Its to do with the viscosity of the lava, the thicker (more viscous) the lava the slower and less far it will travel making a shield volcano. This happens on a constructive plate boundary. on a destructive plate boundary the lava is less viscous and runs further making a conical shaped volcano
Shield Volcanoes - Wide base found at constructive plate margins Composite Volcanoes - Steeper Sides found at Destructive (subduction) margins
Shield Volcanoes - Wide base found at constructive plate margins Composite Volcanoes - Steeper Sides found at Destructive (subduction) margins
It is a shield volcano, as it occurs on a divergent pllate boundary (constructive boundary)
Shield volcanoes are from by divergent boundary's.
The Appalachian mountain.
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hot spots and convergent boundaries
No, Mauna Loa is not located on a transform boundary. It is a shield volcano located on the Big Island of Hawaii and is primarily formed by hotspot volcanism, where magma rises from deep within the Earth's mantle.
Constructive volcanoes, also known as shield volcanoes, are characterized by their broad, gently sloping sides and low viscosity lava flows. These volcanoes are typically formed from multiple eruptions of basaltic lava, which spreads out in thin layers to create a gradual and shield-like shape. Constructive volcanoes are associated with effusive eruptions, where lava flows steadily and continuously.
The Appalachian Mountains form a boundary with the Canadian Shield. The Canadian Shield is a large geological formation covering much of eastern and northern Canada, while the Appalachian Mountains run along the eastern coast of North America, from Alabama in the U.S. to Newfoundland in Canada.
Shield volcanoes usually produce effusive eruptions.
Eruptions at shield volcanoes are almost always non-explosive.