NATURAL FEATURES ANALYSIS
Introduction
The
natural features section of the Master Plan uses the environmental criteria of
topography, slopes, soils, and water resources to evaluate the Town's land area
and its potential for development.
Although natural features can often enhance a particular development
site, they just as often pose significant barriers to development. This can be seen by examining where existing
development has occurred. It is true
that transportation routes are an important factor in the location of
development, however, the location of roads and railroads are also determined
by the natural features of the land.
This
section will enable the Planning Board to identify areas of the Town that are
most suitable for development and evaluate the existing limitations of the land that would impede development. Environmental limitations may include steep
slopes, seasonally wet soils, wetlands, flood-plains, shallow bedrock, and
underground aquifers. This section will
also point out areas which deserve protection due to the environmental function
of the land, for example a specific wetland area that provides flood water storage
during times of heavy rain. In addition,
this section will point out specific areas which the Town may wish to conserve
for future community use due to their aesthetic or historic qualities. Not all open space needs to be steep slopes
or wetlands. Some may be prime lands set
aside for future school sites, parks, intensive farming methods or other
limited low intensity land uses that add value to the overall community.
Walpole
has many natural features which make the Town a very desirable place to
live. Outside of its typical New England
village center, the Town is still quite rural with many rolling hills, green
fields, and streams. Walpole is also in
close proximity to Keene and Brattleboro, Vermont, two regional economic
centers. Outside of the village center,
lots are often five acres or more in size.
As the value of land increases, there is greater motivation to subdivide
large parcels into smaller lots. Using this natural features section will
assist the community and its Planning Board in establishing where they want
growth to occur while they endeavor to preserve the natural environment
currently enjoyed by the residents.
I. Topography
Walpole's
eastern half has a rugged, mountainous terrain compared with the relatively
flat, clear land in the west along the Connecticut River. Steep slopes are a common feature of the
Town's eastern half; also, exposed bedrock can be seen in some places. The Town's western half does have some hills
with steep slopes, however, as one moves toward the Connecticut River the land
becomes flatter. The North Walpole area
is a mirror image of the Town, with steep slopes dominating the eastern half
and flat land throughout the western half.
Derry Hill is Walpole's highest point of elevation at approximately
1,500 feet.
There
are numerous streams which flow in an east to west direction, draining from the
mountainous eastern section to the Connecticut River. Based on the soil properties of the land,
there is an abundance of prime farm land along the banks of the Connecticut
River. However, much of this land is
vulnerable to flooding.
II. Slope
Slope
is a major consideration when examining the Town in respect to future
development. Slope refers to the
gradient or steepness of the land. The
slope of land is defined as the change in elevation (vertical distance) over
horizontal distance; the more abrupt the change in elevation, the steeper the
slope. Slope is measured and expressed
as a percentage that represents the relationship between elevation and
horizontal distance. Below is an example
of an 10% slope, which means that in 100 feet of horizontal distance, the grade
has risen 10 feet.
![]()
10 feet

![]()
100 feet
The
Walpole Slope Map was prepared by enlarging the Walpole portion of a US
Geological Survey topographic map (Bellows Falls quadrangle, prepared by the
USGS in 1957) to a scale of one inch equals 1,000 feet. The contours of the map were then evaluated
in terms of three slope categories: 0 - 8% slopes, 8 - 15% slopes, and over 15%
slopes. The amount of land falling
within these categories was then measured using a planimeter.
A. Development Capability
Land
in the 0-8% slope category is preferred for all types of development. Gradual slopes are most favorable for
building roads, and public water and sewer systems can be installed at the
least cost to the community. Also,
excavations for most structures can be done at a minimal cost and the erosion
associated with such work can be reduced easily on site. The exceptions to this would be wetlands and
floodplains because they occur primarily in the 0-5% slope range. An examination should be made as to the
environmental function of these wetland areas and what risks might be inherent
in their development before such lands are utilized for building sites.
As
slope increases to the 8-15% category, land is less suitable for intensive
development. Carefully placed
residential dwellings and some farm uses (orchards and field crops) are
appropriate for this terrain. As
development approaches a 15% gradient, it requires more careful consideration
for all types of development.
Once
a slope exceeds a 15% gradient, development should be closely monitored. These areas have benefits as conservation
areas for low intensity recreational uses and wildlife habitats. Also, their disturbance has the potential for
serious erosion problems. Forestry
practices on such slopes must be low impact, with proper erosion controls,
minimal basal area cutting (definitely no clear cutting), and skid roads
designed for steep slope harvesting.
When
developing steep terrain, the potential for environmental damage increases as
the degree of slope increases. Overly
steep slopes consisting of sands and gravels left after the excavation of an
area will quickly gully and erode.
Erosion control barriers should be in place at the time of excavation
and prompt reseeding and regrading should take place afterwards. Surface water run-off rates and erodability factors
increase as the slope steepens. This
will cause sedimentation of the lands downslope and clog stream channels and
rivers if no erosion controls are in place.
In Walpole where steep terrain and soils with low infiltration rates
combine together to produce high run-off rates, soil erosion could be a major
problem for future development in Walpole.
Slope
is the major limiting factor for development in Walpole. Approximately 44% of the Town is covered by
slopes of 15% or greater. This
translates into about 10,504 acres of land.
However, some of these steep areas have soil properties that are
considered high in terms of development potential. Many areas along the Town's numerous side
slopes contain deep soil deposits and are well drained. Despite having favorable soil properties,
these areas still have considerable erosion potential and need to be carefully
evaluated during the development review process.
There
are several large land areas located towards the west side of Walpole, along
the banks of the Connecticut River, which are relatively flat and have good
soil properties. However, many of these soils
are also considered "important farmland soils" according to the
Cheshire County Conservation District. These
farmland soils are quite suitable for development, however, they are more
suitable for farming. As Walpole
continues to grow, there will be increased pressure to develop these farmland
soils for residential, commercial, and/or industrial purposes.
The
substantial amount of steep slopes in Walpole makes the issue of hillside
development a critical one. Development
proposals located along the Town's numerous hillsides should be evaluated in
terms of potential soil erosion, septic system placement, water well placement,
roadway and driveway construction, and surface water run-off potential. Soil properties should be considered in
conjunction with slope gradients when evaluating a site's erosion potential.
III. Soils
Soil
information by type is illustrated on the Walpole Soils Map, which was prepared
by the Southwest Region Planning Commission in 1989, by assembling and matching
individual soil survey sheets within the boundaries of the Walpole Base
Map. Soils information for Walpole came
from the following sources:
* Soil
descriptions and mapping:
Soil
Survey of Cheshire County, New Hampshire, published by the US Department of
Agriculture, Natural Resources Conservation Service (formerly, and published
under the name of Soil Conservation
Service), June 1989.
* Soil
development capability:
Soil
Potential Ratings for Development; Cheshire County, NH, prepared by the
Cheshire County Conservation District in
August of 1984.
Despite
the Town's numerous steep sloping areas, approximately half of Walpole's land
area contains soil properties which are suitable for development. This is significant to note in light of the
fact that almost half of the Town's land area contains prohibitive slope
gradients. Many of these sloping areas
contain deep, well drained soil deposits with bedrock well below the surface;
thus the soil is rated high in terms of development potential. However, slope is still the limiting
factor. Although the soil properties are
suitable for development, the potential for erosion and increased surface water
run-off rates are inherent factors in the development of steep sloping
areas. Therefore, erosion control and
stormwater management plans are highly recommended for any development within
areas containing slope gradients of 15% or greater.
The
Town's largest patch of unsuitable soils begins along the west bank of the Cold
River and extends north, covering Mount Kilburn, Fall Mountain, and the
majority of North Walpole. The
restrictive features here are slope and bedrock. Along the banks of the Connecticut River
there are several large areas of productive farmland soils.
Many
of these farmland soils are quite suitable for other types of development. However, the
majority of farmland soils which directly abut the Connecticut River are
subject to flooding, thus making them unsuitable for development. Unsuitable soil properties can also be found
on Hitchcock Mountain, Derry Hill, Kingsbury Hill, and along portions of the
Cold River, Great Brook and Houghton Brook.
The restrictive features in the mountainous areas include slope and
bedrock, while the restrictive features along the riverbanks include wetlands
and floodplains.
A. Steep Soils
Walpole
contains several soil groups associated with steep slopes. These soils are found on the sides of hills,
along ridgetops and as rocky outcrops void of soil cover. They are described below.
Symbol Soil
Type Characteristics
26E Windsor loamy fine
sand, 15 to 50% slopes
60D Tunbridge-Berkshire stony fine sandy loams, 15 to 25% slopes
61D Tunbridge-Lyman rock outcrop, 15 to 25%
slopes
72D Berkshire fine sandy
loam, 15 to 25% slopes
161E Lyman-Tunbridge rock outcrop, 25 to 50%
slopes
230E Poocham very fine
sandy loam, 15 to 50% slopes
330D Bernardston silt loam, 15 to
25% slopes
331D Bernardston stony silt loam, 15
to 25% slopes
331E Bernardston stony silt loam, 25
to 50% slopes
360D Cardigan-Kearsarge silt loams, 15 to 25% slopes
361D Cardigan-Kearsarge rock outcrop, 15 to 25% slopes
362E Kearsarge-Cardigan rock outcrop, 25 to 50% slopes
366D Dutchess silt loam, 15
to 25% slopes
367D Dutchess stony silt
loam, 15 to 25% slopes
367E Dutchess stony silt
loam, 25 to 50% slopes
510E Hoosic gravelly fine sandy loam, 15 to 25% slopes
When
looking at the publication, Soil Potential Ratings for Development; Cheshire
County (prepared by the Cheshire County Conservation District in 1984), one
will notice that the soil symbols are followed by the letters B, C, D, or
E. These letters represent the
percentage of slope that is associated with a particular soil type. Below are the expressions of slope used in
this publication plus their corresponding development capability.
SLOPE DEVELOPMENT
CAPABILITY
0-5% higher
density
B 5-8% higher
density
C 8-15% less
intensive
D 15-25% limited
capability
E over 25% prohibitive
Preparing
the Walpole Slope Map involved combining several of the previously mentioned
slope categories. This is especially
true in the case of slope categories D & E (15-25% slopes and over 25%
slopes respectively). It is important
that the topographic and slope maps be used in conjunction with the soils map,
so the letter symbols on the soils map and the actual topographic lines can be
compared. An on-site analysis should
take place when the topographic maps and the associated soil symbols are in question.
B. Floodplain Soils
According
to the Cheshire County Soil Survey, Walpole does not contain a large amount of
floodplain soils. Only 944 acres (or
slightly less than 4% of the Town's total land mass) can be described as having
floodplain soil characteristics. These
areas are scattered throughout town, however, there are several large patches
of floodplain soils along the banks of Blanchard Brook, Great Brook, the Cold
River, and the Connecticut River.
Floodplain soils in Walpole include:
Symbol Soil
Type Characteristics
2 Suncook loamy fine
sand
4 Pootatuck fine sandy loam
5 Rippowam fine sandy loam
6 Saco mucky
silt loam
9 Winooski
silt loam
107 Rippowam-Saco sandy silt loam
108 Hadley silt loam
109 Limerick silt loam
401 Occum
fine sandy loam
The
Town of Walpole participates in the National Flood Insurance Program sponsored
by the Federal Emergency Management Agency (FEMA). The extent of Walpole's floodplains were
mapped by FEMA in 1981. The FEMA maps
were combined onto one map by Commission personnel in 1989, and the acres of
floodplains were measured using a planimeter.
The FEMA maps show a significantly larger amount of floodprone areas
than the County Soil Survey, although differences in methodology must be taken
into account, as well as an expected margin of error from using photocopied
maps. The FEMA maps show 1,440 acres of
100-year flood areas and 340 acres of 500-year flood areas. According to FEMA, 100-year flood areas have a 1 percent chance
of being flooded in any given year, and 500-year flood areas have a 0.2% chance
of being flooded in any given year.
C. Wetland Soils
The
Natural Resources Conservation Service describes wetland soils as those soils
which are poorly drained or very poorly drained (including muck and peat). Walpole has very few wetland soil areas. Only 1,226 acres (or 5.1% of the Town's total
land area) can be described as having wetland soil characteristics. This wetland acreage total can be broken down
into 955 acres of poorly drained soils and 271 acres of very poorly drained
soils.
The
Wetlands Map shows several small patches of wetland soils scattered throughout
the Town, with concentrations along the banks of Houghton Brook, Great Brook,
Blanchard Brook, and the Cold River.
Wetland soils in Walpole include floodplain soil symbols 5, 6, 107 and
109 which are described on the previous page.
Other wetland soils in Walpole include:
Symbol Soil
Type Characteristics
5 Rippowam fine sandy loam
6 Saco mucky
silt loam
107 Rippowam-Saco sandy silt loam
109 Limerick silt loam
197 Borohemists ponded
214 Naumburg loamy fine sand
295 Greenwood mucky peat
340B Stissing silt loam
341B Stissing
stony
silt loam
347B Lyme stony
fine sandy loam
395 Chocorua mucky peat
414 Moosilauke fine sandy loam
495 Ossipee mucky peat
533 Raynham silt loam
IV. Soil Development Potential
A
Soil Potential for Development Map was created, using the soils information
described above. According to this map,
Walpole has a number of suitable soil areas scattered throughout Town, with the
exception of the Fall Mountain/Mount Kilburn area in North Walpole. Many of the suitable soil areas occur on hill-sides
as deep deposits of quality soil.
Hillside development does create the potential for erosion, however,
this can be mitigated if proper erosion controls are in place. As mentioned previously, the banks of the Connecticut
River are covered by prime farmland soils.
However, many of these farmland soils (the ones outside of the
floodplain) are rated quite high in terms of development potential. Thus, although farming would be the ideal use
of these soils, they are also quite suitable for other types of
development. According to the Cheshire
County Conservation District, the soils in Walpole rated high in terms of
development potential include:
Symbol Soil
Type Characteristics
24A Agawam very fine sandy loam, 0-3%
slopes,important farmland soil
24B Agawam very fine sandy loam,
3-8% slopes, important farmland soil
24C Agawam very fine sandy loam, 8-15% slopes
26A Windsor loamy fine sand, 0-3% slopes
26B Windsor loamy fine sand, 3-8% slopes
26C Windsor loamy fine sand, 8-15% slopes
30A Unadilla
very fine sandy loam,0-3%
slopes, important farmland soil
30B Unadilla very fine sandy loam, 3-8% slopes,
important farmland soil
72D Berkshire fine sandy loam, 15-25% slopes
331C Bernardston stony silt loam, 8-5% slopes
336B Pittstown stony silt loam, 3-8% slopes
366C Dutchess silt loam, 8-15% slopes, important farmland soil
366D Dutchess silt loam, 15-25% slopes
367C Dutchess stony silt loam, 8-15% slopes
367D Dutchess stony silt loam, 15-25% slopes
Some
of the soils in this category are unique in terms of development
potential. Many are prime agricultural
soils that could also be utilized for residential, commercial, or industrial
development. Although there may be
specific costs associated with developing a certain soil in this category, the
soil limitations can be mitigated by designing structures and systems to suit
the site. (Although many of the above
soils occur on land that is not particularly level, the restriction posed by
excessive slope can be minimized through the use of erosion control techniques.
There
are three rating categories developed by the Natural Resource Conservation
Service that are combined to form an overall development potential rating:
Septic systems with absorption fields (40%)
Streets
and roads (30%)
Dwellings
with basements (30%)
Overall
rating 100%
The
Natural Resource Conservation Service considers the siting of on-site septic
systems to be the most important development consideration; thus this category
is given more weight in the rating system.
NRCS classifies soils into five categories (very low, low, medium, high,
and very high) based on development potential.
However, for the purposes of this report and the accompanying Soil
Potential for Development Map, the five categories have been combined to form
three categories (low, medium, and high).
Below is a more detailed description of each category.
Combined
Potential Potential Characteristics
HIGH Very
High Site conditions and the properties
of the soils are favorable for
development. Installation costs
for water and sewer systems are low and
maintenance costs for roads and
utilities would be low as well. Foundation costs are also low.
High Development costs are slightly
higher than for soils in the above class.
MEDIUM Medium Development costs at this level
become significant. Overcoming soil limitations here may include specially designed septic systems, terracing
to prevent soil erosion, or coping
with seasonally high water tables or bedrock close to the surface
when excavating or building.
LOW Low Development costs in these
soils are very high and there may be more soil
limitations to consider than with the
other
classes.
Very Low Severe soil limitations pose very high
to almost prohibitive development costs.
Development
limitations in Walpole are primarily due to steep slopes and thin soil
cover. Floodplains along the Connecticut
River are also a restriction, but to a lesser extent. Restrictive soil properties are scattered
throughout the Town, however, large concentrations of restrictive soils are
found in North Walpole, the Fall Mountain/Mount Kilburn area, the Chenney Hill
area, Drew Mountain, Derry Hill, Watkins Hill, and along the banks of the Cold
River, Great Brook, Houghton Brook, Blanchard Brook, and the Connecticut River.
Farmland
soils may exist in a formation that is too small, inaccessible, or too big for
today's small crop farms. Some of these
soils may be suitable for only specific crops.
The LESA (Agricultural Lands Evaluation and Site Assessment) manual
should be consulted when a choice needs to be made regarding the use of one
particular farmland over another, depending on whether the use is for farming
or development. The LESA system was
designed by the USDA, Soil Conservation Service. The LESA system is used by the Cheshire
County Conservation District when preparing environmental impact statements for
federal, state, or local agencies.
V. Water Resources
Walpole
has a land area of approximately 37.3 square miles, or 23,872 acres. This can be broken down into 36 square miles
(or 23,040 acres) of land and 1.3 square miles (or 832 acres) of surface water. Walpole does not have very many sizable
waterbodies, however, several significant watercourses flow through Town. In addition, there are several large
aquifers located along the banks of the
Connecticut River. A detailed
description of the Town's watersheds, waterbodies, watercourses, and aquifers
is presented below.
A. Watersheds
The
watershed is the principle focus in describing a surface water system. A watershed is the land area made up of a
series of connecting higher ridges that drain surface water to the lowest
point, which is where a stream or a river flows out of the watershed.
The
land area that makes up Walpole is comprised of portions of three major
watersheds: the Lower Connecticut River Watershed, the Cold River Watershed,
and the Ashuelot River Watershed. All
three watersheds drain into the
Connecticut River Basin. The
location and extent of these watersheds can be seen on the accompanying Surface
Water Map. The map also shows all perennial watercourses and waterbodies within
Town boundaries.
The
majority of Walpole's land area (80%) falls within the Lower Connecticut River
Watershed. The only areas of Town which
do not fall within this watershed are: the North Walpole and Drewsville area,
which falls within the Cold River Watershed; and a portion of land in the
Town's southeast corner near Carpenter Hill, which falls within the Ashuelot
River Watershed.
The
steep sloping area of Walpole's eastern half forms a drainage pattern where
surface water flows off the hills in a westerly direction, eventually flowing
into the Connecticut River. The only
exception to this is Merriam Brook, which is located in the Town's southeast
corner and flows in an easterly direction into the Ashuelot River.
B. Watercourses
All
told, there are 27 watercourses in Walpole, the most significant being the
Connecticut River and the Cold River.
The Cold River enters Walpole in two locations: the first spot is in
Drewsville where the river darts into town and then back out into Langdon; it
flows back into Walpole just north of the Whitcomb gravel operation, eventually
emptying into the Connecticut River.
This section of the Cold River is, in effect, the dividing line between
Walpole and North Walpole.
Other
significant watercourses include Houghton Brook in the southern portion of
Town; Great Brook, which enters Walpole just north of Barnett Hill and flows in
a southwesterly direction through Town; Mad Brook, which is in close proximity
to the village area; and Blanchard Brook, which begins in two places in the
Town's northern portion before it converges just south of the Walpole Valley
Road. All of the above mentioned
watercourses eventually empty into the Connecticut River.
C. Waterbodies
All
told, there are 31 waterbodies scattered throughout Town. Walpole does not have any significant
waterbodies, all are very small with the majority falling under five
acres. The largest waterbody is Mill Pond, approximately 10
acres in size. With the exception of the
man-made waterbodies near the airport, all of Walpole's ponds are connected to
the streams and rivers which form the Town's drainage pattern. Walpole's waterbodies are not large enough to
support the type of seasonal residential development associated with larger
waterbodies across the State, nor are they significantly utilized for
recreation.
D. Aquifers
Aquifers
are a concentration of subsurface water, occurring in saturated soils and
geological formations. Water is supplied
through precipitation and surface water discharge. Water infiltrates the ground through an
aerated zone where impurities are filtered out.
The water then moves to a saturated zone where the pore spaces between
soil particles are filled by the water, thus creating a saturated zone, called
aquifers. It is very important that the
earth's surface be able to transmit water so that a certain percentage can be
stored underground as "groundwater".
If excessive compaction or extensive covering of the earth's surface
occurs, the amount of water which can reach the saturated zone and become
groundwater is reduced.
Aquifers
(concentrations of groundwater) are found where saturated layers are permeable,
and the storage and transmission of water can take place. Aquifers having medium to high potential to
yield groundwater occur in Southwest New Hampshire as alluvial deposits of sand
and gravel (unconsolidated deposits) or in bedrock fractures (consolidated
deposits).
The
unconsolidated deposits, also called stratified drift deposits, contain sorted
layers of gravel, sand, silt and clay.
These materials have abundant pore space to store water, in fact, this pore space may amount to more than 30
percent of the deposit's total volume. Consequently, these stratified deposits
of sand and gravel have become good sources of medium to high volume
aquifers. This type of aquifer is found
primarily along valley bottoms.
The
consolidated deposits, or bedrock fractures, are a more productive water source
when covered by a layer of sand and gravel.
This allows recharge to occur directly from above. Bedrock fractures are usually adequate for
domestic wells. In contrast, a till
aquifer is usually low yielding and can have a short well life. This is due to a mixture of clay, silt,
gravel and boulders which tends to compact
due to the different soil particle sizes. The transmission and storage of water is
greatly decreased in this type of aquifer.
Stratified
drift aquifers can be either confined and unconfined. Confined aquifers have a layer of impermeable
material, such as clay, over them.
Unconfined aquifers are covered
by a layer of permeable material so that recharge occurs directly from
above. The water table (the top of the
saturated zone) fluctuates depending on the volume of water stored within this zone. The confined system is under pressure due to
the surface layer of clay and is resupplied where this layer is interrupted or
terminates.
The
US Geological Survey has recently completed aquifer delineation maps for the
entire state of New Hampshire. The
Walpole Aquifer Map was prepared from the USGS study, “Saturated Thickness,
Transmissivity and Materials of Stratified-Drift Aquifers in the Lower
Connecticut River Basin, Southwestern New Hampshire.” The map is essentially a surficial geology
map, showing the distribution of unconsolidated (stratified drift deposits)
geologic material on the land surface.
There do exist bedrock aquifers, but these were not mapped as part of
this study.
The
earlier information being replaced by this USGS study identified aquifers as
having high, medium or low potential yields; this study identifies the
boundaries of the sand and gravel (stratified drift) aquifers, and measures the
rate of transmissivity - that is, the speed with which water passes through the
materials - in increments of 1,000 feet squared per day; the map illustrates
areas of less than 1,000 feet squared per day, 1 - 2,000 feet, 2 - 3,000 feet,
and 3 - 4,000 feet, and over 4,000 feet squared per day. Transmissivity of less than 1,000 is
considered suitable for single family homes, but not for public or community
systems. The map also illustrates the
depth of the aquifer, which relates to the potential for recharge. Since recharge is a function of saturated
thickness and transmissivity, both factors need to be taken into account.
The
map indicates that the primary aquifer area in Walpole follows the Cold River
and the Connecticut River, being bounded in part by Blanchard Brook. There appear to be only two small areas with
a transmissivity of greater than 4,000 feet squared per day: (1) in
North Walpole between the railroad bed and the River; and (2) at the bend in
the Connecticut west of the intersection of Route 12 and Upper Walpole
Road. Both of these locations also
contain the only areas identified as having transmissivities of 2 - 3,000 feet
and 3 - 4,000 feet; these are quite small, however. The remainder of the town is underlain by
till or bedrock, for which, as mentioned above, transmissivity has not been
determined.
VI. Conservation and Preservation Techniques
A
conservation and preservation analysis is the culmination of the natural
features section of the Town's Master Plan.
By analyzing and evaluating the Town's existing physical features such
as topography (slopes), soil conditions, floodplains, and water resources, it
is possible to identify areas within Walpole that have excellent development
potential for residential and non-residential uses.
Conversely,
it is also possible to identify environmentally sensitive areas within Walpole
that should not be subject to intensive development pressure or activity. In fact, there are some areas that should be
protected from almost all types of development activity because of unique or
exceptional environmental considerations.
When such areas are identified, it is desirable to protect them from
intensive and/or extensive development activity through the application of
various conservation and preservation techniques and land use management
practices, such as the use of detailed performance standards and protective
buffers and setbacks.
One
important area of concern when looking at conservation and preservation has to
do with how to manage development within critical resource areas. For the Town of Walpole, critical resource
areas are primarily those that contain steep slopes, floodplains, and
shoreland. Of the three, steep slopes
are the Town's most significant development constraint. Under Walpole's current zoning arrangement,
it is becoming increasingly difficult to find land in the outlying areas of
Walpole that can accommodate a functioning septic system, a water well, and a
building all within the space of an acre.
When hilly areas of Town become developed, erosion problems and
excessive surface water run-off can become more frequent unless the Town
institutes protective measures. The
following pages set forth the kinds of goals and objectives suggested by the
Planning Board to address these two important areas, and further conservation
and preservation techniques and strategies.
A. Steep Slopes
The
discussion on slopes earlier in this chapter indicated that approximately 44%
of Walpole's land area consists of slopes with a 15% gradient or greater. In an effort to refine this information, the
Planning Board also examined slopes of greater than 25%, since it is at this
degree of steepness that the most severe problems are likely to occur with
development. This area is rather small
by comparison, and is situated in parts of Town that are, for the most part,
not accessible by any road. Therefore,
the Planning Board does not see the need for a steep slope overlay protection
district per se, but would rather continue to review any applicable proposals
based on existing regulations.
B. Floodplain Development
Walpole
intends to continue its participation in the National Flood Insurance Program
administered by the Federal Emergency
Management Agency. In the March
1990 Town Meeting, Walpole revised its floodplain development ordinance to
conform with all federal requirements.
For development occurring within the Town's floodplains, the Planning
Board and the Selectmen will continue to enforce the strict construction
standards outlined in the ordinance.
C. Shoreline Development
In
1991 the NH Legislature enacted the Comprehensive Shoreland Protection Act,
which affects all lands within 250 feet of certain public waters. The intent of the law, relative to this
master plan, is to: further the
maintenance of safe and healthful conditions; provide for the wise utilization
of water and related land resources; prevent and control water pollution;
conserve shoreline cover and points of access to inland waters; preserve the
state's lakes in their natural habitat; promote wildlife habitat, scenic
beauty, and scientific study; protect public use of waters, including
recreation; conserve natural beauty and open spaces; and anticipate and respond
to the impacts of development in shoreland areas.
D. Connecticut River Management and
Protection
In
1992 the NH Legislature designated the Connecticut River into the New Hampshire
Rivers Management and Protection Program.
Through the Connecticut River Joint Commissions, five subcommittees were
established along the River to ensure local leadership in implementing the Act;
the Town of Walpole was included in the Wantastiquet Area Subcommittee. Toward this end, the Joint Commissions and
these subcommittees developed a Corridor and Management Plan for the river in
May of 1997. The Plan contains many
recommendations for river management and protection, all of which are advisory,
as is the Joint Commissions. The Plan describes a number of significant
features of the river, identifies problems and potential challenges, and
proposes objectives to meet the overall goal of river protection. A copy of this Plan has been forwarded to the
Planning Board and Board of Selectmen in every riverfront town. The NH Legislature is working to authorize
each riverfront town to adopt a locally-designed program for protecting the
river and the shoreline. The Plan, as it
stands, may now be adopted by local planning boards as an adjunct to the master
plan, and may include methods of implementing any of the appropriate
recommendations.
E. Connecticut River Scenic Byway
Another
endeavor taking place along the River is the Tri-State Connecticut River Scenic
Byway Program, a joint effort of New Hampshire, Vermont and Massachusetts. The purpose of this program is to identify a
scenic corridor along the Connecticut River and then develop a Corridor
Management Plan that would be geared, to large extent, toward promoting tourism
in the Valley. While the goals of this
program are not exclusively environmentally driven, the value of a healthy
natural environment is tantamount to any successful effort to develop and
market a Scenic Byway identity. As of
this writing, the Management Plan is being drafted, and is scheduled to be
presented to the riverfront towns in the Spring of 1998. As with the Management Plan for the river,
any town that chose to do so could adopt the Plan and choose to implement any
of the strategies that will be offered relative to the promotion of tourism -
which will include strategies to protect the natural environment. This plan, when complete, will also be made
available to the Town Planning Board and Board of Selectmen.
F. North Cheshire Branch Hiking Trail
A
multi-use recreational trail has been developed along Walpole's portion of the
abandoned railroad right of way, which was once the North Cheshire Branch of
the B & M Railroad. This branch was
abandoned by B & M in 1972, and purchased by the New Hampshire Department
of Transportation. The DOT used federal
funds for the purchase of the right-of-way, for the purpose of preserving the
land for future transportation uses.
Since 1995, volunteer efforts have resulted in the construction of
bridges and upgrading the trailbed. The
trail is managed by the Trails Bureau of the the NH Department of Resources and
Economic Development, which has appointed the Friends of Pisgah as the regional
coordinator for planning and management.
G. Scenic Road System
The
establishment of a scenic road system would help preserve the rural character
of several of the Town's Class V roads.
As noted in the Transportation Section of this document, Walpole has
several Class V gravel roads that do not meet the minimum width standards
established by the New Hampshire Department of Transportation (NHDOT) for low
volume, lightly traveled roads.
Authorized by RSA 231: 157 & 158, towns in New Hampshire may vote to
designate any of their local roads as Scenic.
The effect of this designation is to require a public hearing before the
Planning Board before any repair, maintenance, reconstruction or paving work is
done within the right-of-way by either the Town itself or any public
utility. This designation does not
affect the rights of any landowner to do work on his/her own property. The law allows Planning Boards to adopt
regulations specific to Scenic Roads. In
Walpole, to date only one road - Farnum Road, has been designated as Scenic at Town
Meeting.
H. Protected Lands
The
accompanying Conservation and Preservation Map shows the location of several
tracts of protected land in Walpole. A description of these lands is presented
in the table on the following pages. The map also shows several tracts of land
which are recommended for protection.
Preserving these tracts from future development can be achieved through
a number of methods, including:
1. Fee simple purchase - which simply means acquiring
the property through negotiated purchase.
2. Purchase of development rights - under this approach, the owner
gets to keep and use his land for various permitted uses that are consistent or
compatible with conservation and preservation practices but he cannot develop
the land for more intensive development activities.
In
addition, other land acquisition programs can be pursued through non-profit
groups such as the Trust for New Hampshire Lands, the Society for the
Protection of New Hampshire Forests, the
New Hampshire Audubon Society, and the Monadnock Conservancy.
Conclusion
The Natural Features section
provides sufficient information for the Town to develop and maintain an
on-going conservation and preservation plan.
The information presented in this section can be used to:
1. Develop various environmental overlay zoning districts, which
can prevent or minimize development activity in environmentally sensitive
areas.
2. Help the Planning Board and developers make better and more
informed decisions relative to how land can be best used to accommodate various
development proposals and projects.
3. Assist the Conservation Commission and Planning Board in:
(1) monitoring development activity;
(2)
monitoring the environmental integrity of the Town's critical resource areas;
(3)
continuing to identify natural and man-made features that should be protected;
(4)
developing an inventory of potential lands that could be preserved through
various conservation and preservation techniques fostered and promoted by
non-profit agencies listed previously.
4. Explore the feasibility of adopting environmental overlay
districts to protect such natural features as wetlands and aquifers.
GOALS AND OBJECTIVES
General
Goal:
To protect and preserve the
Town’s critical resource areas in an effort to maintain a balance between the
Town’s existing and future development needs and its natural environment.
Specific
Objectives:
1. As part of the update of the Land Use Plan, all development
activity since 1986 within the floodplain areas will be examined.
2. The Planning Board will continue to rely on the submission of
contour and erosion control information in its review of development
applications.
3. The Planning Board will pursue the adoption of Driveway
Regulations, in order to ensure that the construction of all driveways in Town,
but in particular those on slopes of over 25%, will address issues of erosion
and sediment control.
4. The Planning Board recommends that, at the building permit
stage, when steep slopes are involved, the Conservation Commission should
review the plans to ensure that erosion and sediment control are adequately
addressed.
5. The Planning Board will pursue an amendment to the Subdivision
Regulations that will require the identification of a safe driveway access for
each newly-created lot.
6. The Planning Board will review all development applications
within the critical areas identified in this section for potential
environmental impacts, and recommend mitigation where appropriate.
7. Despite the absence of Scenic Road designations and
accompanying regulations, the Planning Board recommends that necessary safety
and widening and/or reconstruction projects on Town roads be accomplished in
such a manner that the rural character of these roads is not compromised.
General
Goal:
To enrich the lives of Town
residents by striving to improve the aesthetic quality and visual impact of the
man-made environment as well as preserving and enhancing the attractive visual
features of the natural environment.
Specific
Objectives:
1. Protect the scenic elements of the Town's natural environment
such as steep slopes, hilltops, waterbodies, streams and rivers, particularly
the areas adjacent to Walpole's portion of the Connecticut River and the Cold
River.
2. Encourage the underground placement of utilities when and
where practical; and when underground placement is not practical, utilize
design and landscaping techniques to blend such facilities with the natural
environment to minimize their obtrusiveness.
In the case of wireless communications facilities, all reasonable
efforts should be made to minimize the visual effect of towers and any
appurtenances.
3. Encourage the use of aesthetically pleasing landscaping
practices to enhance the visual quality of the man-made environment. In appropriate cases, the Planning Board may
request landscaping plans to be submitted as part of development applications.
4. Encourage aesthetics and attractive designs of signs in terms of number, type, size and
location.
PROTECTED LANDS WITHIN THE TOWN
OF WALPOLE
Approx. Tax
Map Special
I.D. # Description Acreage Location Features
1. Mason
Forest (Gift- 237 M7-L5 Forest
trails,highway
1951-Fanny
Mason). M7-L6 rest
areas, and
Owner:
Town of Walpole. wildlife
habitat.
2. Hooper Forest 130 M11-L3 Forest recreation
(Bequest-1926- and
wildlife,lean-to,
George
L. Hooper). camp
site, and
Owner:
Town of Walpole. ski
trails.
3. Water
Company Town Forest 134 M11-L2 Woodland
and
Owner: Town of Walpole wildlife
area.
4. Hooper
Farm Woodland 109
M8-L61 Woodland
around
(Bequest-1926-George
M8-L62 golf
course,
L.
Hooper). Owner: M8-L71 garden
lots, and
Town
of Walpole. beaver
pond.
5. Mill
Pond Nature Sanctuary 86 M10-L5 Nature
trails and
(Gift-1977,
R.N. Johnson; M12-L60 Wildlife
habitat.
Purchase-1977,
Lottie Kilburn;
Gift-1979-Hubbard
Farms;
Purchase-1989-Robert
Galloway).
Owner: Town of Walpole.
6. Reservoir Town Forest 54 M10-L32 Forest
area, fishing
Owner:
Town of Walpole and
wildlife.
7. Trombley Town Forest 24
M6-L26 High
elevation,
(Tax
sale-1947). splendid
view of
Owner:
Town of Walpole. countryside.
8. The Pinnacle Town 23 M9-L22 Rocky
peak with
Forest
(Tax sale). great
view, trail
Owner:
Town of Walpole. through
woods.
Approx. Tax
Map Special
I.D. # Description Acreage Location Features
9. Merriam
Town Forest (Gift- 12
M3-L48 Lovely
stream and
Memorial
to Merriam Family) managed
forest.
Owner:
Town of Walpole.
10. Knapp
Cranberry Meadow 10
M8-L71 Beaver
pond.
(Memorial
Gift-Louisa and
Fredrick
Knapp).
Owner:
Town of Walpole.
11. Academy
Ravine, Bellow- 12
M10-L47 Nature
trail,
Knapp
Trail (Gift of Bellows May
Alcott Falls.
Bellows
and Knapp families- Great
variety of
1928,
memory of Henry Bellows shrubs,
plants,
and
Fredrick Knapp; Gift- and
other
Mr.
and Mrs. Alfred Bertin vegetation.
and
Mr. and Mrs. Clair Rogers;
Gift-Mr.
and Mrs. C. Chickering).
Owner:
Town of Walpole.
12. Conservation easement 69
M7-L26 Agricultural,
forestry granted to Town by and
conservation use Beatrice Graves. only.
No commercial development.
13. Conservation easement 35
M4-L50-1 Agricultural, forestry, granted by Wright, conservation
uses Aldrich, and
Hudson. only. No commercial development.
14. "High Blue" area. Owner: 164 M6-L27 Open
fields and wood - Society for the Protection M6-L28 lands. Great views of
of
NH Forests. Green
Mt., Mt.
Monadnock and Connecticut Valley.
15. Jacobs/Faulkner lot. Conser- 49
M3-L17 Open
fields,
tion
easement granted to the beautiful
views.
Society
for the Protection of
NH
Forests.
Approx. Tax
Map Special
I.D. # Description Acreage Location Features
16. Dunshee Island (Great Island) 7 M7-L14 Nature
study area
Owner: NH Fish and Game
Department
17. River Front-Gift from 31 M10-L4
Frontage along the Hubbard Farms. Owner:
NH Connecticut
River. Fish
and Game Department.
Farmland
and wildlife area.
18. Conservation easement granted 8 M10-L4-1 Farmland
and
by
Hubbard Farms to the wildlife
area.
NH
Fish and Game Department.
19. Agricultural preservation 181.5 M4-L3-2 Agricultural
use only.
restriction
given to the 3.75 M4-L1-2 No Commercial
State
of NH by 8.0 M4-L1-3 development.
by
David A. Barrett 9.9 M4-L1-4
TOTAL ACREAGE OF PROTECTED LANDS
IN WALPOLE: 1,397.15 acres.
LANDS RECOMMENDED FOR PROTECTION
1. The Sheep Hill Area - Wildlife habitat and nature
trails.
2. Fay Falls - A natural falls area along Houghton Brook.
3. The Derry Hill Area - Wildlife habitat and nature
trails.
4. Walpole Town Well - This is the land area around the
Town's well located off of Watkins Hill Road, along Great Brook.
5. Great Brook Watershed Protection Corridor - This
includes land along either side of Great Brook, beginning near Ramsey Hill, and
ending at the Town's well located off of Watkins Hill.
6. The Eaton Hill Area - Wildlife habitat and nature
trails.
7. The Mad Brook Watershed Protection Corridor - This
includes land along either side of Mad Brook, beginning near the end of
Reservoir Road, and ending where the Brook meets the downtown area.
8. The Eaton Hills West Area - Wildlife habitat and nature
trails.
9. The Cheney Hill Area - Wildlife habitat and nature
area.
10. The Blanchard Brook Watershed Protection Corridor - This
includes land along either side of Blanchard Brook, beginning at the base of
Hitchcock Mountain, and ending at the Blanchard Brook Dam and Mill Pond
diversion canal. Special features to protect within this corridor include the
Blanchard Brook Dam and Blanchard's Falls.