University of Oregon North Campus Conditional Use Permit Project <br />Riparian Assessment and Management Report <br /> <br />The PSA includes approximately 3 acres of riparian habitat, defined in this report as the area between the OHWM <br />and TOHB along the Willamette River and Millrace Slough, and approximately 33 acres of upland habitat. Aquatic <br />habitat comprises less than an acre of the PSA and is primarily Millrace Slough and Willamette River shoreline. <br />The conservation setback encompasses 14 acres and overlaps with all three habitat types within the PSA. A paved <br />bike and pedestrian path runs east to west within the PSA. The PSA includes a landscaped access ramp south of <br />the Frohnmayer Bridge. The Frohnmayer Bridge serves as a bike and pedestrian bridge that spans Willamette River <br />and connects the North Campus area to Alton Baker Park and Autzen Stadium on the north side of the river outside <br />of the PSA. East of a roundabout within the PSA, the bike and pedestrian pathway merges with Riverfront Parkway <br />which continues to the south under the railroad bridge and outside of the PSA. <br />The open space east of the Millrace Slough within the PSA was historically used for agriculture followed by a sand <br />and gravel mining and processing operation owned by the Eugene Sand and Gravel Company (L.R. Squier <br />Associates, Inc., 1990). The property was purchased by the UO in 1968. This area now includes two recreation <br />fields, bicycle path, mowed pastures with trees scattered throughout, several unmaintained foot paths, and <br />Himalayan blackberry (Rubus armeniacus) patches. The portion of the PSA west of the Millrace Slough was <br />historically a gravel and concrete plant and an EWEB transmission pole yard (L.R. Squier Associates, Inc., 1990). <br />This area currently includes a large fenced field with several small depressions created from years of soil <br />compaction from industrial use that may display wetland characteristics. <br />2.0METHODS <br />MB&G biologists conducted TOHB and OHWM determinations and a riparian assessment within the PSA on July <br />25, 26, and 27, 2017. During the field effort, aquatic, riparian, and upland areas within and around the PSA were <br />examined and photographed. Prior to the field effort, MB&G biologists reviewed 2015 3-foot LiDAR-derived digital <br />elevation models (DEMs) along with 1-foot interpolated contours and aerial imagery (OLC 2015). MB&G biologists <br />created 30 target field points to focus the field effort to areas with unreliable or low point density LiDAR data. <br />These target points identified both TOHB and OHWM sampling areas that required further information gathering <br />in the field. <br />2.1Top of High Bank Determination <br />MB&G determined the TOHB line by visual identification of the highest point at which the bank met the grade of <br />the surrounding topography \[EC 9.4920 (1)c1\]. The TOHB locations were recorded with a Trimble GeoXT 6000 <br />series GPS unit capable of sub-meter accuracy. MB&G collected 27 TOHB points along the Willamette River and <br />Millrace Slough in the PSA. MB&G post-corrected these points using Trimble Pathfinder software and compared <br />them to known monument locations near the PSA, resulting in an absolute accuracy of less than 2 feet. MB&G <br />used the post-corrected points to select contour lines representative of the TOHB line and to serve as guidance in <br />areas where LiDAR data were ambiguous. Finally, MB&G biologists reviewed the TOHB line in-office and refined <br />the line using field photos and riparian information collected on site. <br />2.2Ordinary High Water Mark Determination <br />MB&G determined the OHWM by visual identification of one or more of the following \[EC 9.4920 (1)c2\]: <br />“a. A clear, natural line impressed on the bank by the presence of water, flowing water or waves. <br />b.Changes in the characteristics of soils. <br />c.The presence of water-borne litter and debris. <br />d.The uppermost limit of destruction of terrestrial vegetation by the presence of water, flowing <br />water or waves.” <br /> page 2 <br /> <br />