FCGHT Master Plan Final
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Hydrogeologic Data Update for the Stratified-Drift Aquifer in the Sprout and Fishkill Creek Valleys, Dutchess County, New York
U.S. DEPARTMENT OF THE INTERIOR Prepared in cooperation with the SCIENTIFIC INVESTIGATIONS MAP 3136 U.S. GEOLOGICAL SURVEY NEW YORK STATE DEPARTMENT OF ENVIRONMENTAL CONSERVATION Saturated thickness of the surficial aquifer - SHEET 4 of 4 Reynolds, R.J., and Calef, F.J., III., 2010, Hydrogeologic data update for the stratified-drift aquifer in the Sprout and Fishkill Creek valleys, Dutchess County, New York 73°55' 73°50' 73°45' 41°45' 80˚ 79˚ 78˚ 77˚ 76˚ 75˚ 74˚ 73˚ 72˚ 45˚ CANADA 44˚ Lake Ontario VERMONT NEW 43˚ NEW YORK HAMPSHIRE Lake Erie MASSACHUSETTS 42˚ DUTCHESS COUNTY CONNECTICUT PENNSYLVANIA osg Study area 41˚ NEW 0 25 50 75 100 MILES JERSEY Atlantic 0 25 50 75 100 KILOMETERS Ocean osg t/r t/r EXPLANATION osg Saturated thickness of surficial aquifer, in feet t/r 0 to 10 0 to 10 ft osg 0 to 20 al 0 to 10 ft al 0 to 40 ksg 40 to 100 100 to 180 al ksg ksg Till or bedrock hill—surrounded by aquifer 0 to 20 ft osg Aquifer boundary—Denotes boundary between unconsolidated ksg deposits that comprise the Sprout and Fishkill Creeks aquifer and adjacent deposits of till and bedrock Limit of mapped area—Indicates arbitrary truncation of mapped area Surficial geologic boundary—Denotes boundary between adjacent ksg surficial geologic units. Surficial geologic units explained on Sheet 2 ksg al t/r t/r ksg Saturated Thickness of the Surficial Aquifer ksg col/ksg Sheet 4 shows the estimated saturated thickness of the surficial sand and gravel aquifer in the Sprout Creek-Fishkill Creek t/r study area. -
Beacon New York
Cover Art by Katrina Ross - www.katrinaross.net - curated by CLUB/DRAW by curated - www.katrinaross.net - Ross Katrina by Art Cover This guide is proudly sponsored by: sponsored proudly is guide This #beaconarts #beaconny #beaconarts @beaconarts 12 classical music concerts per year at the Howland Cultural Center. Cultural Howland the at year per concerts music classical 12 /beaconarts.org howlandmusic.org 845.765.3012 - Howland Chamber Music Circle Music Chamber Howland - 5O services, and supporters of the arts. the of supporters and services, PERFORMING ARTS PERFORMING Our members include artists, galleries, specialty shops, restaurants, restaurants, shops, specialty galleries, artists, include members Our cultural vibrancy that has become Beacon, New York’s trademark. trademark. York’s New Beacon, become has that vibrancy cultural Zumba. ages at affordable prices. Tap, jazz, ballet, hip-hop, modern, tumbling, and and tumbling, modern, hip-hop, ballet, jazz, Tap, prices. affordable at ages a 501 (c) 3 non-profit organization promoting and nurturing the the nurturing and promoting organization non-profit 3 (c) 501 a A staple in Beacon, NY for 60 yrs. Quality dance lessons for people of all all of people for lessons dance Quality yrs. 60 for NY Beacon, in staple A Formed in 2002, (BeaconArts Community Association /BACA) is is /BACA) Association Community (BeaconArts 2002, in Formed yanarelladance.com 845.831.9759 St. Main 312 Dance of School Yanarella - 3J music retailer. Locations in Beacon and Brooklyn. and Beacon in Locations retailer. music Classical guitar conservatory for the next generation, and high quality quality high and generation, next the for conservatory guitar Classical ezraguiltar.com 718.434.2103 Ave. -
FISHKILLISHKILL Mmilitaryilitary Ssupplyupply Hubhub Ooff Thethe Aamericanmerican Rrevolutionevolution
Staples® Print Solutions HUNRES_1518351_BRO01 QA6 1234 CYANMAGENTAYELLOWBLACK 06/6/2016 This material is based upon work assisted by a grant from the Department of Interior, National Park Service. Any opinions, fi ndings, and conclusions or recommendations expressed in this material are those of the author(s) and do not necessarily refl ect the views of the Department of the Interior. FFISHKILLISHKILL MMilitaryilitary SSupplyupply HHubub ooff tthehe AAmericanmerican RRevolutionevolution 11776-1783776-1783 “...the principal depot of Washington’s army, where there are magazines, hospitals, workshops, etc., which form a town of themselves...” -Thomas Anburey 1778 Friends of the Fishkill Supply Depot A Historical Overview www.fi shkillsupplydepot.org Cover Image: Spencer Collection, New York Public Library. Designed and Written by Hunter Research, Inc., 2016 “View from Fishkill looking to West Point.” Funded by the American Battlefi eld Protection Program Th e New York Public Library Digital Collections. 1820. Staples® Print Solutions HUNRES_1518351_BRO01 QA6 5678 CYANMAGENTAYELLOWBLACK 06/6/2016 Fishkill Military Supply Hub of the American Revolution In 1777, the British hatched a scheme to capture not only Fishkill but the vital Fishkill Hudson Valley, which, if successful, would sever New England from the Mid- Atlantic and paralyze the American cause. The main invasion force, under Gen- eral John Burgoyne, would push south down the Lake Champlain corridor from Distribution Hub on the Hudson Canada while General Howe’s troops in New York advanced up the Hudson. In a series of missteps, Burgoyne overestimated the progress his army could make On July 9, 1776, New York’s Provincial Congress met at White Plains creating through the forests of northern New York, and Howe deliberately embarked the State of New York and accepting the Declaration of Independence. -
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. -
Hydrogeologic Data Update for the Stratified-Drift Aquifer in the Sprout and Fishkill Creek Valleys, Dutchess County, New York
U.S. DEPARTMENT OF THE INTERIOR Prepared in cooperation with the SCIENTIFIC INVESTIGATIONS MAP 3136 U.S. GEOLOGICAL SURVEY NEW YORK STATE DEPARTMENT OF ENVIRONMENTAL CONSERVATION Location of wells and test holes - SHEET 1 of 4 Reynolds, R.J., and Calef, F.J., III., 2010, Hydrogeologic data update for the stratified-drift aquifer in the Sprout and Fishkill Creek valleys, Dutchess County, New York 73°55' 73°50' 73°45' 41°45' DU4693 DU1222 DU1223 DU4867 DU6531 DU4606 DU5373 DU6954 80˚ 79˚ 78˚ 77˚ 76˚ 75˚ 74˚ 73˚ 72˚ 45˚ DU5993 DU1489 DU 377 DU4691 DU4291 DU3612 DU3491 DU1225 DU3996 CANADA DU4996 DU1224 DU4635 DU3151 DU4582 DU3154 DU3955 DU4659 DU3153 DU3152 44˚ DU4015 DU5915 DU3631 DU 416 Lake Ontario VERMONT DU6214 DU 419 DU1942 DU5400 DU6768 DU6301 DU6445 DU1490 NEW DU4938 DU4894 43˚ DU7088 DU5914 HAMPSHIRE DU1492 DU3641 DU6839 NEW YORK DU6557 DU1491 DU7250 DU7249 DU6415 DU6026 DU6300 DU5213 DU6411 DU5621 Lake DU1226 DU4891 DU4892 Erie DU1461 DU4583 DU6630 DU4766 DU5848 DU6014 DU6374 DU5840 DU3624 MASSACHUSETTS DU1227 DU5841DU4893 DU6777 DU6776 DU5988 DU4890 42˚ DU3623 DUTCHESS DU6879 DU5462 COUNTY DU 461 DU5260 CONNECTICUT DU3625 PENNSYLVANIA DU3211DU3212 DU6631 DU1496 DU1497 DU3213DU3210 Study area DU5632 DU4895 DU6714 DU 386 41˚ NEW DU6590 DU5053 0 25 50 75 100 MILES JERSEY Atlantic DU 481 DU3500 DU6713 025 50 75 100 KILOMETERS Ocean DU 456 DU6077 DU6237 DU6788 DU1994 DU5485 73°49' 73°48' 73°47' DU5319 DU5894 DU3948 DU4401 DU18 81 DU 385 DU5262 DU1805 DU2014 DU 389 DU 462 DU 464 DU4030 DU4966 DU 237 DU 384 DU3177 DU1547 DU1852 DU 61 -
Flood Resilience Education in the Hudson River Estuary: Needs Assessment and Program Evaluation
NEW YORK STATE WATER RESOURCES INSTITUTE Department of Earth and Atmospheric Sciences 1123 Bradfield Hall, Cornell University Tel: (607) 255-3034 Ithaca, NY 14853-1901 Fax: (607) 255-2016 http://wri.eas.cornell.edu Email: [email protected] Flood Resilience Education in the Hudson River Estuary: Needs Assessment and Program Evaluation Shorna Allred Department of Natural Resources (607) 255-2149 [email protected] Gretchen Gary Department of Natural Resources (607) 269-7859 [email protected] Catskill Creek at Woodstock Dam during low flow (L) and flood conditions (R) Photo Credit - Elizabeth LoGiudice Abstract In recent decades, very heavy rain events (the heaviest 1% of all rain events from 1958-2012) have increased in frequency by 71% in the Northeast U.S. As flooding increases, so does the need for flood control Decisions related to flood control are the responsibility of many individuals and groups across the spectrum of a community, such as local planners, highway departments, and private landowners. Such decisions include strategies to minimize future Flood Resilience Education in the Hudson River Estuary: Needs Assessment and Program Evaluation flooding impacts while also properly responding to storm impacts to streams and adjacent and associated infrastructure. This project had three main components: 1) a flood education needs assessment of local municipal officials (2013), 2) an evaluation of a flood education program for highway personnel (2013), and 3) a survey of riparian landowners (2014). The riparian landowner needs assessment determined that the majority of riparian landowners in the region have experienced flooding, yet few are actually engaging in stream management to mitigate flood issues on their land. -
Naturenotes: Madam Brett Park
Over the Creek and Through the Woods— on a Nature Quest NatureNotes Begin by walking across the boardwalk toward the marsh. Fishkill Creek, which flows through Madam • Do you see any fish in Fishkill Creek? MADAM BRETT PARK In spring, fish that normally live in the Brett Park before ocean (such as shad) migrate up the entering the Hudson river and into tributaries like this Beacon River, played a major to spawn. role in Beacon’s history. The creek powered • Look for “helicopter” seeds. What trees Madam Brett’s gristmill do they come from? How do the seed and, later, factories shapes help them spread? such as the Tioronda • As the creek flows from the waterfall Hat Works, the brick to the marsh, how does its speed building next to the change? park. In spring, shad • Can you smell any flowers? Why do and striped bass plants produce a sweet smell? spawning at the • Look for animal tracks in the mud. creek’s mouth, lured commercial fishermen. • Find the trail markers posted on tree While traces of this trunks. Why are they there? past remain, Madam • Take the Red trail and try to walk Brett Park now is an without making a sound. You may be important home for rewarded with many different bird wildlife—and a great calls. place for people to • At the marsh overlook stand quietly connect with it. and you might see some impressive birds! Look and listen for the Who’s Scenic Hudson? red-winged blackbird. We’re a group of dedicated people who care about the • Can you spot a tree trunk that a Josh Clague Hudson River Valley. -
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. -
Description of the New York City District
DESCRIPTION OF THE NEW YORK CITY DISTRICT. -By F. J. H. Merrill, N. H. Dartoii, Arthur Hollick, B. D. Salisbury, li. E. Dodge, Bailey Willis, and H. A. Pressey. GENERAL GEOGRAPHY OF THE DISTRICT. By Richard E. Dodge and Bailey Willis. Position. The district described in tins folio is Gedney, and Main channels. Ambrose and Swash Harlem River and Spuyten Duyvil Creek the Coastal Plain in general are low peninsulas sepa bounded by the meridians of 78° 45' and 74° 15' channels have a least depth of 3-J- fathoms, while water is but 2 to 3^ fathoms deep. rated by estuaries, in which the tide ebbs and west longitude from Greenwich and the parallels Gedney and Main channels are nowhere less than Newark Bay is an extensive water body, but it flows. These peninsulas are composed of beds of of 40° 30' and 41° north latitude. It covers one- 5 fathoms deep. Within the bar the Lower Bay i is not available for sea-going commerce, as the clay, sand, and gravel, or mixtures of these mate quarter of a square degree, equivalent, in this is from 4 to 12 fathoms deep well out from shore, depth is but 2 fathoms or less, except in a little rials constituting loam, and are extensively devel latitude, to 905.27 square miles. The map is but toward the New Jersey and Staten Island j channel near the outlet connecting with the Kill oped in Maryland, Delaware, and New Jersey. divided into four atlas sheets, called the Paterson, shores the water shoals to 3 fathoms or less over \ van Kull. -
Welcome Home to
Welcome Home to . A luxurious community of active-adult condominiums nestled in scenic Hudson Valley. Now is your time to enjoy the finest moments of life. At Regency at Fishkill, you can indulge in a carefree lifestyle of luxury, set admist beautifully kept grounds. A world of amenities close to home ensures that you will enjoy a rich and diverse lifestyle, filled with culture, fine dining, fabulous shopping, and a variety of recreational activities. The good life awaits you at Regency at Fishkill. Wo r l d o f Possibilities . A i n a Co n v e n i e n t lo C a t i o n Just beyond the entrance to your neighborhood, you’ll find the world at your feet! Excellent shopping, a wide choice of recreational options, and fabulous restaurants are close to home! In fact, Regency at Fishkill is within walking distance of fantastic shopping and Vassar Brothers Medical Mall. You are also within 3 minutes of Route 9, Interstate 84, and the Village of Fishkill. The town of Poughkeepsie can be reached in just 15 minutes. Danbury, Connecticut, can be reached in 35 minutes, while White Plains, New York, is 45 minutes away. Traveling to New York City is an easy 72-minute ride on Metro North’s services from either the Beacon or New Hamburg stations, both within 10 minutes of your new home. Stewart International Airport can be reached in just 20 minutes and is serviced by US Airways, Northwest Airlines, and many other carriers. lu x u r y li f e s t y l e th a t ’s Ca r e f r e e AAt Regency at Fishkill, you don’t have to worry about your lawn care, snow removal, and external home maintenance — so you’ll have plenty of time to enjoy the good life. -
Ground-Water Appraisal of the Fishkill-Beacon Area, Dutchess
GROUND-WATER APPRAISAL OF THE FISHKILL-BEACON AREA DUTCHESS COUNTY, NEW YORK By Deborah S. Snavely U.S. GEOLOGICAL SURVEY Water Resources Investigation Open-File Report 80-437 Prepared in cooperation with the Town of Fishkill, New York Albany, New York 1980 UNITED STATES DEPARTMENT OF THE INTERIOR CECIL D. ANDRUS, Secretary GEOLOGICAL SURVEY H. William Menard, Director For additional information write to: U.S. Geological Survey 343 U.S. Post Office & Courthouse P.O. Box 1350 Albany, New York 12201 ii CONTENTS Page Conversion factors and abbreviations. ............................. Ab stract ........................................................... 1 Introduction. ...................................................... 2 Purpose and scope ............................................. 2 Method of study. .............................................. 2 Sources and acknowledgments ................................... 2 Geography .......................................................... 3 Location and setting. ......................................... 3 Climate ....................................................... 3 Topography. ................................................... 3 S treams ....................................................... 3 Geologic setting. .................................................. 5 Surf icial geology. ............................................ 5 Bedrock geology. .............................................. 5 Ground-water resources ............................................. 6 Occurrence. .................................................. -
Analysis of Route Alternatives (Pdf)
Analysis of Route Alternatives Assessing Feasibility - Planning Methodology Community Outreach and the Planning Process Public and stakeholder engagement was a critical part of the master planning process. Four public meetings were held (see photos at right) at key intervals during the planning process. Each of the meetings had strong participation, with over 100 people attending each event. Online outreach included direct emails to several local email lists and meeting notifications on the project’s website and Facebook page. Public comments were also solicited using a dedicated e-mail address as well as an online survey that received more than 450 responses. The Steering Committee helped raise awareness of the planning process and opportunities for public and stakeholder input by compiling a list of, and notifying, public agencies and local organizations that focused on topics such as recreational activities, preservation, and economic development. Many of these organizations distributed meeting announcements to their own lists of constituents, which increased awareness of this project and helped attract public participation. Public Meetings Meeting 1: February 17, 2014 Introduced the project and master planning process, along with trail types that might comprise the different alignment possibilities. edL a table mapping exercise in which participants provided detailed input on the route in three sections. Each section was discussed at three or more tables, after which each group presented their discussion to the larger group. Meeting 2: July 9, 2014 Provided updates on the route analysis, including Breakneck Connector funding application (see page 34 for more info on this project component). Fielded public comments and then responded to open questions, with the design team utilizing display boards and maps.