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Types of unconformities Disconformity: File:Disconformity. jpg | Disconformity A disconformity is an unconformity between parallel layers of
Kaynak: Unconformity

This disconformity is widely assumed to be equivalent to the Hardegsen disconformity of the central European/Southern North Sea Basin,
Kaynak: Geology of Alderley Edge

dinosaur fossils in the Americas, and is separated by a disconformity from the underlying Upper Triassic Chugwater Formation red beds .
Kaynak: Sundance Formation

The contact between the Hatakai Shale and overlying Shinumo Quartzite is a distinct, significant disconformity . This disconformity is
Kaynak: Hakatai Shale

Within the Unkar Group, the contact between the Hakatai Shale and overlying Shinumo Sandstone is a distinct disconformity. This contact is
Kaynak: Unkar Group

Overall, the strata within it are conformable with the exception of a significant disconformity between the Hatakai Shale and Shinumo
Kaynak: Shinumo Quartzite

This is expressed by a disconformity that removed successively deeper reservoir beds to the north and west. Major downwarping to the south
Kaynak: Sarir field

A type of unconformity called a disconformity was formed. Disconformities show erosional features such as valleys, hills and cliffs that
Kaynak: Geology of the Grand Canyon area

It is separated by an erosional disconformity from the next member, the Anembalemba Member. The lower portion of the Anembalemba Member
Kaynak: Maevarano Formation

The ring is about 6.2 | km | mi in radius around the central disconformity. Ring depression The ring depression is the result of the
Kaynak: Kentland crater

000 years at the 15 foot level, a geological disconformity at the 15 foot level, a date of 100,000 years at 20 feet, and some human and
Kaynak: Jeffrey Goodman

The youngest fauna are Maastrichtian, with an apparent disconformity between the Late Cretaceous and Paleocene , marked by high levels of
Kaynak: Maastrichtian

late Cenozoic uplift of the Rocky Mountains , it is separated from the lower Trujillo Formation by a disconformity , and a very long hiatus.
Kaynak: Palo Duro Canyon

and trends within a mineralised belt, is for the sulfide to occupy the disconformity between the komatiitic lava and its underlying substrate.
Kaynak: Kambalda type komatiitic nickel ore deposits

change in bedding orientation across the boundary, which is nowhere well-exposed, suggesting that it may represent some sort of disconformity.
Kaynak: Torridonian

The contact between the Cardenas Basalt and the overlying Nankoweap Formation is an erosion surface that is a disconformity or even a
Kaynak: Cardenas Basalt

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