Storm sedimentation

Publisher Website
Google Scholar
Abstract
Storm‐driven currents can carry sand from the shoreline tens of kilometres out onto the continental shelves where it is moulded by storm waves into a storm‐sand bed showing distinctive sedimentary structures, including hummocky crossstratification. An understanding of the nature of the depositional currents and the processes that form hummocky cross‐stratification comes from the work of oceanographers, observations by geologists and experimental studies in the laboratory, although the conclusions reached are sometimes conflicting. Storm‐sandstone beds provide valuable information about sediment dispersal and depositional systems in nearshore and shelf environments. Hummocky crossstratification indicates the activity of storm waves and hence the approximate depth of ancient shelf seas.