Teton Valley is a mountainous region brought about by uplifts, faults, fault blocks, alluvial deposits and erosion by streams to create steep narrow canyons.
32.
The thick continental crust that made up the new east coast collapsed into a series of down-dropped fault blocks that roughly parallel today's coastline.
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Considerable damage was seen in localized portions of the valley and also in the foothills of the San Gabriel mountains above the fault block.
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Raised coral reefs along the east coast and the frequent occurrences of earthquakes in the rift valley indicate that the fault block is still rising.
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The "'Smorbukk Field "'was discovered in 1984 in 250 300 m of water that produces from Lower to Middle Jurassic sandstone formations within a fault block.
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The uplift of the horst-like fault block was part of the Saxonian tectonic processes and is understood as a long range effect of the Alpine orogeny.
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Other fault blocks in the North Sea, such as the Oseberg fault block, have rounded or flat tops resulting from erosion and peneplanation down to sea level.
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Other fault blocks in the North Sea, such as the Oseberg fault block, have rounded or flat tops resulting from erosion and peneplanation down to sea level.
39.
The tectonic style of the Sierra de Gredos is the so-called Germanic style, i . e . with large upraised fault blocks, known as horst, bounded by graben.
40.
Evidence of the volcanic activity is found in the tilted fault blocks of Jurassic volcaniclastics which are commonly found in the Florida Straits area ( Vacher 95 ).