types of volcanoes and hazards II Flashcards
the order basaltic, andesitic and rhyolitic shows increases is?
silica, viscosity, explosivity
what makes a volcano volatile?
water, various gasses
what are the properties of mafic lava (basalt)?
- low silica = low viscosity (runny)
- gases in magma can easily escape
- less explosive, lava flow dominates (add water, all bets off)
- mafic eruptions most common where magma has the most direct route to surface
- does not produce as much tephra or ash into the air
- lava is spouting !
what are the largest mountains on earth?
shield volcanoes
how are shield volcanoes made?
- basalt flows are fluid and build up one layer upon another layer over time
- may come out from flank eruptions
what are some properties of shield volcanoes?
- low topography
- predominantly build from mafic flows, but can have higher silica eruptions
what are the properties of cinder cone volcanoes?
- smaller than shield volcanoes
- formed by basaltic mafic lava that is very gas charged and rises very quickly
what are fissure eruptions?
- mafic lava not erupted through a central vent / hole
- cracks that open in the earth and lava fountains out of the cracks
- mid-ocean ridges is where the new crust is formed
- largest eruptions in earth’s history (flood basalts)
- can be extremely large and very intense
what are kimberlite eruptions?
- ultramafic
- large gas filled eruption that travels from mantle to surface in a very short period of time (rips a hole in the earth called mars)
what are the properties of felsic or intermediate lava?
- high silica = high viscosity (very thick)
- magma gasses cannot easily escape
- can produce very large eruptions
- large amounts of tephra and gas
where do stratovolcanoes / composite volcanoes form?
along subduction zones
what are some properties of stratovolcanoes?
- white vapor: water
- rock fragments and tephra is grey
- often snow on top of these mountains, meaning lava is immediately interacting with water, which generates large explosions
- produced by alternating layers of lava, tephra, and pyroclastic flow deposits
- classic cone volcanoes !!
- usually eruptions intermediate magma
- major eruptions can destroy
how do lava domes form?
- erupting lava is too thick to flow, causing it to pile up and rebuild stratovolcanoes
- lava reaches surface, very viscous, does not flow easily, pushes up, outside breaks and gets pushed around until whole crater is filled with lava domes, and then could potentially go back to forming a beautiful cone
how can lava domes collapse?
pyroclastic flows
what are calderas?
very large craters or gigantic depressions in the ground; can be very large