A shield volcano is broad with gently sloping sides.
A shield volcano
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 a very large, gently sloping mound composed mainly of basaltic lava flows. These volcanoes have a broad, dome-like shape and their eruptions are typically non-explosive. Examples include Mauna Loa in Hawaii and Galapagos Islands.
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.
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A shield volcano
Shield Volcano
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.
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.
A shield volcano is broad with gently sloping sides.
A shield volcano is a very large, gently sloping mound composed mainly of basaltic lava flows. These volcanoes have a broad, dome-like shape and their eruptions are typically non-explosive. Examples include Mauna Loa in Hawaii and Galapagos Islands.
shield volcano
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.
Shield volcanoes produce fluid basaltic lava due to their gently sloping sides and low viscosity magma. These eruptions tend to be non-explosive and create broad, flat volcanoes over time.
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One example of a volcano with a broad shaped gently sloping cone is called a shield volcano. These volcanoes are characterized by their low profile and large base, typically formed by the eruption of low-viscosity lava flows. An example of a shield volcano is Mauna Loa in Hawaii.
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.