U.S. Geological Survey 20091030 vector digital data Portland, OR U.S. Geological Survey http://water.usgs.gov/lookup/getspatial?spragueriveroregon_bars_1940 The Sprague River drains 4090 square kilometers in south-central Oregon before flowing into the Williamson River and upper Klamath Lake. In cooperation with the U.S. Fish and Wildlife Service, the USGS and University of Oregon conducted a study to evaluate channel and floodplain processes for the 131 km of the Sprague River and its major tributaries, including the lower 20 km of the South Fork Sprague River, the lower 16 km of the North Fork Sprague River, and the lower 62 km of the Sycan River. The study involved multiple analyses, including assessments of historical channel change, riparian and floodplain vegetation, and surficial geology. To support these analyses, digital floodplain and channel maps were prepared from historic notes, maps, and aerial photos to depict channel and floodplain conditions at different times between 1866 and 2005. The geospatial database of current and historic channel and floodplain conditions will also enable evaluation of long-term trends pertaining to aquatic and riparian habitat conditions. These data were created to support understanding of geomorphic conditions and historical changes to channel and floodplain conditions for the Sprague River and the lower portions of its major tributaries. GIS layers depicting channel centerlines, water features, fluvial bars, floodplain vegetation, and floodplain features such as irrigation canals, levees and dikes, and roads were created from aerial photographs dating from 1940, 1968, and 2000. The purpose of this mapping was to track changes in channel and floodplain morphology and vegetation over time and to measure changes in channel position. Historical aerial photographs from 1940 and 1968 were acquired, scanned, and rectified for this project, while digital orthophotographs from 2000 are publicly available. (See metadata for each photograph set for more information on the rectification process and resolution of each dataset). In addition, channel centerlines were mapped from publicly available coverages for 1975 (Natural Resources Conservation Service Soil Survey of Klamath County) and 2005 (U.S. Department of Agriculture NAIP imagery). The surficial geologic mapping was done to support understanding of the geologic context of the modern floodplain, and encompasses the alluvial valleys of the Sprague River and the lower portions of the Sycan, North Fork, and South Fork Sprague Rivers. 1940 ground condition Complete None planned -121.849619 -121.095955 42.609705 42.437173 None geomorphology channel analysis floodplain analysis inlandWaters None Sprague River Oregon Klamath Basin None The U.S. Geological Survey and the University of Oregon should be acknowledged as the data source in products derived from these data. U.S. Geological Survey Tana Haluska Geographer mailing address

2130 SW 5th Avenue

Portland OR 97201 USA 503-251-3212 N/A 503-251-3470 thaluska@usgs.gov (Warning: Although accurate at the time of production, this information may have become obsolete. See the Metadata_Reference_Information section for a current contact.) http://water.usgs.gov/GIS/browse/spragueriveroregon_bars_1940.gif Illustration of data set GIF Microsoft Windows XP Version 5.1 (Build 2600) Service Pack 3; ESRI ArcCatalog 9.3.1.3000 Image evaluation and feature interpretation occurred at a scale of 1:10,000 - 1:500. Digitization of features occurred at a scale of 1:1,000. Topology rules were used to clean and edit features digitized within the floodplain boundary data set for overlap and boundary accuracy. A separate topology was run to edit digitizing overlap with the floodplain boundary data set and the features digitized within it to ensure all features were enclosed within the final floodplain boundary. Data are complete. Digitization of features occurred at a scale of 1:1000. In general, all features that were clearly visible at that scale were digitized. Minimum size and density specifications for digitizing are listed in each attribute definition. Where vegetation overhang and shadows overlapped with other features within the floodplain boundary digitizing an accurate boundary of the covered feature was attempted. Interpreting the boundary of the covered feature (Water, Built Feature or Bar) was done by extrapolating edges from visible data. Varied discharge associated with different photo dates occasionally resulted in discontinuity of water features at photo overlap and boundaries. In the situation of discontinuity at overlap one photo was exchanged for a bordering photo at approximately the mid-point of overlap and features were digitized to the photo being utilized. When discontinuity occurred at image boundaries or the photo exchange point the water feature with the greatest area was digitized. Mean daily discharges associated with different photo dates are recorded in the Photo Sets and Related Stream Discharge.xls spreadsheet located inside the SpragueRiverAnalysis.mdb file. Bars are defined as streamlined and recently active landforms that are formed through depositional processes, typically with an elongate tear-drop shape that is aligned along the x-axis to the direction of surface water flow. Commonly, the bars were not vegetated or only slightly vegetated due to active fluvial processes of erosion and deposition, and therefore had light tones compared to adjacent terrestrial surfaces with established vegetation. Interpretation from aerial photos was based on location, shape, and tonal contrast to surrounding features. The entire streamlined landform was mapped as a bar, even if there was some tonal variation within the feature. Only bars with an area of 16 pixels or more were digitized as bars. A goal of an RMSE less than 5 meters was established for the georectification process. Photo scanning and DPI were calculated to ensure that 2000, 1968, and 1940 photo sets all had the same 1 meter pixel resolution. N/A Watershed Sciences, LLC 2005 raster digital data Watershed Science. 2005. Sprague River LiDAR Remote Sensing and Data Collection. Submitted to the Klamath Tribes. digital elevation model 2005 ground condition WS2005 Used to identify topographic details that assisted in feature classification during digitizing as well as floodplain delineation. Also used for analysis of relative elevation and proximity of features within the delineated floodplain. Department of Interior and Department of Agriculture 1985 map U.S. Geological Survey. Oregon-Klamath Co Quadrangle 7.5-Minute series Topographic Map. 1:24,000. U.S. Department of the Interior and U.S. Department of Agriculture. Variable dates (1985-1998). 24,000 digital topographic map 1985 1998 ground condition USGSTOPO Used as a reference for digitizing roads, railroads and feature names. U.S. Department of Agriculture 1940 remote-sensing image 20,000 digital aerial photography 1940 ground condition USDAAP40 Used to digitized 1940 features. U.S. Geological Survey 2000 remote-sensing image digital orthophoto quadrangle 2000 ground condition USGSDOQ2000 Used in the rectification process for the 1940 aerial photography. Data Acquisition: Remotely sensed imagery (historic aerial photos and LiDAR) researched and digital copies of the 1940s photo set were obtained from the National Archives 2005 Rectification: The photo rectification process warps an image across a set of specified points. The warping leaves the edges of the image less spatially accurate than the center portion of the image. To ensure the best accuracy of data, feature digitizing occurred nearest the center of the photo as possible on the rectified 1940s and 1968 photo sets. One photo was exchanged for a bordering photo at approximately the mid-point of photo overlap. Digitization on a photo's edge only occurred on the final most distal photo when there was no adjacent photo available. The historic 1940 aerial photo set rectified to the USGS 2000 DOQs. A goal of 20 ground control points (GCP) per photo was established (actual: 11-35 GCPs/photo). Hard point landscape features (building or fence corners) were prioritized for rectification, then "soft point" features (trees, etc.) were used. GCP selection prioritized points nearest the river and the active floodplain to ensure accuracy of rectification warping in the study area. A goal of an RMSE < 5m was established (actual: 1.75-4.5, with one outlier in a canyon section with and RMSE of 6.01). Rectification of photos used 2nd order polynomial. USDAAP40 USGSDOQ2000 2005 Digitizing: Began digitizing 1940 water features and river centerlines. Completed in 2008. Digitizing Protocol: The Sprague River Project is focused on geomorphic and vegetation changes over time within the active geomorphic floodplain of the Sprague River watershed. We defined the active geomorphic floodplain as the area adjacent to the channel system that is low-lying and displays geomorphic features typical of channel erosion and depositional processes clearly on imagery, including aerial photos, 7.5 min USGS topo maps, and LIDAR images (Watershed Sciences, 2005). Geomorphic features used to define the extent of the active geomorphic floodplain included point bars, scroll bars, abandoned channels (including oxbows ponds and filled channels), and swell and swale topography. The active geomorphic floodplain was distinguished from adjacent alluvial surfaces that are smoother and show less evidence of erosion and deposition, although some of these adjacent surfaces may be flooded regularly by overbank flows. Digital data sets were first digitized from the 2000 DOQs. High resolution LiDAR imagery data (Watershed Sciences, 2005) was used to identify topographic details that assisted in feature classification. If the feature visible in the LiDAR was not visible in the 2000 DOQ the feature was not digitized. Additional comparison with the 1998 color air photo mosaic (USFWS 1998) aided in evaluating the 2000 DOQs. The 2000 digital data was then used as a template for digitizing features from the 1968 and 1940s photo sets. Because the spatial context of this project is focused within the active geomorphic floodplain, interpreting and digitizing the floodplain boundary was prioritized to define area of digitization in all three year sets. Original data sets were digitized in ArcMap as separate shapefiles (line or polygon). Line files were "buffered" in ArcMAP to generate polygons with a calculable area for these features. All digitizing was reviewed and edited by the graduate research assistants or project leaders for interpretation consistency and data accuracy. After editing, the shapefiles were input into a geodatabase. The geodatabase was used to organize the data sets by data type and subtype, feature prioritization, and topology rules. USDAAP40 WS2005 USGSTOPO 2006 Quality Assurance: Ran two stages of topology as discussed in the Logical Consistency Report 2008 Vector G-polygon 377 Universal Transverse Mercator 10 0.999600 -123.000000 0.000000 500000.000000 0.000000 coordinate pair 0.000100 0.000100 meters North American Datum of 1983 Geodetic Reference System 80 6378137.000000 298.257222 SpragueRiverOregon_Bars_1940 Bars U.S. Geological Survey OBJECTID Internal feature number. ESRI Sequential unique whole numbers that are automatically generated. Shape Feature geometry. ESRI Coordinates defining the features. TYPE Type of bar U.S. Geological Survey FPABAR - Floodplain-attached bar Bar feature that is attached at any point to the floodplain. U.S. Geological Survey ISABAR - Island-attached bar Bar feature that is attached at any point to an Island feature. U.S. Geological Survey MCBAR - Mid-channel bar Bar feature that is located within the channel and not attached at any point to an Island or Floodplain. U.S. Geological Survey OB - Other bar Any other Bar feature not otherwise defined. No Bar features were attributed as Other. U.S. Geological Survey SUBTYPE Subtype code U.S. Geological Survey 30 Floodplain-attached bar U.S. Geological Survey 31 Island-attached bar U.S. Geological Survey 32 Mid-Channel bar U.S. Geological Survey 33 Other bar U.S. Geoloigcal Survey NAME Name of bar U.S. Geological Survey Unique names of bars. NOTE_ Notes U.S. Geological Survey Notes Shape_Length Length of feature in internal units. ESRI Positive real numbers that are automatically generated. Shape_Area Area of feature in internal units squared. ESRI Positive real numbers that are automatically generated. U.S. Geological Survey Ask USGS -- Water Webserver Team mailing address

445 National Center

Reston VA 20192 USA 1-888-275-8747 (1-888-ASK-USGS) http://water.usgs.gov/user_feedback_form.html Downloadable Data 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 PKZIP compression Winzip 1000 http://water.usgs.gov/GIS/dsdl/SpragueRiverAnalysis.zip None. This dataset is provided by USGS as a public service. 20091113 U.S. Geological Survey Ask USGS -- Water Webserver Team mailing address

445 National Center

Reston VA 20192 USA 1-888-275-8747 (1-888-ASK-USGS) http://answers.usgs.gov/cgi-bin/gsanswers?pemail=h2oteam&subject=GIS+Dataset+spragueriveroregon_bars_1940 FGDC Content Standards for Digital Geospatial Metadata FGDC-STD-001-1998