ANALYSIS OF HISTORICAL SEDIMENTATION TRANSECT DATA FOR SIX PERMANENTLY MARKED RIVER MILE TRANSECTS IN POOL 22 OF THE UPPER MISSISSIPPI RIVER. Joseph S. Lundh, Gary V. Swenson, U.S. Army Corps of Engineers, Mississippi River Project, PO Box 534, Pleasant Valley, IA 52767. Sedimentation transects were established by the survey branch of the Rock Island District of the Army Corps of Engineers at or near most whole numbered river miles on the Upper Mississippi River from Lock and Dam 10 to Lock and Dam 22. The first transects were established in the 1890's in Pool 19. The six transects studied (river mile 315, 316, 320.4, 321.5, 323.1, 324.1) were established in 1955 and resurveyed in 1974 to 1975. The permanently marked transects crossed the river perpendicular to flow extending from levee to levee. Elevation and bathymetric measurements to the nearest tenth of a foot were collected at roughly 50 foot increments along the transects and also at major features (ridges, bank-line, water's edge). Comparing the 1955 data to 1975 values showed significant changes. Even though the overall change in elevation for the transects was an average increase of 0.2 feet, summing changes by different geomorphic features provided varying results. Features that increased in elevation include sloughs by an average of 2.8 feet, chutes by 1.4 feet, islands by 0.6 feet, and mainland by 0.7 feet. The main channel and main channel border were the only features that decreased on average. The portion of the transects that were land in 1955 that continued to be land in 1975 raised by an average of 0.9 feet. Due to the dynamic nature of the river, these results can best be applied to the upper part of Pool 22. Resurveying these and other transects in the future would provide better trend data. Comparing more comprehensive sedimentation data to hydrologic trend data will help in understanding the fate of the river's backwaters and floodplain. Keywords: sediment range, sediment transect, sedimentation, Mississippi River, land survey