(PDF) Solution Manual For Viscous Fluid Flow by Frank white | Ali Maboudi - backroadsofamericanmusic.comA shield volcano is a type of volcano usually composed almost entirely of fluid lava flows. It is named for its low profile, resembling a warrior's shield lying on the ground. This is caused by the highly fluid low viscosity lava erupted, which travels farther than lava erupted from a stratovolcano , and results in the steady accumulation of broad sheets of lava, building up the shield volcano's distinctive form. Shield volcanoes are built by effusive eruptions , which flow out in all directions to create a shield like that of a warrior. Shield volcano itself is taken from the German term Schildvulkan. Shield volcanoes are distinguished from the three other major volcanic archetypes— stratovolcanoes , lava domes , and cinder cones —by their structural form, a consequence of their unique magmatic composition. Of these four forms shield volcanoes erupt the least viscous lavas: whereas stratovolcanoes and especially lava domes are the product of highly immotile flows and cinder cones are constructed by explosively eruptive tephra , shield volcanoes are the product of gentle effusive eruptions of highly fluid lavas that produce, over time, a broad, gently sloped eponymous "shield".
Viscous Fluid Flow 3rd
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San Diego State University. Rift zones are a prominent feature on these volcanoes, biscous account for their seemingly random volcanic structure. Retrieved 27 July. A lava lake in the caldera of Erta Alean active shield volcano in Ethiopia.