A report on Volcano and Types of volcanic eruptions
Several types of volcanic eruptions—during which lava, tephra (ash, lapilli, volcanic bombs and volcanic blocks), and assorted gases are expelled from a volcanic vent or fissure—have been distinguished by volcanologists.
- Types of volcanic eruptionsThe material that is expelled in a volcanic eruption can be classified into three types:
- Volcano12 related topics with Alpha
Volcanic ash
2 linksVolcanic ash consists of fragments of rock, mineral crystals, and volcanic glass, created during volcanic eruptions and measuring less than 2 mm (0.079 inches) in diameter.
Lava
2 linksMolten or partially molten rock that has been expelled from the interior of a terrestrial planet (such as Earth) or a moon onto its surface.
Molten or partially molten rock that has been expelled from the interior of a terrestrial planet (such as Earth) or a moon onto its surface.
Lava may be erupted at a volcano or through a fracture in the crust, on land or underwater, usually at temperatures from 800 to 1200 C. The volcanic rock resulting from subsequent cooling is also often called lava.
Lava viscosity determines the kind of volcanic activity that takes place when the lava is erupted.
Lava dome
1 linksIn volcanology, a lava dome is a circular mound-shaped protrusion resulting from the slow extrusion of viscous lava from a volcano.
Around 6% of eruptions on Earth are lava dome forming.
Explosive eruption
1 linksIn volcanology, an explosive eruption is a volcanic eruption of the most violent type.
The sudden release of pressure causes the gases in the magma to suddenly froth and create volcanic ash and pumice, which is then ejected through the volcanic vent to create the eruption column commonly associated with explosive eruptions.
Eruption column
1 linksAn eruption column or eruption plume is a cloud of super-heated ash and tephra suspended in gases emitted during an explosive volcanic eruption.
If it does happen, then material reaching the bottom of the convective thrust region can no longer be adequately supported by convection and will fall under gravity, forming a pyroclastic flow or surge which can travel down the slopes of a volcano at speeds of over 100-200 kph.
Mayon
1 links28th
28th
The concave profile, a hyperbolic sine curve of the volcano is due to the balance between erosion and eruption, defined by the angle of repose of ash.
Nearly 40,000 people were evacuated from the 8 km danger zone on the southeast flank of the volcano.
Volcanology
0 linksVolcanology (also spelled vulcanology) is the study of volcanoes, lava, magma and related geological, geophysical and geochemical phenomena (volcanism).
Volcanologists frequently visit volcanoes, especially active ones, to observe volcanic eruptions, collect eruptive products including tephra (such as ash or pumice), rock and lava samples.
Magma chamber
0 linksLarge pool of liquid rock beneath the surface of the Earth.
Large pool of liquid rock beneath the surface of the Earth.
If the magma finds a path to the surface, then the result will be a volcanic eruption; consequently, many volcanoes are situated over magma chambers.
Volcanic gas
0 linksVolcanic gases are gases given off by active (or, at times, by dormant) volcanoes.
In explosive volcanic eruptions, the sudden release of gases from magma may cause rapid movements of the molten rock.
Hawaii hotspot
0 linksVolcanic hotspot located near the namesake Hawaiian Islands, in the northern Pacific Ocean.
Volcanic hotspot located near the namesake Hawaiian Islands, in the northern Pacific Ocean.
Four of these volcanoes are active, two are dormant; more than 123 are extinct, most now preserved as atolls or seamounts.
Volcanoes fall into several eruptive categories.