This disconformity is widely assumed to be equivalent to the Hardegsen disconformity of the central European / Southern North Sea Basin, although the age of this disconformity is not constrained as it is in Europe by biostratigraphical indicators
22.
This disconformity is widely assumed to be equivalent to the Hardegsen disconformity of the central European / Southern North Sea Basin, although the age of this disconformity is not constrained as it is in Europe by biostratigraphical indicators
23.
In this classification these formations would be much older than the overlying Flathead sandstone from the Middle Cambrian Period, and the division between the older Proterozoic rocks, and the newer Cambrian rocks was considered to be a significant disconformity.
24.
The Unkar Group consists of a sequence of sedimentary rocks that accumulated in a variety of environments ranging from fluvial to shallow-strata within it are conformable with the exception of a significant disconformity between the Hakatai Shale and Shinumo Quartzite.
25.
This disconformity exhibits little relief and is identified by marked differences in color, topography, and rock types between tan, ledge-forming, calcareous sandstones and of the Kaibab Limestone and red, slope-forming siltstones of the Moenkopi formation.
26.
The Sherwood Sandstone Group can be broadly divided into an upper ( previously Keuper ) and a lower ( previously Bunter ) unit, at the level of a widely recognized intra-Sherwood Sandstone disconformity perhaps within the uppermost Lower Triassic This disconformity separates two quite distinct environmental systems.
27.
The Sherwood Sandstone Group can be broadly divided into an upper ( previously Keuper ) and a lower ( previously Bunter ) unit, at the level of a widely recognized intra-Sherwood Sandstone disconformity perhaps within the uppermost Lower Triassic This disconformity separates two quite distinct environmental systems.
28.
Below the intra-Sherwood Sandstone disconformity these deposits are dominated by evidence of a major braided river system, this river system responsible for transporting the sand and gravel to the Alderley area was named by Wills ( 1970 ) the Budleighensis River, after Budleigh Salterton in Devon, where its existence was first established.
29.
Its upper contact is a disconformity that characteristically is a nearly horizontal surface with little or no relief . ( In the Grand Canyon, the upper disconformity forms a horizontal platform at the top of the Redwall Limestone . ) Locally, the bottom unconformity of the Redwall Limestone contains a basal conglomerate that directly rests upon this bottom unconformity.
30.
Its upper contact is a disconformity that characteristically is a nearly horizontal surface with little or no relief . ( In the Grand Canyon, the upper disconformity forms a horizontal platform at the top of the Redwall Limestone . ) Locally, the bottom unconformity of the Redwall Limestone contains a basal conglomerate that directly rests upon this bottom unconformity.
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