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  2. Flood basalt - Wikipedia

    en.wikipedia.org/wiki/Flood_basalt

    A flood basalt (or plateau basalt [1]) 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 . [ 2 ]

  3. Raton Basin - Wikipedia

    en.wikipedia.org/wiki/Raton_Basin

    Ultrapotassic lamprophyre dikes can also be found along the basin flanks, which are highly unusual in the Rocky Mountain region. The site of the Raton Basin was a coastal plain at the end of Cretaceous and beginning of Paleogene time, and has a well-preserved sequence of rocks spanning the Cretaceous–Paleogene boundary.

  4. Columbia River Basalt Group - Wikipedia

    en.wikipedia.org/wiki/Columbia_River_Basalt_Group

    The Columbia River Basalt Group (including the Steen and Picture Gorge basalts) extends over portions of four states. The Columbia River Basalt Group (CRBG) is the youngest, smallest and one of the best-preserved continental flood basalt provinces on Earth, covering over 210,000 km 2 (81,000 sq mi) mainly eastern Oregon and Washington, western Idaho, and part of northern Nevada. [1]

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  6. List of flood basalt provinces - Wikipedia

    en.wikipedia.org/wiki/List_of_Flood_basalt_provinces

    Columbia River Basalt Group [g] Chilcotin Plateau Basalts [e] Increased Antarctic deep waters Yellowstone hotspot Nördlinger Ries (14.5-14.3) Burdigalian: 20.44 Aquitanian: 23.03 * Shield volcanoes of Ethiopia [h] Antarctic ice sheet complete Paleogene: Oligocene: Chattian: 28.1 Ethiopian and Yemen traps (31–30) [h] Fish Canyon Tuff (27.51 ...

  7. Grape Creek (Colorado) - Wikipedia

    en.wikipedia.org/wiki/Grape_Creek_(Colorado)

    Grape Creek is a tributary of the Arkansas River that flows through Custer and Fremont counties in South-Central Colorado. The creek drains much of the Wet Mountain Valley , located between the Sangre de Cristo Mountains and the Wet Mountains in Custer County.

  8. Cardenas Basalt - Wikipedia

    en.wikipedia.org/wiki/Cardenas_Basalt

    The upper unit of the Cardenas Basalt is a series of cliff-forming basaltic and andesitic lava flows that are interbedded with beds of breccia, sandstone, and lapillite. It is about 200 m (660 ft) thick and contains four to six, prominent lava flows that range in composition from quartz tholeiite to tholeiitic andesite ( icelandite ).

  9. Bijou Creek - Wikipedia

    en.wikipedia.org/wiki/Bijou_Creek

    Bijou Creek is a 45.5-mile-long (73.2 km) [2] tributary of the South Platte River in Colorado. The creek flows northeast from elevated terrain in southeastern Adams County to a confluence with the South Platte near Fort Morgan. Bijou Creek is subject to flash floods from time to time. [3]