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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. -
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. -
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 ...................................................................... -
Then & Now: Albany, the South Mall and a Neighborhood Lost
Then & Now: Albany, the South Mall and a Neighborhood Lost City Engineer, Public Works Negatives, 1930-1949. From the Archival Collection of the Albany County Hall of Records. The Princess and “The Gut” 89-01830. Private Donor. Netherlands Royal Family Visit to Albany Photo Collection. Princess Beatrix of the Netherlands, Governor Nelson Rockefeller and Mayor Erastus Corning, September, 1959. “The South Mall will be the greatest single governmental office complex history has ever known.” – Mayor Erastus Corning 2nd In September of 1959, Princess Beatrix of the Netherlands came to Albany, New York to commemorate the 350th anniversary of Henry Hudson’s exploratory voyage on the Hudson River at the Hudson-Champlain Celebration. While giving the young royal a tour of downtown Albany, Governor Nelson A. Rockefeller felt embarrassed by the deteriorating South End neighborhood referred to by some as “The Gut,” an area of many dilapidated buildings and vacant structures. Albany Mayor Erastus Corning 2nd told the Knickerbocker News in 1979 that: “Rockefeller thought [the] buildings the Princess and those with her saw were not as good-looking or appropriate for a capital city as he thought they should be.” In an attempt to revitalize Albany and transform it into a city outsiders would deem worthy of being New York’s capital, Rockefeller proposed the construction of a large, modern governmental complex. In order to create this lavish site he envisioned, Rockefeller seized 98.5 acres of land in Albany’s South End through eminent domain in 1962 and demolition soon began. As a result, thousands of families and business owners lost their properties and were forced to relocate. -
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. -
LINCOLN and the COPPERHEADS in the CIVIL WAR in January 1863
SNAKES LURKING IN THE GRASS: LINCOLN AND THE COPPERHEADS IN THE CIVIL WAR In January 1863, Abraham Lincoln was confronted with a threat more dangerous than that of the Confederate Army. The Union Army was visibly struggling toward victory with each passing battle and it seemed as if the war was far from concluding. Lincoln’s problems were not just limited to the battlefield, but the president was also burdened in dealing with intense opposition toward his government on the homefront. The threat was the Copperhead movement: Congressional Democrats were banning together in opposition to the war and proposing immediate peace through negotiations with the Confederacy. The Copperhead challenge came at an uneasy period in Lincoln’s presidency as the American public became more hostile towards the war effort. Numerous setbacks for the Union troops and the hardships of the war at home wore at the patience of many Americans and the President himself. The Copperheads took advantage of the public agitation by attacking Lincoln’s actions and character while deeming his expansion of power as unconstitutional and dangerous. Lincoln’s suspension of habeas corpus and use of martial law agitated this political opposition. The Copperheads were successful in gaining support before the election of 1864 through their attacks on Lincoln’s perceived abuse of civil liberties and expansion of power; however, Lincoln’s ability to lead the nation in troubling times, as well as a turn in the tide of the war, prevented the election of a Copperhead president and exposed the weaknesses of the movement. The supporters of the Copperhead movement were quite varied and diverse. -
Smith Believes Record Justifies Another Term
Roots and Shoots: Bagging the longhorned beetle | See page 15 FRIDAY, AUGUST 2, 2013 69 MAIN ST., COLD SPRING, N.Y. | www.philipstown.info Storm King reigns on a summer’s morning | For more Summer Photofest images see page 16. Photo by Kevin Harrison Smith Believes Record Manitou Properties Seeks to Justifies Another Term Turn Plumbush Restaurant into Sees opponent’s criticisms as not serious Pre-K to Grade 6 School were the crime other events. Located just outside of Cold By Kevin E. Foley numbers flowing Philipstown Spring, on Route 9D at Peekskill and the other way. s an incumbent, Putnam County Planning Board Moffatt Roads, the property is in a Town So Smith has a Sheriff Donald B. Smith would ap- of Philipstown hamlet-mixed use zoning right to lay claim gets site plan pear to have the wind at his back district. Manitou Properties does not yet A to success and as he seeks re-election to a fourth term submission own the site, with completion of the sale he proudly touts in office. According to the New York state dependent on site-plan approval. Putnam’s safety By Liz Schevtchuk Department of Criminal Justice Services, Sheriff Smith Photo by K.E. Foley When it met July 25, the Planning record as the Armstrong Putnam County has ranked number one Board declared the proposal a major primary reason in criminal safety for the last three years local business has begun efforts to project (triggering higher level scrutiny), voters should return him to office. This in a row. -
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. -
Sault Ste. Marie, 1853-1854 and After $21.50
Sault Ste. Marie, 1853-1854 and After $21.50 TO BUILD A CANAL Sault Ste. Marie, 1853-1854 and After John N. Dickinson Nature has surrounded Lake Superior with immense and valuable forests, and has placed near its shores rich lodes of copper and, in the famed Mesabi Range, the world's largest and most accessible deposits of iron ore. But Na ture has also, by some quirk of geology and accident of geography, caused Lake Superior to have an elevation twenty-one feet higher than that of Lake Huron, into which it flows, and has connected the two by a river that, though sixty-three miles in over-all length, completes the drop in elevation in a stretch of precipitous rapids three-fourths of a mile long and a quarter of a mile wide, down which rushes 74,000 cubic feet of water per second as Superior races into Huron. The story of the construction of a bypass to this formidable natural barrier to the free passage of raw mate rials from the American Midwest to the great commercial centers of the eastern United States and beyond is the subject of this reveal ing and entertaining book. Traders who visited the area that the French had dubbed the Sault Ste. Marie had, as early as the eighteenth century, discerned the need to build a canal to circumvent the falls in the St. Mary's River, and one, of a sort, was indeed already in operation in the days of George Washington. A far more efficient waterway than this primitive expedient was clearly required, however, if the iron ore so abundant in Minnesota and Michigan was to join the coal and limestone of Ohio and Penn sylvania in the mills and furnaces surrounding the lower Great Lakes; and in 1853, after years of legislative haggling and political maneuver ing, construction of the St.