U.S. Geological Survey 2012 raster digital data Open File Report 2012-1064 Reston, VA U.S. Geological Survey http://water.usgs.gov/lookup/getspatial?ofr2012_1064_Bandon_Photo_Mosaic_1939 Jones, Krista L. O'Connor, Jim E. Keith, Mackenzie K. Mangano, Joseph F. Wallick, J. Rose 2012 U.S. Geological Survey Open-File Report 2012-1064 Reston, Virginia U.S. Geological Survey 84 p. http://pubs.usgs.gov/of/2012/1064/ The Coquille River system is an unregulated system that encompasses 2,745 square kilometers of southwestern Oregon and flows into the Pacific Ocean near the town of Bandon, Oregon. Beginning in the Rogue River-Siskiyou National Forest, the South Fork Coquille River gains the Middle Fork Coquille River (drainage area 798 square kilometers) and shortly thereafter the North Fork Coquille River (749 square kilometers). In cooperation with the U.S. Army Corps of Engineers, the U.S. Geological Survey completed a reconnaissance-level assessment of channel condition and bed-material transport relevant to the permitting of in-stream gravel extraction along the the South Fork Coquille River from river kilometer (RKM) 115.4 near its confluence with Upper Land Creek to RKM 58.5 at its confluence with the North Fork Coquille River, the mainstem Coquille River from RKM 58.5 at the confluence of the South and North Forks of the Coquille River to its mouth, the Middle Fork Coquille River from RKM 15.4 to its confluence with the South Fork Coquille River, and the North Fork Coquille River from RKM 14.6 to its confluence with the South Fork Coquille River. To support these analyses, digital channel maps were produced to depict channel and floodplain conditions in the Coquille River basin from different time periods. GIS layers defining the wetted channel and bar features and channel centerline of Hunter Creek were developed for four time periods: 1939, 1967, 2005, and 2009. For this project, the active channel was defined as area typically inundated during annual high flows, and includes the low-flow channel as well as side channels, islands, and channel-flanking gravel bars. The wetted channel and bar feature datasets were developed by digitizing from aerial photographs. Aerial photographs from 1939 and 1967 were scanned, rectified, and mosaicked for this project (See metadata for each photograph set for more information on the rectification process and resolution of each dataset). Digital orthophotographs from 2005 and 2009 are publicly available. These data were created to support preliminary assessment of channel stability and bed-material transport on Coquille, Middle Fork Coquille, and North Fork Coquille Rivers, southwest Oregon. This mapping was used to track changes in channel morphology and planform over time. 1939 ground condition Complete None planned -124.436963 -124.137426 43.206578 43.074471 None channel stability sediment transport historical channel change fluvial geomorphology aerial photograph ISO 19115 Topic Categories inlandWaters Geographic Names Information System (GNIS) North Fork Coquille River Curry County Middle Fork Coquille River Coos County South Fork Coquille River Oregon Coast Range Coquille River None The U.S. Geological Survey should be acknowledged as the data source in products derived from these data. U.S. Geological Survey Mackenzie Keith Hydrologist mailing

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Portland OR 97201 US 503-251-3474 mkeith@usgs.gov http://water.usgs.gov/GIS/browse/ofr2012_1064_Bandon_Photo_Mosaic_1939.pdf Illustration of data set Portable Document Format (PDF) None Unclassified None Microsoft Windows XP Version 5.1 (Build 2600) Service Pack 3; ESRI ArcGIS 10.0.5.4400 Scanned aerial photographs were georeferenced using National Agriculture Imagery Program one-half-meter resolution digital orthophotographs acquired in 2005. Comparison of the 1939 mosaics to National Agriculture Imagery Program digital orthophotographs from 2005 suggest that errors in image alignment are generally less than 4 meters, but may be higher than 9 meters. Data are complete. The 1939 photographs were georeferenced with 9 to 15 ground-control points concentrated near the main channel and rectified with a second-order polynomial transformation. Root mean square error ranged from 1.6 to 4.9 meters. Comparison of the 1939 mosaics to National Agriculture Imagery Program digital orthophotographs from 2005 suggest that errors in image alignment are generally less than 4 meters, but may be higher than 9 meters. Wallick, J. Rose Jim E. O'Connor Anderson, Scott Keith, Mackenzie Cannon, Charles Risley, John C. 2011 U.S. Geological Survey Scientific Investigations Report 2011-5041 Reston, Virginia U.S. Geological Survey 112 p. http://pubs.usgs.gov/sir/2011/5041/ online 1939 2009 ground condition Wallick, 2011 The report describes detailed methods used in photograph rectification and mosaicking, as well as channel centerline, wetted channel, and bar feature delineation. Surdex Corportation, Chesterfield, MO 2006 remote sensing image aerial photograph 20050715 20050805 ground condition NAIP 2005 The aerial photographs provided a base layer from which channel features were delineated. U.S. Army Corps of Engineers unknown remote sensing image 10200 aerial photograph 19390503 19390717 ground condition USACE 1939 The aerial photographs provided a base layer from which channel features were delineated. Digital photographs were obtained from University of Oregon Aerial Photograph Library. Photographs were scanned at 1200 dots per inch to jpeg format. 2011 USACE 1939 The photographs were georeferenced to National Agriculture Imagery Program digital orthophotographs using ArcGIS 9.3. Ground control points were concentrated near the channel. Stationary points, such as bedrock outcrops and building corners, were primarily used to spatially register the photographs, although less static points, such as intersections and trees, were also used. 2011 USACE 1939 NAIP 2005 The photographs were rectified with a second order polynomial transformation and resampled to a 0.5 meter cell size with bilinear interpoloation using the Georeferencing Toolbar in ArcGIS 9.3. 2011 The rectified images were clipped to include the study area where control points were concentrated. 2011 The rectified images were mosaicked into a single ESRI file geodatabase raster dataset. 2011 Raster Grid Cell 28607 48291 Transverse Mercator 0.9996 -123.0 0.0 500000.0 0.0 coordinate pair 0.000000002220024164500956 0.000000002220024164500956 Meters D North American 1983 GRS 1980 6378137.0 298.257222101 ofr2012_1187_Wilson_Kilchis_Photo_Mosaic_1939 Aerial photo mosaic of the Wilson and Kilchis Rivers, Tillamook basin, Oregon in 1939 U.S. Geological Survey Stretched value Value between 0 and 255 corresponding to color ramp display ESRI 0 255 Pixel value Value between 0 and 255 corresponding to color value ESRI 0 255 U.S. Geological Survey Ask USGS -- Water Webserver Team mailing

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Reston VA 20192 US 1-888-275-8747 (1-888-ASK-USGS) http://water.usgs.gov/user_feedback_form.html Although these data have been used by the U.S. Geological Survey, U.S. Department of the Interior, no warranty expressed or implied is made by the U.S. Geological Survey as to the accuracy of the data. The act of distribution shall not constitute any such warranty, and no responsibility is assumed by the U.S. Geological Survey in the use of these data, software, or related materials. The use of firm, trade, or brand names in this report is for identification purposes only and does not constitute endorsement by the U.S. Geological Survey. The names mentioned in this document may be trademarks or registered trademarks of their respective trademark owners. ESRI Geodatabase Feature Class ArcGIS 10 PKZIP compression Winzip http://water.usgs.gov/GIS/dsdl/ofr2012_1064_Coquille_River_Photo_Mosaics.zip None. This dataset is provided by USGS as a public service. 20120918 U.S. Geological Survey Ask USGS -- Water Webserver Team mailing

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Reston VA 20192 US 1-888-275-8747 (1-888-ASK-USGS) http://answers.usgs.gov/cgi-bin/gsanswers?pemail=h2oteam&subject=GIS+Dataset+ofr2012_1064_Bandon_Photo_Mosaic_1939 FGDC Content Standard for Digital Geospatial Metadata FGDC-STD-001-1998 local time