hearing and written comment period, and evaluation of all public comment and assembled data, I, the Secretary of Environmental Affairs, hereby designate the Central Nashua River Valley, located in portions of the municipalities of Bolton, Harvard, Lancaster and Leominster, as an Area of Critical Environmental Concern (ACEC). I take this action pursuant to the authority granted me under Massachusetts General Laws Chapter 21A, Section 2(7). I also hereby find that the wetland resource areas included in the Central Nashua River Valley ACEC are significant to the protection of groundwater supply and private water supplies, the prevention of pollution, flood control, the prevention of storm damage, the protection of fisheries, and the protection of wildlife habitat - all of which are public interests defined in the Wetlands Protection Act and regulations promulgated thereunder. I. Procedures Leading to ACEC Designation On December 23, 1993 I received a letter of nomination from the Lancaster Board of Selectmen pursuant to the ACEC Regulations at 301 CMR 12.05. I acknowledged receipt of the nomination in correspondence to the nominators dated December 28, 1993. In correspondence dated February 7, 1994, I informed the nominators that I was extending the 45-day initial review period pending consultation with the Attorney General's Office regarding procedural questions about the nomination.