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Flood basalt - Wikipedia
A flood basalt (or plateau basalt ) is the result of a giant volcanic eruption or series of eruptions that covers large stretches of land or the ocean floor with basalt lava. Many flood basalts have been attributed to the onset of a hotspot reaching the surface of the Earth via a mantle plume. Flood basalt provinces such as the … See more
Flood basalts are the most voluminous of all extrusive igneous rocks, forming enormous deposits of basaltic rock found throughout the geologic record. They are a highly distinctive form of intraplate volcanism, … See more
Flood basalts contribute significantly to the growth of continental crust. They are also catastrophic events, which likely contributed to many See more
Representative continental flood basalts and oceanic plateaus, arranged by chronological order, together forming a listing of See more
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• Supervolcano – Volcano that has had an eruption with a volcanic explosivity index (VEI) of 8
• Volcanic plateau – Plateau produced by volcanic activity See moreTheories of the formation of flood basalts must explain how such vast amounts of magma could be generated and erupted as lava in such short … See more
Large Igneous Provinces (LIPs) were originally defined as voluminous outpourings, predominantly of basalt, over geologically very short durations. This definition did not specify minimum size, duration, petrogenesis, or setting. A new attempt to refine … See more
Trap rock is the most durable construction aggregate of all rock types, because the interlocking crystals are oriented at random. See more
Wikipedia text under CC-BY-SA license Columbia Plateau Province - U.S. National Park Service
Apr 30, 2018 · Over 170,000 cubic kilometers (105,633 mi) of basaltic lava, known as the Columbia River Basalts, covers the western part of the province. These tremendous flows erupted between 17 million - 6 million years ago.
Volcanic plateau - Wikipedia
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Columbia River Basalt Group Stretches from Oregon to Idaho
Plateau | Definition, Geography, Landform, Types, & Examples
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Apr 18, 2023 · Basaltic lavas have low silica (45-52 weight %), are hot (2200°F; 1200°C), and have low viscosity, meaning that they flow easily. Basaltic lava flows may travel many miles (kms) from their vents, and up to hundreds of miles …
Inflation Structures, Lava-Rise Plateaus & Inflation Pits
Apr 18, 2023 · Inflation is the process that occurs when lava continues to be supplied within a solidified crust of a basaltic lava flow, causing the flow surface to be lifted upward. Inflation can cause lava flows to substantially thicken and …
Morphology and dynamics of inflated subaqueous …
Apr 29, 2014 · During eruptions onto low slopes, basaltic Pahoehoe lava can form thin lobes that progressively coalesce and inflate to many times their original thickness, due to a steady injection of magma beneath brittle and viscoelastic …
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