Wayne Tucker Postcard Collection Index
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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. -
Freshwater Fishing: a Driver for Ecotourism
New York FRESHWATER April 2019 FISHINGDigest Fishing: A Sport For Everyone NY Fishing 101 page 10 A Female's Guide to Fishing page 30 A summary of 2019–2020 regulations and useful information for New York anglers www.dec.ny.gov Message from the Governor Freshwater Fishing: A Driver for Ecotourism New York State is committed to increasing and supporting a wide array of ecotourism initiatives, including freshwater fishing. Our approach is simple—we are strengthening our commitment to protect New York State’s vast natural resources while seeking compelling ways for people to enjoy the great outdoors in a socially and environmentally responsible manner. The result is sustainable economic activity based on a sincere appreciation of our state’s natural resources and the values they provide. We invite New Yorkers and visitors alike to enjoy our high-quality water resources. New York is blessed with fisheries resources across the state. Every day, we manage and protect these fisheries with an eye to the future. To date, New York has made substantial investments in our fishing access sites to ensure that boaters and anglers have safe and well-maintained parking areas, access points, and boat launch sites. In addition, we are currently investing an additional $3.2 million in waterway access in 2019, including: • New or renovated boat launch sites on Cayuga, Oneida, and Otisco lakes • Upgrades to existing launch sites on Cranberry Lake, Delaware River, Lake Placid, Lake Champlain, Lake Ontario, Chautauqua Lake and Fourth Lake. New York continues to improve and modernize our fish hatcheries. As Governor, I have committed $17 million to hatchery improvements. -
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. -
Community Profile
Community Profile City of Schenectady Comprehensive Plan 2020 Reinventing the City of Invention Brian U. Stratton Mayor Community Profile Table of Contents Demographic Characteristics ............................................................................................................ 5 Economic Profile ..........................................................................................................................13 Real Estate and Tax Base Analysis .....................................................................................................31 Housing ......................................................................................................................................43 Infrastructure and Transportation.....................................................................................................59 Natural Resources .........................................................................................................................72 Community Character & Historic Preservation......................................................................................76 Recreation ..................................................................................................................................83 Government, Public Safety and Community Institutions..........................................................................90 List of Tables and Figures Tables Table 1: Summary Demographic Table, City of Schenectady ...................................................................... -
The Lasting Impacts of Large-Volume Runoff Events: Evaluating River
The Lasting Impacts of Large-Volume Runoff Events: Evaluating River Discharge and Suspended Sediment Transfer Patterns Following Hurricane Irene and Tropical Storm Lee, Schoharie Watershed, New York State, USA By Jesse Van Patter A Thesis Presented to The University of Guelph In partial fulfilment of requirements for the degree of Master of Science in Geography Guelph, Ontario, Canada © Jesse Van Patter, May, 2017 ABSTRACT The Lasting Impacts of Large-Volume Runoff Events: Evaluating River Discharge and Suspended Sediment Transfer Patterns Following Hurricane Irene and Tropical Storm Lee, Schoharie Watershed, New York State, USA Jesse Van Patter Advisor: University of Guelph, 2017 Dr. Jaclyn Cockburn Committee Member: Dr. Wanhong Yang Large-volume runoff events have lasting impacts on sediment transfer by providing long-term supplies of transferable sediment. Hurricane Irene and Tropical Storm Lee generated extreme runoff throughout the Northeastern United States. This research evaluated multi-year discharge and suspended sediment transfer patterns for Schoharie Creek, New York State, USA to investigate the lasting impacts associated with extreme (>500-year recurrence interval) runoff generated by Irene and Lee. The relationship for river discharge and suspended sediment transfer was evaluated for 69 runoff events in 2013-2015; results indicated that sediment supply depletion did not occur. The multi-decadal suspended sediment flux was estimated during 1973- 2012 to investigate long-term sediment transfer processes. The suspended sediment flux was primarily transported during high discharge periods in each water year. Annual runoff and the frequency for large-volume runoff events have increased in the Northeastern United States from the mid-20th century to the present, thus suspended sediment transfer has likely increased. -
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. -
VILLAGE of NORTHVILLE DRAFT COMPREHENSIVE PLAN Village Board Review Rev 1
2017 VILLAGE OF NORTHVILLE DRAFT COMPREHENSIVE PLAN Village Board Review Rev 1 ADOPTED: RESOLUTION: ~ 0 ~ VISION STATEMENT In 2035, as you cross the bridge into Northville you will find the Village to be an age diverse yet community minded population living in a quaint and historical atmosphere having a relaxed lifestyle complimented by a strong commercial tax base. The Village's commercial core area will provide residents and visitors with a wide variety of essential goods and services such as grocery, convenience and hardware stores, pharmacy and a bank. The commercial core will 4also be home to a mix of residential uses located above existing commercial buildings providing for an increase in population density to support the commercial establishments. Excellent emergency services to include ambulance, fire and police will continue to serve and be supported by the local population. A healthcare facility will continue to operate within the Village and continue to provide general healthcare services using the latest technologies. Among these essential service establishments, you will find just as many unique family owned and operated businesses such as restaurants, a recreational outfitter, outdoor sporting goods establishment and specialty foods. The Village will feature a low property tax rate and a government that is proactive, ready to assist and support, financially and by other means initiatives important to its citizens. Housing choices will be available for both senior citizens, millennials and young families alike. The Village shall continue to support and be served by a strong school system educating students for both college and the 21st Century workforce through increased educational technologies and disciplines. -
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. -
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. -
January/February 2011
Schenectady County Historical Society Newsletter Volume 54 54 NumberNumber 1-2 1-2 JanuaryJanuary-Februar - Februaryy 2011 2011 3322 Washington Avenue,Avenue, Schenectady, Schenectady, New New York York 12305 12305 (518) 374-0263374-0263 Web site: http://www.schist.org • • Editor Editor email:email: [email protected] [email protected] FAXFAX:: (518)(518) 688688-2825-2825 Librarian email:email: [email protected] [email protected] • Curator• Curator email: email: [email protected] [email protected] FIRST PRESBYTERIAN CHURCH – A Brief History by David Vincent For its first century of existence, regular Christian worship at the Dutch Reformed Church in Schenectady was conducted only in Dutch. As the English-speaking population grew, so did a desire for services in English, primarily driven by members of the Church of England, the official church of the Province. The city‘s population, decimated following its destruction in 1690, was about 300 households in 1759 when land for an English chapel was purchased.1 Ground was broken the same year for a building originally planned as a chapel for all English speaking peoples,2 and Presbyterians and other ―dissenters‖ (non-Anglican Protestants) participated in both land and material acquisition. Construction began in 1762. As for the Presbyterians, while the actual date of organization is unknown, the best current approximation is 1760. Friction developed early on between the two competing English groups. A 1765 letter from the Schenectady Anglican churchwardens to Sir William Johnson sought his acceptance as a trustee and his support for a petition before the Governor to grant the congregation a ―Charter to Secure their Rights and privileges in the Church built here‖ in order to ―prevent for the future the presbyterians from making any unjust attempts on the priviledges in the Church.‖3 –Continued on Page 4 John C.