continental crust
old (1500 million+ y.o.), less dense, cannot sink, cannot be renewed/destroyed, thicker than oceanic (30-50km)
oceanic crust
new (less then 200 y.o.), denser, can sink, can be renewed/destroyed, thinner (5-10km)
two plates are moving towards each other; an oceanic plate meets a continental plate, the denser oceanic plate subducts into the mantle and destroyed creating gas-rich magma. volcanoes and ocean trenches occur here.
two continental plates meet, ground folds upwards creating fold mountains
geothermal energy
ash (to fertilise soil)
tourism
danger
damage to property
difficulty for businesses to operate
damage to habitats/landscapes
volcanic land and ash provides fertile land increasing crop yields for farmers
tourism > money > benefits economy
geothermal energy -> cheaper electricity for locals
minerals in lava make money (diamonds)
gas pollution
uncertain living conditions/evacuation
losing jobs/ no livelihood
no insurance for damage
high vulnerability
homelessness
measuring gas detection released as magma rises
remote sensing detects heat and changes to shape of volcano by satellites
ground deformation shows the changes to the shape of the volcano- measured using laser beams
geographical measurements detect changes in gravity as magma rises to the surface
Seismic Gap Theory
detecting gases Thoron and Boron shows the plates are reacting
EARTHQUAKE PROOF BUILDINGS:
reinforced concrete and steel walls reduce movement
open evacuation areas
shock absorbers to absorb ground shaking
automatic shutters prevents broken glass falling
triangular shaped buildings
hazard maps
training people on earthquake drills or education through TV/RADIO
emergency kits (first aid, blankets, water, tinned food)