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Unconformities Images

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Siccar Point, Scottish Borders, a rocky promontory in the county of Berwickshire. famous in the history of geology for Hutton's unconformity
beach
berwickshire
borders
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Grey Pleistocene alluvial deposits rest on top of much older yellow sandstone of the Cretaceous Pen Formation. The contact is a geological unconformity.
alluvial
alluvium
arid
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The Granite block is part of the ancient Tanzanian Craton. Near the fault line marking the boundary with the Great Rift Valley the pink Granite has been metamorphosed into Granodiorite.
ancient
ancient environments
bands
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Siccar Point, Scottish Borders, a rocky promontory in the county of Berwickshire. famous in the history of geology for Hutton's unconformity
beach
berwickshire
borders
 
Layered deposits in galle crater showing unconformities
galle crater
layered deposits
unconformities
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Angular unconformity: horizontal stratum of conglomerate (Oligocene) deposited in older tilted and eroded layers.
background
detail
geology
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These Jurassic sandstones on the Yorkshire Dinosaur Coast show where two levels of deposition of marine sandstones have been separated by different eras of erosion and tilting of the strata
ancient environments
bands
beds
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An angular unconformity is an unconformity where horizontally parallel strata of sedimentary rock are deposited on tilted and eroded layers.
activity
age
angular
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Grand Canyon West: Witness to the Great Unconformity-A Geological Enigma
250 million years
american landmark
ancient
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The Grear Unconformity identified by John Wesley Powell on the first voyage down the Colorado Rover through the Grand Canyon
adventure
background
backgrounds
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These marine sediments were lain down in a warm marine environment in the Jurassic era. The underlying grey mudstones sit as an unconformity with overlaying shallower habitat and later sandstones
ancient environments
asymmetrical
bed-forms
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Siccar Point, Scottish Borders, a rocky promontory in the county of Berwickshire. famous in the history of geology for Hutton's unconformity
beach
berwickshire
borders
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Jurassic sandstones have overlain mudstones in an unconformity in strata exposed along the Dinosaur Coast. Tilting of the older strata and the subsequent layering of the sandstone creates this feature
170 million years bp
aeolian
ancient environments
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unconformity, river sediment on angled strata, Gros Ventre River, Grand Tetons, WY
erosion
geology
rock layers
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An unconformity occurs when sedimentary layers become compacted and then tilt in the formation means the overlaying deposits lie on top at an angle. This has happened in these Jurassic era sandstones
ancient environments
bed-forms
beds
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Siccar Point, Scottish Borders, a rocky promontory in the county of Berwickshire. famous in the history of geology for Hutton's unconformity
beach
berwickshire
borders
Premium
Layers of sedimentary Sandstone from the Jurassic Period show a feature known as an Unconformity, where layers do not lie in a regular sequence
170million yr bp
ancient environments
bands
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