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  2. Shield volcano - Wikipedia

    en.wikipedia.org/wiki/Shield_volcano

    The most active shield volcano in Africa is Nyamuragira. Eruptions at the shield volcano are generally centered within the large summit caldera or on the numerous fissures and cinder cones on the volcano's flanks. Lava flows from the most recent century extend down the flanks more than 30 km (19 mi) from the summit, reaching as far as Lake Kivu.

  3. List of shield volcanoes - Wikipedia

    en.wikipedia.org/wiki/List_of_shield_volcanoes

    This list of shield volcanoes includes active, dormant and extinct shield volcanoes. Shield volcanoes are one of the three types [ specify ] of volcanoes. They have a short cone shape, and have basaltic lava which means the lava has low viscosity (viscosity is a measure of the ability for a liquid to flow)

  4. Shield (geology) - Wikipedia

    en.wikipedia.org/wiki/Shield_(Geology)

    The Atlantic Shield. The Amazonian (Brazilian) Shield on the eastern bulge portion of South America. Bordering this is the Guiana Shield to the north, and the Platian Shield to the south. The Uruguayan Shield; The Baltic (Fennoscandian) Shield is located in eastern Norway, Finland and Sweden. The African (Ethiopian) Shield is located in Africa.

  5. Macroemulsion - Wikipedia

    en.wikipedia.org/wiki/Macroemulsion

    There are other ways to create emulsions between two liquids, such as adding one phase with droplets already being the required size. An emulsifying agent of some sort is also generally required. This helps form emulsions by reducing the interfacial tension between the two phases, usually by acting as a surfactant and adsorbing to the

  6. Hotspot (geology) - Wikipedia

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

    Most hotspot volcanoes are basaltic (e.g., Hawaii, Tahiti). As a result, they are less explosive than subduction zone volcanoes, in which water is trapped under the overriding plate. Where hotspots occur in continental regions, basaltic magma rises through the continental crust, which melts to form rhyolites. These rhyolites can form violent ...

  7. Pyroclastic shield - Wikipedia

    en.wikipedia.org/wiki/Pyroclastic_shield

    Emi Koussi seen from International Space Station. In volcanology, a pyroclastic shield or ignimbrite shield is an uncommon type of shield volcano.Unlike most shield volcanoes, pyroclastic shields are formed mostly of pyroclastic and highly explosive eruptions rather than relatively fluid basaltic lava issuing from vents or fissures on the surface of the volcano. [1]

  8. Iceland volcano - live: ‘Significant’ eruption risk as ...

    www.aol.com/iceland-volcano-live-shock-images...

    Fears an Icelandic volcano will erupt remain high as magma spreads underground and huge cracks appear in the roads of a town most at risk.. Seismic activity in southwestern Iceland decreased in ...

  9. Billy Mitchell (volcano) - Wikipedia

    en.wikipedia.org/wiki/Billy_Mitchell_(volcano)

    It is a small pyroclastic shield truncated by a 2 km wide caldera filled by a crater lake. [2] It is named after Billy Mitchell, a 20th-century United States Army general who is regarded as the father of the United States Air Force. The last two major eruptions were in 1580 AD ± 20 years and about 1030 AD.