Terra Nova, 24, 273–282, 2012 Abstract Hummocky cross‐stratification (HCS) is considered
a diagnostic structure of surface storm activity at the shoreface–offshore transition. However …

Analog laboratory experiments were conducted to investigate subaqueous bed forms
generated under storm-like oscillatory and combined flow. Experiments were carried out in a …

The dominance of isotropic hummocky cross‐stratification, recording deposition solely by
oscillatory flows, in many ancient storm‐dominated shoreface–shelf successions is …

A series of wave-tunnel experiments was conducted to investigate the conditions under
which hummocky and swaley cross-stratification form. Isotropic 3-dimensional (3-D) …

Hummocky cross-stratification is a type of bedding in sedimentary rocks caused by the
draping of sand around low-steepness three-dimensional bedforms. This distinctive form of …

Abstract The Upper Ordovician Kope and Fairview Formations and the Bellevue Tongue of
the Grant Lake Limestone exposed in the Cincinnati, Ohio region, represent storm …

The orientations of elongate gutter casts occurring in inner shelf storm deposits of the
Proterozoic Bijaygarh Shale Formation, India reveal a modal population oriented roughly …

Hummocky sandstone bodies were deposited on the margin of an Early Cretaceous rift
basin in an overall progradational inner-shelf to lower-shoreface unit. Excellent outcrops of …

Extreme storm events in the coastal zone are one of the main forcing agents of short-term
coastal system behavior. As such, storms represent a major threat to human activities …