"Appendix : 1820 Treaty Negotiation Between the Penobscot Indian
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Penobscot Rivershed with Licensed Dischargers and Critical Salmon
0# North West Branch St John T11 R15 WELS T11 R17 WELS T11 R16 WELS T11 R14 WELS T11 R13 WELS T11 R12 WELS T11 R11 WELS T11 R10 WELS T11 R9 WELS T11 R8 WELS Aroostook River Oxbow Smith Farm DamXW St John River T11 R7 WELS Garfield Plt T11 R4 WELS Chapman Ashland Machias River Stream Carry Brook Chemquasabamticook Stream Squa Pan Stream XW Daaquam River XW Whitney Bk Dam Mars Hill Squa Pan Dam Burntland Stream DamXW Westfield Prestile Stream Presque Isle Stream FRESH WAY, INC Allagash River South Branch Machias River Big Ten Twp T10 R16 WELS T10 R15 WELS T10 R14 WELS T10 R13 WELS T10 R12 WELS T10 R11 WELS T10 R10 WELS T10 R9 WELS T10 R8 WELS 0# MARS HILL UTILITY DISTRICT T10 R3 WELS Water District Resevoir Dam T10 R7 WELS T10 R6 WELS Masardis Squapan Twp XW Mars Hill DamXW Mule Brook Penobscot RiverYosungs Lakeh DamXWed0# Southwest Branch St John Blackwater River West Branch Presque Isle Strea Allagash River North Branch Blackwater River East Branch Presque Isle Strea Blaine Churchill Lake DamXW Southwest Branch St John E Twp XW Robinson Dam Prestile Stream S Otter Brook L Saint Croix Stream Cox Patent E with Licensed Dischargers and W Snare Brook T9 R8 WELS 8 T9 R17 WELS T9 R16 WELS T9 R15 WELS T9 R14 WELS 1 T9 R12 WELS T9 R11 WELS T9 R10 WELS T9 R9 WELS Mooseleuk Stream Oxbow Plt R T9 R13 WELS Houlton Brook T9 R7 WELS Aroostook River T9 R4 WELS T9 R3 WELS 9 Chandler Stream Bridgewater T T9 R5 WELS TD R2 WELS Baker Branch Critical UmScolcus Stream lmon Habitat Overlay South Branch Russell Brook Aikens Brook West Branch Umcolcus Steam LaPomkeag Stream West Branch Umcolcus Stream Tie Camp Brook Soper Brook Beaver Brook Munsungan Stream S L T8 R18 WELS T8 R17 WELS T8 R16 WELS T8 R15 WELS T8 R14 WELS Eagle Lake Twp T8 R10 WELS East Branch Howe Brook E Soper Mountain Twp T8 R11 WELS T8 R9 WELS T8 R8 WELS Bloody Brook Saint Croix Stream North Branch Meduxnekeag River W 9 Turner Brook Allagash Stream Millinocket Stream T8 R7 WELS T8 R6 WELS T8 R5 WELS Saint Croix Twp T8 R3 WELS 1 Monticello R Desolation Brook 8 St Francis Brook TC R2 WELS MONTICELLO HOUSING CORP. -
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 -
KENNEBEC SALMON RESTORATION: Innovation to Improve the Odds
FALL/ WINTER 2015 THE NEWSLETTER OF MAINE RIVERS KENNEBEC SALMON RESTORATION: Innovation to Improve the Odds Walking thigh-deep into a cold stream in January in Maine? The idea takes a little getting used to, but Paul Christman doesn’t have a hard time finding volunteers to do just that to help with salmon egg planting. Christman is a scientist with Maine Department of Marine Resource. His work, patterned on similar efforts in Alaska, involves taking fertilized salmon eggs from a hatchery and planting them directly into the cold gravel of the best stream habitat throughout the Sandy River, a Kennebec tributary northwest of Waterville. Yes, egg planting takes place in the winter. For Maine Rivers board member Sam Day plants salmon eggs in a tributary of the Sandy River more than a decade Paul has brought staff and water, Paul and crews mimic what female salmon volunteers out on snowshoes and ATVs, and with do: Create a nest or “redd” in the gravel of a river waders and neoprene gloves for this remarkable or stream where she plants her eggs in the fall, undertaking. Finding stretches of open stream continued on page 2 PROGRESS TO UNDERSTAND THE HEALTH OF THE ST. JOHN RIVER The waters of the St. John River flow from their headwaters in Maine to the Bay of Fundy, and for many miles serve as the boundary between Maine and Quebec. Waters of the St. John also flow over the Mactaquac Dam, erected in 1968, which currently produces a substantial amount of power for New Brunswick. Efforts are underway now to evaluate the future of the Mactaquac Dam because its mechanical structure is expected to reach the end of its service life by 2030 due to problems with the concrete portions of the dam’s station. -
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.............................................................. -
A Chapter in Penobscot History
The Rebirth of a Nation? A Chapter in Penobscot History NICHOLAS N. SMITH Brunswick, Maine THE EARLIEST PERIOD The first treaty of peace between the Maine Indians and the English came to a successful close in 1676 (Williamson 1832.1:519), and it was quickly followed by a second with other Indians further upriver. On 28 April 1678, the Androscoggin, Kennebec, Saco and Penobscot went to Casco Bay and signed a peace treaty with commissioners from Massachusetts. By 1752 no fewer than 13 treaties were signed between Maine Indians negotiating with commissioners representing the Colony of Massachu setts, who in turn represented the English Crown. In 1754, George II of England, defining Indian tribes as "independent nations under the protec tion of the Crown," declared that henceforth only the Crown itself would make treaties with Indians. In 1701 Maine Indians signed the Great Peace of Montreal (Havard [1992]: 138); in short, the French, too, recognized the Maine tribes as sov ereign entities with treaty-making powers. In 1776 the colonies declared their independence, terminating the Crown's regulation of treaties with Maine Indians; beween 1754 and 1776 no treaties had been made between the Penobscot and England. On 19 July 1776 the Penobscot, Passamaquoddy, Maliseet and Micmac Indi ans acknowledged the independence of the American colonies, when a delegation from the tribes went to George Washington's headquarters to declare their allegiance to him and offered to fight for his cause. John Allan, given a Colonel's rank, was the agent for the Passamaquoddy, Maliseet and Micmac, but refused to work with the Penobscot, .. -
Penobscot River 2007 Data Report July 2008
Penobscot River 2007 Data Report July 2008 Prepared by Donald Albert, P. E. Bureau of Land and Water Quality Division of Environmental Assessment DEPLW-0882 Table of Contents Introduction ...........................................................................................................................1 Technical Design of Study ....................................................................................................1 Hydrologic Data ....................................................................................................................4 Ambient Chemical Data ........................................................................................................4 -DO, Temperature and Salinity .............................................................................................5 -Ultimate BOD ......................................................................................................................8 -Phosphorus Series ................................................................................................................11 -Nitrogen Series.....................................................................................................................13 -Chlorophyll-a .......................................................................................................................15 -Secchi disk transparency......................................................................................................17 Effluent Chemical Data .........................................................................................................18 -
Water Quality in Seboeis River
Water Quality in Seboeis River February 2020 Contact: Emily Zimmermann, Biologist Phone: (207) 446-1003 MAINE DEPARTMENT OF ENVIRONMENTAL PROTECTION 17 State House Station | Augusta, Maine 04333-0017 www.maine.gov/dep Maine Department of Environmental Protection Water Quality in Wassataquoik Stream Introduction Despite the restoration efforts of numerous groups since the 1970s, the population size of Atlantic salmon (Salmo salar) has remained low (USASAC 2018). On the Penobscot River, access has been improved by removing two major dams and constructing a bypass around a third (PRRT 2018), but three main stem dams remain between Seboeis River, a major tributary to the East Branch Penobscot River, and the ocean. The Maine Department of Marine Resources (MDMR) stopped stocking juvenile salmon in Seboeis River in 2014 due to low parr production. This stream has spawning and rearing habitat of good quality, however the watershed is likely oligotrophic, as are many nearby waters. This study investigated the hypothesis that water quality in Seboeis River exceeds stress thresholds or contains levels of nutrients too low for salmon growth. Methods Study Location Seboeis River has a large, undeveloped watershed of 705 km2, with 15% conserved land, including Katahdin Woods and Waters National Monument, Seboeis River Gorge Preserve, and Maine Bureau of Parks and Land (MBPL). The river is Maine Statutory Class AA, and its tributaries are Class A. The area has a history of industrial logging. The bedrock geology in the study area is predominantly marine sandstone and slate with some volcanics in the center of the watershed, and a small amount of granite (MGS 2019). -
Interpreting Penobscot Indian Dispossession Between 1808 and 1835 Jacques Ferland
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by University of Maine Maine History Volume 43 Article 3 Number 2 Reconstructing Maine's Wabanaki History 8-1-2007 Tribal Dissent or White Aggression?: Interpreting Penobscot Indian Dispossession Between 1808 and 1835 Jacques Ferland Follow this and additional works at: https://digitalcommons.library.umaine.edu/ mainehistoryjournal Part of the United States History Commons Recommended Citation Ferland, Jacques. "Tribal Dissent or White Aggression?: Interpreting Penobscot Indian Dispossession Between 1808 and 1835." Maine History 43, 2 (2007): 124-170. https://digitalcommons.library.umaine.edu/mainehistoryjournal/vol43/iss2/3 This Article is brought to you for free and open access by DigitalCommons@UMaine. It has been accepted for inclusion in Maine History by an authorized administrator of DigitalCommons@UMaine. For more information, please contact [email protected]. John Neptune served as Lieutenant-Governor of the Penobscot Nation for over fifty years. He, along with Tribal Governor John Attean, presided over the tribe during a period of turmoil in Penobscot history — a time marked by land dis- possession and subsequent tribal division in the first part of the nineteenth cen- tury. The portrait was painted by Obadiah Dickinson in 1836 and hung in the Blaine House for many years. Courtesy of the Maine Arts Commission. TRIBAL DISSENT OR WHITE AGGRESSION?: INTERPRETING PENOBSCOT INDIAN DISPOSSES- SION BETWEEN 1808 AND 1835. BY JACQUES FERLAND “I now come to the time when our Tribe was separated into two fac- tions[,] the old and the new Party. I am sorry to speak of it as it was very detrimental to our tribe as there was but few of us the remnant of a once powerful tribe.” So spoke Penobscot tribal leader John Attean, re- calling the 1834-1835 breach in tribal politics that shook the edifice of community and cohesion among the Penobscot people. -
Log Driving on the West Branch of the Penobscot River
The University of Maine DigitalCommons@UMaine Maine History Documents Special Collections 2016 Log Driving on the West Branch of the Penobscot River: An Addendum to Alfred Hempstead's Book The eP nobscot Boom and The evelopmeD nt of the West Branch of The eP nobscot River for Log Driving William W. Geller Follow this and additional works at: https://digitalcommons.library.umaine.edu/mainehistory Part of the History Commons Repository Citation Geller, William W., "Log Driving on the West Branch of the Penobscot River: An Addendum to Alfred Hempstead's Book The Penobscot Boom and The eD velopment of the West Branch of The eP nobscot River for Log Driving" (2016). Maine History Documents. 117. https://digitalcommons.library.umaine.edu/mainehistory/117 This Article is brought to you for free and open access by DigitalCommons@UMaine. It has been accepted for inclusion in Maine History Documents by an authorized administrator of DigitalCommons@UMaine. For more information, please contact [email protected]. Log Driving on the West Branch of the Penobscot River: An addendum to Alfred Hempstead’s Book The Penobscot Boom and The Development of the West Branch of The Penobscot River for Log Driving July 2016 William W. Geller 108 Orchard Street Farmington, Maine 04938 207-778-6672 [email protected] 1 Log Driving on the West Branch of the Penobscot River: An addendum to Alfred Hempstead’s Book, The Penobscot Boom and The Development of the West Branch of The Penobscot River for Log Driving Alfred Hempstead’s late 1920’s research on logging on the West Branch of the Penobscot and its tributaries resulted in his publication of The Penobscot Boom and The Development of the West Branch of The Penobscot River for Log Driving in 1930. -
Water Quality Summary for Kenduskeag Stream and Upper Watershed Tributaries
Water Quality Summary for Kenduskeag Stream and Upper Watershed Tributaries By Mark Whiting, Maine Department of Environmental Protection In Collaboration with Ed Lindsey Old Town High School (formerly of Central High School) March 24, 2006 DEPLW0762 Water quality summary for Kenduskeag Stream and upper watershed tributaries By Mark Whiting, Maine DEP, March 2006 Introduction: General Watershed Characteristics: Kenduskeag Stream is the largest tributary to the Penobscot River located below the first dam at Veazie. For this reason, Kenduskeag Stream has been of interest in Maine’s salmon recovery program. The Penobscot River is the largest salmon river in Maine and it has most of the remaining Atlantic salmon (ASC 2004). However a string of dams restricts fish access to the upper river. Salmon have been maintained by fish ladders, natural reproduction in the mainstem and lower tributaries, and fish stocking by Penobscot-specific strains of salmon. Fortunately, an agreement with the dam owners, federal and state agencies, the Penobscot Indian Nation, and other private organizations will provide for the removal of the two lower dams (Veazie and Great Works), a natural looking bypass channel at another dam (Howland), and improved fish passage at four additional dams. This will improve access to over 500 river miles of fish habitat. For details on the Penobscot River recovery plan see the Penobscot River Restoration Trust website (http://penobscotriver.org/index.html). Kenduskeag Stream is 36 miles long and has a watershed of 215 square miles. The mainstem has 12 named tributaries with subwatersheds that range in size from 3-26 square miles. French Stream, Black Stream and Crooked Brook are the largest tributaries with 26.3, 26.0 and 19.2 square miles respectively (Penobscot County Soil and Water Conservation District watershed plan, 1988). -
King Philip's War in Maine
The University of Maine DigitalCommons@UMaine Electronic Theses and Dissertations Fogler Library 1-1970 King Philip's War in Maine John O. Noble Jr. Follow this and additional works at: https://digitalcommons.library.umaine.edu/etd Part of the History Commons Recommended Citation Noble, John O. Jr., "King Philip's War in Maine" (1970). Electronic Theses and Dissertations. 3256. https://digitalcommons.library.umaine.edu/etd/3256 This Open-Access Thesis is brought to you for free and open access by DigitalCommons@UMaine. It has been accepted for inclusion in Electronic Theses and Dissertations by an authorized administrator of DigitalCommons@UMaine. For more information, please contact [email protected]. KING PHILIP’S WAR IN MAINE By JOHN O. NOBLE, JR. A THESIS Submitted in Partial Fulfillment of the Requirements for the Degree of Master of Arts (in History) The Graduate School University of Maine Orono January, 1970 KING PHILIP'S WAR IN MAINE By John 0. Noble, Jr. An Abstract of the Thesis Presented in Partial Fulfillment of the Requirements for the Degree of Master of Arts (in History). January, 1970 A study was made of the Indian war in Maine, which started in the late summer of 1675 and continued until the spring of *1678 The causes and consequences of the war are presented as they relate to the situation on the Northern colonial frontier (Maine), and as they contrast to the war and social situation in southern New England. The two major campaigns of the war in Maine are examined in detail. Three political questions are discussed as related to the war: (1) the legal control of Maine (2) the support of the war effort by the United Colonies of New England; and (3) the pacification effort of Massachusetts and New York to subdue the Maine Indians. -
Centerpiece of Research on the Penobscot Experimental Forest: the U.S
CENTERPIECE OF RESEARCH ON THE PENOBSCOT EXPERIMENTAL FOREST: THE U.S. FOREST SERVICE LONG-TERM SILVICULTURAL STUDY John C. Brissette and Laura S. Kenefic Abstract.—Established between 1952 and 1957, the U.S. Department of Agriculture, Forest Service experiment comparing several silvicultural treatments is not only the centerpiece of research on the Penobscot Experimental Forest in Maine, it is also one of the longest-running, replicated studies of how management techniques influence forest dynamics in North America. Ten treatments representing even- and uneven- aged silvicultural systems and exploitative cutting are replicated twice on operational- scale experimental units averaging 21 acres in size. Treatments are applied uniformly to experimental units in accordance with prescriptions designed to direct both stand structure and composition. In some treatments harvests are scheduled at intervals (e.g., 5, 10, or 20 years); in others, harvests are triggered by stand conditions. Each experimental unit, or compartment (most recently termed management unit), has an average of 18 permanent sample plots (PSPs) for measuring attributes of trees ≥0.5 inches in diameter at breast height. Tree regeneration and other vegetation are measured on multiple subplots within each PSP. Measurements are taken before and after harvests and, in many treatments, at intervals between harvests. Over the past 60 years, this long-term experiment and associated short-term studies have generated fundamental knowledge about forest ecosystems and silvicultural guidelines for the northern conifer forest type, and, in a more general sense, have contributed to our understanding of mixed-species forest science and management. INTRODUCTION research has proceeded on the PEF with periodic harvests and regular re-measurement of treatment Between 1952 and 1957 the U.S.