Click
to
hide
Water-Year
Summary
instructions
and
information
- Water-Year Summary reports summarize a year of hydrologic data in a printer-friendly format.
- For water years 2014 onward, choose a water year and parameter and an on-demand Water-Year Summary report will be generated.
- For water years 2006 through 2013, choose a water year and an Annual Water Data Report will be provided.
- For water years 2005 and earlier, Annual Water Data Reports may be available in digital format.
- Not all sites have reports available for every water year.
USGS Water-Year Summary 2024
07191220 SPAVINAW CREEK NEAR SYCAMORE, OK
LOCATION - Lat 36°20'05", long 94°38'29" referenced to North American Datum of 1983, in NE 1/4 NW 1/4 sec.04, T.21 N., R.25 E., Delaware County, OK, Hydrologic Unit 11070209, on right bank 1.8 mi upstream from Cherokee Creek, 4.8 mi northeast of Row, 6.5 mi southeast of Sycamore, and at mile 35.0.
DRAINAGE AREA - 132 mi². From automated delineation using 10-meter National Elevation Dataset digital elevation model data dated 10/01/2006 and Watershed Boundary Dataset dated 10/01/2006, using Albers Equal-Area Projection, North American Datum 1983.
REVISIONS HISTORY - WSP 2121: 1965 (M). WDR 2012: Drainage area
SURFACE-WATER RECORDS
PERIOD OF RECORD - October 1961 to current year
GAGE - Water-stage recorder. Datum of gage is 868.34 ft NAVD of 1988. Prior to Nov. 6, 2001, elevation published as 875 ft above NGVD of 1929, from topographic map.
REMARKS - Quality of data for all periods can be obtained by contacting the Oklahoma-Texas Water Science Center.
All estimated records are considered poor unless noted otherwise.
EXTREMES OUTSIDE PERIOD OF RECORD - According to local residents, a flood of approximately the same magnitude as the July 27, 1975 flood occurred in the early 1880's.
WATER-QUALITY RECORDS
PERIOD OF RECORD - October 1972 to April 1988, December 2001 to current year.
COOPERATION - All analytical records were furnished by City of Tulsa Quality Assurance Laboratory, Tulsa, Oklahoma.
REMARKS - Samples collected periodically by the U.S. Geological Survey. All water-quality samples were analyzed at the City of Tulsa Quality Assurance Laboratory in Tulsa, Oklahoma. Suspended sediment samples were analyzed by U.S. Geological Survey. Specific conductance, pH, water temperature, air temperature, turbidity, and dissolved oxygen were determined in the field.
