2.1 - EQs and Volcanoes Flashcards
Name the 2 types of volcano:
-shield
-strato (ie composite)
Describe and give an example of a shield volcano:
Mauna Kea
-very wide
-made of layers of basalt (cooled lava) with no ash layers
-thin lava (low viscosity)
Describe and give an example of a strato/composite volcano:
Mt Sinabung/Eyjafjallajökull
-very steep
-made of alternating basalt (cooled lava) and ash layers
-thicker layers than other volcanoes
-thick lava (high viscosity)
Describe the states a volcano can be in:
active - recent activity
dormant - no signs of activity but erupted in past 10,000 years
extinct - no chance of eruptions in future
Draw the internal structure of a general volcano:
draw
How are volcanic eruptions measured?
VEI, Volcanic Explosivity Index (log, goes from 1 to 8)
-factors in the amount of material ejected and how far it was dispersed
Define focus and epicentre:
-focus is exactly where the EQ originated from
-epicentre is the place on the ground directly above the focus
How are EQs measured?
Richter scale (log)
-measured by a seismometer
What is a tectonic plate?
-rock formed from lithosphere
-sits on top of the asthenosphere
-moved by convection currents in mantle
Describe the 2 types of tectonic plates:
continental (never subducts) - granite, thick but less dense
oceanic (subducts continental/less dense oceanic) - basalt, thin but more dense
Name the layers (and their properties) of the Earth:
-inner core (solid)
-outer core (liquid)
-mantle (plastic solid)
-asthenosphere (plastic solid)
-lithosphere (solid)
Describe and give an example of a constructive/divergent margin:
-plates move away
-volcanoes + small EQs
-N. America + Eurasian
Describe and give an example of a destructive/convergent margin:
-plates move towards
-volcanoes + largest EQs
-Nazca + S. American
Describe and give an example of a conservative/transform margin:
-plates move alongside (in different/same directions/speeds)
-EQs ONLY
-Pacific + N. American (San Andreas Fault)
What is a collision zone?
-2 continental plates at a destructive/convergent margin
-both are uplifted, no subduction