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  2. Tumalo Volcanic Center - Wikipedia

    en.wikipedia.org/wiki/Tumalo_Volcanic_Center

    How big was the volcanic eruption?Imagine a cube of lava, one that's 1.5 miles (2.4 km) long by 1.5 miles (2.4 km) wide by 1.5 miles (2.4 km) high. [1]Ashflows include

  3. Volcanic and igneous plumbing systems - Wikipedia

    en.wikipedia.org/wiki/Volcanic_and_igneous...

    Schematic sketch of the volcanic and igneous plumbing systems (after Burchardt, 2018). [1] [2]Volcanic and igneous plumbing systems (VIPS) consist of interconnected magma channels and chambers through which magma flows and is stored within Earth's crust. [1]

  4. File:Combined geology map of Borneo.pdf - Wikipedia

    en.wikipedia.org/wiki/File:Combined_geology_map...

    Permission is granted to copy, distribute and/or modify this document under the terms of the GNU Free Documentation License, Version 1.2 or any later version published by the Free Software Foundation; with no Invariant Sections, no Front-Cover Texts, and no Back-Cover Texts.

  5. Contact (geology) - Wikipedia

    en.wikipedia.org/wiki/Contact_(geology)

    Some of these boundary points are at physical locations, while others are in ice drill core sections, or have been defined chronometrically. The GSSP for the Danian Stage marks the end of the Cretaceous and the beginning of the Paleocene Series. [10] Located in Tunisia, the contact is described as a reddish layer at the base of a dark clay layer.

  6. Plummer's Ledge Natural Area - Wikipedia

    en.wikipedia.org/wiki/Plummer's_Ledge_Natural_Area

    Plummer's Ledge Natural Area in Wentworth, New Hampshire is a 3.5-acre (1.4 ha) plot of land protected by the State of New Hampshire to preserve unique geologic features called glacial potholes. Geologists usually account for the isolated potholes, now high and dry, by the plunging of melt water through vertical cracks or crevasses in the ...

  7. Snake coils (geology) - Wikipedia

    en.wikipedia.org/wiki/Snake_coils_(geology)

    Snake coils is a descriptive term used by physical geologists and glaciologists to describe the "snake coil"-like shape that occurs along certain ablation lines. Essentially miniature tunnel valleys, the peculiar natural shapes were first described by French geologist Jean-Jerome Peytavi in 1973 during an expedition to northern Greenland, and later confirmed by a team of Danish geologists.

  8. Fault block - Wikipedia

    en.wikipedia.org/wiki/Fault_block

    Lifted fault-block geology Tilted fault-block formation in the Teton Range. Fault-block mountains often result from rifting, an indicator of extensional tectonics. These can be small or form extensive rift valley systems, such as the East African Rift zone. Death Valley in California is a smaller example.

  9. Geophysical fluid dynamics - Wikipedia

    en.wikipedia.org/wiki/Geophysical_fluid_dynamics

    Two physical features that are common to many of the phenomena studied in geophysical fluid dynamics are rotation of the fluid due to the planetary rotation and stratification (layering). The applications of geophysical fluid dynamics do not generally include the circulation of the mantle , which is the subject of geodynamics , or fluid ...