inside a shield volcano is a hot surface of mamga
Basaltic magma is hotter than andesitic magma. Basaltic magma typically has temperatures ranging from 1000°C to 1200°C, while andesitic magma has temperatures around 800°C to 1000°C.
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.
A volcano has magma,the molten rock that comes from the core of the earth.
Usually basaltic magma and hot hydrothermal fluids.
Yes!
basaltic
Basaltic
inside a shield volcano is a hot surface of mamga
Basaltic magma is hotter than andesitic magma. Basaltic magma typically has temperatures ranging from 1000°C to 1200°C, while andesitic magma has temperatures around 800°C to 1000°C.
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.
A volcano has magma,the molten rock that comes from the core of the earth.
Cinder cone volcanoes are formed by basaltic magma.
Basaltic magma is forced upward in a vent
Usually basaltic magma and hot hydrothermal fluids.
The Hawaiian Islands were formed by coalesing shield volcanoes. These volcanoes are exclusively composed of Basalt lava. The lava does not readily trap gas and flows very easily giving Mauna Loa, and Kiluaea there pronounced rounded shapes we see today.
rhyolitic mama is associated with explosive volcanism and is ejected (blown out of) a volcano rapidly. Basaltic lavas are released during effusive volcanism that is not explosive, such as hawaii where the lave "flows" into the ocean slowly. Basaltic lavas have a lower silica content as well.