Larson Design Group Choconut Assessment

for Choconut Creek Watershed Association

Funded by Pennsylvania Growing Greener Grant

Draft Choconut Creek Wetland Investigation

 

 

Introduction

 

Choconut Creek experiences high flow events that result in significant bank erosion and flooding.  At several points along the mainstem, the creek currently overflows its banks and flood waters travel in old overflow channel in the floodplain.  However, the floodplain has been altered by residential, agricultural, commercial, and road encroachment.  The members of the watershed association have identified the flooding issue as one of their primary concerns.    One possible solution to reducing the flood volumes is to create additional wetland areas in the floodplain.  There are numerous wetlands throughout the watershed, some of which currently offer some flood flow attenuation.  In addition to flood storage, wetlands enhance water quality and provide habitat for a wide variety of organisms.  The purpose of this investigation was to document the existing major wetland areas in the watershed and identify areas for potential wetland expansion.  Wetlands were identified with aerial photography and locations verified with fieldwork.  The wetland maps presented in this section, were developed based on aerial photography.  The wetland boundaries drawn on these maps do not represent a jurisdictional determination.  Rather, the boundaries indicate major wetland areas in the study area.  The mapping includes other medium size wetlands that may not be discussed in detail in this report.  There are numerous small spring seeps or other wetland pockets that were not sketched on the map.  The primary investigation area focused on the mainstem valley floor since this area offers the greatest potential for wetland expansion.  Most of the tributaries in the Pennsylvania portion of the watershed travel through steep, narrow, wooded valleys and do not have the potential for wetland development.

 

Potential wetland enhancement/creation sites have been identified as part of this field investigation.  The identified sites have been prioritized based on depth of excavation, available acreage, access, likelihood of successful flood attenuation.  Wetland areas identified with an “A” have the highest potential,  B” wetlands have moderate potential, and “C” wetlands may encounter the most difficulty in construction or are smaller areas.  However, all of the sites are viable replacement areas.

 

Prior to development of detailed replacement wetland designs several issues need to be addressed.  A detailed delineation of the existing jurisdictional wetlands must be completed to accurately identify the wetland boundary.  A detailed topographic survey must be completed to located the wetland boundary and establish accurate elevations for development of a grading plan.  Backhoe test pits should be excavated within the chosen replacement wetland area to determine depths of ground water for development of the wetland creation grading plan.

 

Existing Wetland Descriptions

 

General wetland protection notes:  All wetlands should be protected from disturbance to the greatest extend possible.  If landowners are willing, wetlands should be fenced out of pastures and not mowed to allow for development of woody plants.  Woody plants within the floodplain provide greater soil erosion protection, increased roughness coefficient, and improved stream shading.  Some of these benefits can also be realized from the development of riparian upland forest buffers. 

 

Riparian floodplain areas along the mainstem.  Main hydrology sources appear to be spring seeps, high groundwater, and overland flow during flood events.

 

1.  Lake Timberland drainage.  This tributary has a highly sinuous channel flowing through a narrow valley bottom.  It is surrounded by grassland slopes on the valley sides.  The wetland expands downstream into a narrow band of forested hemlock with some grazing. The wetland is comprised primarily of riparian scrub/shrub with emergent plant communities extending up the slopes along spring seep areas.  This wetland includes several wet hillside seeps that discharge into the main channel.  The area appears to have some pasture activity.  Typical dominant plant species include:  speckled alder with some willow, soft rush, sedges, reed canary grass.  Hydrology sources include drainage from the hillside (about 10-12 seeps) and gully drainage from a road culvert. This wetland is approximately 21.50 acres.  Recommended actions – remove wetlands out of grazing acreage to allow natural reestablishment of community.  Photos 1,2.  Expansion area B1 is associated with this system

 

2.  Near the St. Joseph’s Church at intersection of North Road and Route 267 and extends up the shallow valley for quite a distance.  This is a dense sedge community with one dominant bush species (winterberry?) scattered throughout.  There are hemlocks and pines on the fringe of the wetland.  The sedges extend across North Road for a short distance.  The area is partially grazed, although there is not much evidence of grazing in the wetland proper.  There is no discernable stream channel.  This wetland is approximately 3.39 acres.  Photo 3. 

 

3.  Doolittle’s property.  This wetland is located on the west side of valley bottom along the stream.  It is comprised primarily of riparian scrub/shrub with speckled alder.  The area appears to have some pasture activity.  Area C1 is active pasture. Typical dominant plant species include:  speckled alder, willow, soft rush, sedges, reed canary grass.  There are low chroma mineral soils.  The area receives hydrology from hillside seeps to the east (across the road/behind the house), discharge from the pond area, and an elevated water table within the wetland.  Expansion area B2 and C1 are associated with this system.  This wetland is approximately 16.87 acres. Photos 6,7.

 

4.  Near the trailer park.  The wetland is east/northeast of the trailer park on east side of valley along base of hill.  There is a hayfield between the wetland and the trailers.  There is a spring seep emerging from north side of access road and along base of hillside.  The southern half of the wetland is wetter, the northern half is dryer.  PEM system dominated by sedges, cattails, sensitive fern, sweetflags, and willow.  Northern half plant community is dominated by sedges and goldenrod.  A road travels from main road to stream and bisects the wetland.  There is probably a ford in stream and it continues to house on western hillside. There is no evidence of grazing in the area and the wetland is in good shape.  This wetland is approximately 6.06 acres.  Photo 8.

 

5.  Upstream of the school at the confluence of the Stanley Lake tributary and mainstem.  This is an expansive wetland extending across most of the valley bottom.  A long narrow finger of wetland supporting a community of sedges and soft rush extends southward into the middle of the hayfield.  There is a scrub/shrub area with speckled alder and spring seeps emerging in the hayfield south of main wet area.  There is a lot of beaver activity and extensive flood debris.  There was a beaver dam in this area prior to the last high water event.  In 1858 there was a dam in the area that supported a sawmill.  There is recent (within a year or two) excavation along the tributary near school with a large fill pile in the floodplain.  The typical dominant plant species include:  speckled alder, willow, soft rush, sedges, reed canary grass.  There are low chroma mineral soils.  Expansion area A2 is associated with this system.  This wetland is approximately 20.97 acres.  Photos 9, 10.

 

6.  Across from Rounds Propane Company.  This is a mosaic of spring seeps and hummocky topography, with emergent wetland species and old field communities throughout a floodplain meadow.  This wetland system spans the entire valley width.  It is comprised primarily of riparian emergent plants with some shrub/scrub in the drainage areas.  The typical dominant plant species include:  soft rush, sedges, reed canary grass, sensitive fern, and cattails, with speckled alder and willow in the drainages.  There are low chroma mineral soils.  This wetland receives hydrology from hillside seeps that ultimately discharge into the main channel.  Expansion areas A3 and B3 are associated with this system.  This wetland is approximately 22.54 acres in overall size with numerous small upland inclusions.  A detailed delineation of these upland inclusions may prove to be beneficial if wetland expansion work is to occur.  This may provide additional acreage suitable for wetland creation

 

7.  Located downstream of Kellum Road.  This wetland is comprised primarily of riparian scrub/shrub with some areas of emergent plants.  The wetland extends into stand of red pine.  There is a small pocket of larch and spruce on the north side of the red pines.  Typical dominant plant species include:  speckled alder, willow, soft rush, sedges, reed canary grass.  There are low chroma mineral soils.  This wetland includes several seeps that surface within the valley floor and discharge into the main channel.  No expansion areas are currently proposed with this wetland system, as too much excavation is required.  This wetland is approximately 5.36 acres.  Photo 15 looking south.

 

8.  Located in large meadow on the State Line.  It is comprised of riparian emergent wetland species dominated by soft rush, sedges, and reed canary grass.  The area contains low chroma mineral soils.  This wetland includes a hillside seep as well as several seeps within the valley floor that discharge into the main channel.  Expansion areas B4 and C3 are associated with this system.  This wetland is approximately 7.88 acres.  Photo 16 looking northwest.

 

Wetland Expansion Areas

 

A Priorities

 

Top priority areas because:

1. They are currently considered upland areas

2.  They are adjacent to existing wetlands

3.  They are positioned within the floodplain and/or there is evidence of recent flood debris

4.  There is enough land to construct several acres of wetlands

 

Drawbacks

1.  All areas appear to be active hayfields, PC?

2.  Excavated material will need to be hauled off site

3.  Landowner interest is unknown

 

A1 Flaharty site.  This is a large hay field with the main channel along the eastern and southern side.  There is a small tributary that has been ditched on the west side of the field along the base of road bank. There is a seep in the north central section of the field.  There is fairly uniform topography throughout the area.  Photos 4,5. 

 

Expansion issues:

1.  This site is at the confluence of the two main tributaries in the upper Choconut Creek watershed.  This would allow flood waters to be detained in the upper watershed.

2.  It would require shallow excavation of the hayfield between the two channels, which could incorporate the mid-field seep.  There is good access for construction equipment.  Consider constructing a high flow inlet downstream of the barn and discharge to the creek by the bridge.

 

A2, Fields upstream of the elementary school.  This area is a hayfield with a PEM wetland finger bisecting the field, expansion areas could be located around the existing wetland finger.  The soil profile was observed along the cut bank of the stream.

 

Expansion issues:

1.  This area can incorporated flood flow

2.  Shallow excavation, 2-3 feet should expose low chroma soils and high groundwater.

3.  Could incorporate an upstream overflow channel.

4.  Could remove low dike along tributary so the water has access to the floodplain at the school baseball field.

5.  Access may be an issue

 

 

A3, the north end of study area, adjacent to Wetland #6.  This site is positioned between the wetland and Choconut Creek.  The site consists of a mowed hayfield.  There is a flood overflow channel with recent debris on the western edge of the hayfield which enters the scrub/shrub wetland finger.  Photo 13.

 

Expansion issues:

1.  Access to remove excavated any material  will likely require wetland crossings. 

2.  Approx. 2 to 3 ft of excavation.

3.  Could potentially yield several acres of wetlands as an expansion of the existing large wetland system already present. 

 

 

B Priority

Criteria

1.  Smaller acreage than the “A” sites

2. Will require deeper excavation

3.  There is less evidence of recent flood debris

 

B1, Lake Timberline drainage.  This is an active horse pasture and only about an acre in size.  It is adjacent to scrub/shrub wetlands.

 

B2, Doolittle property.  This is an active hayfield on the eastern side of the valley bottom.  There is a scrub/shrub wetland on the northwest side and an emergent community along the ditch on the east side of area.  There is no evidence of recent flood debris and the area may require deeper excavation.  However there is good road access.

 

B3,  across from Rounds Propane.  Part of area near Route 267 is staked out for a lot.  This expansion area would be immediately north of Wetland #6.  There is a tributary entering from the east just downstream of this site.  The tributary appears to have high volume during flood events as the mouth is wide and scoured.  There is a small elevated floodplain along eastern bank of the mainstem with willows and red maple.  It has evidence of flood debris.  This wetland creation may not intercept mainstem floodplain flows.  However, sidehill seeps near the propane company can be intercepted and attenuated.  The northern end of this site could be designed to intercept flow from both the tributary and mainstem.  An elevated wetland bench could be created downstream of the tributary on the eastern side of the channel.  It is also a possibility to expand further east into the hayfield. This section of mainstem channel near Kellum Road is riprapped.  There is good access from Route 267 and Kellum Road.  Photos 12 and 14.

 

B4,  near the state line.  This site is at the north end of the project area.  It is south and west of a new pond built behind the tall wood sided house.  This replacement area is part of a large open field associated with wetland #8 and there is recent flood debris in the field.  This site is positioned close to Route 267.  Access for fill removal is good.  It may require deeper excavation than other expansion areas.  There may be a stability issue as there is already evidence of flood waters flowing in this area.  There is concern that stream channel may relocated into the newly created wetland if excavation is too deep and occurs too close to the existing channel.  Photos 17 and 18.

 

 

C Priority

 

Criteria

1.  Deeper excavation required

2.  Even smaller acreage

3.  Access issues

 

C1,  across from Doolittle’s.  This site is adjacent to the streamside wetlands on western edge of field.  It is an active pasture area with a newly constructed fence.  The existing wetland forms a semi-circle on northern end of area.  There are concerns about stream stability and stream channel relocating into an excavation area.  However this area would be an obvious expansion of the PSS and it had lots of recent flood debris.

 

C2,  Large hayfield downstream of school.  There is a small section of dike along the field on downstream side of bridge.  There is excellent access at this site.  There is an old overflow channel within field but no recent debris.  This area is higher than the other sites and would require deeper excavation. The western edge of site along corn field is higher in elevation.  The expansion could be concentrated along the old channel (not as much excavation needed).   There is a newer upslope diversion ditch west of the cornfield that has cut off upslope runoff to floodplain.   The streambanks are 2 to 3 ft. high at the lower end of the field, providing access for flood flow into the potential wetland.  Photo 11.

 

C3,  near the state line.  This area in at the north end of study area, behind the tall wood-sided house.  The site is part of a large mowed field, associated with wetland system #8 and near expansion area B4.  This expansion area is at the western end of the field near creek.  The concern in this area is the stability of stream channel and the possible relocation into newly excavated wetland.  Photo 17.

 

Headwater ponds – There are several small seeps noted higher in the watershed.  Consider “gully plugs” to create wet bottom ponds with large storage capacity to attenuate floodwaters.  Discuss in land use section.

 

 

 

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