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  2. Rite Rug Flooring - Wikipedia

    en.wikipedia.org/wiki/Rite_Rug_Flooring

    RiteRug Flooring, formerly Rite Rug, is a flooring retailer headquartered in Columbus, Ohio. RiteRug Flooring's current headquarters, distribution center, wholesale and outlet showroom are located in a 150,000 space in the Whitehall area of the city. [1] [2] They sell floor coverings in the Columbus area. [3]

  3. Rift - Wikipedia

    en.wikipedia.org/wiki/Rift

    Accommodation zones may be located where older crustal structures intersect the rift axis. In the Gulf of Suez rift, the Zaafarana accommodation zone is located where a shear zone in the Arabian-Nubian Shield meets the rift. [6] Rift flanks or shoulders are elevated areas around rifts. Rift shoulders are typically about 70 km wide. [7]

  4. Geology of Scotland - Wikipedia

    en.wikipedia.org/wiki/Geology_of_Scotland

    Similarly, there are also Old Red Sandstone deposits and granite intrusions. The most distinctive feature is the ultrabasic ophiolite peridotite and gabbro on Unst and Fetlar, which are remnants of the Iapetus Ocean floor. [6] Much of Shetland's economy depends on oil and gas production from fields in the surrounding seas. [7] [8]

  5. Seychelles microcontinent - Wikipedia

    en.wikipedia.org/wiki/Seychelles_microcontinent

    The granite outcrops of the Seychelles Islands in the central Indian Ocean were amongst the earliest examples cited by Alfred Wegener as evidence for his continental drift theory. [1] Ridge–plume interactions have been responsible for separating a thinned continental sliver from a large continent (i.e. India).

  6. Geology of Ohio - Wikipedia

    en.wikipedia.org/wiki/Geology_of_Ohio

    The Grenville mountains eroded, filling in rift basins and Ohio was flooded and periodically exposed as dry land throughout the Paleozoic. In addition to marine carbonates such as limestone and dolomite , large deposits of shale and sandstone formed as subsequent mountain building events such as the Taconic orogeny and Acadian orogeny led to ...

  7. Midcontinent Rift System - Wikipedia

    en.wikipedia.org/wiki/Midcontinent_Rift_System

    The Midcontinent Rift System (MRS) or Keweenawan Rift is a 2,000 km (1,200 mi) long geological rift in the center of the North American continent and south-central part of the North American plate. It formed when the continent's core, the North American craton , began to split apart during the Mesoproterozoic era of the Precambrian , about 1.1 ...

  8. Decomposed granite - Wikipedia

    en.wikipedia.org/wiki/Decomposed_granite

    Decomposed granite is a kind of granite rock that is weathered to the point that the parent material readily fractures into smaller pieces of weaker rock. Further weathering yields material that easily crumbles into mixtures of gravel -sized particles known as grus that further may break down to produce a mixture of clay and silica sand or silt ...

  9. Geology of Iceland - Wikipedia

    en.wikipedia.org/wiki/Geology_of_Iceland

    The Reykjanes Peninsula Rift in SW Iceland is the landward continuation of the Reykjanes Ridge that connects to the Western Volcanic Zone (WVZ). The more active Eastern Volcanic Zone (EVZ) represents a rift jump, although it is unclear how the eastward propagation of the main rifting activity has occurred. [ 12 ]

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