Lahar
a mudflow associated with a volcanic eruption.
Effusive and Explosive
The explosive nature of a volcano is controlled by the amount of silicon in the silicate mineral in the rocks.
The higher silicon content in felsic minerals, such as quartz, produces a high viscosity lava when they melt.
This thick viscous lava traps a lot of gas (mostly water) thereby creating high, potentially explosive pressures
As time went by, they became convinced the eruption was genuine and that a major catastrophic event was imminent.
What evidence was there to support this conclusion?
Cascade volcanoes, like Mt. St. Helens often emit gases, especially in late winter and early spring.
Harmonic tremors small earthquakes around the magma chamber also occur, so this wasn’t uncommon.
As time passed however, there were more and more signs that a major eruption was likely.
What eventually convinced authorities that an eruption could be expected was ash on the snow around the vent on top of the volcano
This confirmed a direct link between the surface and the magma chamber and that pressures inside the volcano had reached dangerous levels.
These are large, effusive outpourings of mafic lava that cover a very large area of the Earth’s surface.
These eruptions can last thousands of years.
While this outpouring of lava is catastrophic for the immediate area there is a much greater hazard.
The sustained release of volcanic gases, in particular CO2, can change the atmosphere and oceans.
Increased CO2 in the atmosphere will raise air temperatures and the lowering pH (acidity) of ocean water.
The formation of the Siberian Traps, huge flood basalt deposits at the end of the Permian Period, is thought to be the cause of the largest mass extinction on Earth.
Mt. Vesuvius is a a stratovolcano with a long, recorded history of very violent eruptions.
Naples is a large, old city surrounding much of this volcano. Exposure is high. Sensitivity is mixed. So vulnerability is higher than it should be.
What makes Naples worse, like it does for other older European cities, is the infrastructure.
Old, less stable buildings, lack of streets, narrow streets and a lot of people crowded into a small area make evacuation before a catastrophe and response during one more difficult.
Formed beneath the ice after the glacier has formed.
OR
Formed before glacation and have since been covered in ice.
force of the eruption
+
large flood of water that may result if the glacier melts
(may result in a lahar, a mudflow associated with a volcanic eruption.)
Example: Mt. St. Helens Type of Plate: Continental Type of rock: Felsic Lava Viscosity: High Silicon Content: Higher Amount of trapped gas: High Frequency of eruption: Rare Duration of eruption: Short
Example: Hawaii Type of Plate: Oceanic Type of rock: Mafic Lava Viscosity: Low Silicon Content: Lower Amount of trapped gas: Low Frequency of eruption: Common Duration of eruption: Long
Volcano defining factors (mark’s table)
Example Type of Plate Type of Rock Lava Viscosity Silicon Content Amount of trapped gas Frequency of eruption Duration of eruption
Tuya volcano
A volcano in a mountainous area that is partially or completely enclosed by glacial ice.
Siberian Traps.
Huge flood basalt deposits at the end of the Permian Period.
Thought to be the cause of the largest mass extinction on Earth.