Effusive eruption
Encyclopedia
An effusive eruption is a volcanic eruption characterized by the outpouring of lava
onto the ground (as opposed to the violent fragmentation of magma
by explosive eruption
s). Lava flows generated by effusive eruptions vary in shape, thickness, length, and width depending on the type of lava erupted, discharge, slope of the ground over which the lava travels, and duration of eruption.
For example, basalt
lava may become [[ʻaʻā]] or pāhoehoe. Andesite
lava typically forms blocky lava flows, and dacite
lava flows often form steep-sided mounds called lava domes due to their viscosity
.
Effusive eruptions occur when hot, (1200°C) runny magmas reach the surface of the Earth's crust. Dissolved gases escape easily as the magma erupts, forming lava that flows downhill quite quickly and easily. Effusive eruptions build up gently-sloping Volcanoes like the ones in Hawaii.
Lava
Lava refers both to molten rock expelled by a volcano during an eruption and the resulting rock after solidification and cooling. This molten rock is formed in the interior of some planets, including Earth, and some of their satellites. When first erupted from a volcanic vent, lava is a liquid at...
onto the ground (as opposed to the violent fragmentation of magma
Magma
Magma is a mixture of molten rock, volatiles and solids that is found beneath the surface of the Earth, and is expected to exist on other terrestrial planets. Besides molten rock, magma may also contain suspended crystals and dissolved gas and sometimes also gas bubbles. Magma often collects in...
by explosive eruption
Explosive eruption
An explosive eruption is a volcanic term to describe a violent, explosive type of eruption. Mount St. Helens in 1980 was an example. Such an eruption is driven by gas accumulating under great pressure. Driven by hot rising magma, it interacts with ground water until the pressure increases to the...
s). Lava flows generated by effusive eruptions vary in shape, thickness, length, and width depending on the type of lava erupted, discharge, slope of the ground over which the lava travels, and duration of eruption.
For example, basalt
Basalt
Basalt is a common extrusive volcanic rock. It is usually grey to black and fine-grained due to rapid cooling of lava at the surface of a planet. It may be porphyritic containing larger crystals in a fine matrix, or vesicular, or frothy scoria. Unweathered basalt is black or grey...
lava may become [[ʻaʻā]] or pāhoehoe. Andesite
Andesite
Andesite is an extrusive igneous, volcanic rock, of intermediate composition, with aphanitic to porphyritic texture. In a general sense, it is the intermediate type between basalt and dacite. The mineral assemblage is typically dominated by plagioclase plus pyroxene and/or hornblende. Magnetite,...
lava typically forms blocky lava flows, and dacite
Dacite
Dacite is an igneous, volcanic rock. It has an aphanitic to porphyritic texture and is intermediate in composition between andesite and rhyolite. The relative proportions of feldspars and quartz in dacite, and in many other volcanic rocks, are illustrated in the QAPF diagram...
lava flows often form steep-sided mounds called lava domes due to their viscosity
Viscosity
Viscosity is a measure of the resistance of a fluid which is being deformed by either shear or tensile stress. In everyday terms , viscosity is "thickness" or "internal friction". Thus, water is "thin", having a lower viscosity, while honey is "thick", having a higher viscosity...
.
Effusive eruptions occur when hot, (1200°C) runny magmas reach the surface of the Earth's crust. Dissolved gases escape easily as the magma erupts, forming lava that flows downhill quite quickly and easily. Effusive eruptions build up gently-sloping Volcanoes like the ones in Hawaii.