Lecture 6// Volcanoes Flashcards
Chapter 6
3 types of magma (14)
Basaltic:
-Gently sloped shield volcanoes (ex. Mauna Loa, Hawaii).
-MORs
-Basalt plateaus like Columbia Plateau or Hawaiian Islands(fissure eruptions).
Generated at:
-Oceanic hot spots (stationary mantle plumes beneath oceanic crust).
-Fissure eruptions (flood basalts)
-MORs forming new oceanic lithosphere.
Andesitic:
- Composite volcanoes (ex. Mount St. Helens, Mount Rainier).
- Generates steep-sided composite volcanoes. (lava flows & pyroclastics)
Rhyolitic:
- Rhyolitic caldera complexes (ex. Yellowstone volcano)
- Generated at long-lived continental hot spots.
- Felsic magma pools within the lithosphere and adds hear, causing overlying crust to dome upwards and become stressed.
- Cracks form and extention occurs creating down-dropped blocks and an enormous central caldera.
Viscosity (1)
-The resistance to flow, and relates to the number of strong silicon-oxygen bonds that are forming.
Basaltic magma (3)
- Mafic with low viscosity = runny and not explosive.
- Erupts often when active with low gas content (0.5%-2%) with silica content of -50%.
- 2 types of lava: pahoehoe and aa.
- Temperature of -1200°C
Andesitic magma (4)
- Intermediate with intermediate viscosity = sticky and quite explosive (through erupt infrequently).
- 3%-4% gas content with silica content of -60%.
- Temperature of -1000°C
- Formed adjacent to subduction zones, creating volcanic arcs and island arcs.
Andesitic Example: Mount St. Helens (May 18th, 1980) (3)
- Landslide (and pyroclastic flow deposits up to 35 meters thick) and lateral blast followed by a vertical eruption ad lahar (mudflows).
- 57 fatalities who ignored the mandatory evacuation order, the eruption could be heard in the Lower Mainland of BC
- Since then erupting sticky rhyolitic lava that has built a lava dome within the crater.
Andesitic Example: Mt. Mazama (now Crater Lake), Oregon (aprrox. 7700 yrs ago) (3)
- The caldera formed from the eruption of Mazama (44x more powerful than Helens).
- Approx. 250 yrs of rain and snow accumulation for the caldera fill to its present-day lake level.
- The lake level is maintained by a balance between precipitation and evaporation.
Rhyolitic magma
- Felsic with high viscosity = very sticky and very explosive (through there tends to vast amounts of time between eruptions).
- Formed by hot spots beneath continents creating a rhyolite caldera complex.
- Contains Silica content of >70% and gas content of 4%-6%.
- Temperature of - 800°C
Rhyolitic Example (4)
-Yellowstone Supervolcano, Wyoming:
Eruption 1 (640,000 yrs ago):
-1000 km^3 of ash and pumice.
Eruption 2 (2.1 million yrs ago):
-2450 km^3 of ash and pumice.
(Mt. Helens eruption: 2.8 km^3 of material)