A shield volcano
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A shield volcano
Shield volcanoes. They are characterized by their broad, low-profile shape that resembles a warrior's shield. They are formed by the high volume of low-viscosity basaltic lava that flows easily and spreads out over a large area, creating the gentle slopes.
A large volcano with gently sloping sides is called a shield volcano. These volcanoes are primarily built up by the flow of low-viscosity basaltic lava, which can travel long distances, resulting in their broad, shield-like shape. Shield volcanoes typically produce less explosive eruptions compared to stratovolcanoes. Examples include Mauna Loa and Kilauea in Hawaii.
A volcano with gently sloping sides is called a shield volcano. These types of volcanoes are primarily built up by the flow of low-viscosity basaltic lava, which can travel long distances. As a result, shield volcanoes tend to have broad, dome-shaped profiles. Examples include Mauna Loa in Hawaii and Kilauea.
A shield volcano is broad with gently sloping sides.
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shield volcano
A shield volcano
shield
A shield volcano is a domed, broad volcano that has gently sloping sides. They are usually built from the eruption of fluid lava.
A+ answer : shield volcano
Shield volcanoes. They are characterized by their broad, low-profile shape that resembles a warrior's shield. They are formed by the high volume of low-viscosity basaltic lava that flows easily and spreads out over a large area, creating the gentle slopes.
A volcanic mountain with a wide base and gently sloping sides is called a shield volcano. These types of volcanoes are characterized by their low profile and are formed by the slow and steady accumulation of lava flows. They can be found in areas with hot spots or along divergent plate boundaries.
A large volcano with gently sloping sides is called a shield volcano. These volcanoes are primarily built up by the flow of low-viscosity basaltic lava, which can travel long distances, resulting in their broad, shield-like shape. Shield volcanoes typically produce less explosive eruptions compared to stratovolcanoes. Examples include Mauna Loa and Kilauea in Hawaii.
Actually, a volcanic mountain with gently sloping sides made of basalt lava flows is typically called a shield volcano, not a cinder cone. Cinder cones are typically smaller, steeper-sided volcanoes formed from ejected rock fragments.
Actually, a volcanic mountain with a wide base and gently sloping sides is called a shield volcano. Shield volcanoes are typically formed by low-viscosity lava flows that spread out in layers, creating a broad, shield-like shape.