Thursday, April 12, 2012

Political, Social and economic issues associated with a volcanic eruption

A sudden violence of volcanic eruptions causes catastrophe and devastation. Volcanic Eruptions have devastating impact of volcanic activity on nearby landscapes and communities. Many people are killed, and large numbers of people have to abandon their homes and lands forever. Even the whole world’s climate was changed for a while as a result of an eruption. Governments have to pay enormous amounts to rebuild cities and towns. People become more terrified and havoc fills surrounding towns.

Volcanic eruptions are one of Earth's most dramatic and violent agents of change. Not only can powerful explosive eruptions drastically alter land and water for tens of kilometers around a volcano, but tiny liquid droplets of sulfuric acid erupted into the stratosphere can change our planet's climate temporarily. Eruptions often force people living near volcanoes to abandon their land and homes, sometimes forever. Those living farther away are likely to avoid complete destruction, but their cities and towns, crops, industrial plants, transportation systems, and electrical grids can still be damaged by tephra, ash, lahars, and flooding.
Fortunately, volcanoes exhibit precursory unrest that if detected and analyzed in time allows eruptions to be anticipated and communities at risk to be forewarned with reliable information in sufficient time to implement response plans and mitigation measures.

Wednesday, April 11, 2012

Volcano Diagram

The Types of Volcanoes


Cinder cones



Cinder cones are the simplest type of volcano. They are built from particles and blobs of congealed lava ejected from a single vent. As the gas-charged lava is blown violently into the air, it breaks into small fragments that solidify and fall as cinders around the vent to form a circular or oval cone. Most cinder cones have a bowl-shaped crater at the summit and rarely rise more than a thousand feet or so above their surroundings. Cinder cones are numerous in western North America as well as throughout other volcanic terrains of the world.

Composite volcanoes

Some of the Earth's grandest mountains are composite volcanoes--sometimes called stratovolcanoes. They are typically steep-sided, symmetrical cones of large dimension built of alternating layers of lava flows, volcanic ash, cinders, blocks, and bombs and may rise as much as 8,000 feet above their bases. Some of the most conspicuous and beautiful mountains in the world are composite volcanoes


Shield Volcanoes


Shield volcanoes, the third type of volcano, are built almost entirely of fluid lava flows. Flow after flow pours out in all directions from a central summit vent, or group of vents, building a broad, gently sloping cone of flat, domical shape, with a profile much like that of a warrior's shield. They are built up slowly by the accretion of thousands of highly fluid lava flows called basalt lava that spread widely over great distances, and then cool as thin, gently dipping sheets. Lavas also commonly erupt from vents along fractures (rift zones) that develop on the flanks of the cone. Some of the largest volcanoes in the world are shield volcanoes

Mount St. Helens

Elevation: 2,550m / 8,364ft

Location: 46°11’N 122°11’W

Last Eruption: 2008

Country: USA


Volcano Type: Composite Volcano

Mount Rainier

Elevation: 4,392m / 14,411ft

Location: 46°51’N 121°45’W

Last Eruption: 1854

Country: USA


Volcano Type: Cinder Cone

Mount Baker

Elevation: 3,285m / 10,778ft

Location: 48°46’N 121°48’W

Last Eruption: 1880

Country: USA


Volcano Type: Composite Volcano

Mount Adams

Elevation: 3,743m / 12,281ft

Location: 46°12’N 121°29’W

Last Eruption: 500 BC ± 1000 years

Country: USA


Volcano Type: Cinder Cone