Visions for the Whippany Watershed
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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. -
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......................... -
Section 3. County Profile
Section 3: County Profile SECTION 3. COUNTY PROFILE This profile describes the general information of the County (physical setting, population and demographics, general building stock, and land use and population trends) and critical facilities located within Morris County. In Section 3, specific profile information is presented and analyzed to develop an understanding of the study area, including the economic, structural, and population assets at risk and the particular concerns that may be present related to hazards analyzed (for example, a high percentage of vulnerable persons in an area). 2020 HMP Changes The “County Profile” is now located in Section 3; previously located in Section 4. It contains updated information regarding the County's physical setting, population and demographics and trends, general building stock, land use and trends, potential new development and critical facilities. This includes U.S. Census ACS 2017 data and additional information regarding the New Jersey Highlands Region in the Development Trends/Future Development subsection. Critical facilities identified as community lifelines using FEMA’s lifeline definition and seven categories were added to the inventory and described in this section. 3.1 GENERAL INFORMATION Morris County is one of the fastest growing counties in the New York-New Jersey-Connecticut metropolitan region. It is located amid rolling hills, broad valleys, and lakes approximately 30 miles northwest of New York City. The County was created by an Act of the State Legislature on March 15, 1738, separating it from Hunterdon County. Morris County was named after Colonel Lewis Morris, then Governor of the Province of New Jersey (the area that now includes Morris, Sussex, and Warren Counties). -
Morristown National Historical Park Geologic Resources Inventory Report
National Park Service US Department of the Interior Natural Resource Stewardship and Science Morristown National Historical Park Geologic Resources Inventory Report Natural Resource Report NPS/NRSS/GRD/NRR—2014/841 ON THE COVER Cannon at Fort Nonsense overlooking Morristown. Photograph by Jared Kofsky (Creative Commons Attribution-Share Alike 3.0 Unported [CC BY-SA 3.0] license) available at: http://commons.wikimedia.org/wiki/File:Fort_Nonsense_of_Morristown.JPG (accessed 12 August 2014) THIS PAGE Split-rail fence at Jockey Hollow in the winter. Photograph by Daniel Beards, available at: http://albums.phanfare.com/isolated/CUUsqZbg/1/6144461_7039483 (accessed 12 August 2014) Morristown National Historical Park Geologic Resources Inventory Report Natural Resource Report NPS/NRSS/GRD/NRR—2014/841 Trista L. Thornberry-Ehrlich Colorado State University Research Associate National Park Service Geologic Resources Division Geologic Resources Inventory PO Box 25287 Denver, CO 80225 August 2014 US Department of the Interior National Park Service Natural Resource Stewardship and Science Fort Collins, Colorado The National Park Service, Natural Resource Stewardship and Science office in Fort Collins, Colorado, publishes a range of reports that address natural resource topics. These reports are of interest and applicability to a broad audience in the National Park Service and others in natural resource management, including scientists, conservation and environmental constituencies, and the public. The Natural Resource Report Series is used to disseminate high-priority, current natural resource management information with managerial application. The series targets a general, diverse audience, and may contain NPS policy considerations or address sensitive issues of management applicability. All manuscripts in the series receive the appropriate level of peer review to ensure that the information is scientifically credible, technically accurate, appropriately written for the intended audience, and designed and published in a professional manner. -
Problems of Encroachment
THE PASSAIC RIVER FLOOD PLAIN AND BASIN IN NEW JERSEY PROBLEMS OF ENCROACHMENT JOSEPH WEISBERG & JOHN MARCHISIN Department of Geoscience/Geography Jersey City State College The field experience follows parts of the Passaic River The "J ersey" Highlands extends from 8;nd its tributaries beginning at the Newark Campus of Pennsylvania's Reading Hills through New Jersey and Rutgers University. The trip parallels the course of the beyond New York State. The Reading Prong, composed River. It then continues along U.S. Route 46 West to partially of the Highlands, is a series of crystalline Wayne, Oakland, Lincoln Park and Fairfield in Passaic gneiss ridges trending in a Northeast to Southwest direc~ and Essex Counties near the confluence of the major tion. These crystalline ridges are' nearly parallel tributaries; the Pequannock, Ramapo and Pompton throughout most of their length. In the upper western Rivers and returns to Newark. portion, sandstones and conglomerates are common with a veneer of glacial till dominant in the region. See The Passaic River Basin figure 3 and table 1. Created during the Wisconsin age, the present Predominantly, shales and sandstones underlie the drainage basin of the Passaic River trends in a generally Triassic lowlands. These units trend Northeast east-to-southeast direction in the Passaic-Essex County Southwest along extrusions and exposed intrusives of . Region. The River, rising in Mendham Township, N.1. basaltic origin. Both the sedimentary and igneous units in Morris County I receives major tributaries as the Sad of the Triassic Lowlands dip toward the Northwest at dle River, Mahwah River, Third River, Rockaway angles generally between 3~18 degrees. -
APPENDIX E. RISK ASSESSMENT SUPPLEMENT This Appendix Contains Supporting Information for the Risk Assessment (Section 4) As Available
Appendix E: Risk Assessment Supplement APPENDIX E. RISK ASSESSMENT SUPPLEMENT This appendix contains supporting information for the Risk Assessment (Section 4) as available. It contains excerpts of the previous events and losses as presented in the 2015 HMP, organized by hazard of concern. This information has been compiled into one appendix for ease of reference; however, it has not been updated or verified, and is reproduced as documented in the 2015 plan. In order to create a more streamlined plan, the 2020 HMP was reorganized and condensed into a practical and more readable document for the public with the goal of providing a plan easier to implement for the County and all municipalities to support future risk reduction. The information in this appendix supplements the information provided in Section 4.3 of this plan. E.1 CRITICAL FACILITIES AND LIFELINES The identification of community lifelines across Morris County provides an enhancement to the 2020 HMP. FEMA defines a lifeline as: “providing indispensable service that enables the continuous operation of critical business and government functions, and is critical to human health and safety, or economic security.” Identifying community lifelines will help government officials and stakeholders to prioritize, sequence, and focus response efforts towards maintaining or restoring the most critical services and infrastructure within their respective jurisdiction(s). Identifying potential impacts to lifelines can help to inform the planning process and determining priorities in the event an emergency occur. The following page is FEMA’s factsheet that describes lifelines further. DMA 2000 Hazard Mitigation Plan Update – Morris County, New Jersey E-1 July 2020 Community Lifelines National Response Framework Update (Fourth Edition) A lifeline provides indispensable service that What are the opportunities of enables the continuous operation of critical lifelines? business and government functions, and is critical to human health and safety, or economic security. -
Morristown National Historical Park Foundation Document
NATIONAL PARK SERVICE • U.S. DEPARTMENT OF THE INTERIOR Foundation Document Morristown National Historical Park New Jersey June 2018 Foundation Document MORRISTOWN 287 Museum 24 Washington Visitor Information202 Washington’s Fort Nonsense Headquarters 24 510 202 Jockey Hollow 287 Visitor Center New Jersey Brigade Area/ North Cross Estate Gardens 0 0.5 1 Kilometer 0 0.5 1 Mile Tour Road Patriots’ Path Hiking trail 287 Washington- Rochambeau National Historic Trail 202 Morristown National Historical Park Contents Mission of the National Park Service 1 Introduction 2 Part 1: Core Components 3 Brief Description of the Park 3 Park Purpose 5 Park Significance 6 Fundamental Resources and Values 7 Other Important Resources and Values 8 Interpretive Themes 9 Part 2: Dynamic Components 10 Special Mandates and Administrative Commitments 10 Special Mandates 10 Administrative Commitments 11 Assessment of Planning and Data Needs 11 Analysis of Fundamental Resources and Values 11 Analysis of Other Important Resources and Values 24 Identification of Key Issues and Associated Planning and Data Needs 29 Planning and Data Needs 30 Part 3: Contributors 34 Morristown National Historical Park 34 NPS Northeast Region 34 Other NPS Staff 34 Partners 34 Appendixes 35 Appendix A: Enabling Legislation and Legislative Acts for Morristown National Historical Park 35 Appendix B: Interpretive Theme Matrix 42 Appendix C: Inventory of Administrative Commitments 51 Appendix D: Past Park Planning and Data Collection Efforts 52 Foundation Document Morristown National Historical Park Mission of the National Park Service The National Park Service (NPS) preserves unimpaired the natural and cultural resources and values of the national park system for the enjoyment, education, and inspiration of this and future generations. -
Description of the Raritan Quadrangle
DESCRIPTION OF THE RARITAN QUADRANGLE. By W. S. Bayley, H. B. Kiimmel, and B. D. Salisbury.« INTRODUCTION. of the province lose much of their definite character, but the Piedmont Plateau and the Appalachian Mountain belt are not Appalachian Valley is continued in the Champlain Valley of separated by a sharp geologic boundary, and in many places GENERAL RELATIONS. western Vermont. geologic formations extend continuously from the mountain Position and area. The Raritan quadrangle lies between In New Jersey the eastern part of the belt is occupied by the belt into the great valley. In the general region including parallels 40° 30' and 41° and meridians 74° 30' and 75° and broad Kittatinny Valley and the western part by the narrow northern New Jersey, southeastern New York, and eastern comprises four smaller (15') quadrangles the Hackettstown, Delaware Valley, the two being separated by the bold even- Pennsylvania, however, the conditions are somewhat different. Lake Hopatcong, High Bridge, and Somerville covering an crested ridge of Kittatinny Mountain, which, although one of Each of the physiographic subdivisions is strikingly different area of 905.27 square miles. It is in northern New Jersey the minor ridges in the Appalachian Valley belt, reaches a from the others in geologic character, although even here (see fig. 1) and includes parts of Hunterdon, Middlesex, Morris, greater altitude than the Highlands east of the valley. absolute lines can not be drawn, as some formations are com Somerset, Sussex, and Warren counties and contains the cities The Appalachian Valley is bounded on the east by the mon to all three. -
Simulation of Transient Ground-Water Flow in the Valley-Fill Aquifers of the Upper Rockaway River Basin, Morris County, New Jersey
U.S. Department of the Interior U.S. Geological Survey SIMULATION OF TRANSIENT GROUND-WATER FLOW IN THE VALLEY-FILL AQUIFERS OF THE UPPER ROCKAWAY RIVER BASIN, MORRIS COUNTY, NEW JERSEY Water-Resources Investigations Report 01-4174 Prepared in cooperation with the NEW JERSEY DEPARTMENT OF ENVIRONMENTAL PROTECTION Cover photo: View looking upstream from the gaging station on the Rockaway River above the Boonton Reservoir with weir and gage house. Photo about 1940’s. SIMULATION OF TRANSIENT GROUND-WATER FLOW IN THE VALLEY-FILL AQUIFERS OF THE UPPER ROCKAWAY RIVER BASIN, MORRIS COUNTY, NEW JERSEY by Alison D. Gordon U.S. GEOLOGICAL SURVEY Water-Resources Investigations Report 01-4174 Prepared in cooperation with the NEW JERSEY DEPARTMENT OF ENVIRONMENTAL PROTECTION West Trenton, New Jersey 2002 U.S. DEPARTMENT OF THE INTERIOR GALE A. NORTON, Secretary U.S. GEOLOGICAL SURVEY Charles G. Groat, Director For additional information Copies of this report can be write to: purchased from: District Chief U.S. Geological Survey U.S Geological Survey Branch of Information Services Mountain View Office Park Box 25286 810 Bear Tavern Road Denver, CO 80225-0286 West Trenton, NJ 08628 CONTENTS Page Abstract. 1 Introduction. 2 Purpose and scope . 2 Location and physical setting . 2 Site-numbering system . 3 Hydrogeology of the valley-fill aquifer system . 3 Description of hydraulic characteristics . 5 Ground-water levels and directions of flow . 6 Ground-water withdrawals . 14 Aquifer/stream interactions . 14 Simulation of ground-water flow . 18 Model design, grid, and boundary conditions . 18 Model input. 21 Recharge . 21 Hydraulic characteristics . 24 Model calibration and results . -
Hydrologic Conditions in the Upper Rockaway River Basin
HYDROLOGIC CONDITIONS IN THE UPPER ROCKAWAY RIVER BASIN, NEW JERSEY, 1984-86 By F.L. Schaefer, P.T. Harte, J.A. Smith, and B.A. Kurtz U.S. GEOLOGICAL SURVEY Water-Resources Investigations Report 91-4169 Prepared in cooperation with the NEW JERSEY DEPARTMENT OF ENVIRONMENTAL PROTECTION AND ENERGY West Trenton, New Jersey 1993 U.S. DEPARTMENT OF THE INTERIOR MANUEL LUJAN, JR., Secretary U.S. GEOLOGICAL SURVEY Dallas L. Peck, Director For additional information Copies of this report can be write to: purchased from: District Chief U.S. Geological Survey U.S. Geological Survey Books and Open-File Reports Section Mountain View Office Park Federal Center Suite 206 Box 25425 810 Bear Tavern Road Denver, CO 80225 West Trenton, NJ 08628 CONTENTS Page Abstract............................................................. 1 Introduction......................................................... 3 Purpose and scope............................................... 3 Previous studies................................................ 3 Site-numbering system........................................... 4 Acknowledgments................................................. 4 Description of study area............................................ 4 Climate and precipitation....................................... 7 Geohydrologic setting........................................... 7 Bedrock geology............................................ 7 Glacial deposits........................................... 9 Geohydrology............................................... 13 Water -
Draft Section 3 – County Profile
Section 3: County Profile SECTION 3 COUNTY PROFILE The County profile describes the general information (physical setting, population and demographics, general building stock, and land use and population trends) and critical facilities located within Essex County. In Section 4 (Risk Assessment), specific profile information is presented and analyzed to develop an understanding of the study area, including the economic, structural, and population assets at risk and the particular concerns that may be present related to hazards analyzed (for example, a high percentage of vulnerable persons in an area). 3.1 PHYSICAL SETTING Essex County is located in northern New Jersey, approximately 20 miles south of the New York State border, and 10 miles west of Manhattan. The County is bordered by Passaic County to the north, Bergen County to the east-northeast, Hudson County to the east, Union County to the south and Morris County to the west. The eastern and western borders of Essex County are defined by the Passaic River. The County is separated from Morris County by the eastern branch of the Passaic River. The southeast border of the County is situated on the Newark Bay with approximately 3.5 miles of shoreline (The County’s topography is flat in the east and slowly rises toward the west upon the approach of the Watchung Mountains. The Watchung Mountains run roughly north south through the center of Essex County. To the west of the Watchung Mountain, the slope gently declines back to a flatter topography as it approaches the western branch of the Passaic River. The highest elevations in the County are located in three municipalities within the Watchung Mountain range: Essex Fells, North Caldwell and Verona, with the highest point of 691 feet above sea level. -
Hydrology, Channel Morphology, and Holocene
HYDROLOGY, CHANNEL MORPHOLOGY, AND HOLOCENE SEDIMENTATION RECORD OF THE CENTRAL PASSAIC RIVER BASIN, NJ by RACHEL MACKENZIE FILO A thesis submitted to the School of Graduate Studies Rutgers, The State University of New Jersey In partial fulfillment of the requirements For the degree of Master of Science Graduate Program in Geological Sciences Written under the direction of Dr. Gail M. Ashley And approved by New Brunswick, New Jersey October 2017 ABSTRACT OF THE THESIS Hydrology, Channel Morphology, and Holocene Sedimentation Record of the Central Passaic River Basin, NJ By RACHEL MACKENZIE FILO Thesis Director: Dr. Gail M. Ashley The Passaic River Basin, which spans 935 mi² over northern New Jersey and parts of New York, is defined by both its glacial and post-glacial history. The retreating ice sheet (~22-18 ka) created Glacial Lake Passaic, impounded behind the Watchung Mountains until a new outlet was opened at Little Falls. Glacial rerouted the Passaic River to a northeastward course, with wetlands developing on the glacial lake sediments. One such wetland, the Great Piece Meadows, covers 2,343 acres of undeveloped floodplain within the Central Basin. Three oxbows within these wetlands, named Oxbow2, RC, and TZS, were cored to determine the flooding and geomorphological history of the central Passaic’s floodplain. Radiocarbon dates and grain size data suggests that oxbow TZS was cut off from the main channel around 9-9.5 ka B.P., and that the ii Oxbow2 and RC were cut off around 3.6 B.P. These dates fall within a transition from a dry to a wet period during the Holocene, which may have been a cause for the avulsions.