Basaltic lava.
ash cloud lava
Mafic, more commonly called Basaltic.
It is a shield volcano. Rifts typically open in the seaward flanks, with lava fountains and slow-moving lava flows to the ocean.
the Philippines volcano's form thin layer of cooled lava but not really cold like freezing
Lava. When the lava comes out of the volcano, gravity pulls the lava down the cone of the volcano, and depending the the viscocity of the lava, it forms a 'cone' or 'shield' as it cools. Thinner lava forms a shield volcano; thicker lava forms a steeper cone shape.
The amount of lava that comes out of a volcano can vary greatly depending on the eruption type and size of the volcano. In general, volcanoes can produce anywhere from a few cubic meters to millions of cubic meters of lava during an eruption. Some eruptions, such as those from shield volcanoes, can produce lava flows that extend for tens of kilometers.
Haleakala in Hawaii is a shield volcano. Shield volcanoes are characterized by their gentle sloping sides and widespread lava flows, resulting from low-viscosity magma. This type of volcano typically has relatively quiet eruptions.
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.
a shield volcano
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.
Kilauea is a shield volcano, which is a low-profile volcano shaped like a gently sloping shield. This type of volcano is characterized by its frequent eruptions of basaltic lava that flow long distances. Kilauea is one of the most active volcanoes on Earth.
A shield volcano is a type of volcano usually built almost entirely of fluid lava flows. Shield volcanos usually come from highly fluid lava that erupts, which travels farther than lava erupted from stratovolcanos.