A History of Connecticut's Long Island Sound Boundary

Total Page:16

File Type:pdf, Size:1020Kb

A History of Connecticut's Long Island Sound Boundary The Catholic University of America, Columbus School of Law CUA Law Scholarship Repository Scholarly Articles and Other Contributions Faculty Scholarship 1972 A History of Connecticut's Long Island Sound Boundary Raymond B. Marcin The Catholic University of America, Columbus School of Law Follow this and additional works at: https://scholarship.law.edu/scholar Part of the Legal History Commons Recommended Citation Raymond B. Marcin, A History of Connecticut's Long Island Sound Boundary, 46 CONN. B.J. 506 (1972). This Article is brought to you for free and open access by the Faculty Scholarship at CUA Law Scholarship Repository. It has been accepted for inclusion in Scholarly Articles and Other Contributions by an authorized administrator of CUA Law Scholarship Repository. For more information, please contact [email protected]. 506 CONNECTICUT BAR JOURNAL [Vol. 46 A HISTORY OF CONNECTICUT'S LONG ISLAND SOUND BOUNDARY By RAYMOND B. MARciN* THE SCENEt Long before remembered time, ice fields blanketed central India, discharging floes into a sea covering the Plains of Punjab. The Argentine Pampas lay frozen and still beneath a crush of ice. Ice sheets were carving their presence into the highest mountains of Hawaii and New Guinea. On the western land mass, ice gutted what was, in pre-glacial time, a stream valley near the northeastern shore. In this alien epoch, when woolly mammoth and caribou roamed the North American tundra, the ice began to melt. Receding glaciers left an inland lake where the primeval stream valley had been. For a time the waters of the lake reposed in bo- real calm, until, with the melting of the polar cap, the level of the great salt ocean rose to the level of the lake. In in- stant metamorphosis, the glacial lake teemed with life and became a Sound.' For millennia, generations of nameless, unremembered seacoast dwellers watched as the Sound waxed secure. Men later chronicled as Pequot, Mohawk, and Mohegan shared the bounty of the Sound. Adventurers challenged its buffet- ing caps. Then, some twelve thousand years after its birth, the Sound was mute witness to the systematic and organized occupation of its shores. With that, its legal history began. * Of the Hartford Bar; member, Editorial Board, CONNECTICUT BAR JOURNAL; Assistant Professor of Law, the Catholic University of America. t For a discussion of the history of Connecticut's inland boundaries, see Bowen, The Boundary Disputes of Connecticut; James R. Osgood and Co., Boston, 1882; and Hooker, Boundaries of Connecticut; Connecticut Tercentenary Commission; Yale University Press, 1933. 1 See Simpson, ICE AGEs (1938 Annual Report to the Smithsonian Insti- tution) at 289 et seq., and Flint, GLACIAL GEOLOGY OF CONNECTICUT (State Geological and Natural History Survey, 1930), at 34, 217, 218. 1972] LONG ISLAND SOUND BOUNDARY THE CONFLICTING PATENTS The climate which gave the Sound its birth was no less chaotic than the legal climate which drifted to its shores in the early seventeenth century. The initial and obvious question as to the territorial rights of the native occupants of the coastal lands of the "New" World was settled sum- marily by European consensus: [A]ccording to principles of international law, as then understood by the civilized powers of Europe, the Indian tribes in the new world were regarded as mere temporary occupants of the soil, and the absolute rights of property and dominion were held to belong to the European nation by which any2 particular portion of the country was first discovered. Territorial boundaries depended upon often conflicting letters patent, treaties, and land ,grants from various Euro- pean Crowns, and, consequently, overlapped considerably. The coastal boundary of Connecticut seems to have been rooted in three separate documents: The Warwick Patenit of 1631, the Charter of Connecticut of 1662, and the York Patent of 1664. The State of New York, however, has ad- vanced two other patents as supportive of its claims with respect to Long Island Sound: A patent to the Earl of Sterling in 1614 and a York patent of 1674.1 Further com- plicating the situation was the Treaty of Hartford of 1650 between the Colony of Connecticut and the States General of Holland, in which the Dutch gave Connecticut all of 4 Long Island itself east of Oyster Bay. The Warwick Patent is dated March 19, 1631. Robert, 2 Martin v. Waddell, 41 U.S. (16 Pet.) 367, 409 (1842). 3 See Report of the New York Commissioners Appointed to Settle the Disputed Boundary Lines with the State of Connecticut, 1880 New York State Assembly Documents, vol. 3, no. 53, at 7. 4 The treaty is mentioned in Keyser v. Coe, 14 Fed. Cas. 442, 445 (No. 7,750) (C.C.D. Conn. 1871). The Federal Circuit Court for the District of Connecticut, while not called upon to vindicate Connecticut's claims to Long Island itself, nevertheless observed that it was well known that long prior to the York Patent, Connecticut did in fact exercise jurisdiction over a large part of Long Island. CONNECTICUT BAR JOURNAL [Vol. 46 Earl of Warwick, derived his title to the patent lands from the Council of Plymouth by a grant made to him in 1630 and confirmed by a patent from Charles I. The Council of Plymouth, in turn, held the lands under the Great Patent of New England from James I, dated November 3, 1620. In relevant part, the lands granted by the Warwick Patent include: All that part of New England, in America which lies and extends itself from a river there called Narraganset river, the space of forty leagues, upon a straight line, near the sea shore, towards the southwest, west and by south, or west, as the coast lieth, towards Virginia, ac- counting three English miles to the league; and, also all and singular the lands and hereditaments whatsoever, ly- ing and being within the lands aforesaid, north and south, in latitude and breadth, and length and longtitude, of and within all the breadth aforesaid, throughout the main lands there, from the Western Ocean to the South Sea, and all lands and grounds, place and places, soil, wood and woods, grounds, havens, ports, creeks and rivers, waters, fishings, and hereditaments whatsoever, lying within said space, and every part thereof; and, also, all islands lying in America aforesaid, in the said seas, or either of them, on the western or eastern coasts or parts of said tracts of lands by these presents mentioned to be given, granted ....5 So Warwick gave not only Long Island Sound, but also Long Island itself to Connecticut. Right? Not quite. Al- though the Great Patent of New England (out of which the Warwick Patent was carved) granted to the Council of Plymouth the whole region from the fortieth to the forty- eighth degrees of north latitude, "with all the seas, rivers, islands, creeks, inlets, ports, and havens within those de- grees,"' and although the Charter of Connecticut of 1662 bounded the Colony "south by the sea" (ocean), another patent was in conflict. On March 12, 1664, Charles II granted to his brother, the Duke of York, 5 Quoted in Keyser v. Coe, supra n. 4, at 443. Old. at 445. 1972] LONG ISLAND SOUND BOUNDARY . all that island or islands commonly called by the several name or names Matowacks or Long Island . together with all the lands, islands ... harbors, . fishings, . to the said several islands, lands, and premises belonging and appertaining, with their and every of their appurtenances .... The double grant of Long Island was settled in November of 1664, when a royal commission (attended by Connecti- cut delegates, including the Colony's governor) decreed . that the southern boundary of his majestie's colony of Connecticut is the sea, and that Long Island is to be the government of his royal highness the Duke of York ....8 HIGH SEAS, TERRiTORiAL WATERS, OR INLAND WATERWAY From the settlement of 1664 to the latter part of the nine- teenth century, the question as to whether Long Island Sound was (1) high seas and, therefore, the common prop- erty of all nations, (2) territorial waters and, therefore, subject to federal jurisdiction, or (3) an inland waterway owned by New York, Connecticut, or both was as unsettled as ever a question has been. In 1765, in an action of trespass for cutting timber on Great Captain's Island in Long Island Sound, the Connecti- cut Superior Court found that the island in question was within the colony of Connecticut, and not New York.' In 1810, a federal court in New York, drawing on the Charter of Connecticut of 1662 and the York Patent of 1664, found that the Sound belonged neither to Connecticut nor to New York, although it did not reach the question whether it was a territorial sea appertaining to the United States or a part of the high seas and common to all nations. ° In 1843, a federal district court in New York attempted 7 Id. at 444. 8 Id. at 4 45. 9 Id. at 447, discussing Bush v. Anderson, Connecticut Superior Court, February 23, 1765. 10The Sloop Elizabeth, 8 Fed. Cas. 468, 469 (No. 4,352) (C.C.D.N.Y. 1810). 510 CONNECTICUT BAR JOURNAL [Vol. 46 to resolve the controversy when it ruled that Long Island Sound was an arm of the sea under the maritime jurisdiction of the United States: The Sound is an arm of the sea, within the common law acceptation of the term, being navigable tide-water (cita- tions), and more specifically an arm of the sea than mere rivers, bays or inlets; because in addition to its tide- water and navigable quality, it is without the territorial limits of any county (citation).
Recommended publications
  • Long Island Sound Habitat Restoration Initiative
    LONG ISLAND SOUND HABITAT RESTORATION INITIATIVE Technical Support for Coastal Habitat Restoration FEBRUARY 2003 TABLE OF CONTENTS TABLE OF CONTENTS INTRODUCTION ....................................................................i GUIDING PRINCIPLES.................................................................................. ii PROJECT BOUNDARY.................................................................................. iv SITE IDENTIFICATION AND RANKING........................................................... iv LITERATURE CITED ..................................................................................... vi ACKNOWLEDGEMENTS............................................................................... vi APPENDIX I-A: RANKING CRITERIA .....................................................................I-A-1 SECTION 1: TIDAL WETLANDS ................................................1-1 DESCRIPTION ............................................................................................. 1-1 Salt Marshes ....................................................................................................1-1 Brackish Marshes .............................................................................................1-3 Tidal Fresh Marshes .........................................................................................1-4 VALUES AND FUNCTIONS ........................................................................... 1-4 STATUS AND TRENDS ................................................................................
    [Show full text]
  • New York City Comprehensive Waterfront Plan
    NEW YORK CITY CoMPREHENSWE WATERFRONT PLAN Reclaiming the City's Edge For Public Discussion Summer 1992 DAVID N. DINKINS, Mayor City of New lVrk RICHARD L. SCHAFFER, Director Department of City Planning NYC DCP 92-27 NEW YORK CITY COMPREHENSIVE WATERFRONT PLAN CONTENTS EXECUTIVE SUMMA RY 1 INTRODUCTION: SETTING THE COURSE 1 2 PLANNING FRA MEWORK 5 HISTORICAL CONTEXT 5 LEGAL CONTEXT 7 REGULATORY CONTEXT 10 3 THE NATURAL WATERFRONT 17 WATERFRONT RESOURCES AND THEIR SIGNIFICANCE 17 Wetlands 18 Significant Coastal Habitats 21 Beaches and Coastal Erosion Areas 22 Water Quality 26 THE PLAN FOR THE NATURAL WATERFRONT 33 Citywide Strategy 33 Special Natural Waterfront Areas 35 4 THE PUBLIC WATERFRONT 51 THE EXISTING PUBLIC WATERFRONT 52 THE ACCESSIBLE WATERFRONT: ISSUES AND OPPORTUNITIES 63 THE PLAN FOR THE PUBLIC WATERFRONT 70 Regulatory Strategy 70 Public Access Opportunities 71 5 THE WORKING WATERFRONT 83 HISTORY 83 THE WORKING WATERFRONT TODAY 85 WORKING WATERFRONT ISSUES 101 THE PLAN FOR THE WORKING WATERFRONT 106 Designation Significant Maritime and Industrial Areas 107 JFK and LaGuardia Airport Areas 114 Citywide Strategy fo r the Wo rking Waterfront 115 6 THE REDEVELOPING WATER FRONT 119 THE REDEVELOPING WATERFRONT TODAY 119 THE IMPORTANCE OF REDEVELOPMENT 122 WATERFRONT DEVELOPMENT ISSUES 125 REDEVELOPMENT CRITERIA 127 THE PLAN FOR THE REDEVELOPING WATERFRONT 128 7 WATER FRONT ZONING PROPOSAL 145 WATERFRONT AREA 146 ZONING LOTS 147 CALCULATING FLOOR AREA ON WATERFRONTAGE loTS 148 DEFINITION OF WATER DEPENDENT & WATERFRONT ENHANCING USES
    [Show full text]
  • 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. _ _______________
    [Show full text]
  • Bedrock Geologic Map of the New Milford Quadrangle, Litchfield and Fairfield Counties, Connecticut
    U.S. DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY Prepared in cooperation with the State of Connecticut, Geological and Natural History Survey BEDROCK GEOLOGIC MAP OF THE NEW MILFORD QUADRANGLE, LITCHFIELD AND FAIRFIELD COUNTIES, CONNECTICUT By Gregory J. Walsh1 Open-File Report 03-487 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). Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government. ______________________________________________________________________________ 1U.S. Geological Survey P.O. Box 628 Montpelier, Vermont 05601 The map and database of this report are available online at: http://pubs.usgs.gov/of/2003/of03-487/ USGS Open File Report 03-487 On the cover: Photograph of Lake Candlewood from Hubbell Hill in Sherman. View is to the south. Green Island and Deer Island are visible in the center of the view. The Vaughns Neck peninsula is visible on the left side of the photograph. Bedrock Geologic Map of the New Milford Quadrangle, Litchfield and Fairfield Counties, Connecticut 2 USGS Open File Report 03-487 TABLE OF CONTENTS INTRODUCTION .......................................................................................................................... 4 STRATIGRAPHY .......................................................................................................................... 6 MESOPROTEROZOIC GNEISS..............................................................................................
    [Show full text]
  • Long Island Sound Ecologically Significant Areas
    Long Island Sound Ecologically Significant Areas LIS Blue Plan Webinar Speakers: Nathan Frohling Director of Coastal and Marine Initiatives, The Nature Conservancy of CT Blue Plan Advisory Committee member Chair, Ecological Characterization Work Team Emily Shumchenia, PhD. E & C Enviroscape Ecological Consultant to the Blue Plan Ecological Characterization process Presentation Outline: 1. Purpose of the meeting & Blue Plan overview 2. Ecologically Significant Areas (ESA): Basics 3. The ESA Development Process 4. DRAFT Ecologically Significant Areas 5. Ecologically Significant Areas and policy: example 6. Next Steps & Discussion Purpose of webinar: • Preview Draft LIS Ecologically Significant Areas • High level feedback • Encourage deeper review & feedback; March 1, 2019 LIS Blue Plan: Why do we need it? Increasing demands pose potential conflicts with human uses & marine life Insufficient mechanisms for managing use of the Sound as a whole Individual proposals and permit applications set the future course What is the Blue Plan? • 2015 legislation: Develop Blue Plan to guide new uses & “manage Sound as a whole” • Produce an Inventory of Human Uses and Natural Resources • Develop policies about where new things go – marine spatial planning - maps • Policies guide and direct how State permits and decision-making is to be carried out Organization • Led by CT DEEP • Guided by 16 member Advisory Committee • Coordinated with NY as much as possible Principal Goals: • Identify and protect places of ecological significance • Identify and protect
    [Show full text]
  • Trace Metals, Organic Carbon, and Inorganic Nutrients in Surface Waters of the Long Island Sound: Sources, Cycling and Effects on Phytoplankton Growth
    Final Report Grant X982277-01 Trace Metals, Organic Carbon, and Inorganic Nutrients in Surface Waters of the Long Island Sound: Sources, Cycling and Effects on Phytoplankton Growth. Sergio Sañudo-Wilhelmy; Marine Sciences Research Center, SUNY Stony Brook. Christopher Gobler; Southampton College, Long Island University. Summary This study provides an extensive dataset of dissolved trace metals (silver, cadmium, copper, nickel, lead, iron, and zinc), inorganic (ammonia, nitrate, phosphate and silicates), and organic (urea, dissolved organic nitrogen, carbon and phosphorous, as well as particulate carbon and nitrogen) constituents during high and low riverine flow conditions in surface waters of the Long Island Sound. Analysis of the data showed that the mechanisms influencing the biogeochemistry of the Sound are very complex. However, a few preliminary conclusions could be drawn: • There are two distinct biogeochemical regimes within the Long Island Sound: an area of relatively high metal levels in the East River/Narrows and an area in the eastern region of the Sound that had comparatively lower levels. • During low flow conditions, the East River was the most dominant external source of most trace metals, while during high flow conditions; the most important external source was the Connecticut River. • Large internal sources of copper, nickel and zinc were detected under low flow conditions implicating the importance of internal processes such as remobilization from contaminated sediments within the Sound. • The mechanisms controlling the biogeochemistry of the Long Island Sound were different under different river flow. During high flow conditions, the system was most influenced by biological activity. During low flow conditions, the Long Island Sound was influenced by the remobilization of metals from contaminated sediments.
    [Show full text]
  • New York City Area: Health Advice on Eating Fish You Catch
    MAPS INSIDE NEW YORK CITY AREA Health Advice on Eating Fish You Catch 1 Why We Have Advisories Fishing is fun and fish are an important part of a healthy diet. Fish contain high quality protein, essential nutrients, healthy fish oils and are low in saturated fat. However, some fish contain chemicals at levels that may be harmful to health. To help people make healthier choices about which fish they eat, the New York State Department of Health issues advice about eating sportfish (fish you catch). The health advice about which fish to eat depends on: Where You Fish Fish from waters that are close to human activities and contamination sources are more likely to be contaminated than fish from remote marine waters. In the New York City area, fish from the Long Island Sound or the ocean are less contaminated. Who You Are Women of childbearing age (under 50) and children under 15 are advised to limit the kinds of fish they eat and how often they eat them. Women who eat highly contaminated fish and become pregnant may have an increased risk of having children who are slower to develop and learn. Chemicals may have a greater effect on the development of young children or unborn babies. Also, some chemicals may be passed on in mother’s milk. Women beyond their childbearing years and men may face fewer health risks from some chemicals. For that reason, the advice for women over age 50 and men over age 15 allows them to eat more kinds of sportfish and more often (see tables, pages 4 and 6).
    [Show full text]
  • Hudson River National Estuarine Research Reserve Management Plan OCTOBER 1, 2019–OCTOBER 1, 2024
    Hudson River National Estuarine Research Reserve Management Plan OCTOBER 1, 2019–OCTOBER 1, 2024 Andrew M. Cuomo, Governor | Basil Seggos, Commissioner Acknowledgments This plan was prepared by staff of the Hudson River National Estuarine Research Reserve, including Betsy Blair, Chris Bowser, Ann-Marie Caprioli, Brian DeGasperis, Sarah Fernald, Heather Gierloff, Emilie Hauser, Dan Miller, and Sarah Mount, with the assistance of Andy Burgher, Cathy Kittle, and Bill Rudge in the New York State Department of Environmental Conservation; Ed McGowan of the New York State Office of Parks, Recreation and Historic Preservation; and Nina Garfield and Ann Weaver of the National Oceanic and Atmospheric Administration, Office for Coastal Management. We appreciate input that has informed development of this plan provided by other colleagues, local leaders, county officials, environmental organizations, researchers, educators, and marsh managers. Suggested citation: New York State Department of Environmental Conservation (NYSDEC). 2019. Hudson River National Estuarine Research Reserve Management Plan. Albany, NY. Table of Contents Executive Summary ................................................................................................................................... iv Introduction ................................................................................................................................................. 1 The Reserve .........................................................................................................................................
    [Show full text]
  • Long Island Sound Report Card 2018
    Long Island Sound Report Card 2018 Grading the water quality and ecosystem health of the Urban Sea Investing in Sewage Take Action Treatment Improves Reduce water usage Water Quality Install high-efficiency appliances and fixtures. Don’t overwater your lawn. When New York and Connecticut built our sewage treatment plants decades ago, the public appreciated the reduction of fecal bacteria and other contaminants Eliminate or reduce fertilizer use Leave grass clippings on the lawn. Don’t use that allowed for swimming and sports, and harvesting fertilizer. Or reduce amount by 50% and apply of healthy shellfish. Considered less of a threat at the at the right time – around Labor Day or time was the devastating impact of high volumes of Memorial Day. human-sourced nutrients on ecosystem health and the quality of life in coastal communities. Keep litter out of waterways Don’t put garbage in street catch basins. Switch By the 1980s, the steady increase in population and to reusable bags, straws, water bottles, and the nutrients excreted by humans into our toilet bowls coffee mugs. caught up with Long Island Sound; traditional sewage treatment plants do not remove these nutrients. Har- Pump out your septic system bors full of dying fish and shellfish, dirty beaches, and Have your septic system inspected and pumped waters almost devoid of oxygen got the attention of out every 3 years. the public and EPA. Care for your pipes In 2000, EPA, New York State, and Connecticut agreed If you have back-ups in your sewer line, have it to make a significant investment in a clean and healthy video inspected and repair any cracks.
    [Show full text]
  • Interim Guidance for Office-Based Work During the Covid-19 Public Health Emergency
    INTERIM GUIDANCE FOR OFFICE-BASED WORK DURING THE COVID-19 PUBLIC HEALTH EMERGENCY When you have read this document, you can affirm at the bottom. As of June 8, 2021 Purpose This Interim Guidance for Office-Based Work during the COVID-19 Public Health Emergency (“Interim COVID-19 Guidance for Office-Based Work”) was created to provide businesses and entities that operate in office spaces and their employees and contractors with precautions to help protect against the spread of COVID-19 as their businesses reopen or continue to operate. This guidance addresses business activities where the core function takes place within an office setting. This guidance may apply – but is not limited – to businesses and entities in the following sectors: Professional services, nonprofit, technology, administrative support, and higher education administration (excluding full campus reopening). Please note that these guidelines may also apply to business operating parts of their business functions under different guidelines (e.g. front office for a construction company). This guidance does not address medical offices, such as doctors’ offices or dentists’ offices. This guidance also does not address building owners/managers and their employees or contractors. For more information on building management, see, “Interim COVID-19 Guidance for Commercial Building Management.” Owners and operators of offices are authorized to require masks and six feet of social distancing for employees within their establishments or adhere to DOH guidance, consistent with the Centers for Disease Control and Prevention’s (CDC) “Interim Public Health Recommendations for Fully Vaccinated People.” If choosing to adhere to CDC guidance, offices generally do not congregate patrons or operate above the State’s social gathering limits, and must follow applicable guidelines for masks, distancing, and capacity as outlined in New York State’s guidelines on Implementing CDC Guidance.
    [Show full text]
  • GEOLOGY and GROUND WATER RESOURCE S of Stutsman County, North Dakota
    North Dakota Geological Survey WILSON M. LAIRD, State Geologis t BULLETIN 41 North Dakota State Water Conservation Commission MILO W . HOISVEEN, State Engineer COUNTY GROUND WATER STUDIES 2 GEOLOGY AND GROUND WATER RESOURCE S of Stutsman County, North Dakota Part I - GEOLOG Y By HAROLD A. WINTERS GRAND FORKS, NORTH DAKOTA 1963 This is one of a series of county reports which wil l be published cooperatively by the North Dakota Geological Survey and the North Dakota State Water Conservation Commission in three parts . Part I is concerned with geology, Part II, basic data which includes information on existing well s and test drilling, and Part III which will be a study of hydrology in the county . Parts II and III will be published later and will be distributed a s soon as possible . CONTENTS PAGE ABSTRACT 1 INTRODUCTION 3 Acknowledgments 3 Previous work 5 GEOGRAPHY 5 Topography and drainage 5 Climate 7 Soils and vegetation 9 SUMMARY OF THE PRE-PLEISTOCENE STRATIGRAPHY 9 Precambrian 1 1 Paleozoic 1 1 Mesozoic 1 1 PREGLACIAL SURFICIAL GEOLOGY 12 Niobrara Shale 1 2 Pierre Shale 1 2 Fox Hills Sandstone 1 4 Fox Hills problem 1 4 BEDROCK TOPOGRAPHY 1 4 Bedrock highs 1 5 Intermediate bedrock surface 1 5 Bedrock valleys 1 5 GLACIATION OF' NORTH DAKOTA — A GENERAL STATEMENT 1 7 PLEISTOCENE SEDIMENTS AND THEIR ASSOCIATED LANDFORMS 1 8 Till 1 8 Landforms associated with till 1 8 Glaciofluvial :materials 22 Ice-contact glaciofluvial sediments 2 2 Landforms associated with ice-contact glaciofluvial sediments 2 2 Proglacial fluvial sediments 2 3 Landforms associated with proglacial fluvial sediments 2 3 Lacustrine sediments 2 3 Landforms associated with lacustrine sediments 2 3 Other postglacial sediments 2 4 ANALYSIS OF THE SURFICIAL TILL IN STUTSMAN COUNTY 2 4 Leaching and caliche 24 Oxidation 2 4 Stone counts 2 5 Lignite within till 2 7 Grain-size analyses of till _ 2 8 Till samples from hummocky stagnation moraine 2 8 Till samples from the Millarton, Eldridge, Buchanan and Grace Cit y moraines and their associated landforms _ .
    [Show full text]
  • 1997 Connecticut-New York State Boundary Line Perambulation Connecticut Department of Transportation
    1997 CONNECTICUT-NEW YORK STATE BOUNDARY LINE PERAMBULATION CONNECTICUT DEPARTMENT OF TRANSPORTATION 1997 CONNECTICUT-NEW YORK STATE BOUNDARY LINE PERAMBULATION CONNECTICUT DEPARTMENT OF TRANSPORTATION BOUND 46 PHOTOGRAPHED NORTHWESTERLY PHOTOGRAPHED SOUTHWESTERLY 1997 CONNECTICUT-NEW YORK STATE BOUNDARY LINE PERAMBULATION CONNECTICUT DEPARTMENT OF TRANSPORTATION LINE BOUND #46 REGULATION GRANITE MONUMENT PAVED HIGHWAY From the center of the Village of Bulls Bridge at the intersection of US Route 7 and Bulls Bridge Road, proceed westerly and southerly on Bulls Bridge Road to Bound at 0.8 mile. Bound is located 19 feet west of the center of the traveled way and 4.5 feet east of the west highway fence. It is 230 feet north of the point where the highway turns west to Dogtail Corners and 70 feet south of a stone wall running to the west. There is woodland to the west and scrub woodland to the east. Bound is marked by a regulation granite monument showing 4.0 feet above ground. It is 8.4 feet long. Monument was originally set September 29, 1910, 0.17 feet west of the location of the old 1860 marble monument (#26) which was destroyed when the new monument was set. It was reset November 4, 1937, 231.5 feet north of its former location in connection with highway reconstruction. All top corners of Bound are chipped, with a larger chip on the northeast corner. 1909 Station 138036 (present location) Bound #45 - 6693 feet north Bound #47 - 1825 feet south 1997 CONNECTICUT-NEW YORK STATE BOUNDARY LINE PERAMBULATION CONNECTICUT DEPARTMENT OF TRANSPORTATION BOUND 47 PHOTOGRAPHED EASTERLY PHOTOGRAPHED NORTHEASTERLY 1997 CONNECTICUT-NEW YORK STATE BOUNDARY LINE PERAMBULATION CONNECTICUT DEPARTMENT OF TRANSPORTATION LINE BOUND #47 REGULATION GRANITE MONUMENT GRAVEL ROAD From the intersection of Routes U.S.
    [Show full text]