when magma is ejected out of the volcano it is called lava. When it cools and solidifies it is known as laneous rock.
Magma can be classified into basaltic or mafic, intermediate or andesitic and granitic or felsic.
Factors affecting volcanic eruption
Magma’s temperature
Chemical composition
Viscosity
Amount of dissolvedgases it contains
Viscosity
the property of the material‘s resistance to flow.
Basaltic magma or mafic
viscosity: low
temperature: 1000 to 1200C
Gas content: 1-2%
Explosiveness: least explosive
Location of formation: Both oceanic and continental
Andesitic or intermediate magma
Viscosity: Intermediate
temperature: 900-1000C
gas content: 3-4%
Silica content: 60%
explosiveness: intermediate
Location of formation: Continental margins associated with subduction zones.
Rhyolitic magma
Viscosity:high
Temperature: 760-900C
Gas content: 4-6
Silica content: 70%
Explosiveness: most explosive
Location of formation: continental crust
Icelandic
characterized by effusions of molten basaltic lave that flow from such long, parallel fissures. Such as outpourings often build lava plateaus.
hawaiian
Fluid lava flows from a volcano summit and radial fissures to form shield volcanoes. They are quite large and has gentle slopes.
Strombolian
Involve moderate burst of expanding gases that eject clot of incandescent lava in cyclical or nearly continuous small eruptions.
Because of such small frequent outburst, stromboli volcano, located on stromboli island off the northeast coast of italy, has been called the lighthouse of the mediterranean.
Vulcanian
named after the vulcano island near stromboli, generally involves moderate explosions of gas laden with volcanic ash.
This mixture forms dark, turbulent eruption clouds that rapidly ascend and expand in convoluted shapes.
Pelean
associated with explosive outburst that generate pyroclastic flow, dense mixtures of hot volcanic fragments and gas.
Named after for the destructive eruption of mount pelee on the caribbean island of martinique in 1902.
Plinian
intensely violent kind of volcanic eruption
Ash fall - pulverized rocks, sand, gritty and harsh glasses shoot out in the air by volcano.
Mud flow - mixture of water, molten rocks and debris flowing down from the side of volcano to the ground. It is called lahar.
Lava flow - streams of molten rocks and other fragmented materials emitted by erupting volcano.
Pyroclastic flow - fast moving hot mixtures of gas, ash, and molten rocks moving away from the volcano to the ground.
advantages of volcanic eruption: soil fertility, atmospheric cooling, land formation, tourism, raw material.