Volcanoes Flashcards
What is a volcano?
- Any landform (on land or beneath the ocean) that releases lava, gas, or ashes, or has done so in the past
- Most occur at divergent or convergent plate boundaries
- Anomalous volcanism can sometimes occur in the middle of a plate (intraplate volcanism)
- Anomalous volcanoes may be the result of: hot magma rising from the core-mantle boundary or asteroid impacts
Good evidence that Hawaii is situated over a:
hotspot (islands in a row b/c plate is moving making holes as it moves = islands, tells us plate motion)
Magma (and lava) can be:
felsic, intermediate, or mafic
How does magma chemistry influence the nature of volcanic eruptions?
- Fewer covalent bonds between tetrahedra = thin, runny magma (mafic, low silica)
- More covalent bonds b/w tetrahedra = thick magma (felsic, high silica)
Mafic (basaltic) lava flows easily and erupts gently
- Low silica content
- Low viscosity (good at off-gassing (releasing gas) due to low viscosity)
- Low gas
Mafic (basaltic) lava flows easily and erupts gently
- Low silica content
- Low viscosity (good at off-gassing (releasing gas) due to low viscosity)
- Low gas
Mafic lava textures
Aa - rough, fragmented lava blocked called “clinker”
Pahoehoe - smooth, shiny, and ropy surface
Felsic magma tends to erupt catastrophically
- High silica content
- More viscous (resistant to flowing)
- High gas content (trapped between silica tetrahedra/crystals)
- Expanding gases fragment magma and rock, producing pyroclastic debris or tephra
Intermediate magma eruptions are less
explosive
Types of pyroclastic debris
- Ash
- Lapilli (tiny pieces of rock)
- Volcanic bombs (rocks size of fist)
- Volcanic block (house/car size)
- Welded tuff (compacted tiny rocks into rock)
- Pumice (vesicular)
H2O, CO2, SO2 are the most
abundant gases released during an explosion
What happens to the SO2 gas released during an explosion?
Sulphuric acid = acid rain
Volcanoes can be classified into 2 groups:
- Central vent volcanoes: central vent, summit crater
2. Large-scale volcanic terrains: no central vent, network of source material, extend over a large area
Types of central vent volcanoes
- Shield Volcanoes
- Stratovolcanoes
- Rhyolite Caldera Complexes
What is a shield volcano?
low silica, low gas magma originates in mantle, low viscosity creates broad gentle slopes