Lebanon Township
Natural Resources Inventory 2004
Introduction
In March 2001, the Lebanon Township Environmental and Open Space
Commission (EOC) was reinstituted after several years absence. The nine member commission is responsible
for advising the Lebanon Township Committee and Planning Board on issues
relating to the environment and open space.
Based on legislation passed in 1968, and expanded in 1972, the goals of the Lebanon Township EOC are to advise governing bodies on a variety of environmental issues, including informing the Planning and Zoning Boards of Adjustment about environmental impacts of proposals for development and advocating planned open space preservation at the municipal level. Additionally, the EOC investigates environmental problems and proposes solutions, informs residents on environmental matters and ways to help protect the environment, interacts with neighboring commissions to tackle regional and state issues, and maintains a data base on the environmental resources of the municipality, which is known as the Natural Resources Inventory (NRI).
As a planning resource, an NRI is invaluable for township officials in that it is a central resource for environmental information that can impact decisions regarding
The NRI directly supports the State Planning Act
(NJSA 52:18A-196 et seq), which has as some of its primary goals the
conservation of natural resources, the protection of the quality of the environment
and the promotion of beneficial development.
Of primary importance to Lebanon Township is that in the State Plan, the
Highlands region--where Lebanon Township is located--has been recognized as the
first Special Resource Area in New Jersey, containing unique characteristics or
resources of statewide importance for regional planning efforts, making the
Lebanon Township NRI an essential planning document.
Lebanon
Township
Lebanon Township is located in the northwest corner
of Hunterdon County. Founded in 1731
and incorporated in 1798, the township in 2002 had a population of 6,056
according to estimates from the US Census and 5,816 according to the 2000
Census.
Land Usage
According to November 2002 data provided by the Hunterdon
County Division of GIS, the predominant property class in Lebanon Township is
agricultural (47%) representing 9,335 acres of the Townships 20,250 acre land
area. Residential accounts for 29% of
the total, public land 13% and vacant land 8%.
Commercial and industrial usage accounts for 1.3% and 0.2% of the
Township, respectively.
Agricultural uses account for approximately 19% of
the Townships total acreage, or 3,865 acres.
Masses of farmland occur in four general areas: along Forge Hill Road,
around the Borough of Califon, in the Mount Lebanon Road/Sharrer Road/Anthony
Road area, and along West Hill Road.
Comparing the land use by property tax to the land use/land cover,
almost 60% of the land classified as agricultural by tax class is actually
wooded.
The Township has seen an increase in total
agricultural use, from 8,735 acres in 1987 to 9,423 acres in 1997.
Areas reported as urban, or high-density residential
use account for approximately 17% of Township acreage. The highest concentrations in this category
may be found in the hamlets of Bunnvale, Lower Valley, New Hampton and
Woodglen. Other concentrations of
developed land occur along Route 31, East and West Hill Roads, and Sliker
Road. See the Lebanon Township 2002 Farmland
Preservation Plan Element, Lebanon Township 2001 Master Plan: Land Use Plan
Element, and the Lebanon Township 2001 Master Plan: Conservation Plan Element for more information.
Open Space
While Lebanon Township does not own a vast inventory
of recreation and open space lands, the Township contains a variety of
recreational opportunities within its borders.
The majority are State and County parks geared primarily towards passive
recreation activities. These facilities
include Voorhees State Park, the Ken Lockwood Gorge Wildlife Management Area,
the Point Mountain section of the Musconetcong River Reservation, the Columbia
Trail section of the South Branch Reservation and the Teetertown Nature
Preserve/Mountain Farm. These
facilities comprise 2,030 acres or 10.3% of the Townships total parcel acreage
and 90% of the recreation land available to Township residents.
In addition, Lebanon Township has engaged upon an
aggressive program of farmland preservation in order to build core areas of
preserved farmland and agricultural districts, preserving an environment that
will foster the continuation of agriculture for future generations. Farmlands considered for preservation
include traditional field crop and grazing land as well as non-traditional
agricultural activities including timber harvesting, orchards, and growth and
sale of nursery stock.
Historic sites
Founded in 1731, Lebanon Township has a number of
sites designated as historic. The
following sites have been designated historic by the Historians of Lebanon
Township
·
Forks of the Delaware
Raritan Indian Trail
·
New Hampton Village
·
Anthony Village
·
Woodglen Village
·
Teetertown Village
·
Changewater Village
·
Hoffmans Crossing
·
Old American Hotel
·
Vernoy Quarry
·
Sliker Airport
·
Magnetite Mine
·
Zions Evangelical
Lutheran Church
·
Mount Lebanon Methodist
Church
·
Mount Bethel Church
Ruin
·
Changewater Methodist
Church
·
New Hampton Sunday
School
·
Site of Octagonal
School
·
Bunnvale School
·
Dusenbery Mansion
·
General Daniel Morgans
boyhood home
·
Traprock Quarry
·
Weise Home
·
Ken Lockwood Gorge
Indian camp and work site
·
Fort Foss
·
Old Stone Farmhouse on
the Voorhees High School campus
For more information, please see:
·
Abandoned Iron Mines of
Hunterdon County, New Jersey. New
Jersey Department of Labor, Division of Workplace Standards, Office of Safety
Compliance, 1988.
·
Stone Arch Bridge
Inventory, Phase II, Hunterdon County, New Jersey. Hunterdon County Planning
Board and the Hunterdon County Board of Chosen Freeholders, 1998.
·
Lebanon Township
Historical Society (http://www.lebanontownship.net)
·
NJ DEP Historic
Preservation Office, New Jersey and National Register of Historic Places (http://www.nj.gov/dep/hpo/1identify/lists/hunterdon.pdf)
Land and
Water
Topography
Lebanon Township is at the foot of the New Jersey
Highlands physiographic province and represents the beginning of some of the
most varied terrain in New Jersey. The
Highlands are home to some of the most scenic areas in the State and represent
the most significant animal habitats and forest resources found anywhere in New
Jersey outside of the Pinelands area.
Most of the land in the Township is 400 above sea
level, with the exception of lands located directly adjacent to the
Musconetcong River and the South Branch of the Raritan River. The highest elevation in the Township is
located in the vicinity of Pleasant Grove Road and is above 1040.
There are a number of scenic ridgelines in the
Township. The area of Point Mountain, a
County Park, contains some of the most scenic land found in the County. From the peak of Point Mountain, the terrain
runs steeply to the Musconetcong River valley.
Both banks of the South Branch run steeply to the River, making for a
gorge that runs the entire length of the River through the Township.
The two river valleys, the southwestern corner of the
Township bordering Bethlehem Township, the Teetertown Nature Ravine, Rocky Run,
Route 513 areas, and the Turkey Top Road area, possess the majority of the
Townships steep slopes classified as greater than 15%, and comprise nearly 25%
of the Townships land. Slopes greater
than 25% comprise 7% of land area.
Geology
The bedrock of Lebanon Township can be divided into
two general groupings primarily based on age and rock type. Precambrian (older than 570 million years)
igneous and metamorphic rocks underlie approximately 90 percent of the
Township. Gneiss and granite underlie
much of this area. The bedrock in this
portion of the Township includes members of the Byram and Lake Hopatcong
Intrusive Suites, Losee Metamorphic Suite, metasedimentary rocks, diabase
intrusions, Chestnut Hill formation, and other rocks of uncertain origin. The Precambrian rocks have been extensively
deformed into a series of southwest to northeast trending folds.
The second type of bedrock is mapped beneath
approximately 10 percent of the Township along the northern boundary and in the
southeastern portion near the Borough of Califon. These rocks include the Ordovician-Cambrian (440-570 million
years ago) dolomites and limestones of the Leithsville, Allentown, Beekmantown
and Jacksonburg Formations. This group
also includes the shales of the Bushkill Member of the Ordovician Martinsburg
Formation and the quartzites of the Hardyston Formation.
For more information, please see:
·
The Precambrian Geology
of the central and northeastern parts of the New Jersey Highlands. Smith,
Bennett L. In Geology of Selected Areas in New Jersey and Eastern
Pennsylvania. Rutgers University Press, 1969.
·
The New Jersey
Geological Survey (http://www.state.nj.us/dep/njgs/)
Soils
Lebanon Township has just over 6,000 acres of prime
and statewide important soils, as categorized by the State Agricultural
Development Committee (SADC). This
represents 30% of the Townships total acreage.
Three soil associations are found throughout most of
Lebanon Township. Along the
northwestern boundary of Lebanon Township and the Musconetcong River, as well
as near the southeastern border of the Township the soils are comprised of the
Rowland-Birdsboro-Raritan association.
These soils are found in areas with gentle to nearly level slopes and
are well to poorly drained. They are
typically associated with flood plains and may be flooded during parts of the
year.
Near the borough of Califon in the Long Valley
portion of the Township are found Duffield-Washington association soils. These soils are found on gentle to
moderately steep slopes and are considered well drained. These types of soils are derived from
weathering of the underlying limestone and dolomite bedrock. Solution channels such as caverns, sinkholes
and cavities may be present in areas where the Duffield and/or Washington soils
are encountered.
Most of Lebanon Township is underlain by the soils of
the Parker-Edneyville-Califon association.
Soils of this association are found in areas with gentle to steep slopes
and are excessively to poorly drained.
Cobbles and gravel sized weathered residual rock fragments are often
found with these types of soils and in some cases, the gravel fragments
comprise more than 20 percent of the soils.
The percentage of rock fragments increases with increasing elevation. These soils are typically found from 200 to
1,000 above sea level. The Parker and
Edneyville soils form a thin layer (less than 6 feet) over the bedrock
surface. In several areas of the
Township, the bedrock surface outcrops.
In the Califon soils, which are poorly drained, the seasonal water table
is shallow (less than 3 feet). The Soil
Conservation Service indicates severe limitations for these three soils types
and they are considered by this agency inappropriate for septic systems.
A fourth soil association is found in the southern
corner of the Township near Spruce Run Reservoir. The Washington-Berks-Athol association comprise 30, 30 and 20
percent, respectively, of this association.
These well-drained soils are found in areas with gentle to moderately
steep slopes, and are derived from weathering of carbonate bedrock and may
overlie solution features such as sinkholes and/or caverns. The Berks soils are derived from weathering
of shale. For more information see:
·
Soil Survey of
Hunterdon County, New Jersey. US Department of Agriculture Soil Conservation
Service in cooperation with the NJ Agricultural Experiment Station at Rutgers,
1974.
·
Soil Survey of
Hunterdon County, New Jersey. Jablonski, C.F. US Department of Agriculture,
Soil Conservation Service, 1988.
·
Evaluation of Groundwater
Resources of Lebanon Township, Hunterdon County, New Jersey. Mulhall, Matthew
J. Prepared for Lebanon Township Planning Board, 2001.
Hydrology
Lebanon Township is divided into four hydrogeologic
zones with each zone underlain by one of two distinct aquifer systems. The name of each zone is based on the
underlying type of bedrock aquifer systems.
Most of the Township is underlain by the aquifer system comprised of Precambrian
igneous and metamorphic bedrock, known as the Precambrian Crystalline Rock
Zone. Precambrian rocks are considered
to be poor aquifers with low water yields (NJDEP, 1996). A limited area near the northwestern border
of the Township and the area beneath Long Valley in the southeastern portion of
the municipality are underlain by limestone and dolomite aquifer systems,
referenced as the Limestone/Dolomite Zone.
Limestone/dolomite aquifer systems are some of the most prolific in New
Jersey (NJDEP, 1996). For more
information, readers of this document are referred to:
·
Water for the 21st
Century: The vital resource. New Jersey Department of Environmental Protection
Planning, New Jersey Statewide Supply Plan, 1996.
·
Evaluation of
Groundwater Resources of Lebanon Township, Hunterdon County, New Jersey.
Mulhall, Matthew J. Prepared for Lebanon Township Planning Board, 2001.
Water and
Water Quality
The Musconetcong and Raritan River Watersheds divide
Lebanon Township. Twenty percent of
Lebanon Township is in the Upper Delaware Watershed Management area, while the
remaining 80% is in the North and South Branch Raritan Watershed Management
Area. North of this divide, surface
water, and most likely groundwater, flow towards the Musconetcong River. South of the divide, water flows towards the
South Branch of the Raritan River and tributaries.
According
to the Statewide Water Quality Management Program Plan, all surface waters in
Lebanon Township are classified as FW2.
The FW2 classification is divided into three categories: FW2-TP: trout
production, FW2-TM: trout maintenance, and FW2-NT: non-trout. For more information, readers of this
document are referred to:
·
Geology and Ground
Water Resources of Hunterdon County, NJ. Kasaback, Haig F. Special Report No.
24, Bureau of Geology and Topography, Division of Resource Development, Department
of Conservation and Economic Development, 1996.
·
Evaluation of
Groundwater Resources of Lebanon Township, Hunterdon County, New Jersey.
Mulhall, Matthew J. Prepared for Lebanon Township Planning Board, 2001.
Habitats
Lebanon Township contains environmentally sensitive
lands, comprised mainly of forested wetlands and mature deciduous. Geographically, most of the wetlands are
found in the northern half of the Township and are protected by surrounding
forested areas. These wetlands and
forested areas form a symbiotic relationship, which becomes part of an overall
critical habitat system covering 8% of the total area of the township. Overall, wetlands make up 8% of the total
area of the Township with barren land and water comprising 0.3% and 0.6% respectively.
Forests
Nearly 56% of the Township is covered by forest, much
of which represents high priority habitat for wildlife. The spine of the Township is made up of
large contiguous tracts of forest, which provide suitable habitat for a number
of animal species, including some that are threatened or critical. A number of these contiguous forested tracts
are County and State parkland, preserved in perpetuity.
The
wooded tracts of Lebanon Township represent most of the remaining large
contiguous forests in Hunterdon County.
Many of these forested areas are protected as part of State and County
park systems. Voorhees Park, the
Musconetcong River Reservation, Teetertown Ravine, Ken Lockwood Gorge and the
Columbia trail areas all contain significant contiguous forest resources that
are permanently preserved. Nearly 87%
of Lebanon Townships forested areas are deciduous forest, with the remainder
coniferous (2%), deciduous brush and shrub land (5%), former fields (4%), mixed
brush and shrub land (0.7%), mixed forest (3%) and plantations (1.3%).
Wetlands
Wetlands in Lebanon Township are found throughout the
township and can be categorized as:
·
Agricultural wetlands
(modified)
·
Artificial lakes
·
Coniferous wooded
wetlands
·
Deciduous scrub/shrub
wetlands
·
Deciduous wooded
wetlands
·
Disturbed wetlands
(modified)
·
Herbaceous wetlands
·
Managed wetlands
(modified)
·
Mixed forested wetlands
(deciduous dominant)
·
Natural lakes
·
Streams and canals
·
Wetlands right of way
(modified)
The
greatest cluster of wetlands in Lebanon Township occurs below the ridge lines
in linked systems and in clusters. The
vast majority of the wetlands feed into the stream network and are interspersed
with many of the forested areas found throughout the Township. Their primary composition is deciduous
wooded wetlands. For more information, readers
of this document are referred to:
·
Plant Communities of
New Jersey. Collins, B.R. and K.H.
Anderson. Rutgers University Press, 1994.
·
The Vegetation of
Voorhees State Park. McDonough, W.T and M.F. Buell. American Midland
Naturalist. 56:473-490, 1956.
·
The New Jersey
Highlands: Treasures at risk. Mitchell, A.E. New Jersey Conservation
Foundation, 1992.
·
New Jersey Landscape
Project for the Protection of Rare Species (http://www.nj.gov/dep/fgw/ensp/pdf/landbro.pdf).
·
Rare Species and
Natural Communities Presently Recorded in the New Jersey Natural Heritage
Database, Hunterdon County (http://www.nj.gov/dep/parksandforests/natural/heritage/textfiles/njhunt.txt)
Environmental concerns and controls
Concerns
Several
environmental concerns that must be taken into consideration when considering
development in Lebanon Township. The needs of the Township and its
current and future citizens must be considered in light of the potential
effects of
ü Pollution:
Pollution (including solid waste disposal, point and non-point pollution
of water sources, light and noise) affects residents, wildlife and downstream
users of the waters from Lebanon Township.
Pollutants degrade and destroy habitats for indigenous species as well
as affect the quality of life for residents.
ü Soil limitations for septic systems: Most of Lebanon
Township is underlain by the soils of the Parker-Edneyville-Califon
association. The Soil Conservation
Service indicates severe limitations for these soils types for septic
systems. Severe to slight limitations
are associated with the Washington-Berks-Athol soil associations, which are
also found in Lebanon Township. The
Washington soils may be limited for subsurface sewage disposal in areas of
solution channels. The Athol and Berks
soils are moderately to severely limited for subsurface sewage disposal because
of shallow bedrock and/or steep slopes.
ü Geology: The geological underpinning of Lebanon
Township is critical when considering development due to its role in septic
system suitability.
ü Threatened and endangered species: Several
areas in Lebanon Township have been identified as critical for the survival of
native flora and fauna (including more than 60 species classified as threatened
or endangered), the recharging of aquifers, biodegradation of environmental
contaminants, the prevention of flood damage, and the protection of drinking
water and air quality, as well as preservation of open space for outdoor
recreation.
ü Wetlands: Wetlands provide critical habitats for
endangered and threatened species, as well as being vital to the recharge of
aquifers, the prevention of flooding and the removal of pollutants from the
environment.
ü Steep slopes: Steep slopes provide scenic value but
are also sites where environmental degradation can occur quickly if not managed
properly.
ü Farm Preservation: With its rich history of farming,
a quality of life strongly associated with the presence of agriculture, and the
value to serve as corridors for wildlife, the preservation of farmlands in
Lebanon Township is a crucial consideration for their value to residents and
wildlife alike.
ü Water: Lebanon Township is the location of the
headwaters of several of the main water producing streams that serve wide areas
of New Jersey. Water quality is high in
Lebanon Township, with many streams rated as trout producing, the highest State
rating for water quality. Degradation
of water quality will affect local residents, wildlife and users of the water
that flows from the grounds beneath Lebanon Township. Once degraded, it is difficult to impossible to restore water to
its previously pristine state.
ü Each of these factors must be considered as part of
the planning of development and redevelopment in order to maintain the quality
of life and the environment of Lebanon Township.
Controls
As
part of its commitment to maintaining the environmental quality of the area,
Lebanon Township has developed and approved a series of ordinances which help
to preserve the environment. The State
as well has developed controls on planning and development which support
environmental preservation, including controls on septic system development and
critical species and habitats, which can be found on the website http://www.nj.gov/dep/fgw/lndscpe.htm. The New Jersey Department of Environmental Protection
website http://www.state.nj.us/dep/
also covers topics such as noise pollution, air quality, water quality,
hazardous waste management, threatened and endangered species, and historic
preservation.
Bibliography
The data in this NRI is derived from the documents
listed below. These documents can be
viewed at the Lebanon Township Municipal Building.
Lebanon Township 2001 Master Plan
Lebanon
Township 2002 Farmland Preservation Plan Element
Lebanon
Township 2001 Master Plan: Conservation Plan Element
Lebanon Township 2002 Open Space and Recreation Plan
Evaluation of Groundwater Resources of Lebanon
Township, Hunterdon County, New Jersey. Mulhall, Matthew J. Prepared for
Lebanon Township Planning Board, 2001.