The broad, slightly dome-shaped volcanoes of Hawaii are known as shield volcanoes. They are characterized by their gentle slopes, which result from the eruption of low-viscosity basaltic lava that can flow over long distances. This type of volcano typically produces non-explosive eruptions, leading to the formation of wide, expansive landforms. Mauna Loa and Mauna Kea are prominent examples of shield volcanoes in Hawaii.
It is important to know the definition of new terms. The broad slightly dome-shaped volcanoes in Hawaii are Shield Volcanoes.
It is important to know the definition of new terms. The broad slightly dome-shaped volcanoes in Hawaii are Shield Volcanoes.
known as shield volcanoes. They are characterized by their gentle sloping sides and broad, flattened profiles. These volcanoes are formed by quiet eruptions of low-viscosity lava that travels long distances before solidifying, creating a shield-like shape.
a broad-domed volcano is formed by lava flows. the amount of times the volcano has erupted effects how broad the dome would be, because when the lava flows it wears away the dome of the volcano.
shield volcanoes.
Hawaii has shield volcanoes, which are broad, gently sloping volcanoes characterized by eruptions of relatively fluid lava that creates a wide base. These volcanoes are formed by repeated eruptions of low viscosity basaltic magma.
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.
This is called a shield volcano and an example would be Hawaii.
The main kinds of volcanoes according to shape are shield volcanoes, which have a low, broad profile; stratovolcanoes (or composite volcanoes), which are tall and conical with steep slopes; cinder cone volcanoes, which are small, steep-sided cones made of pyroclastic material; and calderas, which are large, basin-shaped volcanic depressions usually formed by the collapse of a magma chamber.
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.
Yes, some volcanoes have a shape called a shield volcano, which is broad and gently sloping with a dome-like structure. This shape is formed by the lava flows spreading outwards rather than erupting explosively. Examples of shield volcanoes include Mauna Loa in Hawaii and Mount Etna in Italy.
No, they're shield volcanoes. The lava in spatter cones is highly viscous whereas the lava that forms shield volcanoes (that you can see flowing in Hawaii) has a very low viscosity. Shield volcanoes are low profile, broad lumps; these are the Hawaiian islands.