Wednesday, May 30, 2007

Laying Floor Tile Of Different Thickness

Parties


-CRATER: The exit of materials from the volcano.
-FIRE: It's where you pass through the magma
-CONE VOLCANIC: Part of the volcano formed by the ejected material.
-magma chamber: It's where magma accumulates before leaving
-FUMAROLAS: Are gas emissions from the lava in the crater.
-Solfatara: emissions are water vapor and hydrogen sulfide.
-SKUNKS: These vents that emit cold carbon dioxide-GEYSERS
: Small volcanoes steam of boiling water
When the magma inside the earth to be accumulated in the magma chambers, the pressure increases until it becomes so strong that you need to leave. Then makes its way down the chimney to the surface and that is when the volcanic eruption occurs. As the magma rises to the surface, it becomes lava down the slopes of the volcanic cone forming large sheets or castings. If the lava is not very liquid quickly solidifies and coats are very short that sometimes obstruct the crater until another explosion occurs where it breaks or is accumulated over crater forming needles that can reach hundreds of meters high. If the pressure inside of a volcano is not high enough for the magma to surface, this may be asleep or off. Is said to be asleep when he can erupt again and off when not expected to erupt. The volcanic eruptions are not always in the same way. Sometimes they are quiet and peaceful and some violent and big explosions. This depends on the composition of the magma and the amount of gases that accompany it.

0 comments:

Post a Comment