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Storm sedimentation
Author(s) -
BRENCHLEY PATRICK J.
Publication year - 1989
Publication title -
geology today
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.188
H-Index - 17
eISSN - 1365-2451
pISSN - 0266-6979
DOI - 10.1111/j.1365-2451.1989.tb00645.x
Subject(s) - geology , sedimentary depositional environment , storm , sedimentary rock , shore , sedimentary structures , geomorphology , continental shelf , oceanography , sedimentation , sediment transport , stratification (seeds) , sediment , paleontology , seed dormancy , botany , germination , structural basin , dormancy , biology
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.