Cumulative Impacts to Environmental Conditions on the Presumpscot River and Its Shorelands, As Distributed at the June 2002 Public Meetings
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Surficial Geology of the Naples 7.5' Quadrangle, Maine
DE PART MENT OF CON SER VA TION Maine Geo logi cal Sur vey Rob ert G. Marv in ney, State Ge olo gist OPEN- FILE NO. 97-65 Ti tle: Sur fic ial Ge ol ogy of the Naples 7.5- minute Quad ran gle, Cum ber land County, Maine Author: Carol T. Hildreth Date: 1997 Fi nan cial Sup port: Funding for the prepara tion of this report was provided in part by the U.S. Geo logi cal Sur vey STATE MAP Pro gram, Co op era tive Agree ment No. 1434- 95- A- 01364. As so ci ated Maps: Sur fic ial ge ol ogy of the Naples quad ran gle, Open- File 97- 50 Surfic ial materials of the Naples quadran gle, Open- File 98-188 Con tents: 9 p. report Maine Geo logi cal Sur vey Open- File 97- 65 Surficial Geology of the Naples 7.5-minute Quadrangle, Cumberland County, Maine Carol T. Hil dreth CTH En ter prizes 135 Wash ing ton Street Hol lis ton, Mas sa chu setts 01746 IN TRO DUC TION The Naples 7.5' quadran gle has an area of about 133 km2 others (1985, p. 52) point out that de posit s of gla cial streams in (52 mi2). It is lo cated in south west ern Maine, within the Sea - Maine form a den dritic pat tern that may reflect pre gla cial drain - board Lowland physiographi c province , about 32 km (20 mi) age (Figure 2). Thus the pregla cia l Androscog gin River may northwest of Portland. -
The Following Document Comes to You From
MAINE STATE LEGISLATURE The following document is provided by the LAW AND LEGISLATIVE DIGITAL LIBRARY at the Maine State Law and Legislative Reference Library http://legislature.maine.gov/lawlib Reproduced from scanned originals with text recognition applied (searchable text may contain some errors and/or omissions) ACTS AND RESOLVES AS PASSED BY THE Ninetieth and Ninety-first Legislatures OF THE STATE OF MAINE From April 26, 1941 to April 9, 1943 AND MISCELLANEOUS STATE PAPERS Published by the Revisor of Statutes in accordance with the Resolves of the Legislature approved June 28, 1820, March 18, 1840, March 16, 1842, and Acts approved August 6, 1930 and April 2, 193I. KENNEBEC JOURNAL AUGUSTA, MAINE 1943 PUBLIC LAWS OF THE STATE OF MAINE As Passed by the Ninety-first Legislature 1943 290 TO SIMPLIFY THE INLAND FISHING LAWS CHAP. 256 -Hte ~ ~ -Hte eOt:l:llty ffi' ft*; 4tet s.e]3t:l:ty tfl.a.t mry' ~ !;;llOWR ~ ~ ~ ~ "" hunting: ffi' ftshiRg: Hit;, ffi' "" Hit; ~ mry' ~ ~ ~, ~ ft*; eounty ~ ft8.t rett:l:rRes. ~ "" rC8:S0R8:B~e tffi:re ~ ft*; s.e]38:FtaFe, ~ ~ ffi" 5i:i'ffi 4tet s.e]3uty, ~ 5i:i'ffi ~ a-5 ~ 4eeme ReCCSS8:F)-, ~ ~ ~ ~ ~ ffi'i'El, 4aH ~ eRtitles. 4E; Fe8:50nable fee5 ffi'i'El, C!E]3C::lSCS ~ ft*; sen-ices ffi'i'El, ~ ft*; ffi4s, ~ ~ ~ ~ -Hte tFeasurcr ~ ~ eouRty. BefoFc tfte sffi4 ~ €of' ~ ~ 4ep i:tt;- ~ ffle.t:J:.p 8:s.aitional e1E]3cfisc itt -Hte eM, ~ -Hte ~ ~~' ~, ftc ~ ~ -Hte conseRt ~"" lIiajority ~ -Hte COt:l:fity COfi111'lissioReFs ~ -Hte 5a+4 coufity. Whenever it shall come to the attention of the commis sioner -
Presumpscot Watershed Initiative Factsheet.Pub
Presumpscot Watershed Initiative PROJECT FACTSHEET Historical Background The success of the Presumpscot The Presumpscot River flows 27 miles from Sebago Lake into Casco Bay and the Watershed Initiative was the result of Gulf of Maine. The river’s watershed encompasses 205 square miles of primarily many partners working together throughout the watershed to improve forested and agricultural land. The river itself has a history of extensive industrial habitat and water quality and to foster use since the early 1700s. By the 1950s, the river had nine ddams an was so stewardship. In addition to the Casco polluted that fumes from the river peeled paint off nearby homes. Prior to Bay Estuary Partnership, partners industrialization, there were abundant salmon, alewife, shad, smelt, and eel included: fisheries, which have since been greatly diminished. Cumberland County Soil and Water Conservation District In recent years the water and habitat quality of the river have improved with the Friends of Casco Bay cessation of pulp mill discharges in the 1990s and the removal of Smelt Hill Dam Presumpscot River Watch in 2002. Anadromous fish are returning to the river’s main stem and tributaries. Presumpscot River Watershed Coalition Environmental Challenges Maine Department of While the river has recovered from some past problems, increased watershed Environmental Protection and shoreline development are leading to environmental impacts: Municipal road crews, state agencies, Toxic chemicals and excess nutrients enter the river system via stormwater golf courses, citizen volunteers, landowners, schools, and many flowing from impervious surfaces. others! Excess sedimentation from roadways and livestock activities deteriorate fish spawning areas. The loss of riparian vegetation causes thermal impacts, which impair water quality for cold water fisheries. -
Geologic Site of the Month: Why Is Sebago Lake So Deep?
Why is Sebago Lake so deep? Maine Geological Survey Maine Geologic Facts and Localities February, 1999 Why is Sebago Lake so deep? 43° 51‘ 13.36“ N, 70° 33‘ 43.98“ W Text by Robert A. Johnston Maine Geological Survey, Department of Agriculture, Conservation & Forestry 1 Why is Sebago Lake so deep? Maine Geological Survey Introduction Modern geophysical equipment allows geologists to investigate previously unmapped environments, including ocean and lake floors. Recent geophysical research studied the types, composition, areal extent, and thickness of sediments on the bottom of Sebago Lake in southwestern Maine. Geologists used side- scan sonar and seismic reflection profiling to map the bottom of the lake. Approximately 58 percent of the lake bottom was imaged with side-scan sonar and over 60 miles of seismic reflection profiles were collected. This web site will discuss the findings of the seismic reflection profiling. Maine Geological Survey, Department of Agriculture, Conservation & Forestry 2 Why is Sebago Lake so deep? Maine Geological Survey Physiographic setting Sebago Lake, although second in surface area to Moosehead Lake, is Maine's deepest lake. With a water depth of 316 feet, its deepest part is 49 feet below sea level! Sebago Lake is located in southwestern Maine 20 miles northwest of Portland and 50 miles southeast of the White Mountains. It lies along the transition between the Central Highlands and the Coastal Lowlands physiographic regions of New England (Figure 1). The abrupt change in landscape can be seen in panoramic views from several vantage points near Sebago Lake. Denny, 1982 Denny, Maine Geological Survey From From Figure 1. -
Total Phosphorus Loads for Selected Tributaries to Sebago Lake, Maine
science for a changing world Total Phosphorus Loads for Selected Tributaries to Sebago Lake, Maine Water-Resources Investigations Report 01-4003 V Prepared in cooperation with the Portland Water District U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior U.S. Geological Survey By Glenn A. Hodgkins Water-Resources Investigations Report 01-4003 Prepared in cooperation with the Portland Water District Augusta, Maine 2001 U.S. DEPARTMENT OF THE INTERIOR GALE A. NORTON, Secretary U.S. GEOLOGICAL SURVEY Charles G. Groat, Director The use of firm, trade, and brand names in this report is for identification purposes only and does not constitute endorsement by the U.S. Government. For additional information write to: Copies of this report can be purchased from: District Chief U.S. Geological Survey U.S. Geological Survey Branch of Information Services 26 Ganneston Dr. Box 25286, Federal Center Augusta, ME 04330 Denver, CO 80225 http://me.water.usgs.gov CONTENTS Abstract.................................................................................... 1 Introduction................................................................................. 2 Description of the study area.................................................................... 2 Data collection and analysis .................................................................... 2 Data-collection networks in the Sebago Lake Basin.......................................... 2 Adequacy of current stream-gaging network .............................................. -
Seventieth Legislature
MAINE STATE LEGISLATURE The following document is provided by the LAW AND LEGISLATIVE DIGITAL LIBRARY at the Maine State Law and Legislative Reference Library http://legislature.maine.gov/lawlib Reproduced from scanned originals with text recognition applied (searchable text may contain some errors and/or omissions) NEW DRAFT. Seventieth Legislature. HOUSE. No. 87 STATE OF MAINE. IN THE YEAR OF OUR LORD ONE THOUSAND NINE HUNDRED AND ONE. RESOLVE to complete the improvements of Songo and Chute River;-;. Resolved, That the sum of five hundred dollars ( 500) is 2 hereby appropriated for the purpose of completing the 3 dredging, construction of jettie::; or break-waters, and 4 other improvements, to render navigable, throughout the 5 entire season, those parts of the interior waterway, in the 6 Sebago Lake Steamboat route, known as Chute's river, 7 situated between Long lake and the bay of Naples, in the 8 town of Naples, county of Cumberland, and at Songo 9 lock and mouth of Songo river, which connects the bay of JO Naples and Sebago lake, in said town and county. 2 HOUSE-No. 87. The expenditure of such appropriation, shall be under 12 the direction of the county commissioners of Cumberland 13 county, who shall employ a competent man to supervise 14 such improvements, in accordance with the plan laid out 15 by the civil engineer employed by said commiseioners, in 16 the fall of 1899. Provided, however, that no part of this appropriation 18 shall be paid by the state, until a total sum of sixteen 19 hundred dollars ($1,600) shall have been expended on the 20 improvements of said Songo and Chute rivers, since such 21 improvements were begun in 1899. -
Surface Water Supply of the United States 1915 Part I
DEPARTMENT OF THE INTERIOR FRANKLIN K. LANE, Secretary UNITED STATES GEOLOGICAL SURVEY GEORGE OTIS SMITH, Director WATER-SUPPLY PAPER 401 SURFACE WATER SUPPLY OF THE UNITED STATES 1915 PART I. NORTH ATLANTIC SIOPE DRAINAGE BASINS NATHAN C. GROVES, Chief Hydraulic Engineer C. H. PIERCE, C. C. COVERT, and G. C. STEVENS. District Engineers Prepared in cooperation with the States of MAIXE, VERMONT, MASSACHUSETTS, and NEW YORK WASHINGTON GOVERNMENT FEINTING OFFICE 1917 DEPARTMENT OF THE INTERIOR FRANKLIN K. LANE, Secretary UNITED STATES GEOLOGICAL SURVEY GEORGE OTIS SMITH, Director Water-Supply Paper 401 SURFACE WATER SUPPLY OF THE UNITED STATES 1915 PART I. NORTH ATLANTIC SLOPE DRAINAGE BASINS NATHAN C. GROVER, Chief Hydraulic Engineer C. H. PIERCE, C. C. COVERT; and G. C. STEVENS, District Engineers Geological Prepared in cooperation with the States MAINE, VERMONT, MASSACHUSETTS^! N«\f Yd] WASHINGTON GOVERNMENT PRINTING OFFICE 1917 ADDITIONAL COPIES OF THIS PUBLICATION MAY BE PROCURED FROM THE SUPEBINTENDENT OF DOCUMENTS GOVERNMENT FEINTING OFFICE "WASHINGTON, D. C. AT 15 CENTS PER COPY V CONTENTS. Authorization and scope of work........................................... 7 Definition of terms....................................................... 8 Convenient equivalents.................................................... 9 Explanation of data...................................................... 11 Accuracy of field data and computed results................................ 12 Cooperation.............................................................. -
Bedrock Valleys of the New England Coast As Related to Fluctuations of Sea Level
Bedrock Valleys of the New England Coast as Related to Fluctuations of Sea Level By JOSEPH E. UPSON and CHARLES W. SPENCER SHORTER CONTRIBUTIONS TO GENERAL GEOLOGY GEOLOGICAL SURVEY PROFESSIONAL PAPER 454-M Depths to bedrock in coastal valleys of New England, and nature of sedimentary Jill resulting from sea-level fluctuations in Pleistocene and Recent time UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1964 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director The U.S. Geological Survey Library has cataloged this publication, as follows: Upson, Joseph Edwin, 1910- Bedrock valleys of the New England coast as related to fluctuations of sea level, by Joseph E. Upson and Charles W. Spencer. Washington, U.S. Govt. Print. Off., 1964. iv, 42 p. illus., maps, diagrs., tables. 29 cm. (U.S. Geological Survey. Professional paper 454-M) Shorter contributions to general geology. Bibliography: p. 39-41. (Continued on next card) Upson, Joseph Edwin, 1910- Bedrock valleys of the New England coast as related to fluctuations of sea level. 1964. (Card 2) l.Geology, Stratigraphic Pleistocene. 2.Geology, Stratigraphic Recent. S.Geology New England. I.Spencer, Charles Winthrop, 1930-joint author. ILTitle. (Series) For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 CONTENTS Page Configuration and depth of bedrock valleys, etc. Con. Page Abstract.__________________________________________ Ml Buried valleys of the Boston area. _ _______________ -
2006 Comprehensive Plan.Pdf
NAPLES COMPREHENSIVE PLAN TABLE OF CONTENTS Page Acknowledgments 1 INTRODUCTION 3 What is a Comprehensive Plan? 3 How can a Comprehensive Plan serve the Town of Naples? 3 What is Smart Growth? 4 Benefits After Adoption 5 Public Participation in the Planning Process 5 Goals, Objectives and Policies 6 Implementation Strategies 6 SECTION 1: ISSUES AND OPPORTUNITIES FOR THE FUTURE 8 1.1 Community Character 9 1.2 Survey Results 15 1.3 Vision Statement 20 SECTION 2: INVENTORY AND ANALYSIS OF EXISTING CONDITIONS 23 2.1 The People of Naples 24 2.2 Housing 38 2.3 The Economy 54 2.4 Existing Land Use 62 2.5 Natural Resources Inventory 75 2.6 Agricultural and Forest Resources 109 2.7 Cultural Resources 112 2.8 Public Facilities and Services 115 2.9 Transportation 122 2.10 Recreation and Public Access 127 2.11 Fiscal Capacity 131 SECTION 3: SUMMARY AND FINDINGS OF EXISTING CONDITIONS AND FUTURE LAND USE NEEDS 139 3.1 Projected Growth and its Impacts 140 3.2 Projected Growth and What Naples Wants 142 3.3 Summary Listing of Planning Issues facing the Town of Naples 142 SECTION 4: GOALS, OBJECTIVES, POLICIES, AND STRATEGIES 148 4.1 Goals, Objectives, Policies and Strategies of the Town of Naples 149 4.1.1 Citizen Participation 150 4.1.2 Fiscal Policy 152 4.1.2.1 Capital Investment Plan 155 4.1.3 Public Facilities and Services 158 4.1.4 Recreation and Public Access 163 4.1.5 Cultural Resources 166 ii 4.1.6 Economic Expansion 170 4.1.7 Housing 176 4.1.8 Future Land Use 181 4.1.9 Transportation 186 4.1.10 Agriculture and Forest Resources 192 4.1.11 Water Resources 196 4.1.12 Critical Natural Resources 204 SECTION 5: FUTURE LAND USE PLAN 209 5.1 Future Land Use Planning Process 210 5.2 Future Land Use Map 210 SECTION 6: APPENDIX 215 A. -
Directions to the Friends of Casco Bay Office 43 Slocum Drive South Portland, Maine 04106 (207) 799-8574
Directions to the Friends of Casco Bay Office 43 Slocum Drive South Portland, Maine 04106 (207) 799-8574 Our office is on the campus of Southern Maine Community College (SMCC) near Spring Point Lighthouse. If using GPS, use SMCC’s address 2 Fort RD, South Portland, ME 04106. From I-95 & I-295 . Take the exit 45 toward I-295/US-1/ME-114/Maine Mall Rd/Payne Rd . Merge onto Maine Turnpike Approach . Take the exit onto I-295 N toward Portland . Take exit 4 toward Casco Bay Br/Portland/Waterfront . Continue onto Veterans Memorial Bridge . Continue onto Fore River Pkwy . Continue onto W Commercial St . Turn left to merge onto Casco Bay Bridge / Route 77 S . Continue onto Broadway (straight through the lights at the end of the bridge) . Follow Broadway all the way to its dead end at Benjamin W. Pickett Street (about 1.3 miles) . Turn right onto Benjamin W. Pickett Street . Take the 2nd left onto Slocum Drive (it looks like you’re entering a parking lot in front of a big dormitory; if you get to the stop sign at Fort Road, you missed Slocum) . Our office is a small one-story building at 43 Slocum, toward the end of the road on the left. Look for a small blue sign that reads “Friends of Casco Bay” in front of our building. From the South via Route 1 . Follow Route 1 N to South Portland . At the intersection with Broadway, turn right onto Broadway. Continue for 1.9 miles. Just past the fire station, turn right to stay on Broadway/77 S. -
The Dirty History of Portland Harbor
Reprinted from a 1994 publication The Dirty History of Portland Harbor hen scientists began looking closely at the sediments and at W the bottom of Casco Bay beginning in the early 1980s, they confronted a pollution puzzle. Sediments taken from various locations throughout the Bay, and especially in Portland Harbor, held a wide variety of potentially toxic chemicals. Until we know more about how these heavy metals, pesticides and other compounds affect marine life, it’s hard to know what lasting impact the pollution in Casco Bay may have. But it was decided that the more we know about where those pollutants came from, the better chances we will have in preventing future problems. The Casco Bay Estuary Project (now Casco Bay Early industry was limited by natural energy sources, like this tidal mill at Estuary Partnership) commissioned environmental Stroudwater. (courtesy: Sullivan Train & Photo) historian Edward Hawes to do some detective work, hoping that he could turn up some puzzle pieces from the Casco Bay. Lead, cadmium and mercury concentrations were watersheds that feed the Bay. The industrial legacy he found comparatively high in Back Cove, as were lead and mercury was a surprise to almost anyone who thinks they know the in the inner Fore River. Lead was also relatively high in the Portland area. Presumpscot River estuary. Additional metals — nickel, silver, arsenic, chromium A Pollution Problem and zinc — were evident in lesser concentrations. This widespread contamination was a little mystifying. In this age hen investigators began sampling Casco Bay’s of environmental regulation, how could so much pollution sediments in the 1980s, levels of pollution have landed in the Bay? W were found that merited additional attention. -
A Dirty History of Casco Bay
University of Southern Maine USM Digital Commons Graphics, Maps, and Posters Casco Bay Estuary Partnership (CBEP) 2010 Portland Waterfront Sign: A Dirty History of Casco Bay Casco Bay Estuary Partnership Montgomery Designs Follow this and additional works at: https://digitalcommons.usm.maine.edu/cbep-graphics-maps-posters Recommended Citation Casco Bay Estuary Partnership and Montgomery Designs, "Portland Waterfront Sign: A Dirty History of Casco Bay" (2010). Graphics, Maps, and Posters. 6. https://digitalcommons.usm.maine.edu/cbep-graphics-maps-posters/6 This Book is brought to you for free and open access by the Casco Bay Estuary Partnership (CBEP) at USM Digital Commons. It has been accepted for inclusion in Graphics, Maps, and Posters by an authorized administrator of USM Digital Commons. For more information, please contact [email protected]. Custom H ouse 1 You are standing in the SAME PLACE SHOWN in 1 C this 1900 photo. Can you imagine the sounds and smells on OAL the day this picture was taken? RIGHT: This 1914 map shows R & M x the Randall & McAllister Coal Wharf located here, COAL A Dirty History of Casco Bay other industrial shipping piers, and railroad tracks. YOU BacK COVE C By the summer of 1866, Portland was the OAL ARE HERE 3 Randall & largest commercial shipping port in the nation. G The coal dust from the harbor M ALT WHA F R aine Steamship Co. Industries sprouted up everywhere. Much of their “ ANKLIN WHArf 2 PAINT FacTORIES like this one on Munjoy Hill (1899) used Eastern Steamship Co. was so thick we had to sweep up the M lead and mercury.