2. Biophysical Regions and a Landscape Perspective for Conservation and Management
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Brooklyn College and Graduate School of the City University of NY, Brooklyn, NY 11210 and Northeastern Science Foundation Affiliated with Brooklyn College, CUNY, P.O
FLYSCH AND MOLASSE OF THE CLASSICAL TACONIC AND ACADIAN OROGENIES: MODELS FOR SUBSURFACE RESERVOIR SETTINGS GERALD M. FRIEDMAN Brooklyn College and Graduate School of the City University of NY, Brooklyn, NY 11210 and Northeastern Science Foundation affiliated with Brooklyn College, CUNY, P.O. Box 746, Troy, NY 12181 ABSTRACT This field trip will examine classical sections of the Appalachians including Cambro-Ordovician basin-margin and basin-slope facies (flysch) of the Taconics and braided and meandering stteam deposits (molasse) of the Catskills. The deep water settings are part of the Taconic sequence. These rocks include massive sandstones of excellent reservoir quality that serve as models for oil and gas exploration. With their feet, participants may straddle the classical Logan's (or Emmon 's) line thrust plane. The stream deposits are :Middle to Upper Devonian rocks of the Catskill Mountains which resulted from the Acadian Orogeny, where the world's oldest and largest freshwater clams can be found in the world's oldest back-swamp fluvial facies. These fluvial deposits make excellent models for comparable subsurface reservoir settings. INTRODUCTION This trip will be in two parts: (1) a field study of deep-water facies (flysch) of the Taconics, and (2) a field study of braided- and meandering-stream deposits (molasse) of the Catskills. The rocks of the Taconics have been debated for more than 150 years and need to be explained in detail before the field stops make sense to the uninitiated. Therefore several pages of background on these deposits precede the itinera.ry. The Catskills, however, do not need this kind of orientation, hence after the Taconics (flysch) itinerary, the field stops for the Catskills follow immediately without an insertion of background informa tion. -
Introduction
Introduction This is the fourteenth edition of Profiles of New York State—Facts, Figures & Statistics for 2,570 Populated Places in New York. As with the other titles in our State Profiles series, it was built with content from Grey House Publishing’s award-winning Profiles of America—a 4-volume compilation of data on more than 43,000 places in the United States. We have included the New York chapter from Profiles of America, and added several new chapters of demographic information and ranking sections, so that Profiles of New York State is the most comprehensive portrait of the state of New York ever published. Profiles of New York State provides data on all populated communities and counties in the state of New York for which the US Census provides individual statistics. This edition also includes profiles of 444 unincorporated places and neighborhoods (i.e. Flushing, Queens) based on US Census data by zip code. This premier reference work includes five major sections that cover everything from Education to Ethnic Backgrounds to Climate. All sections include Comparative Statistics or Rankings. A section called About New York at the front of the book includes detailed narrative and colorful photos and maps. Here is an overview of each section: 1. About New York This 4-color section gives the researcher a real sense of the state and its history. It includes a Photo Gallery, and comprehensive sections on New York’s Government, Timeline of New York History, Land and Natural Resources, New York State Energy Profile and Demographic Maps. These 42 pages, with the help of photos, maps and charts, anchor the researcher to the state, both physically and politically. -
Champlain Valley (Why Are Clay Soils Where They Are?)
Geomorphic history of the Champlain Valley (why are clay soils where they are?) part 1) How did landscape evolve and where do “clay” minerals come from? part 2) How were they deposited in Lake Vermont/ Champlain Sea? part 3) Can we predict the distribution of “clay” thickness? (…can we compare prediction with what people observe) 500,000,000 years Today ~500,000,000 years: Sediments of “Champlain Valley Sequence” deposited on shoreline of ancient ocean Monkton quartzite + Taconic Slates Limestones + Marbles ~460,000,000 years: Collision of island arc causes thrusting + metamorphism Champlain Thrust Fault Champlain Thrust: -Exposed at Snake Mtn + Mt. Philo -delineates boundary between “low” and “mid” grade metamorphic rocks -Marbles pf middlebury syncline folded along back of thrust -Topography of Addison County reflects erodibility of bedrock: T1: lower surface: “low grade” sedimentary rocks below thrust (e.g. shale) T2: upper surface: “mid grade” meta-sedimentary rocks above thrust (e.g. marble) Green Mountains= “high grade” metamorphic rocks (e.g. schist and gneiss) T1 T2 Green Mtn gneiss Geologic map of Addison County Taconics Part 2: How were clays deposited in Lake Vermont and the Champlain Sea? 500,000,000 years Today ~96,000 - 20,000 years (i.e. yesterday…): Champlain Valley sat below 1-3 km of ice Soils and clay minerals from previous inter-glacial cycles were stripped by advancing glaciers Rocks were ground into “clay size fraction” and trapped under ice retreating glacial ice withdrew from Champlain Valley between ~14-13 kyr Many depositional features in Champlain Valley record ice retreat -Layers of “basal till” deposited beneath ice sheets (coarse, angular, poorly sorted debris) -Meltwater streams flow between glacier and hillslopes -Sedimentary deposits accumulate, leaving ‘kame terraces’ when glacier retreats Lake Vermont had 2+ stages: Coveville: Ice dammed in So. -
Research Bibliography on the Industrial History of the Hudson-Mohawk Region
Research Bibliography on the Industrial History of the Hudson-Mohawk Region by Sloane D. Bullough and John D. Bullough 1. CURRENT INDUSTRY AND TECHNOLOGY Anonymous. Watervliet Arsenal Sesquicentennial, 1813-1963: Arms for the Nation's Fighting Men. Watervliet: U.S. Army, 1963. • Describes the history and the operations of the U.S. Army's Watervliet Arsenal. Anonymous. "Energy recovery." Civil Engineering (American Society of Civil Engineers) 54 (July 1984): 60- 61. • Describes efforts of the City of Albany to recycle and burn refuse for energy use. Anonymous. "Tap Industrial Technology to Control Commercial Air Conditioning." Power 132 (May 1988): 91–92. • The heating, ventilation and air–conditioning (HVAC) system at the Empire State Plaza in Albany is described. Anonymous. "Albany Scientist Receives Patent on Oscillatory Anemometer." Bulletin of the American Meteorological Society 70 (March 1989): 309. • Describes a device developed in Albany to measure wind speed. Anonymous. "Wireless Operation Launches in New York Tri- Cities." Broadcasting 116 10 (6 March 1989): 63. • Describes an effort by Capital Wireless Corporation to provide wireless premium television service in the Albany–Troy region. Anonymous. "FAA Reviews New Plan to Privatize Albany County Airport Operations." Aviation Week & Space Technology 132 (8 January 1990): 55. • Describes privatization efforts for the Albany's airport. Anonymous. "Albany International: A Century of Service." PIMA Magazine 74 (December 1992): 48. • The manufacture and preparation of paper and felt at Albany International is described. Anonymous. "Life Kills." Discover 17 (November 1996): 24- 25. • Research at Rensselaer Polytechnic Institute in Troy on the human circulation system is described. Anonymous. "Monitoring and Data Collection Improved by Videographic Recorder." Water/Engineering & Management 142 (November 1995): 12. -
Municipal Plan for the Town and Village of Ludlow, Vermont
Municipal Plan For the Town and Village of Ludlow, Vermont Adopted by the Ludlow Village Trustees on October 8, 2019 Adopted by the Ludlow Select Board on October 7, 2019 Ludlow Municipal Plan Adopted October 2019 Adopted by the Ludlow Village Trustees on January 2, 2018 Adopted by the Ludlow Select Board on December 4, 2017 Amended by the Ludlow Select Board on November 7, 2016 Amended by the Ludlow Select Board on August 3, 2015 Amended by the Ludlow Village Trustees on August 4, 2015 Adopted by the Ludlow Select Board on November 5, 2012 Adopted by the Ludlow Village Trustees on March 5, 2013 This Ludlow Municipal Plan was developed in 2018-2019 by the Ludlow Planning Commission with assistance from the Southern Windsor County Regional Planning Commission, Ascutney, VT. Financial support for undertaking this and previous revisions was provided, in part, by a Municipal Planning Grant from the Vermont Agency of Commerce and Community Development. Photo Credits: Many of the pictures found throughout this document were generously provided by Tom Johnson. ii Ludlow Municipal Plan Adopted October 2019 Contents 1 Introduction .................................................................................................................................. 1 1.1 Purpose .................................................................................................................................. 1 1.2 Public Process ....................................................................................................................... 1 1.3 -
Taconic Physiography
Bulletin No. 272 ' Series B, Descriptive Geology, 74 DEPARTMENT OF THE INTERIOR . UNITED STATES GEOLOGICAL SURVEY CHARLES D. WALCOTT, DIRECTOR 4 t TACONIC PHYSIOGRAPHY BY T. NELSON DALE WASHINGTON GOVERNMENT PRINTING OFFICE 1905 CONTENTS. Page. Letter of transinittal......................................._......--..... 7 Introduction..........I..................................................... 9 Literature...........:.......................... ........................... 9 Land form __._..___.._.___________..___._____......__..__...._..._--..-..... 18 Green Mountain Range ..................... .......................... 18 Taconic Range .............................'............:.............. 19 Transverse valleys._-_-_.-..._.-......-....___-..-___-_....--_.-.._-- 19 Longitudinal valleys ............................................. ^...... 20 Bensselaer Plateau .................................................... 20 Hudson-Champlain valley................ ..-,..-.-.--.----.-..-...... 21 The Taconic landscape..................................................... 21 The lakes............................................................ 22 Topographic types .............,.....:..............'.................... 23 Plateau type ...--....---....-.-.-.-.--....-...... --.---.-.-..-.--... 23 Taconic type ...-..........-........-----............--......----.-.-- 28 Hudson-Champlain type ......................"...............--....... 23 Rock material..........................'.......'..---..-.....-...-.--.-.-. 23 Harder rocks ....---...............-.-.....-.-...--.-......... -
Fostertext Pdf, Rev
HISTORY AND DYNAMICS OF A RIDGETOP PITCH PINE COMMUNITY MOUNT EVERETT, MASSACHUSETTS GLENN MOTZKIN DAVID A. ORWIG and DAVID R. FOSTER HISTORY AND DYNAMICS OF A RIDGETOP PITCH PINE COMMUNITY MOUNT EVERETT, MASSACHUSETTS GLENN MOTZKIN DAVID A. ORWIG and DAVID R. FOSTER 2002 HARVARD FOREST HARVARD UNIVERSITY PETERSHAM, MASSACHUSETTS HARVARD FOREST PAPER NO. 25 Copyright © 2002 by the President and Fellows of Harvard College All rights reserved. Printed in the United States of America Front cover: Southern slope of Mt. Everett viewed from Mt. Race. Back cover: Contorted crown of red oak (Quercus rubra) with scars and broken branches from winter storms. SUMMARY 1. The summit of Mt. Everett in the Town of Mount early historical periods. Because the site has long Washington, Massachusetts supports a highly been a destination for local residents for recre- unusual dwarf pitch pine-oak community; similar ation and for berry gathering, it is possible that vegetation is found on only a few sites throughout fire or cutting were used historically to improve the northeastern United States. Age-structure fruit production or expand views, but we found analyses and historical records of human and no documentation of such activities. natural disturbance were used to investigate the 5. During the twentieth century, under management long-term history and dynamics of the summit by the Commonwealth of Massachusetts, access vegetation. trails and two fire towers were constructed on the 2. Throughout the historical period, the summit of summit, one of which still stands although it is in Mt. Everett has been dominated by dwarf pitch poor repair and has rarely, if ever, been staffed. -
Smuggling Into Canada: How the Champlain Valley Defied Jefferson's Embargo
Wimer 1970 VOL. XXXVIII No. I VERMONT History The 'PROCEEDINGS of the VERMONT HISTORICAL SOCIETY Smuggling into Canada; How the Champlain Valley Defied Jefferson's Embargo by H. N. MULLER HEN Britain resumed open hostilities against France in 1803, the W relative tranquillity of Anglo-American relations was among the first casualties. By 1805, after Napoleon's success at AusterlilZ and Nel son's decisive victory at Trafalgar, the contest became a stalemate. With the French dominating the Continent and the British the sea, neither side could afford to observe the amenities of neutral rights. Britain took steps to close the loop-holes by which American merchantmen evaded the notorious orders-in-eouncil. and her navy renewed in earnest its harassing and degrading practice of impressing American citizens. III feeling and tension mounted as Anglo-American relations disinte grated. Then in late June 1807 tbe British frigate uopard fired on the United States Frigate Chesapeake, killing three American seamen and wounding eighteen others, and a party from the Leopard boarded the American warship and removed four alleged British deserters. The Chesapeake affair precipitated an ugly crisis. Americans, now more united in hostility toward Britain than at any time since the Revolution, demanded action from their government.l President Thomas Jefferson responded with the Embargo Act, hastily pushed through a special session of Congress and signed in December 1807. Jefferson held the illusory hope that by withholding its produce and its merchant marine, tbe United States would forcc Britain and c"en I. Burl. Th~ Uniud S/a'~. Grea/Britain, lind British Nor/II Amerjea (New Haven. -
Central Champlain Valley Trail
C ENTRAL C HAMPLAIN V ALLEY “This world needs many paths into the future and some of the sweetest C D E F G are on CATS trails.” Champlain Area Trails also publishes a map – Bill McKibben, acclaimed author of of NY’s Northern Champlain Valley Trails. Wandering Home, A Walk Through Central To get your free copy, contact us at 518-962-2287 the Champlain Valley and other books. Champlain Valley or [email protected] 1 2 2019 - 2020 Join us! 3 Hike, volunteer, and contribute to save land and make trails Box 193, 6482 Main Street, Westport, NY 12993 518-962-CATS (2287) [email protected] 4 www.champlainareatrails.com ©2018 Champlain Area Trails Photo by Jen Zahorchak The Central Champlain Valley features a scenic Edgemont B&B landscape of forests, farms, fields, wetlands, and historic 284 Edgemont Rd hamlets nestled in the Adirondack foothills with beautiful views of Lake Champlain, the Adirondack 5 Moriah, New York High Peaks, and the Green Mountains of Vermont. (917) 757-0313 Champlain Area Trails (CATS) creates trails that link communities, connect people to nature, and promote edgemontbandb.com economic vitality. Please enjoy the trails and our wonderful landscape and support local businesses. CATS invites you to get out on the trails and share the vision of New York’s Champlain Valley where productive forests and farms surround vibrant hamlets and people hike, snowshoe, and ski on a network of public trails. 6 You will go through woods and meadows with easy to moderate hills and great views. Bring family and friends together for pleasant walks. -
Appendix a Places to Visit and Natural Communities to See There
Appendix A Places to Visit and Natural Communities to See There his list of places to visit is arranged by biophysical region. Within biophysical regions, the places are listed more or less north-to-south and by county. This list T includes all the places to visit that are mentioned in the natural community profiles, plus several more to round out an exploration of each biophysical region. The list of natural communities at each site is not exhaustive; only the communities that are especially well-expressed at that site are listed. Most of the natural communities listed are easily accessible at the site, though only rarely will they be indicated on trail maps or brochures. You, the naturalist, will need to do the sleuthing to find out where they are. Use topographic maps and aerial photographs if you can get them. In a few cases you will need to do some serious bushwhacking to find the communities listed. Bring your map and compass, and enjoy! Champlain Valley Franklin County Highgate State Park, Highgate Vermont Department of Forests, Parks, and Recreation Temperate Calcareous Cliff Rock River Wildlife Management Area, Highgate Vermont Department of Fish and Wildlife Silver Maple-Sensitive Fern Riverine Floodplain Forest Alder Swamp Missisquoi River Delta, Swanton and Highgate Missisquoi National Wildlife Refuge U.S. Fish and Wildlife Service Protected with the assistance of The Nature Conservancy Silver Maple-Sensitive Fern Riverine Floodplain Forest Lakeside Floodplain Forest Red or Silver Maple-Green Ash Swamp Pitch Pine Woodland Bog -
Geology and Topography of Dutchess County (.Pdf)
Chapter 3: The Geology and Topography of Dutchess County Chapter 3: Geology and Topography of Dutchess County, NY ______________________________________________________________________________ Roy T. Budnik, Jeffery R. Walker, and Kirsten Menking1 May 2010 INTRODUCTION The topography, settlement patterns, and mineral resources of Chapter Contents Dutchess County are all influenced by the underlying geology. Geologic History For example, the highest mountains contain the hardest rocks, Bedrock Formations Structural Geology communities in the county are generally located in areas of Surficial Deposits sand and gravel because of the relatively level terrain and Mineral Resources Topography abundant water supplies they contain, and construction Trends and Changes Over aggregates are mined where suitable deposits are found. Time Implications for Decision- Understanding geologic materials and processes is essential to Making sound resource management because the geology affects the Resources 1 This chapter was written during 2010 by Dr. Roy T. Budnik (President, Roy T. Budnik & Associates), Dr. Jeffrey R. Walker (Professor of Earth Science & Geography, Vassar College), and Dr. Kirsten Menking (Associate Professor of Earth Science and Geography, Vassar College). It is an updated and expanded version of the Hydrology chapter of the 1985 document Natural Resources, Dutchess County, NY (NRI). Natural Resource Inventory of Dutchess County, NY 1 Chapter 3: The Geology and Topography of Dutchess County quality and quantity of groundwater resources, the migration of pollutants, potential hazards to inhabitants, drainage patterns, mineral resources, and soil characteristics. Geology is the study of the earth, including all materials found at and below the earth’s surface. Geologists analyze the composition, origin, and ongoing changes in the rocks and sediments that compose the earth. -
This Article Was Originally Published in a Journal Published by Elsevier
This article was originally published in a journal published by Elsevier, and the attached copy is provided by Elsevier for the author’s benefit and for the benefit of the author’s institution, for non-commercial research and educational use including without limitation use in instruction at your institution, sending it to specific colleagues that you know, and providing a copy to your institution’s administrator. All other uses, reproduction and distribution, including without limitation commercial reprints, selling or licensing copies or access, or posting on open internet sites, your personal or institution’s website or repository, are prohibited. For exceptions, permission may be sought for such use through Elsevier’s permissions site at: http://www.elsevier.com/locate/permissionusematerial Estuarine, Coastal and Shelf Science 71 (2007) 259e277 www.elsevier.com/locate/ecss Regional patterns and local variations of sediment distribution in the Hudson River Estuary F.O. Nitsche a,*, W.B.F. Ryan a, S.M. Carbotte a, R.E. Bell a, A. Slagle a, C. Bertinado a, R. Flood c, T. Kenna a, C. McHugh a,b a Lamont-Doherty Earth Observatory of Columbia Univeristy, Palisades, NY 10964, USA b Queens College, City University New York, Flushing, NY, USA c Stony Brook University, Stony Brook, USA Received 3 November 2005; accepted 27 July 2006 Available online 2 October 2006 Abstract The Hudson River Benthic Mapping Project, funded by the New York State Department of Environmental Conservation, resulted in a com- prehensive data set consisting of high-resolution multibeam bathymetry, sidescan sonar, and sub-bottom data, as well as over 400 sediment cores and 600 grab samples.