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Continuation Sheet Historic District Branford, Connecticut
NPS Form 10-900 OUB No. 1024-0018 (Rev. 8-86) United States Department of the Interior National Park Service NOV 1 4 1988 National Register of Historic Places Registration Form NATIONAL REGISTER This form is for use in nominating or requesting determinations of eligibility for individual properties or districts. See instructions in Guidelines for Completing National Register Forms (National Register Bulletin 16). Complete each item by marking "x" in the appropriate box or by entering the requested information. If an item does not apply to the property being documented, enter "N/A" for "not applicable." For functions, styles, materials, and areas of significance, enter only the categories and subcategories listed in the instructions. For additional space use continuation sheets (Form 10-900a). Type all entries. 1. Name of Property_________________________________________________ historic name other names/site number Stony Creek/Thimble Islands Historic District 2. Location street & number See continuation sheets I I not for publication city, town Branford T I vicinity" stateConnecticut code 09 county New Haven code 009 zip code 06405 3. Classification Ownership of Property Category of Property Number of Resources within Property |X2l private I I building(s) Contributing Noncontributing lot public-local |X}| district 14.1 buildings I I public-State Flsite 1 sites I I public-Federal I I structure structures I I object . objects 355 142 Total Name of related multiple property listing: Number of contributing resources previously N/A _____________________ listed in the National Register 1____ 4. State/Federal Agency Certification As the designated authority under the National Historic Preservation Act of 1966, as amended, I hereby certify that this [x~l nomination EH request for determination of eligibility meets the documentation standards for registering properties in the National Register of Historic Places and meets the procedural and professional requirements set forth in 36 CFR Part 60. -
Erie Canalway Map & Guide
National Park Service Erie Canalway National Heritage Corridor U.S. Department of the Interior Erie Canalway Map & Guide Pittsford, Frank Forte Pittsford, The New York State Canal System—which includes the Erie, Champlain, Cayuga-Seneca, and Oswego Canals—is the centerpiece of the Erie Canalway National Heritage Corridor. Experience the enduring legacy of this National Historic Landmark by boat, bike, car, or on foot. Discover New York’s Dubbed the “Mother of Cities” the canal fueled the growth of industries, opened the nation to settlement, and made New York the Empire State. (Clinton Square, Syracuse, 1905, courtesy Library of Congress, Prints & Photographs Division, Detroit Publishing Extraordinary Canals Company Collection.) pened in 1825, New York’s canals are a waterway link from the Atlantic Ocean to the Great Lakes through the heart of upstate New York. Through wars and peacetime, prosperity and This guide presents exciting Orecession, flood and drought, this exceptional waterway has provided a living connection things to do, places to go, to a proud past and a vibrant future. Built with leadership, ingenuity, determination, and hard work, and exceptional activities to the canals continue to remind us of the qualities that make our state and nation great. They offer us enjoy. Welcome! inspiration to weather storms and time-tested knowledge that we will prevail. Come to New York’s canals this year. Touch the building stones CONTENTS laid by immigrants and farmers 200 years ago. See century-old locks, lift Canals and COVID-19 bridges, and movable dams constructed during the canal’s 20th century Enjoy Boats and Boating Please refer to current guidelines and enlargement and still in use today. -
Rogers Island Bicycle Loop South Shore Rd
327 Terrebonne SStt.. 158 Bois-des-Filion LLaawwrreennccee RRiivveerr 132 Pointe-aux-Trembles Varennes Saint-Amable 116 125 224 Sainte-Thérèse 50 148 Rosemère Montréal-Est 40 15 Saint-Hyacinthe 640 138 440 25 223 Sainte-Julie 20 344 Saint-Léonard Boucherville 229 40 Beloeil LLaaccddeess 148 OOuuttaarrddeess Laval-Ouest Mont-Saint-Hilaire 417 117 Ferry St-Valérien 344 13 116 Longueuil 137 La Montréal Route Ve Ottawa rte Ottawa Sainte-Marthe-sur-le-Lac Aéroport Saint-Basile-le-Grand RRiivveerr Mont-Royal Aéroport SSaaiinntt--HHuubbeerrtt Outremont Landmark Bridge Saint-Laurent ddee LLoonngguueeuuiill L'Île-Bizard Dollard-des-Ormeaux Greenfield 231 342 Aéroport International Westmount Park 133 Aéroport International Saint-Hubert PPiieerrrree--EElllliiootttt--TTrruuddeeaauu Saint-Lambert Saint-Mathias-sur-Richelieu RRiivveeiirree Côte YYaammaasskkaa ddee MM 30 Saint-Luc La Pierrefonds Pointe-Claire Route Verte Kirkland 20 Montréal-Ouest Verdun Brossard 235 233 Sainte-Anne-de-Bellevue Lachine 134 Chambly 40 Beaconsfield Canton-de-Granby Lasalle 201 Terrasse-Vaudreuil La Prairie Vaudreuil-Dorion 10 112 L'Île-Perrot Candiac Notre-Dame-de-l'Île-Perrot 227 La Route Verte Route La 104 Pincourt 139 Maple 35 Saint-Constant Granby Grove Saint-Jean-sur-Richelieu 132 338 Melocheville 340 Grande-Île Saint-Timothée 207 20 Farnham 30 104 325 Cartiers Jacques Rue 241 221 Montee de la Cannerie 15 Salaberry-de-Valleyfield 217 Rue Principale 223 236 Saint-Jean-Baptiste rand 401 Ch. G Bernier Eglise l’ 219 e 235 Rue d Cowansville 132 209 205 Mtee Blais 223 Rg. St. Jo se ph 133 203 202 201 138 Mont Guay 225 St. -
The Erie Canal in Cohoes
SELF GUIDED TOUR THE ERIE CANAL IN COHOES Sites of the Enlarged Erie Canal Sites of the Original Erie Canal Lock 9 -In George Street Park, north oF Lock 17 -Near the intersection oF John Old Juncta - Junction of the Champlain Alexander Street. and Erie Sts. A Former locktender’s house, and Erie Canals. Near the intersection of Lock 10 -Western wall visible in George now a private residence, is located to the Main and Saratoga Sts. Street Park. A towpath extends through west of the lock. A well-preserved section the park to Lock 9 and Alexander Street. of canal prism is evident to the north of Visible section of “Clinton’s Ditch” southwest of the intersection of Vliet and Lock 11 -Northwest oF the intersection oF the lock. N. Mohawk Sts. Later served as a power George Street and St. Rita’s Place. Lock 18 -West oF North Mohawk Street, canal for Harmony Mill #2; now a park. Lock 12 -West oF Sandusky Street, north of the intersection of North Mohawk partially under Central Ave. Firehouse. and Church Sts. Individual listing on the Old Erie Route - Sections follow Main National Register of Historic Places. and N. Mohawk Streets. Some Lock 13 - Buried under Bedford Street, structures on Main Street date from the south of High Street. No longer visible. early canal era. Lock 14 - East of Standish Street, The Pick of the Locks connected by towpath to Lock 15. A selection of sites for shorter tours Preserving Cohoes Canals & Lock 15 - Southeast of the intersection of Locks Spindle City Historic Vliet and Summit Streets. -
Cohoes-Waterford Concept Plan.Pub
Cohoes—Waterford Canalway Trail Connection Study Prepared for New York State Canal Corporation By Parks and Trails New York Final Draft Version Cohoes-Waterford Canalway Trail Connection Study Final Draft Version September 2004 Page 2 Table of Contents Acknowledgements ............................................................................................................ 2 Executive Summary ............................................................................................................ 3 Introduction ......................................................................................................................... 5 Existing trail initiatives in the study area ...................................................................... 6 Purpose of Study .......................................................................................................... 7 Inventory and Analysis of Study Area ................................................................................. 7 Canalway Trail Resources ........................................................................................... 7 Waterford Canal Harbor Visitor Center ........................................................................9 Hudson Valley Greenway Trail ...................................................................................10 Street System Resources ................................................................................................. 11 Streets ....................................................................................................................... -
Distribution of Ddt, Chlordane, and Total Pcb's in Bed Sediments in the Hudson River Basin
NYES&E, Vol. 3, No. 1, Spring 1997 DISTRIBUTION OF DDT, CHLORDANE, AND TOTAL PCB'S IN BED SEDIMENTS IN THE HUDSON RIVER BASIN Patrick J. Phillips1, Karen Riva-Murray1, Hannah M. Hollister2, and Elizabeth A. Flanary1. 1U.S. Geological Survey, 425 Jordan Road, Troy NY 12180. 2Rensselaer Polytechnic Institute, Department of Earth and Environmental Sciences, Troy NY 12180. Abstract Data from streambed-sediment samples collected from 45 sites in the Hudson River Basin and analyzed for organochlorine compounds indicate that residues of DDT, chlordane, and PCB's can be detected even though use of these compounds has been banned for 10 or more years. Previous studies indicate that DDT and chlordane were widely used in a variety of land use settings in the basin, whereas PCB's were introduced into Hudson and Mohawk Rivers mostly as point discharges at a few locations. Detection limits for DDT and chlordane residues in this study were generally 1 µg/kg, and that for total PCB's was 50 µg/kg. Some form of DDT was detected in more than 60 percent of the samples, and some form of chlordane was found in about 30 percent; PCB's were found in about 33 percent of the samples. Median concentrations for p,p’- DDE (the DDT residue with the highest concentration) were highest in samples from sites representing urban areas (median concentration 5.3 µg/kg) and lower in samples from sites in large watersheds (1.25 µg/kg) and at sites in nonurban watersheds. (Urban watershed were defined as those with a population density of more than 60/km2; nonurban watersheds as those with a population density of less than 60/km2, and large watersheds as those encompassing more than 1,300 km2. -
Fort Edward / Rogers Island History and Timeline
HISTORY OF FORT EDWARD AND ROGERS ISLAND The present village of Fort Edward, New York, was called “The Great Carrying Place” because it was the portage between the Hudson River and Lake Champlain. The first recorded military expedition to have passed through the Great Carrying Place, led by Major General Fitz-John Winthrop, occurred in 1690. The following year, Peter Schuyler led another expedition against Canada. The first fortification to have been built in Fort Edward was under the command of Colonel Francis Nicholson in 1709, during the conflict known as “Queen Anne’s War.” Fort Nicholson was garrisoned by 450 men, including seven companies of “regulars in scarlet uniform from old England.” A crude stockade was built to protect storehouses and log huts. John Henry Lydius, a Dutch fur trader, came to the site of Fort Nicholson to construct a trading post in 1731. Lydius claimed this land under a title granted to the Rev. Dellius in 1696. According to a 1732 French map, the trading post may have been surrounded by storehouses and fortified. Lydius may also have built a sawmill on Rogers Island. It is unknown whether the Lydius post was destroyed and later reconstructed in 1745 when many French and Indian raids were being conducted on the Hudson River. Many Provincial troops arrived at the Great Carrying Place during July and August of 1755. Among these were the celebrated Rogers’ Rangers. Rogers Island became the base camp for the Rangers for about 2 ½ years during the French and Indian War. Many Ranger huts, a blockhouse, a large barracks complex, and a large smallpox hospital were constructed on Rogers Island between 1756 and 1759. -
Protecting and Managing Hudson River Streams: Overview, Scales and Definitions
Protecting and managing Hudson River streams: Overview, scales and definitions A comprehensive approach to stream management yields many benefits for a local community and its water resources including improving water quality, reducing and mitigating flooding, protecting wildlife habitat and maintaining and enhancing public access and recreational activities. Although much attention has been placed on the health of the Hudson River in recent years, resulting in a dramatic improvement in water quality in the river, the health of the many streams and tributaries of the Hudson River Basin also play an important role for the water quality and overall health of the watershed. Overview Streams are part of larger systems called a stream or riparian corridors, which often include floodplains and wetlands adjacent to streams. Streams include the water flowing through them and the land beneath them called the stream bed or channel. Other spatial scales to consider are the lands around the stream – including the stream or riparian buffer, adjacent floodplains and wetlands, upland habitat and watershed. Size and Scale of Watersheds • Everyone lives in a watershed. Wherever you are in the world, you are in a watershed. • A watershed supports a web of life that is interconnected, meaning that every plant and animal interacts with many other organisms in the watershed during their life cycle. A typical watershed is a network of smaller rivers or streams called tributaries, which are connected and eventually flow into a larger stream or river. • Watersheds are divided into smaller drainage areas or subwatersheds. For example, in the Hudson Source: Sandusky River Watershed Coalition Valley, the Quassaick Creek Watershed (56 square miles) and Moodna Creek Watershed (180 square miles) are subwatersheds of the larger Hudson Hudson River Watershed River Watershed, which drains about 13,500 The Hudson River flows from its highest point at square miles of land. -
Most Popular Hikes
Most Popular Hikes Rip Van Winkle Skywalk – Crossing over the Hudson River with views Rip Van Winkle Monument – Larger than life Blue stone carving Kaaterskill Falls – Highest cascading waterfall in NYS of the mountains and the Hudson River Valley at the top of Hunter Mountain Acra Point and Batavia Kill Loop Escarpment Trail, Windham Trailhead Plateau Mountain (via Warner Creek Trail) (Moderate to Difficult: 5.3-mile circuit) (Moderate to Difficult: 23-mile circuit) (Difficult: 8-mile circuit) Affords breathtaking views of the Black Dome Range. Enjoy The trail offers challenging terrain over ever changing scenery Perfect for avid climbers and hikers, both scenic and rugged. scenery of the Hudson Valley from the summit before descending with mixed hardwood forests, dark hemlock groves along swift- The trail intersects with the Devil’s Path and offers views of along the Batavia Kill. Trailhead located on Big Hollow Road flowing creeks and a spruce-fir cap on the higher peaks. Trailhead Kaaterskill High Peak and Hunter Mountain. Trailhead located (County Route 56) in Maplecrest. located on Route 23 in East Windham. on Notch Inn Road (off Route 214) in Hunter. Devil’s Path Hunter Mountain Fire Tower Pratt Rock (Difficult: 24.15 miles) (Moderate to Difficult: 8 miles, round trip) (Difficult: 3.1 miles, round trip) Described as the toughest and most dangerous hiking trail in the One of the Catskills’ iconic hikes located on the summit of The climb to the rock is steep, and may be unfit for young Eastern United States, the Devil’s Path is one of the most popular Hunter Mountain. -
Southerly Mohawk Hudson Convergence”- an Exploratory Case Study of Terrain-Induced Wind Convergence on the Formation of Thunderstorms in New York’S Capital Region
University at Albany, State University of New York Scholars Archive Atmospheric & Environmental Sciences Honors College 5-2014 “Southerly Mohawk Hudson Convergence”- An exploratory case study of terrain-induced wind convergence on the formation of thunderstorms in New York’s Capital Region Christine Elizabeth Bloecker University at Albany, State University of New York Follow this and additional works at: https://scholarsarchive.library.albany.edu/honorscollege_daes Part of the Oceanography and Atmospheric Sciences and Meteorology Commons Recommended Citation Bloecker, Christine Elizabeth, "“Southerly Mohawk Hudson Convergence”- An exploratory case study of terrain-induced wind convergence on the formation of thunderstorms in New York’s Capital Region" (2014). Atmospheric & Environmental Sciences. 7. https://scholarsarchive.library.albany.edu/honorscollege_daes/7 This Honors Thesis is brought to you for free and open access by the Honors College at Scholars Archive. It has been accepted for inclusion in Atmospheric & Environmental Sciences by an authorized administrator of Scholars Archive. For more information, please contact [email protected]. “Southerly Mohawk Hudson Convergence”- An exploratory case study of terrain-induced wind convergence on the formation of thunderstorms in New York’s Capital Region An honors thesis presented to the Department of Atmospheric and Environmental Sciences, University at Albany, State University of New York in partial fulfillment of the requirements for graduation with Honors in Atmospheric Sciences and graduation from The Honors College. Christine Elizabeth Bloecker Research Mentor and Advisor: Hugh Wood Johnson III June, 2014 Abstract Southerly Mohawk-Hudson Convergence (SMHC) is a mesoscale phenomenon over New York’s Capital Region whereby a southwesterly wind flow over Eastern New York is channeled by the mountainous terrain westerly through the Mohawk River Valley and southerly through the Hudson River Valley. -
Copyrighted Material
1 An Uncommon Defense (1607–1775) Introduction On September 24, 1759, a force of nearly 150 men maneuvered in the marshy woods of North America. They included Indians, provincials, and regulars, although most of them possessed no formal military training. After entering Quebec, they gathered to the north- east of Missisquoi Bay for a “council of war.” Major Robert Rogers, their commander, addressed the gathering. Clothed in a green- jacket and bonnet, he stood over 6 feet tall. His face was marked by smallpox scars and gunpowder burns. His forehead revealed a line carved into his fl esh by a lead bullet. He spoke deliberately with few words, exhibiting a coolness that inspired confi dence in the weary men. Their line of retreat was cut off by their enemy, he announced, while an ambush awaited them ahead. Drawing upon his understanding of the terrain, he quickly designed a plan of action. Although the mission that he outlined seemed impossible, they voted to “prosecute our design at all adventures.” Modifying their route, Rogers guided them through the spruce bogs in the boreal forests. As they stepped into the cold, acidic water, the submerged branches, needles, roots, and logs tore their moccasins to shreds and left many of them barefoot. They marched abreast in a single “Indian fi le,” so as to prevent their enemy from tracking them. Their movement through theCOPYRIGHTED bogs continued for nine days an dMATERIAL culminated near the Saint-Francois River. T he men stood almost 6 miles away from their target, an Abenaki village on the other side of the waterway. -
Water-Quality Assessment of the Hudson River Basin in New York and Adjacent States −
Water-quality Assessment Of The Hudson River Basin In New York And Adjacent States − Analysis of available nutrient, pesticide, volatile organic compound, and suspended-sediment data, 1970-90 By Patrick J. Phillips and Dorothea W. Hanchar _____________________________________ U.S. GEOLOGICAL SURVEY Water-Resources Investigations Report 96-4065 Troy, New York 1996 i U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY Gordon Eaton, Director For additional information Copies of this report can be write to: purchased from: U.S. Geological Survey District Chief Branch of Information Services U.S. Geological Survey, WRD Federal Center 425 Jordan Road Box 25425 Troy, N.Y. 12180 Denver, CO 80225-8286 ii FOREWORD The mission of the U.S. Geological Survey (USGS) is to assess the quantity and quality of the earth resources of the Nation and to provide information that will assist resource managers and policymakers at Federal, State, and local levels in making sound decisions. Assessment of water-quality conditions and trends is an important part of this overall mission. One of the greatest challenges faced by water-resources scientists is acquiring reliable information that will guide the use and protection of the Nation's water resources. That challenge is being addressed by Federal, State, interstate, and local water-resource agencies and by many academic institutions. These organizations are collecting water-quality data for a host of purposes that include: compliance with permits and water-supply standards; development of remediation plans for a specific contamination problem; operational decisions on industrial, wastewater, or water-supply facilities; and research on factors that affect water quality.