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Initiation of the channel complex, which forms part of a seismic-scale channel complex set, is marked by a basal erosion surface interpreted to have been carved by multi-event erosive sediment gravity flows, which bypassed sediment down dip farther into the basin.
The new erosion surface must postdate all units, dikes, veins, and deformation features that it crosses.
In this hypothesis, an erosion surface is developed across the structure zone by long-continued planation.
The Sheikh El-Obeiyid Village lies on the second erosion surface of the Northern Plateau.
The Grand Canyon Series actually dips slightly eastward and is separated from the overlying Cambrian sandstones by a major erosion surface unconformity.
The steeply dipping beds of blocky mudstone give an interesting asymmetry to this miniature canyon, with the smooth erosion surface on the southern side countered by jagged exposed strata to the north.
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Encircled numbers 1 6 refer to the numbering of glacial erosion surfaces (see Supplementary Fig. 1).
MFS and a variety of erosion surfaces have been delineated in the field.
Much of the western massif, notably Limousin, consists of monotonous erosion surfaces.
Many erosion surfaces are developed in step formation, as is evident on Mount Teshio.
Here, we present such a framework, based on the recognition of genetic stratigraphic sequences (GSSs) and intervening erosion surfaces (see Methods).
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