Convectioncurrents in the mantle that drive plate movement
Alfred Wegener's theory of continental drift proposed that all continents were once part of a supercontinent called Pangea
Paleomagnetism theory shows patterns of the Earth's magnetic field on the seafloor, proving seafloor spreading
Subduction
Denser oceanic plate sinks under lighter continental plate, causing earthquakes and volcanoes
Gravitational sliding
Occurs at constructive margins, where rising magma creates a slight slope for the plates to slide apart
Slab pull
The dense, cold oceanic plate pulls itself into the mantle as it subducts
Constructive margin hazards
1. Shallow,low-magnitude earthquakes
2. Small, slow, effusive volcanoes with low gas content
Destructive margin hazards
1. Deep,high-magnitude earthquakes
2. Violent, explosive volcanoes
Plate boundary activities
Shallow earthquakes
Low magnitude earthquakes
Small, slow volcanoes
Low gas content volcanoes
High viscosity volcanoes
Destructive margin (oceanic and continental)
Large earthquakes up to 9 magnitude
Frequent, violent volcanic eruptions
Composite volcanoes with high gas and silica content
Destructive margin (oceanic and oceanic)
Frequent earthquakes but not as large as oceanic-continental
Violent volcanic eruptions
Creates volcanic islands
Collisional margin (continental and continental)
Largeshallow fault lines
High magnitude earthquakes
No volcanic eruptions
Conservative margin
High magnitudeshallow earthquakes
Very destructive
Primary waves (P waves)
Fastest seismic waves, cause least damage
Secondary waves (S waves)
Arrive after P waves, shake ground violently, cause damage
Love waves (L waves)
Arrive last, travel horizontally, cause significant damage including crustal fracturing
Crustalfracturing
Buckling and cracking of Earth's surface, primary earthquake hazard
Liquefaction
Soil loosening and water rising through cracks, secondary earthquake hazard
Landslides
Soil and sediment dislodging and falling downhill, secondary earthquake hazard
Pyroclasticflows
Dense, fast-moving, hot ash and gas clouds, primary volcanic hazard
Ashfall
Ash particles falling and damaging vegetation, buildings, water sources, primary volcanic hazard
Lavaflows
Extensive areas covered in destructive lava, primary volcanic hazard
Gas eruptions
Poisonous gases released, primary volcanic hazard
Lahars
Volcanic mudflows, secondary volcanic hazard
Jökulhlaups
Flooding from melting glaciers, secondary volcanic hazard
Tsunami
Large, fast-moving ocean waves caused by submarine earthquakes, volcanic eruptions, or landslides
Earthquake is when two plates move past one another, causing friction between rocks which builds up energy until it suddenly releases as an earthquake.
Natural hazard
A natural event that has the potential to harm people, property, and society
Natural disaster
The realization or the impact of the natural hazard itself, the harm that has occurred and the damage that has been done