NYSSA Bulletin 131-132 2017-2018
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Burial Information for These Recipients Is Here
Civil War Name Connection Death Burial Allen, James Enlisted 31Aug1913 Oakland Cemetery Pottsdam, NY St Paul, MNH Anderson, Bruce Enlisted 22Aug1922 Green Hill Cemetery Albany, NY Amsterdam, NY Anderson, Charles W Served 25Feb1916 Thornrose Cemetery (Phorr, George) 1st NY Cav Staunton, VA Archer, Lester Born 27Oct1864 KIA - Fair Oaks, VA Fort Ann, NY IMO at Pineview Cemetery Queensbury, NY Arnold, Abraham Kerns Died 23Nov1901 St Philiips in the Highlands Church Cold Springs, NY Garrison, NY Avery, James Born 11Oct1898 US Naval Hospital New York City, NY Norfolk, VA Avery, William Bailey Served 29Jul1894 North Burial Grounds 1st NY Marine Arty Bayside, RI Baker, Henry Charles Enlisted 3Aug1891 Mount Moriah Cemetery New York City, NY Philadelphia, PA Barnum, Henry Alanson Born 29Jan1892 Oakwood Cemetery Jamesville, NY Syracuse, NY Barrell, Charles Luther Born 17Apr1913 Hooker Cemetery Conquest, NY Wayland, MI Barry, Augustus Enlisted 3Aug1871 Cold Harbor National Cemetery New York City, NY Mechanicsville, VA Barter, Gurdon H Born 22Apr1900 City Cemetery Williamsburg, NY Moscow or Viola, ID** Barton, Thomas C Enlisted Unknown - Lost to History New York City, NY Bass, David L Enlisted 15Oct1886 Wilcox Cemetery New York City, NY Little Falls, NY Bates, Delavan Born 19Dec1918 City Cemetery Seward, NY Aurora, NE Bazaar, Phillip Died 28Dec1923 Calvary Cemetery (Bazin, Felipe) New York City, NY Brooklyn, NY Beddows, Richard Enlisted 15Feb1922 Holy Sepulchre Cemetery Flushing, NY New Rochelle, NY Beebe, William Sully Born 12Oct1898 US Military -
Civil War Heritage
Civil War Heritage Day Albany Rural Cemetery, Menands, New York Saturday, September 13, 2008 Tours, Music, Events: 10 am - 5 pm Reception and Parade for President Lincoln! 3:00 pm On February 18, 1861 , Jefferson Davis was sworn in as President of the Confederacy and a celebration was held to mark the establishment of the Confederate States of America. On February 18, 1861 , Abraham Lincoln had been elected President of the United States but had not yet reached Washington. On February 18, 1861 , Abraham Lincoln was in Albany , New York. Albany’s Mayor George Thacher met Lincoln at the train station, and they rode in a carriage to the Capitol. As the carriage proceeded down Broadway and turned right to go up State Street, it passed Stanwix Hall, the current residence of John Wilkes Booth. Undoubtedly, Booth watched with almost all of Albany as the new President went by. Another spectator was Clara Harris, daughter of Senator Ira Harris. Clara and her fiancé Major Henry Rathbone would be reunited with President and Mrs. Lincoln at a later encounter with Booth. On June 7, 1862, in the midst of the war, the Trustees of Albany Rural donated a section named the Soldiers’ and Sailors’ Plot. One hundred and forty-nine Civil War Veterans were buried in this plot and at least 600 more were buried in family plots throughout the cemetery. The Grand Army of the Republic Civil War Monument at Albany Rural contains the names of 648 Albany City residents who “ Died in Action.” The bronze plates on the monument were cast from a melted down Civil War cannon. -
A Hand Book for the Albany Rural Cemetery
(lacnell HninetBttg iCibtarg BOUGHT WITH THE INCOME OF THE JACOB H. SCHIFF ENDOWMENT FOR THE PROMOTION OF STUDIES IN HUMAN CIVILIZATION 1916 3 1924 025 961 123 Cornell University Library The original of tiiis bool< is in tine Cornell University Library. There are no known copyright restrictions in the United States on the use of the text. http://www.archive.org/details/cu31924025961123 4 " And behold, there was a great earthquake, for the Angel of the Lord descended fpom heaven, and came and.roUed back the stone ftom thedoo?, and satupon it His coant? nance was like lightning, and his raiment white as snow. And for feai keepers did shake, and oeoame ofhim tte as dead men."—Matthew'xxvhi,2| 3, : HAND BOOK l^lbang |lural Cmrterg, APPENDIX ON EMBLEMS. By EDWARD FITZGERALD. ALBANY VAN BENTHUYSEN PKINTING HOUSE. 1871. %> ^f Un bfd Entered, according to Act of Congress, in the year one . thousand eight hundred and seventy-one, by EDWARD FITZGERALD, in the office of the Liljrarian of Congress, at Washington. : : OFFICERS ALBANY CEMETERY ASSOCIATION. President THOMAS W. OI.COTT. Secretary : CHAULES VAJf BENTHUYSEN. ""JTrustees : THOMAS W. OLCOTT, I. W. VOSBURGH, IRA HARRIS, SAMUEL H. RANSOM, WILLIAM H. De WITT, E. I>. PALMER, JOHN F. RATHBONE, JAMES H. AEMSBY, S. O. SHEPARD, JOHN T. NORTON, PETER GANSEVOORT, THOMAS HILLHOUSE. CHARLES VAN BENTHUTSEN. Superintendent and Surveyor JEFFREY P. THOMAS. — HINTS TO THE VISITOR. oXKo AS we deem it superfluous to apologize to you especially if it happens that you are a stranger to these highly diversified grounds, with their weirdly wrought net work of serpentine avenues and paths, so perfectly bewildering in the intensity of its complication—for introducing to you this little manual, and recommending it as an intelligent and agreeable companion for a ramble among the Silent, we will lose but little time in proceeding to ex- plain how you may avail yourself of its services to the best advantage. -
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. -
The Albany Rural Cemetery
<^ » " " .-^ v^'*^ •V,^'% rf>. .<^ 0- ^'' '^.. , "^^^v ^^^os. l.\''' -^^ ^ ./ > ••% '^.-v- .«-<.. ^""^^^ A o. V V V % s^ •;• A. O /"t. ^°V: 9." O •^^ ' » » o ,o'5 <f \/ ^-i^o ^^'\ .' A. Wo ^ : -^^\ °'yi^^ /^\ ^%|^/ ^'%> ^^^^^^ ^0 v^ 4 o .^'' <^. .<<, .>^. A. c /°- • \ » ' ^> V -•'. -^^ ^^ 'V • \ ^^ * vP Si •T'V %^ "<? ,-% .^^ ^0^ ^^n< ' < o ^X. ' vv-ir- •.-.-., ' •0/ ^- .0-' „f / ^^. V ^ A^ »r^. .. -H rr. .^-^ -^ :'0m^', .^ /<g$S])Y^ -^ J-' /. ^V .;••--.-._.-- %^c^ -"-,'1. OV -^^ < o vP b t'' ^., .^ A^ ^ «.^- A ^^. «V^ ,*^ .J." "-^U-o^ =^ -I o >l-' .0^ o. v^' ./ ^^V^^^.'^ -is'- v-^^. •^' <' <', •^ "°o S .^"^ M 'V;/^ • =.«' '•.^- St, ^0 "V, <J,^ °t. A° M -^j' * c" yO V, ' ', '^-^ o^ - iO -7-, .V -^^0^ o > .0- '#-^ / ^^ ' Why seek ye the living among the dead }"—Luke xxiv : s. [By i)ormission of Erastus Dow Palmer.] e»w <:3~- -^^ THE ALBANY RURAL ^ CEMETERY ITS F A3Ts^ 5tw copies printeil from type Copyn.y:ht. 1S92 Bv HKNkv 1*. PiiKi.rs l*lioto>;raphy by l*iiic MarPoiiaUl, Albany Typogrnpliy and Prcsswork by Brnndow l^rintinj; Comimny, Albany ac:knowledgments. rlfIS hook is tlir D/i/i^mio/fi of a proposilioii on lite pari ot the Iriixtccx to piihlisli a brief liislorv of the .llhaiiy Cemetery A ssoeiation, iiieliidiiiQa report of the eonseeration oration, poem and other exercises. It li'as snoocsted that it niioht be well to attempt son/e- thino- more worthy of the object than a mere pamphlet, and this has been done with a result that must spealc for itself. Jl'h/le it would be impi-aclicable to mention here all who have kindly aided in the zvork, the author desi/'cs to express his particular oblioations : To Mr. -
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. -
Report Prepared By: ARCADIS US 855 Route 146, Suite 210 Clifton Park, New York 4279011 518-250-7300
City of Albany 200 Henry Johnson Boulevard Albany, NY 12210 USEPA BROWNFIELDS HAZARDOUS SUBSTANCES ASSESSMENT GRANT ASSISTANCE ID No. BF-97249507-0 Phase I Environmental Site Assessment 566 Washington Avenue Albany, New York September 2011 Report Prepared By: ARCADIS US 855 Route 146, Suite 210 Clifton Park, New York 4279011 518-250-7300 Table of Contents Contents Limitations L-1 Certifications C-1 1. Introduction 1-1 1.1. Purpose of ESA ............................................................................................................ 1-1 1.2. General Site Description ............................................................................................... 1-1 1.3. General Vicinity Description .......................................................................................... 1-2 1.4. Physical Environmental Setting .................................................................................... 1-2 1.4.1. General Topography ..................................................................................... 1-2 1.4.2. Geology and Soils ......................................................................................... 1-2 1.4.3. Surface Water and Wetlands ........................................................................ 1-3 1.4.4. Hydrogeology ................................................................................................ 1-3 2. Records Review (40 CFR §312.24, 312.25 & 312.26) 2-1 2.1. Site Contact Information .............................................................................................. -
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. -
CDTC NEW VISIONS 2050 FREIGHT WHITE PAPER February 2020 DRAFT
CDTC NEW VISIONS 2050 FREIGHT WHITE PAPER February 2020 DRAFT Capital District Transportation Committee One Park Place Albany NY 12205 518-458-2161 www.cdtcmpo.org CDTC Freight White Paper Table of Contents Introduction .................................................................................................................................................. 3 CDTC Regional Freight Plan (2016) ........................................................................................................... 4 Freight Advisory Committee ..................................................................................................................... 4 Freight Planning & Investment Principle ...................................................................................................... 5 Freight Priority Network ............................................................................................................................... 5 FPN Route Designation Methodology....................................................................................................... 6 Truck Count Data .................................................................................................................................. 6 National Highway System (NHS) Criteria .............................................................................................. 6 Criteria from Other US Studies ............................................................................................................. 7 Land Use Connections .......................................................................................................................... -
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. -
Guidebook: American Revolution
Guidebook: American Revolution UPPER HUDSON Bennington Battlefield State Historic Site http://nysparks.state.ny.us/sites/info.asp?siteId=3 5181 Route 67 Hoosick Falls, NY 12090 Hours: May-Labor Day, daily 10 AM-7 PM Labor Day-Veterans Day weekends only, 10 AM-7 PM Memorial Day- Columbus Day, 1-4 p.m on Wednesday, Friday and Saturday Phone: (518) 279-1155 (Special Collections of Bailey/Howe Library at Uni Historical Description: Bennington Battlefield State Historic Site is the location of a Revolutionary War battle between the British forces of Colonel Friedrich Baum and Lieutenant Colonel Henrick von Breymann—800 Brunswickers, Canadians, Tories, British regulars, and Native Americans--against American militiamen from Massachusetts, Vermont, and New Hampshire under Brigadier General John Stark (1,500 men) and Colonel Seth Warner (330 men). This battle was fought on August 16, 1777, in a British effort to capture American storehouses in Bennington to restock their depleting provisions. Baum had entrenched his men at the bridge across the Walloomsac River, Dragoon Redoubt, and Tory Fort, which Stark successfully attacked. Colonel Warner's Vermont militia arrived in time to assist Stark's reconstituted force in repelling Breymann's relief column of some 600 men. The British forces had underestimated the strength of their enemy and failed to get the supplies they had sought, weakening General John Burgoyne's army at Saratoga. Baum and over 200 men died and 700 men surrendered. The Americans lost 30 killed and forty wounded The Site: Hessian Hill offers picturesque views and interpretative signs about the battle. Directions: Take Route 7 east to Route 22, then take Route 22 north to Route 67. -
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.