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Delaware River Restoration Fund 2018 Grant Slate
Delaware River Restoration Fund 2018 Grant Slate NFWF CONTACTS Rachel Dawson Program Director, Delaware River [email protected] 202-595-2643 Jessica Lillquist Coordinator, Delaware River [email protected] 202-595-2612 PARTNERS • The William Penn Foundation • U.S. Forest Service • U.S. Department of Agriculture (NRCS) • American Forest Foundation To learn more, go to www.nfwf.org/delaware ABOUT NFWF Delaware River flowing through the Delaware Water Gap National Recreation Area | Credit: Jim Lukach The National Fish and Wildlife Foundation (NFWF) protects and OVERVIEW restores our nation’s fish and The National Fish and Wildlife Foundation (NFWF) and The William Penn Foundation wildlife and their habitats. Created by Congress in 1984, NFWF directs public conservation announced the fifth-year round of funding for the Delaware River Restoration Fund dollars to the most pressing projects. Thirteen new or continuing water conservation and restoration grants totaling environmental needs and $2.2 million were awarded, drawing $3.5 million in match from grantees and generating a matches those investments total conservation impact of $5.7 million. with private funds. Learn more at www.nfwf.org As part of the broader Delaware River Watershed Initiative, the William Penn Foundation provided $6 million in grant funding for NFWF to continue to administer competitively NATIONAL HEADQUARTERS through its Delaware River Restoration Fund in targeted regions throughout the 1133 15th Street, NW Delaware River watershed for the next three years. This year, NFWF is also beginning to Suite 1000 award grants that address priorities in its new Delaware River Watershed Business Plan. Washington, D.C., 20005 Delaware River Restoration Fund grants are multistate investments to restore habitats 202-857-0166 and deliver practices that ultimately improve(continued) and protect critical sources of drinking water. -
NJGS Contracted with Greater New York City Through the Borough of Richmond President Cromwell, to Provide Water for 1835 Staten Island
UNEARTHING NEW JERSEY NEW JERSEY GEOLOGICAL SURVEY Vol. 5, No. 2 Summer 2009 Department of Environmental Protection MESSAGE FROM THE STATE GEOLOGIST A PLAN TO PLUNDER NEW JERSEY’S WATER This issue of Unearthing New Jersey continues the series of historic stories with Mark French’s article A Plan to Plunder New Jersey’s Water. This story concerns a plan by By Mark French the Hudson County Water Company and its myriad political allies to divert an enormous portion of the water resources of INTRODUCTION New Jersey to the City of New York. The scheme was driven At the turn of the 20th century, potable water in New by the desire for private gain at the expense of the citizens of Jersey was managed by private companies or municipalities New Jersey. Thanks to the swift action of the Legislature, the through special grants from the State Legislature or State Attorney General, the State Geologist and the highest certificates of incorporation granted by the State under the courts in the land, the Hudson County Water Company General Incorporation Law of 1875. Clamoring for oversight, plot was stymied setting a riparian rights precedent in the the citizenry and the Legislature tried to create a State process. Water Commission in 1894, but the effort was quashed by A second historic article, The New York-New Jersey Line water business interests and their friends in the Legislature. War by Ted Pallis, Mike Girard and Walt Marzulli discusses Companies were mostly free to traffic in water as they saw the geographic boundaries of New Jersey. -
Climate Change, Delaware Water Gap National Recreation Area Patrick Gonzalez
Climate Change, Delaware Water Gap National Recreation Area Patrick Gonzalez Abstract Greenhouse gas emissions from human activities have caused global climate change and widespread impacts on physical systems, ecosystems, and biodiversity. To assist in the integration of climate change science into resource management in Delaware Water Gap National Recreation Area (NRA), particularly the proposed restoration of wetlands at Watergate, this report presents: (1) results of original spatial analyses of historical and projected climate trends at 800 m spatial resolution, (2) results of a systematic scientific literature review of historical impacts, future vulnerabilities, and carbon, focusing on research conducted in the park, and (3) results of original spatial analyses of precipitation in the Vancampens Brook watershed, location of the Watergate wetlands. Average annual temperature from 1950 to 2010 increased at statistically significant rates of 1.1 ± 0.5ºC (2 ± 0.9ºF.) per century (mean ± standard error) for the area within park boundaries and 0.9 ± 0.4ºC (1.6 ± 0.7ºF.) per century for the Vancampens Brook watershed. The greatest temperature increase in the park was in spring. Total annual precipitation from 1950 to 2010 showed no statistically significant change. Few analyses of field data from within or near the park have detected historical changes that have been attributed to human climate change, although regional analyses of bird counts from across the United States (U.S.) show that climate change shifted winter bird ranges northward 0.5 ± 0.3 km (0.3 ± 0.2 mi.) per year from 1975 to 2004. With continued emissions of greenhouse gases, projections under the four emissions scenarios of the Intergovernmental Panel on Climate Change (IPCC) indicate annual average temperature increases of up to 5.2 ± 1ºC (9 ± 2º F.) (mean ± standard deviation) from 2000 to 2100 for the park as a whole. -
Beyond the Exit
New Jersey Road Trips Beyond the Exit ROUTE 80 Mountain Magic NJ TURNPIKE Bridge to Bridge ROUTE 78 Farm to City ROUTE 42 Wine Trail GARDEN STATE PARKWAY Down the Shore BY THE ROUTE: Six major road ROUTE 40 Southern trips across the River to state where you Shore can stop along the way and experience New Jersey’s best! Due to COVID19, some attractions may be following adjusted hours and attendance guidelines. Please contact attraction for updated policies and procedures. NJ TURNPIKE – Bridge to Bridge 1 PALISADES 8 GROUNDS 9 SIX FLAGS CLIFFS FOR SCULPTURE GREAT ADVENTURE 5 6 1 2 4 3 2 7 10 ADVENTURE NYC SKYLINE PRINCETON AQUARIUM 7 8 9 3 LIBERTY STATE 6 MEADOWLANDS 11 BATTLESHIP PARK/STATUE SPORTS COMPLEX NEW JERSEY 10 OF LIBERTY 11 4 LIBERTY 5 AMERICAN SCIENCE CENTER DREAM 1 PALISADES CLIFFS - The Palisades are among the most dramatic 7 PRINCETON - Princeton is a town in New Jersey, known for the Ivy geologic features in the vicinity of New York City, forming a canyon of the League Princeton University. The campus includes the Collegiate Hudson north of the George Washington Bridge, as well as providing a University Chapel and the broad collection of the Princeton University vista of the Manhattan skyline. They sit in the Newark Basin, a rift basin Art Museum. Other notable sites of the town are the Morven Museum located mostly in New Jersey. & Garden, an 18th-century mansion with period furnishings; Princeton Battlefield State Park, a Revolutionary War site; and the colonial Clarke NYC SKYLINE – Hudson County, NJ offers restaurants and hotels along 2 House Museum which exhibits historic weapons the Hudson River where visitors can view the iconic NYC Skyline – from rooftop dining to walk/ biking promenades. -
Delaware Water Gap U.S
National Park Service Delaware Water Gap U.S. Department of the Interior National Recreation Area Summer/Fall 2015 Guide to the Gap N A YEARS A T E I 50 1965-2015 R O A N N AL IO RECREAT Your National Park Celebrates 50 Years! The Delaware Water Gap National Recreation Area was established by a park for the people. Today, visitors roam a landscape carved by uplift, Congress on September 1, 1965, to preserve the natural, culture, and scenic erosion, and glacial activity that is marked by hemlock and rhododendron- resources of the Delaware River Valley and provide opportunities for laced ravines, rumbling waterfalls, fertile floodplains and is rich with recreation, education, and enjoyment to the most densely populated region archaeological evidence and historic narratives. This haven for natural of the nation. Sprung out of the Tocks Island Dam controversy, the last and cultural stories is your place, your park, and we invite you to celebrate 50 years has solidified Delaware Water Gap National Recreation Area as with us in 2015. The River, the Valley, and You . 2 Events. 4 Delaware River . 6 Park Trails . 8. Fees and Passes . 2 Park Map and Visitor Centers . 3 Are you curious about the natural and cultural Delaware Water Gap National Recreation Area From ridgetop to riverside, vistas to ravines, Activities and Events in 2015 . 4 history of the area? Would you like to see includes nearly 40 miles of the free-flowing from easy to extreme, more than 100 Delaware River Water Trail . 6 artisans at work? Want to experience what it Middle Delaware River Scenic and Recreational miles of trail offer something for every mood. -
How the Gap Formed
Delaware Water Gap National Recreation Area How the Gap formed What is a water gap? Several words in the English language The Delaware Water Gap is justly famous for denote a “break” or “cleft” in the moun- its depth, width, and scenic beauty. The Gap tains. Chasm and notch are popular in New is a mile wide from New Jersey’s Mount England; pass and gorge in the South and Tammany (1,527 feet) to Pennsylvania’s West of the United States. Gap is especially Mount Minsi (1,463 feet.) The Gap is about common in this part of the country. 1,200 feet deep from the tops of these mountains to the surface of the river, which A gap or wind gap is a break or pass through at this point is 290 feet above sea level. The the mountains, in this case the Appalachian maximum depth of the river at the Gap is Mountains. A water gap is a pass that a river about 55 feet. runs through. How does a gap form? Geology is the study of the earth’s forma- Starting with Native American legend, there tion. Though the geologist’s time frame may have been many ideas about how the seem vast and remote, the results of Delaware Water Gap formed. One current geological processes are the mountains we theory explains the Gap through a series of hike on, the river we swim in, and the processes: continental shift (involving plate scenery we admire. tectonics), mountain building (orogeny), erosion, and the “capturing” of rivers and streams. -
Delaware Water Gap National Recreation Area: Outstanding Basin Waters
Delaware Water Gap National Recreation Area: Outstanding Basin Waters Delaware River Basin Commission Page 122 2502 ICP Delaware River at DWGNRA Northern Boundary Delaware River Basin Commission Page 123 2502 ICP Delaware River at DWGNRA Northern Boundary Latitude 41.343611 Longitude -74.757778 by GPS NAD83 decimal degrees. No nearby USGS or State monitoring sites Watershed Population figures were not calculated for main-stem Delaware River sites. Drainage Area: 3,420 square miles, Delaware River Zone 1C Site Specific EWQ defined 2006-2011 by the DRBC/NPS Scenic Rivers Monitoring Program. This site is located at the Delaware Water Gap National Recreation Area northern boundary Classified by DRBC as Significant Resource Waters (Outstanding Basin Waters downstream of this location) Nearest upstream Interstate Control Point: 2547 ICP Delaware River at Port Jervis Nearest downstream Interstate Control Point: 2464 ICP Delaware River at Montague Known dischargers within watershed: Undefined Tributaries to upstream reach: Major tributary 2536 BCP Neversink River, NY; small tributary 250.8 Rosetown Creek, PA. No Stream Stats web site data available (drainage area too large to calculate on web site). Flow Statistics (calculated by drainage area weighting from Port Jervis USGS gage data): Max Flow 90% Flow 75% 60% 50% 40% 25% Flow 10% Flow (CFS) Min (CFS) (CFS) Flow Flow Flow Flow (CFS) Flow (CFS) (CFS) (CFS) (CFS) (CFS) 172,966 12,088 6,752 4,531 3,587 2,860 2,074 1,720 884 Delaware River Basin Commission Page 124 Existing Water Quality: 2502 ICP -
Hemlock Woolly Adelgid and the Disintegration of Eastern Hemlock Ecosystems
Hemlock woolly adelgid and the disintegration of eastern hemlock ecosystems By Richard A. Evans An alien insect is causing decline in eastern hemlock forests, many species of wildlife. In contrast, the species most leading to the loss of native biodiversity, and opening the likely to expand in declining hemlock stands include way for invasions of alien plants deciduous trees, white pine (Pinus strobus), and invasive alien plants like “tree-of-heaven” (Ailanthus altissima), Hemlock woolly adelgid (Adelges tsugae) is an aphid- Japanese barberry (Berberis thunbergii), and Japanese like insect native to Asia that feeds exclusively on hem- stiltgrass (Microstegium vimineum) (Orwig and Foster lock (Tsuga spp.) trees. First documented in Richmond, 1996, Battles et al. 1999). These species will not provide Virginia, in 1951, hemlock woolly adelgid (HWA) now habitat or ecological functions resembling those of east- occurs in 13 states, from Georgia to New Hampshire. ern hemlock (fig. 1). During the past decade, HWA has been associated with widespread, severe decline and mortality of eastern hem- lock (T. canadensis) trees. The insect also debilitates Carolina hemlock (T. caroliniana), the other hemlock species native to the eastern United States. The geograph- ic range of Carolina hemlock is limited to the southern- most Appalachian Mountains, which has just recently been infested by HWA. Examples of National Park System areas affected by HWA include Great Smoky Mountains and Shenandoah National Parks, New River Gorge National River, Catoctin Mountain Park, and Delaware Water Gap National Recreation Area. Eastern hemlock is an ecologically important and influ- ential conifer that for thousands of years was a major component of forests over much of the eastern United States. -
Map # Trail Name Distance Rating ‡ Pg
Park Trails MILFORD Map # Trail Name Distance Rating ‡ Pg # 1 1 Buchanan 1.1mi / 1.8km 10 Milford Beach (fee area) 84 Cliff 2.8mi / 4.5km Appalachian Trail North Contact Station 8 To Scranton Cliff Park Inn golf course Hackers 1.4mi / 2.3km Other hiking trail Montague North Milford Knob 1.3mi / 2.0km Joseph M. McDade 1 206 Recreational Trail (biking and hiking) Pond Loop 0.7mi / 1.1km Joseph M. McDade Recreational Trail (hiking only) Quarry Path 0.5 mi / 0.8km 2 r 209 e 0 5 Kilometers d v Raymondskill Creek 0.3mi / 0.4km a i C o o R R 0 5 Miles n Jager Ro e ad a 2001 s n i h 2 Conashaugh View CLOSED in 2019 a M d u a g d h l o O R R d o a 3 George W. Childs Park CLOSED in 2019 a o 739 d 5 R d r 2 e 4 o Dingmans Creek 0.4mi / 4.0km e f r l i g a d i M Marie w R a 5 Zimmermann l 645 Upper Ridge Road 2.5mi / 4.0km 11 House e D 6 Hornbecks Creek CLOSED in 2019 To 560 Branchville Dingmans Ferry Layton 7 Fossil 1.0mi / 1.6km 11 Access e (fee area) Lak R oad 4 Ridgeline 3.0mi / 4.8km ilver 560 S George W. Childs 3 Park Dingmans Ferry 615 Scenic Gorge 2.0mi / 3.2km Dingmans Campground Dingmans Falls Tumbling Waters 2.8mi / 4.5km Peters Valley Visitor Center School of Craft (open seasonally) Two Ponds 1.5mi / 2.4km 8 E d m a o e R r 8 McDade Recreational 32mi / 51.5km 14 y e n i M PENNSYLVANIA STOKES 6 d l 9 Military Road 1.0mi / 1.6km 15 R O o NPS a d 615 STATE Walpack Ridge 3.0mi / 4.8km 7 FOREST 9 10 Buttermilk Falls 1.4mi / 2.3km 15 Pocono Environmental Education Center Walpack Center 11 Toms Creek 0.8mi / 1.3km 14 7 209 12 Blue Mountain Lakes -
Black Bear Regulations
Black Bear Regulations Black Bear Hunting After Harvesting a Bear —Mandatory Bear Check included in Area 2. Black Bear Hunting Area 1 is Season: Requirement surrounded by Black Bear Hunting Area 2. Firearm or Bow and Arrow: Properly licensed hunters who harvest a black bear September 18 and must immediately tag the bear with a “bear transporta- The season will close when the black bear harvest September 22, 2000 in Bear tion tag” indicating the current and valid hunting objective of 175 is achieved. The notification number Hunting Area 1; Bow and license number, hunter’s name and address, date and for season closures is the permit hotline number, 609- Arrow Only: September 30 time of kill, county and township of kill and sex of 292-9192. Notification will also be announced by - October 27, 2000 in Bear bear. The Division will supply the bear transportation press, radio, and the Division’s website Hunting Area 1 and 2 tag, which will be available at Division offices, at (www.state.nj.us/dep/fgw). Firearm or Bow and Arrow: December 4 -9, 2000 in license issuing agencies, and at bear hunting seminars Bear Hunting Area 1 and 2 conducted by the Division. Hunters must get a bear Mandatory Black Bear Check Stations: transportation tag prior to hunting for bear. All black Hunterdon County: Firearms, Bows and Ammunition Legal bear must be taken by the hunter who killed the bear Clinton Wildlife Management Area Office, 7 Van for Bear Hunting: to a designated bear checking station by 10:00 p.m. to Syckel’s Road, Hampton Shotgun: Not smaller than 20 gauge and not larger be tagged with a “Black Bear Possession Tag” provid- Sussex County: than 10 gauge, capable of holding no more than 3 ed by the Division. -
Lower Delaware River Special Protection Waters
2016 ASSESSMENT OF MEASURABLE CHANGES TO EXISTING WATER QUALITY, ROUND 1: BASELINE EWQ (2000-2004) VS. POST-EWQ (2009-2011) DELAWARE RIVER BASIN COMMISSION, SCENIC RIVERS MONITORING PROGRAM DRBC | West Trenton, NJ Delaware River Basin Commission Lower Delaware River Special Protection Waters Assessment of Measurable Changes to Existing Water Quality, Round 1: Baseline EWQ (2000- 2004) vs. Post-EWQ (2009-2011) Citation Delaware River Basin Commission. 2016. Lower Delaware River Special Protection Waters Assessment of Measurable Changes to Existing Water Quality, Round 1: Baseline EWQ (2000-2004) vs. Post-EWQ (2009-2011). Delaware River Basin Commission, DRBC/NPS Scenic Rivers Monitoring Program, West Trenton, NJ. Authors: Robert Limbeck, Eric Wentz, Erik Silldorff, John Yagecic, Thomas Fikslin, Namsoo Suk. Delaware River Basin Commission Page 1 Executive Summary Introduction: The Lower Delaware is a 76-mile reach of the Delaware River extending from just below the Delaware Water Gap at Portland, PA (River Mile 209.5) to Calhoun Street Bridge at Trenton, NJ (River Mile 134.3). In 2000, federal legislation was enacted adding key segments of the Lower Delaware and selected tributaries to the National Wild and Scenic Rivers System. This designation was followed in April 2001 with a petition to DRBC from the Delaware Riverkeeper Network to classify the Lower Delaware as Special Protection Waters (SPW). In 2008, the DRBC by unanimous vote (DRBC 2008) added the Lower Delaware to Special Protection Waters as Significant Resource Waters, and adopted Existing Water Quality definitions for specific control points. In partnership with the National Park Service (NPS), the Delaware River Basin Commission established the Scenic Rivers Monitoring Program (SRMP) to define the water quality for this reach of the river and assess any measurable changes to these high quality waters. -
Vanderpoel-De Hooges-Post-Bradt
Chapter X: VanderPoel-De Hooges-Post-Bradt Last Revised: October 29, 2014 Ironically, we may know more about Abraham Vanderpool’s Dutch ancestors than we do about him. Because he was born in Albany, New York, we are able to forge a solid link between our Abraham born in 1709 (and, by extension, the Indiana Vanderpools) and the parent Vanderpool family of New York – and so the Dutch community there. Unusually rich information exists about the Vanderpool family and its associated families in New York, extending back to the earliest settlement of New Netherland (as it was called before the English conquest in 1664). Some of what we know comes from several published Vanderpool family histories, some from an excellent network of Vanderpool researchers, and some from documentary and scholarly sources, including the New Netherland Project in the New York State Archives. 1 Indeed, the Vanderpool line as a whole may be not only the lengthiest documented line in our entire family but the best- documented of all these lines as well. Because the half-century of Dutch dominion in what is now New York State and surrounding areas is not so well known today, it may be useful to profile here the major features of that era as a context for our discussion of the Vanderpools and their family 1 This heroic project is endeavoring to translate into English and make accessible all the surviving records (written in old Dutch, of course) relating to New Netherland. Some of the records from New Netherland were damaged or destroyed in a fire in the New York State Capitol Building in 1911.