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| Board/Commission | Conservation Commission |
|---|---|
| Meeting Date | March 12, 2026 |
| Pages | 313 |
| File Size | 79.3 MB |
| OCR Status | Searchable (OCR processed) |
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February 17, 2026 Waterford Conservation Commission c/o Maureen FitzGerald 15 Rope Ferry Road Waterford, CT 06385 Re.: Mamacoke Brook Outfall Channel Stabilization & Restoration Dear Ms. FitzGerald: Connecticut College received grant funding to stabilize and restore Mamacoke Brook, a coastal lowland stream located on Connecticut College Arboretum property between Mohegan Avenue (Route 32) and the Thames River, north of Benham Avenue. The principal investigator at Connecticut College is Ms. Maria Rosa, with technical support from Dr. Doug Thompson, Connecticut College and Ms. Maggie Redfern, the Director of Connecticut College Arboretum. For the design team, GreenVest, LLC is the College’s implementation partner for the broader Mamacoke Island Aquatic Habitat Resilience (MIAHR) initiative and Biohabitats is the project ecological and engineering lead The project site, located at 435 Mohegan Avenue Parkway, is 54.10 wooded acres and contains approximately 0.82 acres of inland wetlands and watercourses and 2.25 acres of tidal wetlands. The proposed project intends to restore 0.27 acres of wetland and watercourse and enhance 0.47 acres of wetlands and watercourse. A detailed assessment of the project site and Mamacoke Brook is discussed in the attached design report. This includes assessments of watershed characteristics, geology, soil, wetlands and watercourses, hydrology, vegetation and ecological communities, listed species, and cultural resources. These existing condition are accounted for in the design approach discussed in the report as well as depicted in the design plans. Below is a summary of design report and plans, specifically the project need, objectives and approach. Mamacoke Brook currently exhibits substantial instability, including bank erosion and channel incision, producing excessive sediment that is transported downstream into Mamacoke Cove and ultimately the Thames River. Primary drivers include concentrated stormwater outfalls, a steep flow path, and reduced riparian vegetation in portions of the corridor. To reduce erosion and improve hydrologic and ecosystem function, the Mamacoke Brook restoration projected intends to: February 17, 2026 Re.: Mamacoke Brook Outfall Channel Stabilization & Restoration Page 2 of 5 1. Improve geomorphic function to promote long-term bed and bank stability 2. Reduce sediment transport downstream 3. Attenuate stormwater flows from concentrated sources by increasing infiltration/groundwater recharge where feasible, and reduce nonpoint source pollutants (e.g., roadway contaminants and fertilizers) 4. Enhance ecological functions and stream habitat quality 5. Maximize reuse of onsite native rock and wood in restoration features 6. Control invasive species and improve riparian vegetation conditions through treatment and native plantings The design prioritizes long-term stability, floodplain reconnection, and water quality improvement while accommodating constraints such as steep terrain, limited construction access in forested reaches, and avoidance of significant impacts on Connecticut Department of Transportation (CTDOT) right-of-way. The project is divided into three segments based on field conditions and the related the design approach. 1. Upstream Restoration Reach - Although a reinforced plunge pool and outfall energy dissipation could reduce erosive power, this approach is not feasible under current constraints (e.g., pipe elevations, access limitations, and CTDOT right-of-way impacts). Instead, restoration in the upstream reach focuses on limited, low-impact measures to increase sediment trapping and habitat complexity. This approach uses wood augmentation, including Post-Assisted Log Structures (PALS) where feasible and/or strategic use of existing fallen trees. This is expected to provide modest functional uplift given the high-gradient environment and limited upstream wood recruitment potential (culvert constraints). 2. Middle Restoration Reach - The middle reach is identified as the most actively enlarging and degrading portion of the system. The proposed design will restore stability in a steep intermittent channel (~8–10% slope) using a series of cascade grade control structures spaced roughly every 70–100 feet, over a total length of approximately 560 feet to the more stable downstream reach. Key elements of the proposed design include: • Cascade structures that provide ~3–4 feet of vertical drop over short distances using large subangular boulders sized for stability during the 100- year storm, with plunge pools for energy dissipation. February 17, 2026 Re.: Mamacoke Brook Outfall Channel Stabilization & Restoration Page 3 of 5 • Between cascades, the restored channel bed is set higher (within ~1–2 feet of top-of-bank) and designed at ~5% slope to support riffle/pool formation and wood retention. • Two complementary restoration techniques are incorporated to encourage geomorphic/habitat diversity and support adaptive learning: o Regenerative Stormwater Conveyance (RSC) riffle/pool step-pool approach, with riffles sized to convey approximately the 5-year storm (10 ft wide by 1 ft deep), plus shallow pools enhanced with woody material for roughness and habitat. o Dynamic boulder cluster / woody streambed approach to partially fill incised sections and promote a roughened bed surface that may evolve toward multi-threaded flow patterns (with performance standards acknowledging material sorting and wood decay over time). • Because there are known sensitive archaeological resources within the project area, specific steps have been taken to avoid or limit ground disturbance that is otherwise not necessary or associated with the restoration of the stream channel through this reach. 3. Downstream Restoration Reach - Downstream, where the stream slope softens, the valley widens, and stability is greater, a Stage 0, full-valley restoration concept is proposed to maximize floodplain reconnection, wetland function, and water quality benefits. In this reach, design intent is to restore the wetland/valley complex with multiple anabranching flow paths, high habitat diversity, and enhanced sediment/nutrient retention across the floodplain. Because this downstream reach includes dense stands of Phragmites australis, an integrated management approach (i.e., timed chemical treatment combined with biomass removal) will be coordinated with the Arboretum’s policies and long-term stewardship capacity. Additionally, because there are known sensitive archaeological resources within the project area, specific steps have been taken to avoid or limit ground disturbance that is otherwise not necessary or associated with the enhancement through this reach. When implemented as designed, the project is expected to: • Reduce active erosion and sediment delivery to the salt pond and Thames River through grade control, raised bed profiles, and floodplain reconnection February 17, 2026 Re.: Mamacoke Brook Outfall Channel Stabilization & Restoration Page 4 of 5 • Improve stormwater attenuation, infiltration opportunities, and pollutant processing by re-establishing floodplain and wetland function—especially within the Stage 0 restoration area • Increase habitat complexity and ecological function through wood structures, dynamic bed features, invasive species management, and native plant community restoration • Avoid and minimize impacts, to the greatest extent practicable, to trees along the restoration reach • Protect known and potential areas of archaeological resources • Preserve and avoid potential areas of state-listed species. • Provide a high-value, long-term teaching and research opportunities for Connecticut College students, staff and partners While the proposed project will result in 0.74 acres of direct wetland impacts, we believe that this restoration activity is not a significant impact. • Deposition and/or removal of material will have substantial long-term benefits to the watercourse and overwhelm any potential negative short-term effects related to construction. Construction will include an erosion and sediment control plan consistent with CTDEEP guidelines that will minimize impacts to downstream wetlands and watercourses. • The natural channel has been greatly impacted by erosion associated with increased runoff from Mohegan Avenue Parkway. Natural dynamics of the watercourse will be reintroduced through the construction of a natural channel to the extent practicable based on current climatic and land use conditions. • The project will not diminish but rather enhance the watercourses’ ability to: support aquatic life and wildlife; reduce flooding in established areas by reconnecting existing floodplains; promote improved water quality; and enhance recreational opportunities and safety at the site. • Water quality will be further improved by reestablishing a riparian buffer within the upland review area and improving groundwater connections. Reducing erosion also decreases water turbidity and establishing a canopy will address increased water temperature relative to solar energy input. • The project will be conducted during a period of low-flow when the Mamacoke Brook is typically dry. Turbidity, siltation, and sedimentation will be addressed during construction by using established erosion and sediment control techniques. Over the long-term, the proposed restoration will reduce turbidity, siltation, and sedimentation. February 17, 2026 Re.: Mamacoke Brook Outfall Channel Stabilization & Restoration Page 5 of 5 • The proposed restoration includes educational and scientific benefits by allowing students and faculty of Connecticut College to support the assessment and design process, observe construction, and complete monitoring to document project outcomes along with adaptive management if needed. A detailed assessment of the project site and Mamacoke Brook and the resultant design are discussed in the attached design report and depicted in the attached design plans. It is anticipated that the project will begin during the low-flow period (summer) and take approximately 3 months to complete. Plantings will be installed immediately following construction, but no later than October 31. Should you have any questions about the proposed project, please do not hesitate to contact me directly at 860.968.2738 or jwilson@biohabitats.com. Sincerely, Biohabitats, Inc. Joshua H. Wilson, PWS Sr. Ecologist Enclosures 2/12/26 Conservation Commission Permit Application Attachment Properties Adjacent to: Owner Parcel ID# Property Address Mailing Address 435 Mohegan Ave Pkwy BLAHUN, GEORGE JR BLAHUN, GEORGE JR & DIANE CLEIN, ROBERT H CONNECTICUT COLLEGE CONNECTICUT COLLEGE PINKOWITZ, BARRY M & SHELBURN, JEANNE L SHELBURN, JEANNE LEE TREDWAY, LORAINE & KAPLAN, MICHAEL W 393500 393900 437500 393800 436800 24400 436500 24800 7 MAMACOKE ROAD 5 MAMACOKE ROAD 449 MOHEGAN AVE PKWY 14 MAMACOKE ROAD 435 MOHEGAN AVE PKWY 30 BENHAM AVENUE 417 MOHEGAN AVE PKWY 34 BENHAM AVENUE 7 MAMACOKE ROAD 449 MOHEGAN AVE PKWY 30 BENHAM AVENUE 34 BENHAM AVENUE 451 MOHEGAN AVENUE PARKWAY 270 MOHEGAN AVE 270 MOHEGAN AVE 30 BENHAM AVENUE QUAKER HILL, CT 06374 QUAKER HILL, CT 06374 QUAKER HILL, CT 06374 QUAKER HILL, CT 06374 QUAKER HILL, CT 06374 QUAKER HILL, CT 06374 NEW LONDON, CT 06320 NEW LONDON, CT 06320 QUAKER HILL, CT 06374 QUAKER HILL, CT 06374 QUAKER HILL, CT 06374 QUAKER HILL, CT 06374 QUAKER HILL, CT 06374 QUAKER HILL, CT 06374 QUAKER HILL, CT 06374 QUAKER HILL, CT 06374 TOWN OF WATERFORD Instruction Guide for Inland Wetland / Watercourse Permit Application Fees: All Application fees include $60.00 for the State of Connecticut. Residential Improvements, Additions & New Structures: $110.00 Residential Subdivision, 3 or more Lots: $160.00 Commercial/Industrial Development: $160.00 Major or Significant Impact Activity: $360.00 Public Hearing Fee: $400.00 Permit Extension/Modification: $ 110.00 Permitted Use: No Fee Unregulated Activity: No Fee All applications shall include a completed original application and 14 copies to be submitted to the Conservation Commission office. The wetlands application checklist is for your convenience, it is not necessary to submit this document with your application. Incomplete applications will not be completed by staff, they will be returned. 1. Applicant Include the full name, address, zip code and telephone number of the applicant(s). 2. Owner Include the name(s) of the owner(s) of record as it appears on the land records (deed) of the Town of Waterford. The owners’ complete address, zip code and telephone number are required. 3. Agent Include the full name, address, zip code, and telephone number of the agent. An agent prepares the application for submission or will represent the owner / applicant at a meeting. 4. Address Provide street name and number of subject property. 5. List of Abutters Complete the attached form with the name, address, and assessor’s map and parcel numbers for all adjacent properties. 6. Activity to Be Reviewed Briefly describe the type or nature of permit requested. Attach additional sheet(s) if necessary. 7. Description of Proposed Activity Describe in detail all proposed work. Scope of all work shall be included. Attach additional sheet(s) if necessary. 8. Purpose of Activity Describe in detail the purpose of the permit request. Attach additional sheet(s) if necessary. 9a. Acreage of Property Provide the size of the subject parcel and the area of all wetlands on site. [Note: one acre = 43,560 square feet.] 9b. Area of Wetlands and Watercourses Provide the area of all wetlands on the site in acres. [Note: one acre = 43,560 square feet.] 10. Wetlands Altered Indicate the area of the wetlands to be altered by proposed activity. 11. Wetland Mitigation Describe measures incorporated in the plan to mitigate the wetland impacts associated with the proposed activity, including restoration, enhancement or creation of wetland area. 12. Regulations Indicate you have reviewed the “Waterford Inland Wetlands and Watercourses Regulations” and have complied with the application requirements. WETLAND DELINEATION REPORT Connecticut College Mamacoke Brook Outfall Channel Stabilization and Restoration Waterford, Connecticut February 6, 2026 Project #25201.01 ii C:\Users\JWilson\AppData\Local\Temp\Bluebeam Software\11576599.doc WETLAND DELIENATION REPORT CONNECTICUT COLLEGE MAMACOKE BROOK OUTFALL CHANNEL STABILIZATION AND RESTORATION, WATERFORD, CT TABLE OF CONTENTS SECTION PAGE 1.0 INTRODUCTION ....................................................................................................................... 4 1.1 Background ............................................................................................................... 4 1.2 Objectives ................................................................................................................... 5 2.0 WETLAND DELINEATION ....................................................................................................... 5 2.1 Federal Jurisdictional Wetlands .................................................................... 5 2.1.1 Regulatory Definition .............................................................................. 5 2.1.2 Methodology ............................................................................................... 5 2.1.2.1 Hydrophytic Vegetation ...................................................... 6 2.1.2.2 Hydric Soils .................................................................................. 7 2.1.2.3 Wetland Hydrology ................................................................. 7 2.1.3 Determination and Identification of Federal Wetlands ..... 8 2.2 Connecticut Jurisdictional Wetlands ......................................................... 8 2.3 Field Investigation .................................................................................................. 9 3.0 RESULTS OF THE WETLAND DELINEATION .................................................................. 10 3.1 US Fish and Wildlife Service National Wetland Inventory ............. 10 3.2 Natural Resource Conservation Service Soil Map ............................ 10 3.3 Field Delineated Wetland Units .................................................................... 11 3.3.1 Wetland Unit A .......................................................................................... 12 3.3.2 Watercourse A .......................................................................................... 12 4.0 CONCLUSIONS ...................................................................................................................... 13 5.0 REFERENCES ............................................................................................................................ 13 iii C:\Users\JWilson\AppData\Local\Temp\Bluebeam Software\11576599.doc APPENDICES END OF REPORT A Existing Conditions Mapping B Natural Resources Conservation Service (NRCS) Soils Report C Wetland Delineation Forms Certification of Wetland Delineation State jurisdictional wetlands and watercourses were delineated in accordance with the State of Connecticut Inland Wetlands and Watercourses Act (CGS 22a-36 to 22a-45 inclusive). Federal jurisdictional wetlands were delineated in accordance with U.S. Army Corps of Engineers Wetlands Delineation Manual (Technical Report Y-87-1) and Regional Supplement to the Corps of Engineers Wetland Delineation Manual: Northcentral and Northeast Region (ERDC/EL TR-12-1) pursuant to Section 404 of the Federal Clean Water Act (33 U.S.C. 1344). To the best of my knowledge, the delineations depicted hereon are true and accurate. The wetland and watercourses were delineated in accordance with applicable local, state and federal statutes, regulations and guidance. Classification and mapping of soils on site were conducted in a manner consistent with the U.S. Department of Agriculture Soil Survey Manual (Soil Science Division Staff, 2017). This delineation does not constitute an official wetland boundary until such time as it is accepted and approved by local, state or federal regulatory agencies. Joshua H. Wilson, PWS #1992 Date Registered Soil Scientist 2/6/26 C:\Users\JWilson\AppData\Local\Temp\Bluebeam Software\11576599.doc 1.0 INTRODUCTION The Connecticut College Mamacoke Brook Outfall Channel Stabilization and Restoration (the Site) is along an intermittent channel extending from the culvert outfall east of CT Route 32, located at approximately 600 feet north of the intersection with Benham Avenue, to a culvert under a private railroad berm, approximately 0.3 miles east in Quaker Hill, Waterford (New London County, Connecticut) (Figure 1). The Site historically was an agricultural homestead site but is now mixed hardwood/softwood forest, hedgerow, open field and open water. Figure 1 Site vicinity map. 1.1 Background Connecticut College received grant funding for the stabilization and restoration of the Mamacoke Brook, which is located on Connecticut College Arboretum property between Route 32 and the Thames River. The Brook will be stabilized and restored as part of the Mamacoke Island Aquatic Habitat Resilience (MIAHR) Project, which also includes tidal C:\Users\JWilson\AppData\Local\Temp\Bluebeam Software\11576599.doc marsh restoration along the Thames River. The Brook is laterally and vertically unstable, with eroded banks 4-6 feet in height and deep channel incision along portions of its approximate 1,500-foot length. This instability is likely caused by concentrated stormwater flow contributions, a steeply sloped flow path, and a reduction in vegetation along portions of the channel. Consequently, this has resulted in channel enlargement and excessive sediment generation due to bank erosion. The proposed stream restoration will stabilize the flowpath, enhance the overall health and stability of the stream system, and reduce pollutant loading into the Thames River. 1.2 Objectives The objective of this report is to describe any regulated jurisdictional wetlands within the Site project boundaries. 2.0 WETLAND DELINEATION 2.1 Federal Jurisdictional Wetlands 2.1.1 Regulatory Definition The Army Corps of Engineers (Federal Register 1982) and the Environmental Protection Agency (Federal Register 1980) jointly define wetlands as: Those areas that are inundated or saturated by surface or ground water at a frequency and duration sufficient to support, and that under normal circumstances do support, a prevalence of vegetation typically adapted for life in saturated soil conditions. Wetlands generally include swamps, marshes, bogs and similar areas. Wetlands are generally identified and delineated through the positive evidence of the following diagnostic environmental characteristics: 1) hydrophytic vegetation, 2) hydric soil, and 3) evidence of hydrological indicators. The 1987 USACE Wetland Delineation Manual (Technical Report Y-87-1) and the Interim Regional Supplement to the Corps of Engineers Wetland Delineation Manual: Northcentral and Northeast Region (ERDC/EL TR- 09-19) provides the specific guidelines and methodology required to complete federal wetland delineations. 2.1.2 Methodology The 1987 USACE Wetlands Delineation Manual and the Interim Regional Supplement to the Corps of Engineers Wetland Delineation Manual: Northcentral and Northeast Region C:\Users\JWilson\AppData\Local\Temp\Bluebeam Software\11576599.doc provide definitions and guidelines pertaining to the diagnostic environmental characteristics: 1) hydrophytic vegetation, 2) hydric soil, and 3) hydrological indicators. These three characteristics were evaluated during the Onsite Inspection (Level 2) and using the methods for Routine Determinations, Comprehensive Determinations, Atypical Situations, and Problem Areas. 2.1.2.1 Hydrophytic Vegetation Vegetation that occurs in wetlands or hydrophytic vegetation is defined by the USACE as: …the sum total of macrophytic plant life that occurs in areas where the frequency and duration of inundation or soil saturation produce permanently or periodically saturated soils of sufficient duration to exert a controlling influence on the plant species present (USACE 1987:12). Whether the hydrophytic vegetation is prevalent in an area is dependent on the presence of dominate species comprising the plant community or communities that are typically adapted for life in saturated soil conditions (USACE 1987:13). Plant species are assigned a wetland by the US Fish and Wildlife Service’s (USFWS) National Wetland Inventory (NWI) program. Plant species with an indicator status of obligate (OBL), facultative wetland (FACW) or facultative (FAC) are considered to be typically adapted for life in flooded or saturated conditions. The indicator status of vegetation identified in this survey follows the PLANTS Database (USDA, NRCS 2006): • Obligate wetland (OBL) plants are species that occur almost exclusively in wetlands; Estimated probability of time is >99% • Facultative wetland (FACW) plants are species that usually occur in wetlands; Estimated probability of time is 67%–99% • Facultative wetland (FAC) plants are species that are equally likely to occur in wetlands or non-wetlands; Estimated probability of time is 34%–66% Hydrophytic vegetation is considered to be a primary characteristic of a wetland when “more than 50 percent of the dominant species are OBL, FACW, or FAC” (USACE 1987:17). At an observation point in each wetland area, the dominate plant species were determined as those having the greatest relative basal area (woody overstory or tree layer), greatest height (wood understory or shrub layer), and greatest percentage of areal coverage (herbaceous understory or herb layer) (USACE 1987:53). C:\Users\JWilson\AppData\Local\Temp\Bluebeam Software\11576599.doc 2.1.2.2 Hydric Soils Wetland or hydric soils are defined by the U.S. Department of Agriculture (USDA) Natural Resource Conservation Service (NRCS) as: …a soil that formed under conditions of saturation, flooding, or ponding long enough during the growing season to develop anaerobic conditions in the upper part ((Federal Register, July 13, 1994; USDA- NRCS Hydric Soils Technical Note 1: Proper use of Hydric Soil Terminology). A soil is considered to be a wetland soil by the USACE when the “hydric soil supports hydrophytic vegetation and the area has indicators of wetland hydrology” (USACE 1987:21). Hydric soils are typically poorly and very poorly drained soils. They undergo chemical reactions and physical processes as a result of soil saturation and reducing conditions which differ from those found in upland soils. 2.1.2.3 Wetland Hydrology The USACE defines the term wetland hydrology as: …all hydrologic characteristics of areas that are periodically inundated or have soils saturated to the surface at some time during the growing season (USACE 1987:28). Thus, “areas with evident characteristics for wetland hydrology are those where the presence of water has an overriding influence on the characteristics of vegetation” (USACE 1987:28). The criterion for hydrology consists of inundation or saturation “to the surface continuously for at least 5% of the growing season in most years (50% probability of recurrence)” (USACE 1987:30). The presence of primary and secondary wetland hydrological indicators was noted at each observation point selected in the wetland area. The guidelines (USACE 1987:34) consider that “wetland hydrology is present when any of these primary indicators is present when combined with a hydrophytic plant community and hydric soils.” Additionally, the USACE guides that “in the absence of a primary indicator, any two secondary indicators must be present to conclude that wetland hydrology is present.” C:\Users\JWilson\AppData\Local\Temp\Bluebeam Software\11576599.doc 2.1.3 Determination and Identification of Federal Wetlands The determination and identification of federal wetlands used the methods for Routine Determinations, Comprehensive Determinations, Atypical Situations, and Problem Areas. Overall, the generalized methods (based on USACE 1987, Figure 16, pages 63-64) involve the following: A. Hydrophytic Vegetation (Step 13) • Characterize each plant community types (i.e. trees, saplings, shrubs, herbs, moss/lichens, and vines) • Record USFWS NWI indicator status of dominant species • Determine if more than 50 percent of the dominant species are OBL, FACW, or FAC B. Hydric Soils (Step 14) • Gather soil profile data by using a spade or auger to dig a soil pit • Record soil profile data • Document hydric soil indicators C. Wetland Hydrology (Step 15) • Observe the presence of primary hydrologic indicators • Observe the presence of secondary hydrologic indicators D. Wetland Determination (Steps 16 and beyond) • Using the guidelines determine if hydrophytic vegetation is present based on “A” • Using the guidelines determine if hydric soils are present based on “B” • Using the guidelines determine if wetland hydrology is present based on “C” • Make the wetland determination based on the following: • A wetland exists if all three of the wetland criteria (vegetation, hydrology, and soils) exists for a observation point • The observation point is not a wetland if one or more of the wetland criteria are absent • For Atypical Situations or Problem Areas, all three wetland criteria may not be met. Consideration for modifications or disturbances should be considered and greater weight may be assigned to on criteria over the others. 2.2 Connecticut Jurisdictional Wetlands A wetland, regulated under the Connecticut Inland Wetland and Watercourses Act, is, in general, defined as a soil that is saturated to within 20 inches of the surface during a portion of the growing season. These soils have redoximorphic features, a deficiency of oxygen near the surface, and/or ponded water during the growing season. They are C:\Users\JWilson\AppData\Local\Temp\Bluebeam Software\11576599.doc poorly drained, very poorly drained, alluvial, or fluvial as specified by the USDA Natural Resource Conservation Service (NRCS). Depth to seasonal high water table is determined by low-chroma mottling or wetness indicators. Hydric soils have a similar definition. Watercourses are also regulated under the Connecticut Inland Wetland and Watercourses Act. Watercourses are rivers, streams, brooks, waterways, lakes, ponds, marshes, swamps, bogs, and all other bodies of water including natural or artificial, vernal or intermittent, public or private. A defined permanent channel and bank, and the occurrence of two or more of the following characteristics delineate intermittent watercourses: • Evidence of scour or deposits of recent alluvium or detritus • Presence of standing or flowing water for a duration longer than a particular storm incident • Presence of hydrophytic vegetation 2.3 Field Investigation To prepare for the field investigation, the following current literature and mapping were reviewed: • NRCS Web Soil Survey (http://websoilsurvey.nrcs.usda.gov/) • USFWS Wetlands Online Mapper (http://wetlandsfws.er.usgs.gov/) • Keys to Soil Taxonomy, Tenth Edition (Soil Survey Staff, 2006) • Soil Survey Manual (Soil Survey Staff, 1993) In September 2025, Biohabitats delineated the Federal and State wetlands on site. Soils were inspected on-site by a Biohabitats Soil Scientist using a soil auger or spade, digging at least 20 inches to view the soil profile at the observation point selected for each wetland area. Soil types were identified by observation of soil morphology (matrix color, mottle colors, mottle abundance/size/contrast, and soil texture/structure, etc.) using the terminology and abbreviations found in the “Field Book for Describing and Sampling Soils” (Schoneneberg et al., 2002). The hydric soil indicators and soils sections of the wetland determination form were completed using “Field Indicators for Identifying Hydric Soils in New England” (New England Hydric Soils Technical Committee 1998). Wetland and watercourse (waterway) limits were demarcated (flagged) with pink surveyor’s tape (hung from vegetation) or small flags (on wire stakes) labeled “WETLAND C:\Users\JWilson\AppData\Local\Temp\Bluebeam Software\11576599.doc DELINEATION” that were generally spaced at every 30 feet. Complete boundaries are located along the lines that connect sequentially numbered flags. 3.0 RESULTS OF THE WETLAND DELINEATION 3.1 US Fish and Wildlife Service National Wetland Inventory The USFWS NWI (Figure 2) maps wetlands based on analyses of reconnaissance level information on the location, type, and size of wetlands habitats such that they are accurate at the nominal scale of the 1:24,000 USGS quadrangle base map. Wetlands identified are based on the classification of Cowardin et al. (1979) and the letter and number codes used in that reference. Thus, the maps provide a planning tool to determining whether a site contains wetlands. The USFWS identifies the wetlands occurring on-site as: • Estuarine Intertidal Scrub-Shrub Broad-leaved Deciduous Irregularly Flooded Mesohaline (E2SS1P5) • Estuarine Subtidal Unconsolidated Bottom Subtidal (E1UBL) Use of this resource, however, does not take the place of on-site wetland delineation and evaluation. As part of the field investigation, wetland areas were identified, characterized as to their hydrophytic vegetation, hydric soils, and hydrological indicators and assigned a wetland classification based on this information. 3.2 Natural Resource Conservation Service Soil Map Wetland soils are identified by soil scientists based on established hydric criterion and boundaries depicted on aerial photographs and are accurate at a scale of three acres. Thus, the maps provide a planning tool to determining whether a site contains wetlands. (Figure 2) The upstream limits of the project area are classified as Canton and Charlton soils (60D), a steep-sloped, well-drained soil. The majority of soils within the project area are classified as Sutton fine sandy loams (51B), which is a moderately well-drained soil typically found on hillslopes and classified as having high runoff potential. The northern side and downstream limits of the project area are Charlton-Chatfield complex (73E), a very rocky, well-drained soil found on 15 to 45 percent slopes. All of these soil classes are derived from granite, gneiss, and/or schist. C:\Users\JWilson\AppData\Local\Temp\Bluebeam Software\11576599.doc Use of NRCS soil mapping, however, does not take the place of on-site wetland delineation and evaluation. As part of the field investigation, wetland areas were identified, characterized as to their hydrophytic vegetation, hydric soils, and hydrological indicators and assigned a wetland classification based on this information. Soil characteristics were recorded during on-site field inspections of soil borings and test pits. Details of soil observations are provided in the wetland delineation forms (Appendix B). Figure 2 Site soils map. 3.3 Field Delineated Wetland Units Three (3) wetland/watercourse units were identified on the property. One of the 3 were outside of the investigated area of disturbance and were not delineated or inspected at the same level of detail as the remaining 2 wetland/watercourse units. Appendix A provides the location of the 2 wetland/watercourse units that were characterized and are described in this report. The limits of the wetlands and watercourses on site were flagged C:\Users\JWilson\AppData\Local\Temp\Bluebeam Software\11576599.doc in the field and enumerated WA-1 to WA-35. A generalized description for each wetland and watercourse unit is provided below. 3.3.1 Wetland Unit A Wetland Unit A is a freshwater nontidal scrub-shrub broad-leaved deciduous wetland present along the western edge of the salt pond impoundment at the eastern extent of the project area. This wetland is fed partially by a seep at the toe of slope to the west and the pond to the west and is characterized by shrub layer that is dominated by grey alder (Alnus incana) and spicebush (Lindera benzoin). The herb layer is dominated by common reed (Phragmites australis), skunk cabbage (Symplocarpus foetidus) and beggarsticks (Bidens frondosa). Hydric soils were encountered at the toe of the surrounding slope and the following indicators were met: stratified layers (A5), dark surface (S7), thin dark surface (S9). The wetland hydrology present in Wetland Unit A included primary indicators of surface water (A1), saturation (A3), sparsely vegetated concave surface (B8) and secondary indicators of drainage patterns (B10), dry season water table (C2), geomorphic position (D2) and the plant community passes the FAC neutral test (D5). The upland conditions adjacent to Wetland Unit A consist of steep sideslopes of coarse material that drain well. Hillslope forests are dominated by American beech (Fagus grandifolia), black birch (Betula lenta), sugar maple (Acer saccharum) and black oak (Quercus velutina) species in the tree layer with the shrub layer dominated by burning bush (Euonymus alatus), maple leaved viburnum (Viburnum acerifolium), sassafras (Sassafras albidum), arrowwood (Viburnum dentatum) and barberry (Berberis thunbergii). The herb layer is composed of wintergreen (Chimaphila maculata), white wood aster (Eurybia divaricate), garlic mustard (Alliaria petiolate), woodland sedge (Carex , burnweed, and woodland sedge (Carex sylvatica) poison ivy (Toxicodendron radicans), Japanese honeysuckle (Lonicera japonica) and Asiatic bittersweet (Celastrus orbiculatus) vines. No wetland hydrology or vegetation was present and there were no hydric soil indicators present. 3.3.2 Watercourse A The project site centers around Watercourse A (Mamacoke Brook) which is an intermittent channel that is laterally and vertically unstable, with eroded banks 4-6 feet in height and deep channel incision along portions of its approximate 1,500-foot length. sediment generation due to bank erosion. C:\Users\JWilson\AppData\Local\Temp\Bluebeam Software\11576599.doc 4.0 CONCLUSIONS This Wetland Survey and Evaluation has been prepared to determine the wetlands and watercourses occurring on the Connecticut College Arboretum property in Waterford, Connecticut. Two wetland and watercourse units were identified on the property in the area of USEPA and USACE interest. 5.0 REFERENCES Brinson, M.M. 1993. A Hydrogeomorphic Classification for wetlands, Wetlands Research Program Tech. Report WRP-DE-4, U.S. Army Corps of Engineers, Waterways Experiment Station, Vicksburg, MS. Cowardin, L. M., V. Carter, F. C. Golet, and E. T. LaRoe. 1979. Classification of wetlands and deepwater habitats of the United States. U.S. Fish and Wildlife Service, Biological Service Program. FWS/OBS-79/31. Washington, DC. Hagstrom, N.T., Humphreys, M., and Hyatt, W.A. 1994. A Survey of Connecticut Streams and Rivers—Lower Thames River, Pawcatuck River, and Easter Coastal Drainages. F- 66-R-6: Progress Report, CT DEP Inland Fisheries, April 1, 1993-March 31, 1994, Hartford, CT. New England Hydric Soils Technical Committee. 1998. Field Indicators for Identifying Hydric Soils in New England. New England Interstate Water Pollution Control Commission, Lowell, Massachusetts. Schoenberger, P.J., D.A. Wysocki, E.C. Benham, and W.D. Broderson (editors). 2002. Field Book for Describing and Sampling Soils, Version 2.0. Natural Resource Conservation Service, National Soil Survey Center, Lincoln, NE. Soil Survey Staff. 2006. Keys to Soil Taxonomy, 10th ed. USDA-Natural Resources Conservation Service, Washington, DC. United States Army Corps of Engineers (USACE). 1987. Wetland Delineation Manual, Waterways Experiment Station, Vicksburg, MS, Wetland Research Program Technical Report Y-87-1, On-line Edition. United States Department of Agriculture (USDA). 1993. Soil Survey Manual, Handbook No. 18 U.S. Government Printing office. Washington, DC. C:\Users\JWilson\AppData\Local\Temp\Bluebeam Software\11576599.doc United States Department of Agriculture (USDA), Natural Resources Conservation Service (NRCS). 2006. PLANTS Database. http://plants.usda.gov, 30 October 2006. National Plant Data Center, Baton Rouge, LA 70874-4490 USA). C:\Users\JWilson\AppData\Local\Temp\Bluebeam Software\11576599.doc APPENDIX A – EXISTING CONDITIONS MAPPING MAMACOKE BROOK OUTFALL CHANNEL Waterford, Connecticut 1 of 3 State jurisdictional wetlands and watercourses were delineated in accordance with the State of Connecticut Inland Wetlands and Watercourses Act (CGS 22a-36 to 22a-45 inclusive). Federal jurisdictional wetlands were delineated in accordance with U.S. Army Corps of Engineers Wetlands Delineation Manual (Technical Report Y-87-1) and Regional Supplement to the Corps of Engineers Wetland Delineation Manual: Northcentral and Northeast Region (ERDC/EL TR-12-1) pursuant to Section 404 of the Federal Clean Water Act (33 U.S.C. 1344). To the best of my knowledge, the delineations depicted hereon are true and accurate. Joshua H. Wilson, PWS #1992 Registered Soil Scientist S 2 of 3 3 of 3 C:\Users\JWilson\AppData\Local\Temp\Bluebeam Software\11576599.doc APPENDIX A – NRCS SOILS REPORT MAMACOKE BROOK OUTFALL CHANNEL Waterford, Connecticut Soil Map—State of Connecticut, Eastern Part (Mamacoke Stream Restoration) Natural Resources Conservation Service Web Soil Survey National Cooperative Soil Survey 9/8/2025 Page 1 of 4 4585400 4585500 4585600 4585700 4585800 4585900 4586000 4586100 4586200 4585400 4585500 4585600 4585700 4585800 4585900 4586000 4586100 4586200 741500 741600 741700 741800 741900 742000 742100 742200 742300 742400 742500 742600 742700 741500 741600 741700 741800 741900 742000 742100 742200 742300 742400 742500 742600 742700 41° 23' 28'' N 72° 6' 45'' W 41° 23' 28'' N 72° 5' 47'' W 41° 23' 0'' N 72° 6' 45'' W 41° 23' 0'' N 72° 5' 47'' W N Map projection: Web Mercator Corner coordinates: WGS84 Edge tics: UTM Zone 18N WGS84 0 250 500 1000 1500 Feet 0 50 100 200 300 Meters Map Scale: 1:6,150 if printed on A landscape (11" x 8.5") sheet. Soil Map may not be valid at this scale. MAP LEGEND MAP INFORMATION Area of Interest (AOI) Area of Interest (AOI) Soils Soil Map Unit Polygons Soil Map Unit Lines Soil Map Unit Points Special Point Features Blowout Borrow Pit Clay Spot Closed Depression Gravel Pit Gravelly Spot Landfill Lava Flow Marsh or swamp Mine or Quarry Miscellaneous Water Perennial Water Rock Outcrop Saline Spot Sandy Spot Severely Eroded Spot Sinkhole Slide or Slip Sodic Spot Spoil Area Stony Spot Very Stony Spot Wet Spot Other Special Line Features Water Features Streams and Canals Transportation Rails Interstate Highways US Routes Major Roads Local Roads Background Aerial Photography The soil surveys that comprise your AOI were mapped at 1:12,000. Warning: Soil Map may not be valid at this scale. Enlargement of maps beyond the scale of mapping can cause misunderstanding of the detail of mapping and accuracy of soil line placement. The maps do not show the small areas of contrasting soils that could have been shown at a more detailed scale. Please rely on the bar scale on each map sheet for map measurements. Source of Map: Natural Resources Conservation Service Web Soil Survey URL: Coordinate System: Web Mercator (EPSG:3857) Maps from the Web Soil Survey are based on the Web Mercator projection, which preserves direction and shape but distorts distance and area. A projection that preserves area, such as the Albers equal-area conic projection, should be used if more accurate calculations of distance or area are required. This product is generated from the USDA-NRCS certified data as of the version date(s) listed below. Soil Survey Area: State of Connecticut, Eastern Part Survey Area Data: Version 2, Aug 30, 2024 Soil map units are labeled (as space allows) for map scales 1:50,000 or larger. Date(s) aerial images were photographed: Jun 14, 2022—Oct 6, 2022 The orthophoto or other base map on which the soil lines were compiled and digitized probably differs from the background imagery displayed on these maps. As a result, some minor shifting of map unit boundaries may be evident. Soil Map—State of Connecticut, Eastern Part (Mamacoke Stream Restoration) Natural Resources Conservation Service Web Soil Survey National Cooperative Soil Survey 9/8/2025 Page 2 of 4 Map Unit Legend Map Unit Symbol Map Unit Name Acres in AOI Percent of AOI 3 Ridgebury, Leicester, and Whitman soils, 0 to 8 percent slopes, extremely stony 1.7 1.1% 12 Raypol silt loam, 0 to 3 percent slopes 2.8 1.7% 34A Merrimac fine sandy loam, 0 to 3 percent slopes 14.0 8.8% 34B Merrimac fine sandy loam, 3 to 8 percent slopes 0.5 0.3% 38C Hinckley loamy sand, 3 to 15 percent slopes 2.3 1.5% 50B Sutton fine sandy loam, 3 to 8 percent slopes 3.7 2.3% 51B Sutton fine sandy loam, 0 to 8 percent slopes, very stony 23.9 15.1% 60B Canton and Charlton fine sandy loams, 3 to 8 percent slopes 13.1 8.3% 60C Canton and Charlton fine sandy loams, 8 to 15 percent slopes 10.9 6.9% 60D Canton and Charlton soils, 15 to 25 percent slopes 6.9 4.4% 61B Canton and Charlton fine sandy loams, 0 to 8 percent slopes, very stony 23.9 15.2% 61C Canton and Charlton fine sandy loams, 8 to 15 percent slopes, very stony 11.2 7.1% 68C Narragansett silt loam, 3 to 15 percent slopes, extremely stony 0.7 0.5% 73C Charlton-Chatfield complex, 0 to 15 percent slopes, very rocky 0.5 0.3% 73E Charlton-Chatfield complex, 15 to 45 percent slopes, very rocky 20.9 13.2% 84B Paxton and Montauk fine sandy loams, 3 to 8 percent slopes 5.2 3.3% 84C Paxton and Montauk fine sandy loams, 8 to 15 percent slopes 9.3 5.9% Soil Map—State of Connecticut, Eastern Part Mamacoke Stream Restoration Natural Resources Conservation Service Web Soil Survey National Cooperative Soil Survey 9/8/2025 Page 3 of 4 Map Unit Symbol Map Unit Name Acres in AOI Percent of AOI 98 Westbrook mucky peat, 0 to 2 percent slopes, very frequently flooded 1.4 0.9% 997 Thames silt loam, subtidal 3.6 2.3% W Water 1.6 1.0% Totals for Area of Interest 158.0 100.0% Soil Map—State of Connecticut, Eastern Part Mamacoke Stream Restoration Natural Resources Conservation Service Web Soil Survey National Cooperative Soil Survey 9/8/2025 Page 4 of 4 C:\Users\JWilson\AppData\Local\Temp\Bluebeam Software\11576599.doc APPENDIX B – WETLAND DELINEATION FORMS MAMCOKE BROOK OUTFALL CHANNEL Waterford, Connecticut Project/Site: Applicant/Owner: State: Investigator(s): Lat: Soil Map Unit Name: NWI classification: x Are Vegetation , Soil , or Hydrology Yes x Are Vegetation , Soil , or Hydrology SUMMARY OF FINDINGS – Attach site map showing sampling point locations, transects, important features, etc. X No X No X X No X x X x x x X x x x Yes X ENG FORM 6116-8, SEP 2024 Northcentral and Northeast – Version 2.0 U.S. Army Corps of Engineers WETLAND DETERMINATION DATA SHEET – Northcentral and Northeast Region See ERDC/EL TR-12-1; the proponent agency is CECW-CO-R OMB Control #: 0710-0024, Exp: 9/30/2027 Requirement Control Symbol EXEMPT: (Authority: AR 335-15, paragraph 5-2a) Mamacoke Brook Outfall Channel Stabilization & Restoration City/County: Waterford/New London Sampling Date: 09/12/2025 Landform (hillside, terrace, etc.): Floodplain Local relief (concave, convex, none): concave Slope %: 1 Connecticut College CT Sampling Point: Wet 1 B. Salladin Section, Township, Range: NAD83 Charlton-Chatfield complex N/A Are climatic / hydrologic conditions on the site typical for this time of year? Yes No (If no, explain in Remarks.) Subregion (LRR or MLRA): Long: 41.388310 Datum: LRR R -72.102159 significantly disturbed? Are “Normal Circumstances” present? No naturally problematic? (If needed, explain any answers in Remarks.) Hydrophytic Vegetation Present? Yes Wetland Hydrology Present? Yes If yes, optional Wetland Site ID: Is the Sampled Area Hydric Soil Present? Yes within a Wetland? Yes No Remarks: (Explain alternative procedures here or in a separate report.) HYDROLOGY Wetland Hydrology Indicators: Secondary Indicators (minimum of two required) Primary Indicators (minimum of one is required; check all that apply) Surface Soil Cracks (B6) Surface Water (A1) Water Marks (B1) Hydrogen Sulfide Odor (C1) Crayfish Burrows (C8) Sediment Deposits (B2) Oxidized Rhizospheres on Living Roots (C3) Saturation Visible on Aerial Imagery (C9) Water-Stained Leaves (B9) Drainage Patterns (B10) High Water Table (A2) Aquatic Fauna (B13) Moss Trim Lines (B16) Saturation (A3) Marl Deposits (B15) Dry-Season Water Table (C2) Iron Deposits (B5) Thin Muck Surface (C7) Shallow Aquitard (D3) Inundation Visible on Aerial Imagery (B7) Other (Explain in Remarks) Microtopographic Relief (D4) Drift Deposits (B3) Presence of Reduced Iron (C4) Stunted or Stressed Plants (D1) Algal Mat or Crust (B4) Recent Iron Reduction in Tilled Soils (C6) Geomorphic Position (D2) 1.5 Water Table Present? Yes No Depth (inches): 16.8 Sparsely Vegetated Concave Surface (B8) FAC-Neutral Test (D5) Field Observations: Surface Water Present? Yes No Depth (inches): Remarks: No (includes capillary fringe) Describe Recorded Data (stream gauge, monitoring well, aerial photos, previous inspections), if available: Saturation Present? Yes No Depth (inches): 0 Wetland Hydrology Present? ENG FORM 6116-8, SEP 2024 Northcentral and Northeast – Version 2.0 Sampling Point: (Plot size: 1. 2. 3. 4. 5. 6. (A/B) Sapling/Shrub Stratum (Plot size: x 1 = 1. x 2 = 2. x 3 = 3. x 4 = 4. x 5 = 5. Column Totals: (B) 6. Herb Stratum (Plot size: X 1. X 2. 4 - Morphological Adaptations1 (Provide supporting 3. 4. 5. 6. 7. 8. 9. 10. 11. 12. (Plot size: 1. 2. 3. 4. X ENG FORM 6116-8, SEP 2024 Northcentral and Northeast – Version 2.0 VEGETATION – Use scientific names of plants. Wet 1 Tree Stratum ) Absolute % Cover Dominant Species? Indicator Status Dominance Test worksheet: Number of Dominant Species That Are OBL, FACW, or FAC: 6 (A) Total Number of Dominant Species Across All Strata: 8 (B) Percent of Dominant Species That Are OBL, FACW, or FAC: 75.0% Lindera benzoin 10 Yes FACW Prevalence Index worksheet: 10 Yes FACU FAC species 15 45 43 43 Total % Cover of: 190 OBL species Multiply by: FACW species 95 40 418 UPL species 20 100 Alnus incana 30 Yes FACW FACU species 10 Prevalence Index = B/A = 2.28 183