Appendix a PSS Filing Notice FLINT MINE SOLAR FACILITY Greene County, New York
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Glacial Lake Albany Butterfly Milkweed Plant Release Notice
UNITED STATES DEPARTMENT OF AGRICULTURE NATURAL RESOURCES CONSERVATION SERVICE BIG FLATS, NEW YORK AND ALBANY PINE BUSH PRESERVE COMMISSION ALBANY, NEW YORK AND THE NATURE CONSERVANCY EASTERN NEW YORK CHAPTER TROY, NEW YORK AND NEW YORK STATE DEPARTMENT OF ENVIRONMENTAL CONSERVATION ALBANY, NEW YORK NOTICE OF RELEASE OF GLACIAL LAKE ALBANY GERMPLASM BUTTERFLY MILKWEED The Albany Pine Bush Preserve Commission, U.S. Department of Agriculture, Natural Resources Conservation Service, The Nature Conservancy, and the New York State Department of Environmental Conservation, announce the release of a source-identified ecotype of Butterfly milkweed (Asclepias tuberosa L.). As a source identified release, this plant will be referred to as Glacial Lake Albany Germplasm butterfly milkweed, to document its original location. It has been assigned the NRCS accession number, 9051776. This alternative release procedure is justified because there is an immediate need for a source of local ecotype of butterfly milkweed. Plant material of this specific ecotype is needed for ecosystem and endangered species habitat restoration in the Pine Barrens of Glacial Lake Albany. The inland pitch pine - scrub oak barrens of Glacial Lake Albany are a globally rare ecosystem and provide habitat for 20 rare species, including the federally endangered Karner blue butterfly (Lycaeides melissa samuelis). The potential for immediate use is high and the commercial potential beyond Glacial Lake Albany is probably high. Collection Site Information: Stands are located within Glacial Lake Albany, from Albany, New York to Glens Falls, New York, and generally within the Albany Pine Bush Preserve, just west of Albany, New York. The elevation within the Pine Barrens is approximately 300 feet, containing a savanna-like ecosystem with sandy soils wind- swept into dunes, following the last glacial period. -
Mohawk River Canoe Trip August 5, 2015
Mohawk River Canoe Trip August 5, 2015 A short field guide by Kurt Hollocher The trip This is a short, 2-hour trip on the Mohawk River near Rexford Bridge. We will leave from the boat docks, just upstream (west) of the south end of the bridge. We will probably travel in a clockwise path, first paddling west toward Scotia, then across to the mouth of the Alplaus Kill. Then we’ll head east to see an abandoned lock for a branch of the Erie Canal, go under the Rexford Bridge and by remnants of the Erie Canal viaduct, to the Rexford cliffs. Then we cross again to the south bank, and paddle west back to the docks. Except during the two river crossings it is important to stay out of the navigation channel, marked with red and green buoys, and to watch out for boats. Depending on the winds, we may do the trip backwards. The river The Mohawk River drains an extensive area in east and central New York. Throughout most of its reach, it flows in a single, well-defined channel between uplands on either side. Here in the Rexford area, the same is true now, but it was not always so. Toward the end of the last Ice Age, about 25,000 years ago, ice covered most of New York State. As the ice retreated, a large valley glacier remained in the Hudson River Valley, connected to the main ice sheet a bit farther to the north, when most of western and central New York was clear of ice. -
Catskill Trails, 9Th Edition, 2010 New York-New Jersey Trail Conference
Catskill Trails, 9th Edition, 2010 New York-New Jersey Trail Conference Index Feature Map (141N = North Lake Inset) Acra Point 141 Alder Creek 142, 144 Alder Lake 142, 144 Alder Lake Loop Trail 142, 144 Amber Lake 144 Andrus Hollow 142 Angle Creek 142 Arizona 141 Artists Rock 141N Ashland Pinnacle 147 Ashland Pinnacle State Forest 147 Ashley Falls 141, 141N Ashokan High Point 143 Ashokan High Point Trail 143 Ashokan Reservoir 143 Badman Cave 141N Baldwin Memorial Lean-To 141 Balsam Cap Mountain (3500+) 143 Balsam Lake 142, 143 Balsam Lake Mountain (3500+) 142 Balsam Lake Mountain Fire Tower 142 Balsam Lake Mountain Lean-To 142, 143 Balsam Lake Mountain Trail 142, 143 Balsam Lake Mountain Wild Forest 142, 143 Balsam Mountain 142 Balsam Mountain (3500+) 142 Bangle Hill 143 Barkaboom Mountain 142 Barkaboom Stream 144 Barlow Notch 147 Bastion Falls 141N Batavia Kill 141 Batavia Kill Lean-To 141 Batavia Kill Recreation Area 141 Batavia Kill Trail 141 Bear Hole Brook 143 Bear Kill 147 Bearpen Mountain (3500+) 145 Bearpen Mountain State Forest 145 Beaver Kill 141 Beaver Kill 142, 143, 144 Beaver Kill Range 143 p1 Beaver Kill Ridge 143 Beaver Meadow Lean-To 142 Beaver Pond 142 Beaverkill State Campground 144 Becker Hollow 141 Becker Hollow Trail 141 Beech Hill 144 Beech Mountain 144 Beech Mountain Nature Preserve 144 Beech Ridge Brook 145 Beecher Brook 142, 143 Beecher Lake 142 Beetree Hill 141 Belleayre Cross Country Ski Area 142 Belleayre Mountain 142 Belleayre Mountain Lean-To 142 Belleayre Ridge Trail 142 Belleayre Ski Center 142 Berry Brook -
Upper Hudson Basin
UPPER HUDSON BASIN Description of the Basin The Upper Hudson Basin is the largest in New York State (NYS) in terms of size, covering all or part of 20 counties and about 7.5 million acres (11,700 square miles) from central Essex County in the northeastern part of the State, southwest to central Oneida County in north central NYS, southeast down the Hudson River corridor to the State’s eastern border, and finally terminating in Orange and Putnam Counties. The Basin includes four major hydrologic units: the Upper Hudson, the Mohawk Valley, the Lower Hudson, and the Housatonic. There are about 23,000 miles of mapped rivers and streams in this Basin (USGS Watershed Index). Major water bodies include Ashokan Reservoir, Esopus Creek, Rondout Creek, and Wallkill River (Ulster and Orange Counties) in the southern part of the Basin, Schoharie Creek (Montgomery, Greene, and Schoharie Counties) and the Mohawk River (from Oneida County to the Hudson River) in the central part of the Basin, and Great Sacandaga Lake (Fulton and Saratoga Counties), Saratoga Lake (Saratoga County), and Schroon Lake (Warren and Essex Counties) in the northern part of the Basin. This region also contains many smaller lakes, ponds, creeks, and streams encompassing thousands of acres of lentic and lotic habitat. And, of course, the landscape is dominated by one of the most culturally, economically, and ecologically important water bodies in the State of New York - the Hudson River. For hundreds of years the Hudson River has helped bolster New York State’s economy by sustaining a robust commercial fishery, by providing high value residential and commercial development, and by acting as a critical transportation link between upstate New York/New England and the ports of New York City. -
Episodes from a Hudson River Town Peak of the Catskills, Ulster County’S 4,200-Foot Slide Mountain, May Have Poked up out of the Frozen Terrain
1 Prehistoric Times Our Landscape and First People The countryside along the Hudson River and throughout Greene County always has been a lure for settlers and speculators. Newcomers and longtime residents find the waterway, its tributaries, the Catskills, and our hills and valleys a primary reason for living and enjoying life here. New Baltimore and its surroundings were formed and massaged by the dynamic forces of nature, the result of ongoing geologic events over millions of years.1 The most prominent geographic features in the region came into being during what geologists called the Paleozoic era, nearly 550 million years ago. It was a time when continents collided and parted, causing upheavals that pushed vast land masses into hills and mountains and complementing lowlands. The Kalkberg, the spiny ridge running through New Baltimore, is named for one of the rock layers formed in ancient times. Immense seas covered much of New York and served as collect- ing pools for sediments that consolidated into today’s rock formations. The only animals around were simple forms of jellyfish, sponges, and arthropods with their characteristic jointed legs and exoskeletons, like grasshoppers and beetles. The next integral formation event happened 1.6 million years ago during the Pleistocene epoch when the Laurentide ice mass developed in Canada. This continental glacier grew unyieldingly, expanding south- ward and retreating several times, radically altering the landscape time and again as it traveled. Greene County was buried. Only the highest 5 © 2011 State University of New York Press, Albany 6 / Episodes from a Hudson River Town peak of the Catskills, Ulster County’s 4,200-foot Slide Mountain, may have poked up out of the frozen terrain. -
Community Relations Plan
f COMMUNITY RELATIONS PLAN HUDSON RIVER PCB REASSESSMENT RI/FS EPA WORK ASSIGNMENT NO. 013-2N84 DECEMBER, 1990 c»o REGION II ALTERNATIVE REMEDIAL CONTRACTING STRATEGY (ARCS) FOR HAZARDOUS WASTE REMEDIAL SERVICES 3B » ^ EPA Contract No. 68-89-2001 o TAMS CONSULTANTS, Inc. u> 00 77 TAMS CONSULTANTS, INC. COMMUNITY RELATIONS PLAN HUDSON RIVER PCB REASSESSMENT RI/FS Contents Page 1. OVERVIEW OF THE COMMUNITY RELATIONS PLAN 1 2. SITE BACKGROUND 3 2.1 Site and Problem Description 2.2 Site History 3. AREA PROFILE 9 3.1 Geographic Characterization 3.2 Land Use, Facilities, and Lifestyle 4. COMMUNITY RELATIONS/PUBLIC PARTICIPATION PROFILE 12 4.1 History of Community Involvement 4.2 Key Concerns and Anticipated issues 5. OBJECTIVES AND DESCRIPTION OF THE COMMUNITY INTERACTION PROGRAM (CIP) FOR THE HUDSON RIVER PCB REASSESSMENT RI/FS 16 5.1 Program Objectives 5.2 Program Description 6. COMMUNITY RELATIONS/PUBLIC PARTICIPATION ACTIVITIES 22 6.1 Basic Community Relations Activities 6.2 CiP-Specific Community Relations/Public Participation Activities 6.3 Optional Community Relations/Public 0 Participation Activities ^ o o CO (O HR-PCB.CRP/CONTENTS TAMS CONSULTANTS, INC. COMMUNITY RELATIONS PLAN HUDSON RIVER PCB REASSESSMENT RI/FS Appendices Page Appendix A Section 1 Governmental Liaison Group Committee Participation Mailing List 27 Section 2 Governmental Liaison Group Information Mailing List 35 Section 3 Citizen Liaison Group Committee Participation Mailing List 47 Section 4 Citizen Liaison Group Information Mailing List 54 Section 5 Environmental -
Joint Annual Meeting of the New York State Geological Association and the New England Inter Collegiate Geological Conference
Rensselaer New York State Polytechnic Guidebook Geological Institute For Fieldtrips Survey New York Sta-te Joint Annual New England Geo I o·g ica I lntercoll egiate Association Meeting Geological Conference 51st annua 1 meeting 7JSI annual mee11ng October 5,6,7, 1979 JOINI' ANNUAL MEEI':m3 OF NE.W YORK STATE GOOI..CGICAL ASSOCIATION 51st Annual Meeting and 7lst Annual Meeting TIDY, NEW YORK October 5, 6, and 7, 1979 GUIDEI3(X)K Gerald M. Friedman, editor Hosts: Depari:It'ent of Geology Rensselaer Polytechnic Institute Troy, New York 12181 and New York State Geological Survey CUltural Education Center Empire State Plaza Albany, New York 12230 Table of Contents Preface and Acknowledgements, by Gerald H. Friedman........ v Field Trips ............................................... v i Geology at Rensselaer: A Historical Perspective. Address of the Retiring President of the New York State Geological Association, by Gerald M. Friedman...... 1 Devonian Stratigraphy and Paleoecology in the Cherry Valley, New York Region, by Donald w. Fisher •..••••.•..•. 20 Sedimentary Environments and Their Products: Shelf, Slope, and Rise of Proto-Atlantic (Iapetus) Ocean, Cambrian and Ordovician Periods, Eastern New York State, b y Gerald M, Friedman...................................... 47 Sedimentary Environments in Glacial Lake Albany in the Albany Section of the Hudson - Champlain Lowlands, by Robert J. Dineen and William B. Rog ers ......•......... 87 The Structural Framework of the Southern Adirondacks, by James McLelland .........•....• , ........•.. , ........... 120 Microstructure of a Vermont Slate, An Adirondack Gneiss, and Some Laboratory Specimens, W.D. Means and M.B. Bayly. 147 Cleavage in the Cossayuna Area, as Seen at the Outcrop, by Lucian B. Platt. 152 Thrust Sheets of the Central Taconic Region, by Donald B. -
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. -
Summits on the Air – ARM for USA - Colorado (WØC)
Summits on the Air – ARM for USA - Colorado (WØC) Summits on the Air USA - Colorado (WØC) Association Reference Manual Document Reference S46.1 Issue number 3.2 Date of issue 15-June-2021 Participation start date 01-May-2010 Authorised Date: 15-June-2021 obo SOTA Management Team Association Manager Matt Schnizer KØMOS Summits-on-the-Air an original concept by G3WGV and developed with G3CWI Notice “Summits on the Air” SOTA and the SOTA logo are trademarks of the Programme. This document is copyright of the Programme. All other trademarks and copyrights referenced herein are acknowledged. Page 1 of 11 Document S46.1 V3.2 Summits on the Air – ARM for USA - Colorado (WØC) Change Control Date Version Details 01-May-10 1.0 First formal issue of this document 01-Aug-11 2.0 Updated Version including all qualified CO Peaks, North Dakota, and South Dakota Peaks 01-Dec-11 2.1 Corrections to document for consistency between sections. 31-Mar-14 2.2 Convert WØ to WØC for Colorado only Association. Remove South Dakota and North Dakota Regions. Minor grammatical changes. Clarification of SOTA Rule 3.7.3 “Final Access”. Matt Schnizer K0MOS becomes the new W0C Association Manager. 04/30/16 2.3 Updated Disclaimer Updated 2.0 Program Derivation: Changed prominence from 500 ft to 150m (492 ft) Updated 3.0 General information: Added valid FCC license Corrected conversion factor (ft to m) and recalculated all summits 1-Apr-2017 3.0 Acquired new Summit List from ListsofJohn.com: 64 new summits (37 for P500 ft to P150 m change and 27 new) and 3 deletes due to prom corrections. -
Annual Report of The
Annual Report of the 2019-2020 To protect and manage the unique and endangered natural communities and species of the Albany Pine Bush, for ecological benefits and controlled and appropriate public recreational and educational use. Table of Contents Overview ....................................................... 1 Background and Mission .............................. 2 Board of Directors ........................................ 3 Project & Programatic Highlights ............... 4 Financial Highlights ..................................... 8 Become a Member ........................................ 10 Preserve Staff & Contact Info ....................... 11 Cover photo by Marty Bannan Photo by Dean Bouton Dear friends, The Albany Pine Bush Preserve Visit us at AlbanyPineBush.org to We’re proud to offer the Albany Pine Commission is a public-private donate to the Friends of the Pine Bush Preserve Commission’s Annual partnership created by the NYS Bush Community or to get details Report. It provides some of the past Legislature in 1988 to protect and on self-guided programs including a year’s highlights from April 1, 2019 manage the preserve and provide StoryWalk, Photo Exhibit submissions, to March 31, 2020 including ways we the public with educational and scavenger hunts and the Karner Kids manage the Globally Rare, Nationally recreational opportunities. Film Festival. You can volunteer as a Significant and Locally Distinct community scientist or as a preserve Albany Pine Bush Preserve and the As the gateway or “front door” to the naturalist, sign up for our newsletter opportunities offered by the Albany Pine Bush, the Discovery Center is a and follow us on social media, Pine Bush Discovery Center. gold LEED-certified interpretive center including Facebook, Instagram and where visitors come to understand Twitter. For some background, the 3,350+/- why the Pine Bush is rare and special. -
Timeline of Maine Skiing New England Ski Museum in Preparation for 2015 Annual Exhibit
Timeline of Maine Skiing New England Ski Museum In preparation for 2015 Annual Exhibit Mid 1800s: “…the Maine legislature sought to populate the vast forests of northern Maine. It offered free land to anyone who would take up the challenge of homesteading in this wilderness. ...Widgery Thomas, state legislator and ex-Ambassador to Sweden…suggested that the offer of free land be made to people in Sweden. In May, 1870 Thomas sailed for Sweden to offer 100 acres of land to any Swede willing to settle in Maine. Certificates of character were required. Thomas himself had to approve each recruit.” Glenn Parkinson, First Tracks: Stories from Maine’s Skiing Heritage . (Portland: Ski Maine, 1995), 4. March 1869: “In March 1869 the state resolved “to promote the settlement of the public and other lands” by appointing three commissioners of settlement. William Widgery Thomas, Jr., one of the commissioners, had extensive diplomatic experience as ambassador to Sweden for Presidents Arthur and Harrison. Thomas had lived among the Swedes for years and was impressed with their hardy quality. He returned to the United States convinced that Swedes would make just the right sort of settlers for Maine. When Thomas became consul in Goteborg (Gothenburg), he made immediate plans for encouraging Swedes to emigrate to America.” E. John B. Allen, “”Skeeing” in Maine: The Early Years, 1870s to 1920s”, Maine Historical Society Quarterly , 30, 3 & 4, Winter, Spring 1991, 149. July 23, 1870 "Widgery Thomas and his group of 22 men, 11 women and 18 children arrived at a site in the woods north of Caribou. -
A Wintry Mix 2015.Indd
Explore Hudson Valley JANUARY 2015 • ULSTER PUBLISHING • WWW.EXPLOREHUDSONVALLEY.COM A Wintry Mix Seasonal activities plus The State of Our Valley Skiing the Berkshires & Catskills, the Culinary Institute's long reach, what's up with the real estate market, long drives for battling cabin fever, creative economies and the threat of gentrifi cation, and what to do with the kids this time of year. Winter 2015 2 | Explore Hudson Valley The healthcare industry is evolving, thanks to policy changes, socioeconomic shifts and technological advances. Amid these changes, HealthAlliance of the Hudson Valley is ensuring we consistently provide the best possible care to every patient today, while becoming the hospital of tomorrow. HealthAlliance is among the state’s leaders in mounting a new strategy for healthcare delivery. The new strategy is based on maximizing value for patients and families — that is, achieving the best outcomes, at a lower cost, with the highest patient satisfaction. $WWKHVDPHWLPHZH·UHZRUNLQJZLWKORFDOGRFWRUVWRUHSODFHWKHLQGXVWU\·VIUDJPHQWHGVWUXFWXUHZLWKDXQLÀHGV\VWHP organized around patients and their needs. This is known as clinical integration. Clinical integration is a strategy, led by area physicians with We’re working on plans to convert the other campus HealthAlliance support, to create a dedicated, multidisciplinary, into a “medical village.” The medical village will be similar mutually reinforcing network of local doctors working together WRDKHDOWKFDUHPDOO³DRQHVWRSGHVWLQDWLRQZKHUH to provide patient care. consumers will have easy access to outpatient, preventive and other health and wellness services. Under the new network, the doctors and other clinicians will treat not simply a disease but rather the “whole person” along Key to the medical village will be enhanced access to the continuum of care.