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File FY17 Scope of Work
This document describes the EBTJV Coordinator's scope of work supported by FY17 FWS-NFHAP funds.
Located in About EBTJV / EBTJV Management / EBTJV Coordinator - Scope of Work Descriptions
FY18 EBTJV Coordination and Operations_FWS-NFHAP Funded Agreement
This folder contains documents related to the EBTJV's FY18 Coordination and Operations agreement supported by FWS-NFHAP Funds.
Located in Projects / EBTJV Operational Grants
File FY18 Scope of Work
This document describes the EBTJV Coordinator's scope of work supported by FY18 FWS-NFHAP funds.
Located in About EBTJV / EBTJV Management / EBTJV Coordinator - Scope of Work Descriptions
FY19 EBTJV Coordination and Operations_FWS-NFHAP Funded Agreement
This folder contains documents related to the EBTJV's FY19 Coordination and Operations agreement supported by FWS-NFHAP Funds.
Located in Projects / EBTJV Operational Grants
File FY19 Scope of Work
This document contains the EBTJV Coordinator's scope of work supported by FY19 FWS-NFHAP funding.
Located in About EBTJV / EBTJV Management / EBTJV Coordinator - Scope of Work Descriptions
File Troff document Geomorphic, Flood, and Groundwater-Flow Characteristics of Bayfield Peninsula Streams, Wisconsin, and Implications for Brook-Trout Habitat
In 2002–03, the U.S. Geological Survey conducted a study of the geomorphic, flood, and groundwater-flow characteristics of five Bayfield Peninsula streams, Wisconsin (Cranberry River, Bark River, Raspberry River, Sioux River, and Whittlesey Creek) to determine the physical limitations for brook-trout habitat. The goals of the study were threefold: (1) to describe geomorphic characteristics and processes, (2) to determine how land-cover characteristics affect flood peaks, and (3) to determine how regional groundwater flow patterns affect base flow. The geomorphic characterization consisted of analyses of historical aerial photographs and General Land Office Survey notes, observations from helicopter video footage, surveys of valley cross sections, and coring. Sources of sediment were identified from the helicopter video and field surveys, and past erosion-control techniques were evaluated. Geomorphic processes, such as runoff sediment erosion, transport, and deposition, are driven by channel location within the drainage network, texture of glacial deposits, and proximity to postglacial lake shorelines; these processes have historically increased because of decreases in upland forest cover and channel roughness. Sources of sediment for all studied streams mainly came from bank, terrace, or bluff erosion along main stem reaches and along feeder tributaries that bisect main-stem entrenched valley sides. Bluff, terrace, and bank erosion were the major sources of sediment to Whittlesey Creek and the Sioux River. No active bluff erosion was observed on the Cranberry River or the Bark River but anecdotal information suggests that landslides occasionally happen on the Cranberry River. For the Bark River, sources of sediment were somewhat evenly divided among road crossings (bridges, culverts, and unimproved forest lanes), terrace erosion, bank erosion, and incision along upper main stems and feeder channels along valley sides. Evaluation of past erosion-control techniques indicated that bluffs were stabilized by a combination of artificial hardening and bioengineering of the bluff base and reducing mass wasting of the tops of the bluffs. Flood hydrographs for the Cranberry River were simulated for four land-cover scenarios—late 20th century (1992–93), presettlement (before 1870), peak agriculture (1928), and developed (25 percent urban). Results were compared to previous simulations of flood peaks for Whittlesey Creek and for North Fish Creek (southern adjacent basin to Whittlesey Creek). Even though most uplands are presently forested, flood peaks simulated for 1992–93 were 1.5 to 2 times larger than presettlement flood peaks. The increased flood peaks caused (1) increased incision along upper main stems and tributaries that bisect entrenched valley sides, (2) bluff and terrace erosion along reaches with entrenched valleys, (3) overbank deposition and bar formation in middle and lower main stems, and (4) aggradation in mouth areas. A base-flow survey was conducted and a groundwater-flow model was developed for the Bayfield Peninsula to delineate groundwater contributing areas. A deep aquifer system, which includes thick deposits of sand and the upper part of the bedrock, is recharged through the permeable sands in the center of the peninsula. Base flow is unevenly distributed among the Bayfield streams and depends on the amount of channel incision and the proximity of the channels to the recharge area and coarse outwash deposits. Groundwater contributing areas for the five streams do not coincide with surface-water-contributing areas. About 89 percent of total recharge to the deep aquifer system discharges to Bayfield streams; the remaining 11 percent directly discharges to Lake Superior. Historical land-cover changes have had negligible effects on groundwater-flow from the deep aquifer system. Available brook-trout habitat is dependent on the locations of groundwater upwellings, the sizes of flood peaks, and sediment loads. Management practices that focus on reducing or slowing runoff from upland areas and increasing channel roughness have potential to reduce flood peaks, erosion, and sedimentation and improve brook-trout habitat in all Bayfield Peninsula streams.
Located in Science and Data / Brook Trout Related Publications
File Get to Know Your Native Brook Trout Poster
PDF version of a Brook Trout Poster developed by Trout Unlimited's Native Trout Workgroup and was provided funding support by the EBTJV.
Located in Groups / Outreach and Education Committee / Outreach Materials
File Great Pond Tributary Culvert Replacement, Little Cards Brook, Franklin, Maine
Project application
Located in Projects / … / 2016 Projects / Little Cards Brook Culvert Replacement, Franklin ME
File Troff document Habitat Restoration in Chattahoochee National Forest Streams, GA_FY07 Project
Twenty-six habitat improvement structures were installed in six Chattahoochee NF streams. In addition, a fish barrier was constructed in Tate Branch to exclude invasive Rainbow Trout, thus improving habitat for Southern Appalachian Brook Trout.
Located in Projects / Project Completion Reports
File Troff document Harvey’s Lake Dam Removal, South Peacham Brook, Barnet, Vermont
Removal of the Harvey's Lake dam improves natural flow regimes, free-flowing river conditions, water quality and temperature, sediment release and transport, and connectivity to 27 miles within the Stevens River watershed. Floodplain restoration and large wood installations provides additional habitat in South Peacham Brook. The project cost is $861,750 and the estimated socioeconomic benefit is $14.7 million.
Located in Projects / 2019 Projects
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