The Hazel Hole and Gold Basin landslides are large deep-seated glacial failures. They have contributed and continue to contribute large amounts of fine sediments to the North and South Forks of the Stillaguamish River. In recent years pool shallowing, fine sediment intrusion to the spawning gravels, and overall total suspended solids have negatively impacted salmon habitat throughout the watershed. This project provides for planning related activities in support of log jam construction at the Hazel Hole and Gold Basin sites. These strategically placed engineered log jams will help prevent toe-cutting of the slides and channeling the flow away from sediment sources. A similar project was completed this past summer just upstream of the Hazel slide and is functioning as designed to date. Preliminary baseline data will be gathered this spring and summer, on water quality, fish use, and flow.