Week 6 Flashcards
What are shield volcanoes
- Low aspect ratio due to the fluidity of lava
- non-explosive eruptions are common
- broad and gentle slopes
e.g Mauna Loa
What is the magma type for shield volcanoes
- lavas that erupt in Hawaii are basaltic and contain about 50% silica
- They erupt at about 1200 degrees c
- very fluid and pasty
- effusive
- low silica
- low viscosity
What is the eruption type for shield volcanoes
Hawaiian type eruption
Hawaiian type eruption
- Lava is very fluid and hot
-Bubbles can expand and escape easily - relatively gentle
- low energy eruption
What are stratovolcanoes
- Higher aspect ratio because of lava viscosity
- Explosive and non explosive eruptions
- e.g Mt rainier: subduction zone volcano
What is the magma type for stratovolcanoes
- most lavas that erupt on volcanoes like mt st helens are closer to rhyolitic and are about 65 to 75% silica
- they erupt at about 900 degrees and are pretty stiff
- high viscosity
- high silica magma
What is the eruption type for stratovolcanoes
Plinian type eruption
Plinian type eruption
- Lava is sticky and cooler
- Bubbles can’t expand or escape easily
- Explosive
- starts with glowing pyroclastic flows
- forms lava domes with steep sides
Characteristics of Plinian type eruptions
- Ash and smoke column that can extend to stratosphere
- large amounts of pumice
- powerful gas blasts
- large amounts of magma erupted
- caldera formation possible
What are the three parts of a plinian column
- lower kilometer or two is the gas thrust region
- the next few kilometers is the convective region
- the upper part is the umbrella region
What is calderas (ultra-plinian)
- formed by very voluminous and explosive eruption
What are the key characteristics of calderas
- caldera formation
- large ejecta volumes
- high energy release
- massive plumes
- magma is rhyolitic
What are cinder cones
- smallest in size
- e.g sunset crater, flagstaff , Arizona
Comparison of shield and stratovolcanoes
Shield volcanoes are far larger than stratovolcanoes
What are igneous rocks
-formed from the crystallization of magma
-extrusive: fine grained and quickly cooled
-intrusive: coarse grained and slowly cooled