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Passaic Falls
THE GEOLOGICAL HISTORY OF THE PASSAIC FALLS Paterson New Jersey Bv WILLIAM NELSON PATERSON, N. J. : THE PRESS PRINTING AND PUBLISHING COMPANY. 1892. COPYRIGHT x892 Bv WILLIAM NELSON The Passaic Falls are the most remarkable bit of natural scenery in New Jersey. In some respects they are unique. For more than two centuries they have been visited by travelers from all parts of the world. Their peculiar formation, and the strange rocks in the neighborhood, have excited the wonder and curiosity of all beholders, and have of ten suggested the thought, "How was this cataract formed? Why these peculiar 1·ocks and mountains?" In preparing a History of the City of Paterson-a city which was located at the Great Falls to take advantage of the water-power-the writer's attention was naturally di rected to the question which has arisen in the minds of all who have stood at the spot where the Passaic river takes its mad plunge over the precipice. In the following pages he has attempted an answer, by giving some account of the Geological History of the Passaic Falls. This paper is the first Chapter of the more extended History of Paterson mentioned. Only one hundred copies have been printed separately in this form. The writer will be pleased to receive suggestions and corrections from any who may receive a copy of this pamphlet. The references and notes have been made full, as a guide to those unfamiliar with the subject, who may wish to pursue it further. PATERSON, N. J., November 24, 1892. -
2020 Freshwater Fishing Digest Pages 16-33
License Information 2020 REGULATIONS Regulations in red are new this year. New Jersey National Guard Summary of General Only New Jersey National Guard personnel in good Licenses standing are entitled to free sporting licenses, per- Fishing Regulations mits and stamps. These privileges are not available The season, size and creel limits for freshwater • A valid New Jersey fishing license is required for using Fish and Wildlife’s website. However, the NJ species apply to all waters of the state, including residents at least 16 years and less than 70 years Dept. of Military and Veterans Affairs can issue tidal waters. of age (plus all non-residents 16 years and older) fishing licenses through their DMAVA website at • Fish may be taken only in the manner known as to fish the fresh waters of New Jersey, includ- www.nj.gov/military/iasd/fishing.html. For all other angling with handline or with rod and line, or ing privately owned waters. See page 17 for free sporting licenses, call (609) 530-6866, email as otherwise allowed by law. information on the money-saving Buddy Fish- [email protected], or write to: MSG (Ret.) • When fishing from the shoreline, no more than ing License, coming to Internet sales in 2020. Robert Greco, NJ DMAVA, 101 Eggert Crossing three fishing rods, handlines or combination • For fishing-related license and permit fees, see Rd., Lawrenceville, NJ 08648. thereof may be used (except on the Delaware page 1. River. There is no rod limit when fishing from • Resident anglers age 70 and over do not require a Disabled Veterans Licenses, a boat except for the Delaware River.) For the fishing license. -
Army Corps of Engineers Response Document Draft
3.0 ORANGE COUNTY Orange County has experienced numerous water resource problems along the main stem and the associated tributaries of the Moodna Creek and the Ramapo River that are typically affected by flooding during heavy rain events over the past several years including streambank erosion, agradation, sedimentation, deposition, blockages, environmental degradation, water quality and especially flooding. However, since October 2005, the flooding issues have severely increased and flooding continues during storm events that may or may not be considered significant. Areas affected as a result of creek flows are documented in the attached trip reports (Appendix D). Throughout the Orange County watershed, site visits confirmed opportunities to stabilize the eroding or threatened banks restore the riparian habitat while controlling sediment transport and improving water quality, and balance the flow regime. If the local municipalities choose to request Federal involvement, there are several options, depending on their budget, desired timeframe and intended results. The most viable options include a specifically authorized watershed study or program, or an emergency streambank protection project (Section 14 of the Continuing Authorities Program), or pursing a Continuing Authorities Program study for Flood Risk Management or Aquatic Ecosystem Restoration (Section 205 and Section 206 of the Continuing Authorities Program, respectively). Limited Federal involvement could also be provided in the form of the Planning Assistance to States or Support for Others programs provide assistance and limited funds outside of traditional Corps authorities. A watershed study focusing on restoration of the Moodna Creek, Otter Creek, Ramapo River and their associated tributaries could address various problems using a systematic approach. -
The Mountain Shadows Property Is Part of Pruddentown by Arthur
The Mountain Shadows Property is Part of Pruddentown ountain Shadows, Thanksgiving and Christmas Jersey was occupied by a branch of situated along Mount holidays. Also occasionally a car the Delaware Indians called the MKemble Avenue in with a “Zamrok” license plate is Lenni Lenape—“original people.” historic Morris Township, is a spotted in the area—perhaps Sam The Indians came from the west colonial styled townhouse complex. Masucci is related to a Zamrok. with the Mengwe or Iroquois Fifteen single family townhouses The land occupied by Mountain tribes and occupied the region on Zamrok Way are at the base of Shadows has historical significance bordered by the great salt water the eastern face of Mount Kemble. being next to Pruddentown, a lake and bounded by four great The complex, two miles south of 1770s colonial manufacturing rivers; the Hudson, Delaware, the Morristown Green, was built in community. At the entrance to Susquehanna and Potomac. 1984, and has blended in with the Zamrok Way is a two hundred year In the 1600s, New Jersey was wooded countryside. Sam Masucci, old hickory tree that can attest to inhabited by Swedish and Dutch of Forest Dale Associates, built the changes to the landscape as settlers who traded for furs with Mountain Shadows, the Shadow Pruddentown expanded along the Native Americans. The settlers Brook Townhouses and the Mount Kemble Avenue from multiplied and in the early 1700s, Applewood homes. For several Skyline Drive to Sand Spring the land was politically subdivided years after the completion of the Road. into counties. Morris County, townhouses, the residents were originally part of Hunterdon amazed when an unknown The First Settlers County, was created in 1738, and benefactor decorated the “Zamrok The story of Mount Kemble named after the Governor of the Way” street sign with straw and Avenue and Pruddentown begins at Province, Lewis Morris. -
Total Maximum Daily Load Report for the Non-Tidal Passaic River Basin Addressing Phosphorus Impairments
Amendment to the Northeast, Upper Raritan, Sussex County and Upper Delaware Water Quality Management Plans Total Maximum Daily Load Report For the Non-Tidal Passaic River Basin Addressing Phosphorus Impairments Watershed Management Areas 3, 4 and 6 Proposed: May 7, 2007 Adopted: April 24, 2008 New Jersey Department of Environmental Protection Division of Watershed Management P.O. Box 418 Trenton, New Jersey 08625-0418 Table of Contents 1.0 Executive Summary……………………………………………………..…………….. 4 2.0 Introduction……………………………………………………………………….…... 13 3.0 Pollutant of Concern and Area of Interest…………………………………….……. 14 4.0 Source Assessment………………………………………………………………..….. 29 5.0 Analytical Approach and TMDL Calculation …………………………………..… 36 6.0 Follow-up Monitoring…………………………………………………………..…….47 7.0 Implementation Plan……………………………………………………………..……48 8.0 Reasonable Assurance…………………………………………………………….…..58 9.0 Public Participation…………………………………………………………………... 61 Appendix A: Cited References………………………………………………………..... 67 Appendix B: Municipalities and MS4 Designation in the Passaic River Basin ….… 71 Appendix C: Additional Impairments within TMDL Area ………………………….. 73 Appendix D: TMDLs completed in the Passaic River Basin ……………………...….. 75 Appendix E: Rationale for Establishing Chlorophyll-a as Watershed Criteria to Protect Designated Uses of the Wanaque Reservoir and Dundee Lake……… 78 Appendix F: Response to Comments…………………………………………………… 92 Tables Table 1. Stream segments identified on Sublists 3 and 5 of the 2004 Integrated List assessed for phosphorus impairment………………………………………6 Table 2. Assessment Units Analyzed from the 2006 Integrated List………………….....7 Table 3. Sublist 5 and Sublist 3 stream segments in spatial extent of non-tidal Passaic River basin TMDL study……………………………….. 20 Table 4. HUC 14 Assessment Units from 2006 Integrated List addressed in this and related TMDL studies………………………………………………………….. 21 Table 5. Description of Reservoirs……………………………………………………… 25 Table 6. -
92 Passaic River Basin 01387000 Wanaque River at Wanaque, Nj
92 PASSAIC RIVER BASIN 01387000 WANAQUE RIVER AT WANAQUE, NJ LOCATION.--Lat 41°02'39", long 74°17'35", Passaic County, Hydrologic Unit 02030103, on left bank 750 ft downstream from Raymond Dam in Wanaque, and 50 ft upstream from bridge on County Route 511 (Ringwood Avenue). DRAINAGE AREA.--90.4 mi2, considered as 94 mi2 Oct. 1, 1928 to Sept. 30, 1934. PERIOD OF RECORD.--December 1903 to December 1905 (gage heights only), September 1912 to April 1915, May 1919 to current year. GAGE.--Water-stage recorder and concrete control. Datum of gage is 210.00 ft above NGVD of 1929(levels from New Jersey Geological Survey bench mark). Dec. 16, 1903, to Dec. 31, 1905, nonrecording gage on highway bridge at site 50 ft downstream at different datum. Sept. 15, 1912, to Apr. 1, 1922, nonrecording gage at site 200 ft downstream from present concrete control at different datum. Apr. 1, 1922 to Mar. 14, 1931, water-stage recorder at site 400 ft downstream from present concrete control at present datum. REMARKS.--Records good, except for estimated daily discharges which are fair. Flow regulated by Greenwood Lake 11 mi above station, since October 1987 by Monksville Reservoir just upstream from Wanaque Reservoir, and since 1928 by Wanaque Reservoir (see Passaic River basin, reservoirs in). North Jersey District Water Supply Commission diverts water for municipal supply from Wanaque Reservoir. Water is diverted to Wanaque Reservoir from Posts Brook at Wanaque and from Ramapo River at Pompton Lakes (see Passaic River basin, diversions). Water diverted into basin above gage from Upper Greenwood Lake (Hudson River basin) by North Jersey District Water Supply Commission since 1968. -
Greenwood Lake Water Level Management Plan
Greenwood Lake Water Level Management Plan A Collaborative Effort by Greenwood Lake Commission P.O Box 1110 Greenwood Lake, NY 11025 with New Jersey Department of Environmental Protection Division of Parks and Forestry State Park Service Ringwood State Park and New York Department of Environmental Conservation 2011 – 2031 Project Report No. 3 - 1 - GREENWOOD LAKE COMMISSION Ella Filippone, New Jersey Chair Steve Defeo, New York Chair Clinton Smith Kerry Kirk-Pflugh Eric Hastings Bill Olsen George Verno Pat Ferracane Karen Emrich Ben Winstanley Christine McAteer-Purdy, Secretary - 2 - TABLE OF CONTENTS Page No. I. INTRODUCTION 4 II. GOALS AND OBJECTIVES 4 III. FACTS 5 A. CONSIDERATIONS 5 B. PROCEDURES 5 C. FACTS 6 IV. DRAWDOWN SCHEDULE – 20-Year Plan 6 V. OVERVIEW OF PROCDEURES FOR DRAWDOWN 6 VI. PRIMARY PARTNERS AND ROLES 8 A. THE ROLE OF THE STATE OF NEW JERSEY 8 B. THE ROLE OF THE GREENWOOD LAKE COMMISSION 9 VII. OTHER PARTIES INVOLVED AND THEIR ROLES 10 A. NEW YORK STATE DEPARTMENT OF ENVIRONMENTAL CONSERVATION 11 B. NEW JERSEY HIGHLANDS COUNCIL 11 C. NEW YORK DISTRICT, CORPS OF ENGINEERS 11 D. THE NORTH JERSEY DISTRICT WATER SUPPLY COMMISSION 12 E. PASSAIC COUNTY, NEW JERSEY AND ORANGE COUNTY, NEW YORK 12 F. TOWNSHIP OF WEST MILFORD, NEW JERSEY; VILLAGE OF GREENWOOD LAKE, NEW YORK; AND TOWN OF WARWICK, NEW YORK 13 G. UNITED STATES GEOLOGICAL SURVEY 13 H. UNITED STATES COAST GUARD 13. VIII. DRAWDOWN PACKAGE CONTENTS 13 - 3 - I. Introduction This document is to be used as a Water Level Management Plan that is the source for directing future drawdowns of the waters which lie within Passaic County, New Jersey and Orange County, New York. -
Water Resources of the New Jersey Part of the Ramapo River Basin
Water Resources of the New Jersey Part of the Ramapo River Basin GEOLOGICAL SURVEY WATER-SUPPLY PAPER 1974 Prepared in cooperation with the New Jersey Department of Conservation and Economic Development, Division of Water Policy and Supply Water Resources of the New Jersey Part of the Ramapo River Basin By JOHN VECCHIOLI and E. G. MILLER GEOLOGICAL SURVEY WATER-SUPPLY PAPER 1974 Prepared in cooperation with the New Jersey Department of Conservation and Economic Development, Division of Water Policy and Supply UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1973 UNITED STATES DEPARTMENT OF THE INTERIOR ROGERS C. B. MORTON, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress catalog-card No. 72-600358 For sale bv the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 - Price $2.20 Stock Number 2401-02417 CONTENTS Page Abstract.................................................................................................................. 1 Introduction............................................................................................ ............ 2 Purpose and scope of report.............................................................. 2 Acknowledgments.......................................................................................... 3 Previous studies............................................................................................. 3 Geography...................................................................................................... 4 Geology -
Prepared in Cooperation with the NEW JERSEY DEPARTMENT of ENVIRONMENTAL PROTECTION, DIVISION of WATER RESOURCES
UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY LOW-FLOW CHARACTERISTICS AND FLOW DURATION OF NEW JERSEY STREAMS By Brian D. Gillespie and Robert D. Sehopp Open-File Report 81-1110 Prepared in cooperation with the NEW JERSEY DEPARTMENT OF ENVIRONMENTAL PROTECTION, DIVISION OF WATER RESOURCES Trenton, New Jersey January 1982 UNITED STATES DEPARTMENT OF THE INTERIOR JAMES G. WATT, Secretary GEOLOGICAL SURVEY Dallas L. Peck, Director Tor additional information, write to: U.S. Geological Survey Room 430, Federal Building 402 East State Street Trenton, New Jersey 08608 Ill CONTENTS Page Abstract................................................... 1 Introduction............................................... 1 Method of study ............................................ 2 Flow-duration analysis..................................... 5 Low-flow frequency analysis................................ 7 Continuous gaging stations............................... 7 Partial-record sites..................................... 10 Selected references........................................ 14 Low-flow characteristics of gaging sites................... 15 Hudson, Hackensack, Passaic, Elizabeth, and Rahway River basins.............................................. 17 Station index, in downstream order..................... 19 Station descriptions and data.......................... 21 Raritan River basin...................................... 53 Station index, in downstream order..................... 55 Station descriptions and data......................... -
Extensions of Remarks E1261 EXTENSIONS of REMARKS
September 17, 2018 CONGRESSIONAL RECORD — Extensions of Remarks E1261 EXTENSIONS OF REMARKS INTRODUCTION OF THE HUMAN With poor traceability and a lack of account- and his parent’s before him. They always re- TRAFFICKING AND IUU FISHING ability in the global seafood supply chain, we mained optimists and Mike is someone who ACT simply do not know where our seafood prod- from humble beginnings built an enviable leg- ucts come from or the conditions under which acy in our state. We can all take a lesson in HON. MADELEINE Z. BORDALLO they are harvested and processed. hard work, determination, and the entrepre- OF GUAM We must ensure that American fishermen neurial spirit from Mike Leprino. He is pre- IN THE HOUSE OF REPRESENTATIVES are never expected to compete against foreign ceded in death by his wife Joan, son Michael, seafood imports harvested with slave labor. Monday, September 17, 2018 sister Ange Testa, and brother Lou. Mike is Our bipartisan bill builds upon the Victims of survived by his wife Suzy, daughters; Laurie Ms. BORDALLO. Mr. Speaker, today I intro- Trafficking and Violence Protection Act of Leprino, Nancy Leprino, and Mary Leprino. He duce the Human Trafficking and IUU Fishing 2000 (Public Law 106–386), sponsored by is also survived by 6 grandchildren, 2 great- Act. I thank my colleagues, Congressman GRI- Congressman SMITH (R–NJ) from New Jersey. grandchildren, sister Marie Videtto and brother JALVA (D–AZ) and Congresswomen I urge all my colleagues to join us in co- Jim Leprino. Those of us who were fortunate RADEWAGEN (R–AS) and BONAMICI (D–OR), for sponsoring the Human Trafficking and IUU enough to know Mike and his indomitable opti- their support as original cosponsors. -
Lower Devonian Glacial Erratics from High Mountain, Northern New Jersey, USA: Discovery, Provenance, and Significance
Lower Devonian glacial erratics from High Mountain, northern New Jersey, USA: Discovery, provenance, and significance Martin A. Becker1*and Alex Bartholomew2 1. Department of Environmental Science, William Paterson University, Wayne, New Jersey 07470, USA 2. Geology Department, SUNY, New Paltz, New York 12561, USA *Corresponding author <[email protected]> Date received 31 January 2013 ¶ Date accepted 22 November 2013 ABSTRACT Large, fossiliferous, arenaceous limestone glacial erratics are widespread on High Mountain, Passaic County, New Jersey. Analysis of the invertebrate fossils along with the distinct lithology indicates that these erratics belong to the Rickard Hill Facies of the Schoharie Formation (Lower Devonian, Tristates Group). Outcrops of the Rickard Hill Facies of the Schoharie Formation occur in a narrow belt within the Helderberg Mountains Region of New York due north of High Mountain. Reconstruction of the glacial history across the Helderberg Mountains Region and New Jersey Piedmont indicates that the Rickard Hill Erratics were transported tens of kilometers from their original source region during the late Wisconsinan glaciation. The Rickard Hill Erratics provide a unique opportunity to reconstruct an additional element of the complex surficial geology of the New Jersey Piedmont and High Mountain. Palynology of kettle ponds adjacent to High Mountain along with cosmogenic-nuclide exposure studies on glacial erratics from the late Wisconsinan terminal moraine and the regional lake varve record indicate that the final deposition of the Rickard Hill Erratics occurred within a few thousand years after 18 500 YBP. RÉSUMÉ Les grand blocs erratiques fossilifères apparaissent disperses dans les formations basaltiques de Preakness (Jurassique Inférieur) sur le mont High, dans le conte de Passaïc, dans l’État du New Jersey (NJ). -
Ii. Natural Resources of the Greenwood Lake Watershed
II. NATURAL RESOURCES II. NATURAL RESOURCES OF THE GREENWOOD LAKE WATERSHED A. LAND RESOURCES Geologic History The Greenwood Lake Watershed is located in the Highlands Physiographic Province, as shown in Figure II.A-1. The Highlands are underlain by the oldest rocks in New Jersey. These Precambrian igneous and metamorphic rocks were formed between 1.3 billion and 750 million years ago by the melting and recrystallization of sedimentary rocks that were deeply buried, subjected to high pressure and temperature, and intensely deformed.1 The Precambrian rocks are interrupted by several elongate northeast-southwest trending belts of folded Paleozoic sedimentary rocks equivalent to the rocks of the Valley and Ridge Province. Figure II.A-1 - Physiographic Provinces of New Jersey 1 New Jersey Geological Survey, NJ Department of Environmental Protection. 1999. The Geology of New Jersey. II-1 II. NATURAL RESOURCES The Highlands ridges in New Jersey are a southward continuation of the Green or Taconic Mountains of Vermont and Massachusetts, the New England Upland of Connecticut, and the Hudson Highlands of New York.2 The ridges continue through Pennsylvania to the vicinity of Reading. This Reading Prong of the New England Physiographic Province plunges beneath the surface of younger rocks for a distance of about fifty miles southwest of Reading and reappears where the northern end of the Blue Ridge Mountains begins to rise above the surrounding country. The Blue Ridge Mountains of the Virginia Appalachians, the mountains of New England, and the Highlands of New Jersey and New York all have a similar geologic history and character. Topography The granites and gneisses of the Highlands are resistant to erosion and create a hilly upland dissected by the deep, steep-sided valleys of major streams.3 The Highlands can be characterized as broad high ridges composed of complex folded and faulted crystalline rocks and separated by deep narrow valleys.4 The topography follows the northeast-southwest trend of the geologic structure and rock formations.