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[Music playing]
Faith: We're at Schweitzer Natural Area along Johnson Creek. An area that's been recently rehabilitated upstream, but downstream we're looking at some of the old urban channel that shows both effects of agriculture and urbanization over time. I have with me Gardner and Janine here. And Gardner, you're familiar with the area. What's been some of the history on the watershed as far as the development over time? Gardner: Well, Johnson Creek watershed upstream at this point is fairly highly developed, both in urbanization as well as agricultural impacts. A lot of the areas along the stream historically would have been cedar forest with a lot of interconnected wetlands that were connected to the channel that provided all sorts of complex fish habitat. Agriculture and urbanization have been the primary impacts here, as well as timber harvest very early on. And those impacts have resulted in lots of changes to the stream channel in this area. Once of the most fundamental changes in this area was confinement of the channel into a straightened and hardened channel, and this was done in the '30's by the Works Progress Administration, WPA. And, you can see that here there's a grouted stone bank, trapezoidal channel, very straight, very simplified. The wood's been pulled out, the habitat has been severely degraded for aquatic species like salmon which we had in large numbers historically, but in very few numbers relatively now. So, there's been some large impacts. Faith: So, we have some changes in the watershed and then also, some changes of remediate effects in the channel itself. Janine, what's changed about the sediment characteristics as well in this watershed? Janine: Well, it's very common in urbanized watersheds to see a change in the sediment, the type of sediment in the stream. And, in Johnson Creek in particular, we've seen a decrease in the coarse sediment, the gravels and the cobbles, the bigger material, which creates the habitat, physical habitat for the fish. And, we've seen an increase in the fine sediment, so the silts and the clays, which end up as more turbid, kind of muddy water coming through during storm events. Faith: So, basically, we have a very mature, somewhat mature forest behind us. It looks very beautiful. But yet, you know, we have the stream channel that's been disconnected from its floodplain, as well as the changes within the channel itself with the habitat, as well as the watershed changes in hydrology and sediment. So, a lot of things are going on here. [Music playing] [End of Audio] |
DetailsTitle: Rehabilitating urban streams for salmon habitat improvement, Johnson Creek Schweitzer Natural Area, Portland, Oregon Description: Faith Fitzpatrick (U.S. Geological Survey), Gardner Johnston (Interfluve, Inc.), and Janine Castro (U.S. Fish and Wildlife Service) discuss watershed changes associated with urbanization that have led to degraded channel conditions and altered salmon habitat. Location: Portland, OR, Johnson Creek Schweitzer Natural Area, USA Date Taken: 12/13/2010 Length: 2:52 Video Producer: Douglas A. Harned , National Water-Quality Assessment Program (NAWQA), USGS, North Carolina Water Science Center, Raleigh, NC Note: This video has been released into the public domain by the U.S. Geological Survey for use in its entirety. Some videos may contain pieces of copyrighted material. If you wish to use a portion of the video for any purpose, other than for resharing/reposting the video in its entirety, please contact the Video Producer/Videographer listed with this video. Please refer to the USGS Copyright section for how to credit this video. Additional Video Credits: Faith Fitzpatrick: Scriptwriter, Narrator, Scientist Consultant Gerard McMahon: Producer Douglas Harned: Producer, Video, Editor Alan Cressler: Video Luke McMahon: Video Gardner Johnston (Interfluve, Inc.) Janine Castro (U.S. Fish and Wildlife Service) File Details: Suggest an update to the information/tags? Tags: |
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