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.
Eyjafjallajökull Volcano produces basaltic and andesitic lava. The eruption in 2010 resulted in the release of both types of lava, creating a mix of volcanic products.
Eyjafjallajokull volcano in Iceland produces andesitic lava, which is a type of intermediate lava that is typically more viscous than basaltic lava. This can lead to explosive eruptions as gases get trapped within the molten rock before being released.
Eyjafjallajökull volcano produced a type of lava called basaltic lava. Basaltic lava is low in silica content, which makes it less viscous and allows it to flow more easily over the surface, leading to the formation of shield volcanoes like Eyjafjallajökull.
Mauna Kea is a shield volcano, which is a type of volcano with gentle sloping sides caused by basaltic lava flows. It is known as a dormant volcano, last erupting about 4,500 years ago.
The opposite of basaltic is rhyolitic. Basaltic rocks are formed from lava that is low in silica content, while rhyolitic rocks are formed from lava that is high in silica content.
it has aa lava, so it is not fluid like, but still basaltic.
Paricutin is a volcano in Michoacán, Mexico. The volcano is a cinder cone volcano. This means that the volcano is made up of layers of ash and stones that erupt out of the earth when the volcano erupts.
A shield volcano is most likely to form fluid lava because it is characterized by gentle sloping sides and eruptions of low-viscosity magma. This type of volcano typically produces basaltic lava that flows easily and spreads over large distances.
The San Cristobal volcano in Nicaragua primarily produces basaltic lava, which is low in silica content and flows easily. This type of lava typically results in effusive eruptions with lava flows that can travel long distances from the volcano. The lava from the San Cristobal volcano tends to be relatively fluid and forms shield volcanoes.
Eyjafjallajökull Volcano produces basaltic and andesitic lava. The eruption in 2010 resulted in the release of both types of lava, creating a mix of volcanic products.
The Thera volcano, also known as Santorini, has both basaltic and andesitic lava. Basaltic lava is more fluid and flows easily, while andesitic lava is thicker and can lead to explosive eruptions. Thera's volcanic activity has produced different types of lava throughout its history.
Kilauea generally produces lava flows and lava fountains. Its current activity has also involved the formation of lava lakes. All of the lava involved is basaltic.
Kilauea produces a'a and pahoehoe lava flows.
Basaltic lava.
Shield volcanoes will erupt basaltic lava. Cinder cones erupt basaltic lava or basaltic andesite lava. Stratovolcanoes often erupt andesite lava, but may erupt basaltic or rhyolitic lava and all intermediate types as well.
Lava plateaus are typically made from basaltic magma, which is low in silica content and flows easily when erupted from a volcano. This type of magma produces large, flat expanses of solidified lava called flood basalts, which create the extensive lava plateau formations often seen in volcanic regions.
Shield volcanoes are fed by basaltic magma.