Volcanoes Flashcards
What is a volcano
A landmass that produces lava, gas, ash or has done so in the past
Where do volcanos form
Convergent boundaries, divergent boundaries, and hot spots
What happens to the viscosity of the magma as it goes from mafic to felsic and why
As magma becomes more felsic the viscosity increases because there are more covalent bonds causing a greater resistance to flow
Does mafic magma or felsic magma have more violent eruptions and why
Felsic has far more violent eruptions because the viscosity doesn’t allow gas to escape slowly, so it can build up lots of gas pressure before finally releasing
What are the mafic lava textures and describe each
Aa is a very rough and ragged formation and Pahoehoe is very smooth and shiny surface
What are the seven things that are produced by a felsic volcanic eruption
Tephra (fine rock powder that settles, ash, lapilli, volcanic bombs, volcanic block, weld tuff, and pumice
What three gasses are most abundantly produced during an eruption
H2O, CO2, and SO2
What two groups that classify volcanoes called
Central vent volcanoes and large-scale volcanic terrains
What are the types of central vent volcanoes
Shield volcano, stratovolcano, and rhyolite caldera complexes
What is common in the composition of magmas found in shield volcanos and how does that affect the structure of the volcano
The magma is low in silica content meaning eruptions are less violent causing broad and gentle slopes down the side of the volcano
Is there a common composition of magmas found in stratovolcanoes
No, stratovolcanoes vary from mafic all the way to felsic in their magmas composition but have to have some kind of alternating layer between the different compositions
What is common in the composition of magmas found in rhyolite caldera complexes and how does that affect the structure of the volcano
The magma is high in silica contents meaning eruptions are more violent causing the ground to collapse after an eruption because the built-up pressure from the gas is released
What do rhyolite caldera complexes look like before and after an eruption
A rhyolite caldera complex often looks like a number of vents at the earth’s surface with no structure around it and after it erupts it seems like an “inverse volcano” because it is sunk into the ground because all the gas and some magma comes out