A HIGH RESOLUTION RECORD OF LATE-PLEISTOCENE PROVO SHORELINE DEVELOPMENT FROM LAKE BONNEVILLE, WESTERN UTAH
Gravel pit exposures reveal several 30-cm thick packages of inversely graded coarse sand and gravel. These packages consist almost entirely of shoreface deposits and are interpreted to represent annual cycles. Most of the annual shoreface deposition probably occurred in the spring, at the time of maximum fluvial delivery of sediment to the shorezone. The finer fraction of the sediment load was rapidly incorporated into the longshore transport system and therefore deposited prior to the coarser gravel that arrived slightly later in the annual cycle. Sand was simultaneously winnowed from the shoreface and deposited as an apron that extended into the deeper water of the nearshore zone. The high rate of deposition (30 cm/yr) can be attributed to an abundance of alluvium proximal to the shorezone and is consistent with the total amount of shoreface accretion that occurred within the interval of time represented by the Provo shoreline. Morphological evidence indicates that the direction of longshore transport reversed at least once from a dominantly westerly flow to a dominantly easterly flow toward the end of Provo shoreline development.