NATURAL RESOURCE INVENTORY UPDATED 2012 & 2015 West Amwell Township HUNTERDON CO NEW JERSEY 2008 NATURAL RESOURCE INVENTORY UPDATED 2012 & 2015 West Amwell Township

Total Page:16

File Type:pdf, Size:1020Kb

NATURAL RESOURCE INVENTORY UPDATED 2012 & 2015 West Amwell Township HUNTERDON CO NEW JERSEY 2008 NATURAL RESOURCE INVENTORY UPDATED 2012 & 2015 West Amwell Township 2008 NATURAL RESOURCE INVENTORY UPDATED 2012 & 2015 West Amwell Township HUNTERDON CO NEW JERSEY 2008 NATURAL RESOURCE INVENTORY UPDATED 2012 & 2015 West Amwell Township DEDICATIONS TO THE NATURAL ENVIRONMENT OF WEST AMWELL TOWNSHIP for providing unique beauty and healthful resources for our community TO THE RESIDENTS OF WEST AMWELL TOWNSHIP who depend on and enjoy these precious resources ACKNOWLEDGEMENTS TO THE HUNTERDON COUNTY PLANNING BOARD for assistance with maps and data interpretation TO THE STONYBROOK MILLSTONE WATERSHED ASSOCIATION for review of the Natural Resource Inventory and assistance with maps TO THE DELAWARE TOWNSHIP ENVIRONMENTAL COMMISSION for permission to use their Natural Resource Inventory TO THE ASSOCIATION OF NEW JERSEY ENVIRONMENTAL COMMISSIONS — ANJEC for providing model Natural Resource Inventories TO THE MEMBERS OF THE WEST AMWELL TOWNSHIP ENVIRONMENTAL COMMISSION who have volunteered hundreds of hours to research, write and assemble this document Original NRI July 2008, updated December 2012 and July 2015 2008 NATURAL RESOURCE INVENTORY UPDATED 2012 & 2015 West Amwell Township TABLE OF CONTENTS List of Tables, Figures and Appendices.......................……1 Section 1 Introduction ...........................................…. 2 Section 2 Climate ……………………………………...………..… 3 Section 3 Land Use / Land Cover ………………………………………..4 Section 4 Hydrogeology ..........................…………........7.……6 Section 5 Well Head Protection Areas ……………………………..9 Section 6 Soils ...................................……………………….....…..10 Section 7 Known Contaminated Sites …………………………..12 Section 8 Streams and Subwatersheds …..……………............14 Section 9 Surface Water Quality ………………………………………..16 Section 10 Special Protection Waters Designation for the Lower Delaware River ………….....................18 Section 11 AMNET Biological Monitoring and Water Quality .......................................20 Section 12 Vernal Pools …….............……………………............…..21 Section 13 Wetlands …………………………………............….......…..22 Section 14 Floodplains ……..........................……………………..24 Section 15 Steep Slopes ……....................………………………..26 Section 16 Forested Areas ...............…………………………………..26 Section 17 Riparian Areas ………...................…………………..31 Section 18 Agriculture ……..........................…………………………..33 Section 19 Wildlife and Critical Habitiat …………………………..35 Section 20 The Sourland Region ………………………………………..37 Section 21 Natural Heritage Priority Site ………………………………39 References and Credits ...................................……………40 Map Data Sources ...................................……………………42 2008 NATURAL RESOURCE INVENTORY OF WEST AMWELL TOWNSHIP 1 List of Tables Tables are located throughout the main body of the 2008 West Amwell Township Natural Resource Inventory (NRI) on the pages indicated below. Table 1 West Amwell Population Change, 1970-2000...….5 Table 2 Septic Limitations …...........…………………..............….12 Table 3 Known Contaminated Sites …...........……..................….13 Table 4 Subwatersheds …...........…………………..................….16 Table 5 AMNET Monitoring, 1997 …...........…………............21.20 Table 6 AMNET Monitoring, 2003 …...........………..............….21 Table 7 Wetland Types …...........…………………...................….23 Table 8 Forest Types …...........…………………......................….27 List of Figures Figures are located in a separate section or folder entitled “2008 WEST AMWELL TWP NRI - FIGURES.” Figure 1 Land Use, NJDEP, 1995 Figure 2 Land Use, NJDEP, 2007 (replaces 2002 map) Figure 3 Sole Source Aquifers Figure 4 Bedrock Geology Figure 5 Well Head Protection Areas Figure 6a Highly Erodable Soils Figure 6b Soil Classification Figure 7 Known Contaminated Sites Figure 8a Streams and Waterbodies Figure 8b Subwatersheds Figure 9 Surface Water Quality Figure 10 AMNET Monitoring Stations Figure 11 FEMA, Hunterdon County Flood Map Figure 12 Steep Slopes Figure 13 Farmland Assessed Figure 14 Agricultural Soils Figure 15 Critical Habitat for Threatened and Endangered Species Figure 16 The Sourland Region Figure 17 Natural Heritage Priority Site List of Appendices Appendices are located in a separate section or folder entitled “2008 WEST AMWELL TWP NRI - APPENDICES” Appendix 1 Build-Out Analysis Appendix 2 Evaluation of Groundwater Resources Appendix 3 Category 1 Guidelines, January 2008 Appendix 4 FEMA Critical Areas Appendix 5 Woodlands Ordinance Appendix 6 Stream Corridor Ordinance Appendix 7 New Jersey Threatened and Endangered Wildlife Appendix 8 Sourland Mountain Smart Growth Planning Project Appendix 9 Alexauken Creek Wildlife Management Area Biological Inventory Report Appendix 10 Exotic and Invasive Plants To Avoid and Do Not Plant List Appendix 11 Invasive Species and Native Alternatives 2008 NATURAL RESOURCE INVENTORY OF WEST AMWELL TOWNSHIP 2 SECTION 1 Introduction “We are starting to see that our energy and environmental ills stem, essentially, from the same source: from patterns of growth and development that waste our energy resources just as liberally as they lay waste our natural environment. We no longer live in a time when we were few and the land was wide and waiting for us. We have reached a point where we can no longer insulate ourselves from the punishment and pollution we visit upon the earth and the atmosphere, and where the natural resources we once regarded as so endlessly available and expendable are becoming increasingly hard to get.” — EXCERPTED FROM 1977 NATURAL RESOURCE INVENTORY OF WEST AMWELL TOWNSHIP This Natural Resource Inventory documents the natural resource base of West Amwell Township and presents considerations for public policy and land use. All maps and data presented here represent the most up-to-date information available. Our valuable natural resources merit consideration during the planning process and may be indicators of larger issues that require further study. This NRI is not intended to produce original research and is not meant to replace the primary data sources upon which it is based. It is intended for preliminary assessments of projects and cannot substi- tute for on-site testing and evaluations. Some components of the environment have been studied or presented in detail, while other important factors may have been minimally addressed. When new or Map of updated information becomes available New Jersey Political Subdivisions or new issues emerge, updates will be appended to the NRI. Existing map sources provided the basis for establishing the location of natural resources presented in this NRI. Since the maps were not field verified, the resource mapping is intended for general planning purposes and should not substitute for LOCATION OF site-specific surveys. WEST AMWELL TOWNSHIP 2008 NATURAL RESOURCE INVENTORY OF WEST AMWELL TOWNSHIP 3 SECTION NEW JERSEY CLIMATE ZONES 2 Climate Viewed on a global scale, West Amwell Township is situated in the North Temperate Zone, the part of the Earth’s surface between the Arctic Circle and the Tropic of Cancer. Temperate forested areas occur in eastern North America and central Europe. This forest biome has well-defined seasons with distinct winters but also has a moderate climate and a growing season of 140-200 days during four to six frost-free months. Fertile soils support temperate forests and moderately dense forest canopy, which allows light penetration and promotes well-developed NORTH CENTRAL and richly diversified understory and animal life. SOUTHWEST PINE BARRENS At the local level, West Amwell Township is in the northern COASTAL climate zone of New Jersey. Hunterdon County is generally not influenced by the Atlantic Ocean and therefore has a continental type of climate. Prevailing winds are from the southwest in summer and from the northwest in winter. The average low temperature is 32 degrees and the average high temperature is 78 degrees. The annual average temperature is 53 degrees. Compared with central and southern New Jersey, West Amwell Township generally has colder temperatures and greater snowfall in winter, with a greater average annual precipitation overall. Precipitation amounts (rain- fall and rainfall equivalent of snowfall) average 48.8 inches annually. Spring and summer months tend to experience temperatures consistent with those found in the rest of the state, averaging between 51 and 73 degrees Fahrenheit. The difference between the continental and coastal climate types has a profound effect on length of growing season, characterized by the dates of first and last killing frost. Varying within the region as well as from year to year, the growing season averages 155 days. The average date of the last killing frost is May 4 and the average date of the first killing frost is October 7. Areas within the northern climate zone have, however, experienced killing frosts as early as mid-September and as late as mid-June. Another climate indicator is the hardiness zones established by the United States Department of Agriculture. NEW JERSEY HARDINESS ZONES As depicted on the adjacent map, West Amwell Township falls within Zone 6b, with an average annual minimum temperature range of 0 to -5 degrees Fahrenheit. The Indicator Plant Examples 5b -10 TO -15 6a -5 TO -10 for Zone 6b that are native to the region include: 6b 0 TO -5 • Red Maple (Acer rubrum) 7a 0 TO 5 • Tulip Tree (Liriodendron tulipifera) 7b 5 TO 10 • Dogwood (Cornus spp.) • Red Oak (Quercus rubra) • Spicebush (Lindera benzoin) • Viburnum (Viburnum spp.) Hardiness zones are critical for successful cultivation or mainte-
Recommended publications
  • Igneous Processes During the Assembly and Breakup of Pangaea: Northern New Jersey and New York City
    IGNEOUS PROCESSES DURING THE ASSEMBLY AND BREAKUP OF PANGAEA: NORTHERN NEW JERSEY AND NEW YORK CITY CONFERENCE PROCEEDINGS AND FIELD GUIDE EDITED BY Alan I. Benimoff GEOLOGICAL ASSOCIATION OF NEW JERSEY XXX ANNUAL CONFERENCE AND FIELDTRIP OCTOBER 11 – 12, 2013 At the College of Staten Island, Staten Island, NY IGNEOUS PROCESSES DURING THE ASSEMBLY AND BREAKUP OF PANGAEA: NORTHERN NEW JERSEY AND NEW YORK CITY CONFERENCE PROCEEDINGS AND FIELD GUIDE EDITED BY Alan I. Benimoff GEOLOGICAL ASSOCIATION OF NEW JERSEY XXX ANNUAL CONFERENCE AND FIELDTRIP OCTOBER 11 – 12, 2013 COLLEGE OF STATEN ISLAND, STATEN ISLAND, NY i GEOLOGICAL ASSOCIATION OF NEW JERSEY 2012/2013 EXECUTIVE BOARD President .................................................. Alan I. Benimoff, PhD., College of Staten Island/CUNY Past President ............................................... Jane Alexander PhD., College of Staten Island/CUNY President Elect ............................... Nurdan S. Duzgoren-Aydin, PhD., New Jersey City University Recording Secretary ..................... Stephen J Urbanik, NJ Department of Environmental Protection Membership Secretary ..............................................Suzanne Macaoay Ferguson, Sadat Associates Treasurer ............................................... Emma C Rainforth, PhD., Ramapo College of New Jersey Councilor at Large………………………………..Alan Uminski Environmental Restoration, LLC Councilor at Large ............................................................ Pierre Lacombe, U.S. Geological Survey Councilor at Large .................................
    [Show full text]
  • Bedrock Geologic Map of the Monmouth Junction Quadrangle, Water Resources Management U.S
    DEPARTMENT OF ENVIRONMENTAL PROTECTION Prepared in cooperation with the BEDROCK GEOLOGIC MAP OF THE MONMOUTH JUNCTION QUADRANGLE, WATER RESOURCES MANAGEMENT U.S. GEOLOGICAL SURVEY SOMERSET, MIDDLESEX, AND MERCER COUNTIES, NEW JERSEY NEW JERSEY GEOLOGICAL AND WATER SURVEY NATIONAL GEOLOGIC MAPPING PROGRAM GEOLOGICAL MAP SERIES GMS 18-4 Cedar EXPLANATION OF MAP SYMBOLS cycle; lake level rises creating a stable deep lake environment followed by a fall in water level leading to complete Cardozo, N., and Allmendinger, R. W., 2013, Spherical projections with OSXStereonet: Computers & Geosciences, v. 51, p. 193 - 205, doi: 74°37'30" 35' Hill Cem 32'30" 74°30' 5 000m 5 5 desiccation of the lake. Within the Passaic Formation, organic-rick black and gray beds mark the deep lake 10.1016/j.cageo.2012.07.021. 32 E 33 34 535 536 537 538 539 540 541 490 000 FEET 542 40°30' 40°30' period, purple beds mark a shallower, slightly less organic-rich lake, and red beds mark a shallow oxygenated 6 Contacts 100 M Mettler lake in which most organic matter was oxidized. Olsen and others (1996) described the next longer cycle as the Christopher, R. A., 1979, Normapolles and triporate pollen assemblages from the Raritan and Magothy formations (Upper Cretaceous) of New 6 A 100 I 10 N Identity and existance certain, location accurate short modulating cycle, which is made up of five Van Houten cycles. The still longer in duration McLaughlin cycles Jersey: Palynology, v. 3, p. 73-121. S T 44 000m MWEL L RD 0 contain four short modulating cycles or 20 Van Houten cycles (figure 1).
    [Show full text]
  • Rock Climbing Inventory of NJ's State Parks and Forest
    Allamuchy Mountain, Stephens State Park Rock Climbing Inventory of NJ’s State Parks and Forest Prepared by Access NJ Contents Photo Credit: Matt Carlardo www.climbnj.com June, 2006 CRI 2007 Access NJ Scope of Inventory I. Climbing Overview of New Jersey Introduction NJ’s Climbing Resource II. Rock-Climbing and Cragging: New Jersey Demographics NJ's Climbing Season Climbers and the Environment Tradition of Rock Climbing on the East Coast III. Climbing Resource Inventory C.R.I. Matrix of NJ State Lands Climbing Areas IV. Climbing Management Issues Awareness and Issues Bolts and Fixed Anchors Natural Resource Protection V. Appendix Types of Rock-Climbing (Definitions) Climbing Injury Patterns and Injury Epidemiology Protecting Raptor Sites at Climbing Areas Position Paper 003: Climbers Impact Climbers Warning Statement VI. End-Sheets NJ State Parks Adopt a Crag 2 www.climbnj.com CRI 2007 Access NJ Introduction In a State known for its beaches, meadowlands and malls, rock climbing is a well established year-round, outdoor, all weather recreational activity. Rock Climbing “cragging” (A rock-climbers' term for a cliff or group of cliffs, in any location, which is or may be suitable for climbing) in NJ is limited by access. Climbing access in NJ is constrained by topography, weather, the environment and other variables. Climbing encounters access issues . with private landowners, municipalities, State and Federal Governments, watershed authorities and other landowners and managers of the States natural resources. The motives and impacts of climbers are not distinct from hikers, bikers, nor others who use NJ's open space areas. Climbers like these others, seek urban escape, nature appreciation, wildlife observation, exercise and a variety of other enriching outcomes when we use the resources of the New Jersey’s State Parks and Forests (Steve Matous, Access Fund Director, March 2004).
    [Show full text]
  • Spring 2021 Newsletter
    Spring | 2021 New Jersey Conservation FINDING PEACE in the PANDEMIC Getting outdoors for body and mind PIPELINE CASE HEADS TO U.S. SUPREME COURT 10 High court will decide if private PennEast company can seize public lands to build a for‐profit pipeline. SOMEWHERE, OVER THE RAINBOW 12 Rainbow Hill at Sourland Mountain Preserve offers sweeping views, including rainbows after storms! TEN MILE TRAIL VISION REALIZED 14 Newly‐preserved land helps connect 1,200 acres of open space and farmland in Hunterdon County. ABOUT THE COVER “During the pandemic this past year, being outdoors in natural surroundings simply felt nice, sane, and free.” MaryAnn Ragone DeLambily took this stunning photo while hiking through Franklin Parker Preserve, one of the many places New Jerseyans found solace over the past year. Trustees Rosina B. Dixon, M.D. HONORARY TRUSTEES PRESIDENT Hon. James J. Florio Wendy Mager FIRST VICE PRESIDENT Hon. Thomas H. Kean Joseph Lemond Hon. Maureen Ogden SECOND VICE PRESIDENT Hon. Christine Todd Whitman Finn Caspersen, Jr. TREASURER From Our Pamela P. Hirsch SECRETARY Executive Director ADVISORY COUNCIL Penelope Ayers ASSISTANT SECRETARY Bradley M. Campbell Michele S. Byers Cecilia Xie Birge Christopher J. Daggett Jennifer Bryson Wilma Frey Roger Byrom John D. Hatch Theodore Chase, Jr. Douglas H. Haynes It seems like we all need inspiration and hope this year given the not‐over‐yet pandemic, Jack Cimprich H. R. Hegener David Cronheim Hon. Rush D. Holt climate change, species extinction, tribalism, isolation and the news! Getting outdoors is one John L. Dana Susan L. Hullin way to find “Peace in the Pandemic” as you can read about in the pages that follow.
    [Show full text]
  • 2020 Natural Resources Inventory
    2020 NATURAL RESOURCES INVENTORY TOWNSHIP OF MONTGOMERY SOMERSET COUNTY, NEW JERSEY Prepared By: Tara Kenyon, AICP/PP Principal NJ License #33L100631400 Table of Contents EXECUTIVE SUMMARY ............................................................................................................................................... 5 AGRICULTURE ............................................................................................................................................................. 7 AGRICULTURAL INDUSTRY IN AND AROUND MONTGOMERY TOWNSHIP ...................................................... 7 REGULATIONS AND PROGRAMS RELATED TO AGRICULTURE ...................................................................... 11 HEALTH IMPACTS OF AGRICULTURAL AVAILABILITY AND LOSS TO HUMANS, PLANTS AND ANIMALS .... 14 HOW IS MONTGOMERY TOWNSHIP WORKING TO SUSTAIN AND ENHANCE AGRICULTURE? ................... 16 RECOMMENDATIONS AND POTENTIAL PROJECTS .......................................................................................... 18 CITATIONS ............................................................................................................................................................. 19 AIR QUALITY .............................................................................................................................................................. 21 CHARACTERISTICS OF AIR .................................................................................................................................. 21
    [Show full text]
  • Land, Natural Resources, and Geology
    Land and Natural Resources of West Amwell By Fred Bowers, Ph.D Goat Hill from the north Diabase Boulders are common. Shale and Argillite outcrops appear like this. General Description of the Area West Amwell Township is in Hunterdon County, New Jersey, USA. It is a 22 square mile rural township with just over 2200 people, located near Lambertville, New Jersey. It is one of the more scenic parts of the New Jersey Piedmont. It is identified in red on the maps below. West Amwell is characterized by most people as a "rocky land." One of the oldest villages in the township is called Rocktown. If you visit or look around the township, you cannot avoid seeing rocks and outcrops like those pictured above. Hunterdon County New Jersey, with West Amwell located at the southern border, marked in red The physiographic provinces of New Jersey, with Hunterdon County and West Amwell marked in red Rocks The backbone of West Amwell Township's land is the Sourland Mountain; a typical Piedmont ridge formed by a very hard igneous rock called diabase or "Trap Rock." The Sourland Mountain ends at the Delaware River below Goat Hill which you see in the picture above, looking south from the Lambertville toll bridge. To the south and north of the diabase, shale and argillite occurs, and these rocks form the lower lands we know of as Pleasant Valley and the shale ridges and valleys you see from around Mt. Airy. In order to appreciate the rocks and the influence they have on the look of the land, it is useful to have a short review of rocks.
    [Show full text]
  • Settings Report for the Central Delaware Tributaries Watershed Management Area 11
    Settings Report for the Central Delaware Tributaries Watershed Management Area 11 02 03 05 01 04 06 07 08 11 09 10 12 20 19 18 13 14 17 15 16 Prepared by: The Regional Planning Partnership Prepared for: NJDEP October 15, 2001 TABLE OF CONTENTS List of Figures v List of Tables vi Acknowledgements vii 1.0 Introduction 1 2.0 Importance of Watershed Planning 1 3.0 Significance of the Central Delaware Tributaries 2 4.0 Physical and Ecological Characteristics 4.1 Location 2 4.2 Physiography and Soils 3 4.3 Surface Water Hydrology 4 4.3.1 Hakihokake/Harihokake/Nishisakawick Creeks 5 4.3.2 Lockatong/Wickecheoke Watershed 6 4.3.3 Alexauken/Moores/Jacobs Watershed 6 4.3.4 Assunpink Creek Above Shipetaukin Creek 7 4.3.5 Assunpink Below Shipetaukin Creek 7 4.4 Land Use/Land Cover 9 4.4.1 Agricultural Land 9 4.4.2 Forest Land 11 4.4.3 Urban and Built Land 12 4.4.4 Wetlands 12 4.4.5 Water 14 4.4.6 Barren Lands 14 4.5 Natural Resource Priority Habitat 14 5.0 Surface Water Quality 5.1 Significance of Streams and Their Corridors 15 5.2 Federal Clean Water Act Requirements for Water Quality in New Jersey 15 5.3 Surface Water Quality Standards 16 5.4 Surface Water Quality Monitoring 18 i TABLE OF CONTENTS 5.4.1 Monitoring Stations in the Central Delaware Tributaries 18 5.5 Surface Water Quality in the Hakihokake/Harihokake/ Nishisakawick 5.5.1 Chemical and Sanitary Water Quality 19 5.5.2 Biological Evaluation 19 5.6 Surface Water Quality in the Lockatong/Wickecheoke Watershed 5.6.1 Chemical and Sanitary Water Quality 20 5.6.2 Biological Evaluation 20 5.7
    [Show full text]
  • Sourland Mountain Preserve
    About Sourland Mountain Preserve Sourland Mountain Preserve Trail Information Sourland Mountain The name “Sourlands” is derived from the fact Location: Sourland Mountain is located in Main Trail: The main trail in Sourland that early settlers found the rocky soils difficult East Amwell Township, in the southeastern Mountain Preserve is very wide and flat, with Preserve to farm. The limited supply of groundwater section of Hunterdon County. There is a a short uphill slope at the end. The trail winds saved the forest from destruction by small parking area at 233 Rileyville Road, through a beautiful deciduous forest, strewn developers. Its woodlands shelter a very rich Ringoes 08551. Please note: No restrooms with large boulders. Along this trail is a Trail Map and Guide and diverse native plant community. facilities are available. floodplain with a rich diversity of aquatic life. Directions from the Flemington Area: Yellow Trail: This trail branches off the Main The park’s 388 acres are comprised of a Trail, about a quarter of a mile from the deciduous forest with a swamp surrounded by Take Route 202/31 south from the Flemington Circle for 5 miles to the jug handle for parking area. It can be a very wet trail and two streams. Formed almost 200 million years crosses a small stream where hikers must rock ago, the rocks of the Sourlands, called diabase Wertsville Road (Route 602). Use the traffic light to cross over Route 202/31. Continue on hop. In spring, many wildflowers can be or “trap rock,” were used to produce railroad found along this trail.
    [Show full text]
  • 1 Alexauken Creek Wildlife Management Area Biological Inventory Report Washington Crossing Audubon Society Introduction The
    Alexauken Creek Wildlife Management Area Biological Inventory Report Washington Crossing Audubon Society Introduction The New Jersey Department of Fish and Wildlife recently purchased a tract of approximately 415 acres along Alexauken Creek in West Amwell Township to create the Alexauken Creek Wildlife Management Area (ACWMA). In the summer of 2002, Washington Crossing Audubon Society (WCAS) was contacted by Jamie Kampf and Hal Shute, neighbors of ACWMA, and invited to take a tour of the property. WCAS was also asked to consider conducting a biological inventory of the property and making recommendations for its management, based on information gathered in the inventory. On June 5, 2002 WCAS current and former board members Hannah Suthers, Pat Sziber, Rick Dutko and Herb Lord joined Hal Shute, Jamie Kampf and Gary Robinson for a tour of the property, and agreed that WCAS would conduct the study and provide a report in early 2004. The following sections provide a description of the property, a description of how the inventory was conducted, summaries of the results, and our recommendations for management of the property. View across formerly cultivated field. Old stone wall in the woods. Mantell Cottage. Pond. 1 Location Alexauken Creek Wildlife Management Area is located in the northeastern part of West Amwell Township, Hunterdon County, west of State Highway 31 and south of US Highway 202, on the edge of Sourland Mountain. Access and a parking area are on Rocktown-Lambertville Road, and the property extends northward and westward to Old York Road. A nearby but non-adjacent addition to the area on State Highway 31 was purchased in 2003 but was not surveyed by WCAS.
    [Show full text]
  • Triassic and Jurassic Formations of the Newark Basin
    TRIASSIC AND JURASSIC FORMATIONS OF THE NEWARK BASIN PAUL E. OLSEN Bingham Laboratories, Department of Biology, Yale University, New Haven, Connecticut Abstract Newark Supergroup deposits of the Newark Basin 1946), makes this deposit ideal for studying time-facies (New York, New Jersey and Pennsylvania) are divided relationships and evolutionary phenomena. These into nine formations called (from bottom up): Stockton recent discoveries have focused new interest on Newark Formation (maximum 1800 m); Lockatong Formation strata. (maximum 1150 m); Passaic Formation (maximum 6000 m); Orange Mountain Basalt (maximum 200 m); The Newark Basin (Fig. 1 and 2) is the largest of the Feltville Formation (maximum 600 m); Preakness exposed divisions of the Newark Supergroup, covering Basalt (maximum + 300 m); Towaco Formation (max- about 7770 km2 and stretching 220 km along its long imum 340 m); Hook Mountain Basalt (maximum 110 axis. The basin contains the thickest sedimentary se- m); and Boonton Formation (maximum + 500 m). Each quence of any exposed Newark Supergroup basin and formation is characterized by its own suite of rock correspondingly covers the greatest continuous amount - types, the differences being especially obvious in the of time. Thus, the Newark Basin occupies a central posi- number, thickness, and nature of their gray and black tion in the study of the Newark Supergroup as a whole. sedimentary cycles (or lack thereof). In well over a century of study the strata of Newark Fossils are abundant in the sedimentary formations of Basin have received a relatively large amount of atten- the Newark Basin and provide a means of correlating tion. By 1840, the basic map relations were worked out the sequence with other early Mesozoic areas.
    [Show full text]
  • Profile Final Draft of Nri.Pub
    Natural Resources County Profile—Natural Resources Physiography Given an area of only 429 square miles, Hunterdon Hunterdon County falls within two of five regions passing through New Jersey known as “physiographic provinces.” Each County’s landscape is tremen- province reflects distinct characteristics associated with its topog- dously diverse. This is as much raphy, soils, hydrology and vegetation (Map 1). a function of its intricate, inter- The Highlands connected system of natural re- The Highlands physiographic province, extending from Pennsyl- vania to Connecticut, crosses all or portions of 15 municipalities sources as it is human activities in northwestern Hunterdon County. It comprises one-third of the that occurred over time. Some- County’s land base. times these activities work in The hard igneous and metamorphic rocks of the Precambrian Era, unity with the natural environ- including gneiss and granite, are resistant to erosion. They form broad, flat-topped ridges and steep-sided valleys. The valleys ment whereas other times, they consist of softer carbonate rock and shales, which are less resis- cause significant, if not irre- tant to erosion. versible change. Maintaining a Rock outcroppings, typical of carbonate rock landscapes, coupled delicate balance between a with ridgetops and slopes, provide varied conditions to support a healthy diversity of plant and animal habitats. The broader fertile healthy economy and healthy en- valley of the Musconetcong River is an important grassland habi- vironment demands a basic un- tat and contains prime agricultural soils that are still farmed today. derstanding of Hunterdon Despite the development constraints posed by steep slopes, ridges, County’s unique ecological com- wetlands and geology, significant growth has occurred in the plexion.
    [Show full text]
  • Description of the Trenton Quadrangle
    DESCRIPTION OF THE TRENTON QUADRANGLE. By F. Bascom, N. H. Barton, H. B. Kummel, W. B. Clark, B. L. Miller, and B. D. Salisbury. INTRODUCTION. contemporaneous origins. Although topographically there is subsequent streams, on the other hand, show adjustment to the usually a more or less abrupt passage from a trenched upland constitution of the rock floor and by means of them the By F. BASCOM. to an area of level-topped mountain ridges, geologically there is heterogeneity of rock character and complexity of rock struc­ LOCATION AND AREA. no transition, the same geologic formations and structures ture are finding expression. The general trend of the high­ The Trenton quadrangle, described in this folio, lies between appearing in both Mountains and Plateau. lands, which is northeast and southwest in harmony with the 40° and 40° 30' north latitude and 74° 30' and 75° west longitude. On the east the Plateau is separated from the margin of the strike of the underlying rocks, does not accord with the main This is one-fourth of a square degree and is equivalent in this continental shelf by a belt of coastal province 250 miles in drainage lines of the Plateau, but with the courses of the sub­ latitude to approximately 911.94 square miles or about 34.50 width. The greater part of this is under water in the region sequent streams. The main streams of the Plateau, rising miles from north to south and 26.43 miles from east to west. discussed. The land portion, which is called the coastal plain, either in the Appalachian Mountains or on the inland border dips gently eastward under the sea; it increases greatly in width of the Piedmont district, pursue courses consequent upon-the 77 toward the south.
    [Show full text]