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20-084 Lyashenko <br />PAGE 3 OF 22 <br />3/27/2C <br />This mapped stream is fed by stormwater infrastructure along S 2nd Ave (see Appendix) <br />and exits a 12" culvert approximately 1.5' above grade, as the pipe emerges from a <br />weedy ditch at a topographic break; the streambed under the pipe is <1' wide, shallow, <br />and composed of gravelly -loamy substrate; from this point, the stream is conveyed by <br />an excavated ditch into a brushy area dominated by Red -Alder and Himalayan <br />blackberry (Alnus rubra and Rubus armeniacus, respectively) of the easterly buffer. <br />The buffer at the head of the stream, as it exits stormwater infrastructure, slopes <br />upward to the west at approximately 16% and breaks at S 2nd Ave; to the southwest the <br />buffer is paved with gravel; and to the northwest the buffer is composed of maintained <br />lawn, R. Armeniacus, and a hedgerow of even -age Douglas -Fir (Pseudotsuga menziesii, <br />see photo sheet); no surfacewater was observed in the western buffer. Wildlife <br />observed in the buffer was limited to passerine birds; indicators of other wildlife <br />presence, such as browsing, trails, scat, and beaver activity, were not observed at the <br />time of the site visit. <br />Figure 3. Approximate Type Ns standard buffer. <br />Image Source: Snohomish County PDS, 2018. All locations are approximate. <br />Soil at the site is mapped as Everett very gravelly sandy loam, 0-8 percent slopes, which <br />does not carry a hydric soil rating; the minor components of the soil mapped in the area <br />do not carry hydric soil ratings. In consideration of the mapped soil data, the plant <br />composition on the property, and the absence of wetland hydrology, I did not sample <br />the site for hydric soil indicators. <br />