The Hawaiian Islands were formed from this type of volcano.
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.
Massive gently sloping volcanoes built of successive basaltic lava flows are called shield volcanoes. Examples of shield volcanoes include Mauna Loa in Hawaii and Mount Etna in Italy. These volcanoes are characterized by their broad, low-profile shape and the relatively peaceful eruptions of fluid lava.
Hawaiian volcanoes are shield volcanoes because they are characterized by their broad, gently sloping shape resembling a warrior's shield. This is due to the low viscosity of the basaltic lava they erupt, allowing it to flow easily and travel long distances before solidifying. As a result, shield volcanoes tend to build up gradually over time with successive eruptions, creating their distinctive shape.
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
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.
Massive gently sloping volcanoes built of successive basaltic lava flows are called shield volcanoes. Examples of shield volcanoes include Mauna Loa in Hawaii and Mount Etna in Italy. These volcanoes are characterized by their broad, low-profile shape and the relatively peaceful eruptions of fluid lava.
A shield volcano is broad with gently sloping sides.
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.
Hawaiian volcanoes are shield volcanoes because they are characterized by their broad, gently sloping shape resembling a warrior's shield. This is due to the low viscosity of the basaltic lava they erupt, allowing it to flow easily and travel long distances before solidifying. As a result, shield volcanoes tend to build up gradually over time with successive eruptions, creating their distinctive shape.
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.
Both shield volcanoes and cinder cones erupt low-viscosity basaltic lava and have eruptions that are only mildly explosive if at all.Cinder cones are small, steep-sloped volcanoes composed primarily of a chunky variety of basalt called scoria.Shield volcanoes are large, gently sloping volcanoes composed primarily of layers of lava flows.
Mafic, usually basaltic lava.
Shield volcanoes are primarily composed of basaltic rock, which is a type of volcanic rock that is low in silica content and high in iron and magnesium. This type of rock creates gently sloping shield volcanoes due to its low viscosity and ability to flow easily during eruptions.
Of the common types of lava, basaltic lava is the most fluid. However, one volcano, Ol Doinyo Lengai in Africa erupts unique carbonatite lava, which is extremely fluid. This lava appears to be closer in viscosity to water than basaltic lava.
not a clue!