In ancient storm-influenced prograding shoreline sequences, sole marks (mainly tool marks)
from hummocky crossstratified storm deposits are commonly oriented normal to …

Unidirectional, oscillatory and combined-flow paleocurrent data from many ancient wave-
dominated coastlines indicate that sediment transport was directed offshore at angles of 70 …

A new depositional model for hummocky cross-stratified sandstones is based on the
following observations.(1) Storms transport coastal sand to the inner shelf under oscillatory …

Hummocky cross-stratification in ancient sedimentary deposits is considered to be
diagnostic of inner shelf storm deposits. Megaripples of 2-5 m spacing are typical responses …

Member 2 of the late Precambrian to Lower Cambrian Chapel Island Formation of southeast
Newfoundland was primarily deposited in storm-influenced, nearshore and shelf …

A model is developed to explain the wide range of sedimentary structures found in ancient
storm-deposited beds. The model predicts the nature and association of internal …

A sequence of graded sand layers, interbedded with mud, extends offshore over 100 km
from the Yukon Delta shoreline across the flat, shallow (< 20 m depth) epicontinental shelf of …

Advances in acoustic imaging of submarine canyons and channels have provided accurate
renderings of sea‐floor geomorphology. Still, a fundamental understanding of channel …

Hummocky cross-stratification is believed to be one of the diagnostic sedimentary structures
of storm-dominated shallow-marine environments. The wavelength of this stratification …

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