A shield volcano is a type of volcano usually built almost entirely of fluid lava flows. Shield volcanos usually come from highly fluid lava that erupts, which travels farther than lava erupted from stratovolcanos.
Shield volcanoes -Hawaiian volcanoes -red lava -usually oozing strait out of science notes...
shield volcanoes have cinders that come out then land on it. that's what makes them bigger than cinder cone volcanoes.
Lava
shield volcanoes have cinders that come out then land on it. that's what makes them bigger than cinder cone volcanoes.
The Hawaiian islands are made of two types of volcanoes, shield volcanoes and cinder cone volcanoes. Shield volcanoes have broad bases with gentle slopes. Cinder cone volcanoes have steeper sides, are made from fragments of lava, and are usually located at the base of shield volcanoes.
Shield volcanoes usually produce effusive eruptions.
Pyroclastic materials from shield volcanoes generally consist of basaltic lava flows and minor amounts of tephra, such as ash and cinder. These materials are typically low in silica content and flow easily, producing gentle, broad slopes characteristic of shield volcanoes. Explosive eruptions from shield volcanoes are less common compared to stratovolcanoes due to the lower viscosity of the magma.
Shield volcanoes are wide because they are made to function as an island, much to the surprise of many scientists. These volcanoes are enormously big, usually spreading out over 300 miles.
There are three. From smallest to largest, they are: Cinder Cones, Composite Volcanoes (also called Strata Volcanoes), and then Shield Volcanoes.
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Because if you look at them from above, they look like a warrior's shield.
No, shield volcanoes are a specific type of volcano characterized by their broad, gentle slopes and low viscosity lava flows. "Volcano" is a general term that refers to any landform where volcanic activity occurs, encompassing a variety of volcano types such as shield, composite, and cinder cone volcanoes.