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Τι (ποιος) είναι UNCONFORMITY - ορισμός
![John Clerk]] in 1787 and photographed in 2003.](https://commons.wikimedia.org/wiki/Special:FilePath/Hutton Unconformity , Jedburgh.jpg?width=200 "John Clerk]] in 1787 and photographed in 2003.")
![''Disconformity'' at [[Horni Pocernice]], Czech Republic](https://commons.wikimedia.org/wiki/Special:FilePath/Disconformity Horni Pocernice.jpg?width=200 "''Disconformity'' at [[Horni Pocernice]], Czech Republic")
![Mississippian]] [[Borden Formation]] and overlying Pennsylvanian Sharon Conglomerate, near [[Jackson, Ohio]]](https://commons.wikimedia.org/wiki/Special:FilePath/Borden-Sharon unconformity.jpg?width=200 "Mississippian]] [[Borden Formation]] and overlying Pennsylvanian Sharon Conglomerate, near [[Jackson, Ohio]]")
![dolomite]] ''nonconformably'' overlies 1.5-billion-year-old [[rhyolite]], near [[Taum Sauk Hydroelectric Power Station]], Missouri.](https://commons.wikimedia.org/wiki/Special:FilePath/Taum Sauk precambrian-cambrian unconformity.jpg?width=200 "dolomite]] ''nonconformably'' overlies 1.5-billion-year-old [[rhyolite]], near [[Taum Sauk Hydroelectric Power Station]], Missouri.")
![''Nonconfirmity'' at Ratssteinbruch near [[Dresden]], Germany](https://commons.wikimedia.org/wiki/Special:FilePath/Ratssteinbruch Dresden-Doelzschen.jpg?width=200 "''Nonconfirmity'' at Ratssteinbruch near [[Dresden]], Germany")
![Praia do Telheiro]], Portugal](https://commons.wikimedia.org/wiki/Special:FilePath/Angular Unconformity at Praia do Telheiro in Algarve in Portugal.png?width=200 "Praia do Telheiro]], Portugal")
![''Angular unconformity'' between the underlying [[Dockum Group]] and the overlying [[Exeter Sandstone]] at Steamboat Butte in the valley of the Dry Cimmarron, New Mexico](https://commons.wikimedia.org/wiki/Special:FilePath/Steamboat Butte New Mexico.jpg?width=200 "''Angular unconformity'' between the underlying [[Dockum Group]] and the overlying [[Exeter Sandstone]] at Steamboat Butte in the valley of the Dry Cimmarron, New Mexico")
![Angular unconformity in [[Jingtai County]], China](https://commons.wikimedia.org/wiki/Special:FilePath/Winkeldiskordanz.JPG?width=200 "Angular unconformity in [[Jingtai County]], China")
![Angular unconformity in [[pyroclastic rock]] layers erupted by [[Chimborazo]] volcano, Ecuador](https://commons.wikimedia.org/wiki/Special:FilePath/Tephra Layers at Chimborazo Volcano in Ecuador.jpg?width=200 "Angular unconformity in [[pyroclastic rock]] layers erupted by [[Chimborazo]] volcano, Ecuador")
Βικιπαίδεια
An unconformity is a buried erosional or non-depositional surface separating two rock masses or strata of different ages, indicating that sediment deposition was not continuous. In general, the older layer was exposed to erosion for an interval of time before deposition of the younger layer, but the term is used to describe any break in the sedimentary geologic record. The significance of angular unconformity (see below) was shown by James Hutton, who found examples of Hutton's Unconformity at Jedburgh in 1787 and at Siccar Point in Berwickshire in 1788, both in Scotland.
The rocks above an unconformity are younger than the rocks beneath (unless the sequence has been overturned). An unconformity represents time during which no sediments were preserved in a region or were subsequently eroded before the next deposition. The local record for that time interval is missing and geologists must use other clues to discover that part of the geologic history of that area. The interval of geologic time not represented is called a hiatus. It is a kind of relative dating.
