The earths crust is broken into large pieces called tectonic plates
Continental Plates
Thicker, older and lighter, they do not subduct
Oceanic Plates
Thinner, younger and denser so they can subduct under another plate
Plate boundaries/ margins are the same thing. They describe the location Earth where 2 tectonic plates meet or sit next to each other
Tectonic plates move according to the movement below in the mantle
Convection currents are caused by heat from the core which causes hot rock to rise upwards and cool down as it moves away from the core.
Some plates are pushed apart and some are being dragged together
In convection, hot things that are less dense and have more energy rise
Constructive Plate Margins
Plates move apart
Convection currents diverge, causing a gap to form between the plates
Magma rises up to fill the gap between the 2 plates
Conservative Plate Boundaries
Plates slide past each other
Friction and pressure build up
They slip past each other, may resulting in the ground to shake (earthquake)
Destructive Plate Boundaries
Oceanic plate slides under the continental plate (subduction)
Pressure builds up
May result in earthquakes
Volcano
An opening in the Earths crust that is formed when magma rises from inside the Earth and erupts through the Earths crust. Can be formed at destructive and constructive plate boundaries
Hotspots happen at the Earths crust over hotter parts of the earths mantle
Destructive Plate Margins
Highlyexplosive
Producealotofgas
Producealotoflava
Volcanic Eruption
Lava
Gases-sulphur
Ash
Pyroclasticflows
Pyroclasticflows
Currents of hotash, lava and gas that can move downhill at speeds up to 500km/h during an eruption
PrimaryEffects: Lava, ash, gas, suffocation, crop and livestock deaths, humandeaths and damagedbuildings