Tectonic theory explains that Earth's outer shell (lithosphere) is divided into plates that glide over the Earth's rocky inner layer above the soft core (mantle)
Plate boundaries:
Destructive plate boundaries occur when continental and oceanic plates meet, potentially forming a collision zone when two continental plates meet
Constructive boundaries happen when continental or oceanic plates move apart, allowing magma to rise between the plates
Conservative boundaries are when two plates slide alongside each other
sometimes secondary vents appear during eruptions
The 3 P's of volcanoes:
predict, estimate when an eruption may happen
prepare, get ready for eruption
protect, getting buildings ready
Hazards and responses to volcanic eruptions:
Pyroclastic flows are the most dangerous kind of eruption
Methods for dealing with volcanic eruptions include spraying lava with water, making earth barriers to channel lava, dropping concrete blocks via helicopter, ariel bombing of lava tubes with dynamite, and evacuating people from affected areas
Iceland's geothermal energy process:
Stage 1: cold water gets pumped under the ground
Stage 2: water passes near the magma causing it to heat up
Stage 3: the water vaporizes, turning into steam, which is then pumped around and turned into energy
Earthquakes are sudden violent shaking of the ground due to movement within the crust.
Parts of a volcano:
crater = hollow space at the top of a volcano
main vent = where the magma rises through
magma chamber = where the magma comes from
volcanic bombs, ash and gases = ejected by eruption
secondary vent = sometimes appear during eruption
why live near volcanoes?
lots of resources, soil, mud, tourism, cool to see, geothermal enrgy, cheaper, to study them, scientific research, quiet, water, views, agriculture, the soil is more nutritious and historical
Earthquakes:
seismic waves = energy that is released during an earthquake
focus = the place where the earthquake originally occurs deep inside the earth
epicentre = the place on the earths surface which is the shortest distance directly above the focus. It is the place where the maximum intensity of the earthquake is left.