Geo - Tectonic plates Flashcards
(44 cards)
tectonic plates
- large slabs of solid rock that floats on the mantle
- constantly move
layers of the earth
- crust
- mantle
- outer core
- inner core
crust
- a layer of sand and rock
- 5-50km thick
mantle
- 2850km thick
- reaches about half distance to the center of the earth
- hot enough to liquify and become slow moving molten rock or magma
outer core
- mass of molten iron
- 2200km thick
- surround the solid inner core
inner core
- mass of iron
- 3870oC
- iron melts at this temp but immense pressure keeps it solid
- 2400km in diameter
movement of plates
convection currents
core heats rock in mantle => hot semi-molten rock becomes less dense than its surrounding and rises => semi-molten rock reaches the crust above => semi-molten rock spreads out carrying the plates above it (conveyor belt) => semi-molten rock cools and sinks back down to be re-heated
2 types of crusts
- oceanic crust
- continental crust
oceanic crust
- 6km (4 miles) thick
- 200 million years old
- made of basalt
- density: 3g/cm
continental crust
- 6 to 47 miles in thickness depending on location
- 1 to 4 billion years old
- made of granite
- density: 2.6g/cm
where do earthquakes happen
- margins / boundaries of tectonic plates
- pacific ring of fire
- hotspots (areas under the crust where magma is hotter than surrounding magma)
pacific ring of fire
- string of tectonic activity
- 90% of all earthquakes
- 75% of all active volcanoes on Earth
4 types of plates boundaries / margins
- constructive boundaries
- conservative boundaries
- destructive boundaries
- destructive boundaries - collision zones
constructive boundaries
plates are moving apart (convection currents) => magma rises from the mantle => magma erupts to surface of earth (accompanied by earthquakes) => magma reaches the surface and cools => solidifies to form new crust of igneous rock => repeated
- new rocks builds up to form a volcano
- constructive boundaries tend to be found under the sea, eg. mid Atlantic
conservative plate boundary
slide in opposite direction / same direction different speed => plates move and create friction and get stuck => pressure builds => pressure releases and sends out huge amounts of energy => causes earthquake
- earthquakes on conservative plates can be destructive bec occurs to earths surface
destructive boundaries
- oceanic plate and continental plate
o.p and c.p collide => o.p forced beneath the c.p (subduction) => results in ocean trench => plate sinks into mantle and melts into magma => pressure builds up beneath earth surface => magma escapes thru weaknesses in rock and rises up thru a composition volcano (stratovolcano)
- volcanic eruptions are often violent with steam, gas and ash
destructive boundaries - collision boundaries
2 continental plates collide => weigh the same so both are forced up => forms fold mountains
- can be very powerful and destructive
- landslides can be triggered by earthquakes
how are volcanoes formed
- rupture in the crust of the earths
- allows hot lava, volcanic ash and gases to escape from a magma chamber below the surface
- volcanoes are most found where tectonic plates are diverging / converging and most are underwater
main features of a volcanoes
- ash cloud
- pyroclastic flow
- crater
- main vent
- lava flow
- magma chamber
- secondary vent
- secondary cone
- volcanic bombs
2 types of volcanoes
- composite volcanoes
- shield volcanoes
composite volcanoes
- found at destructive plate margins
- steep sides
- made up of alternate layers of ash and lava
- doesn’t flow far, sticky acidic lava
- eruptions can be violent
shield volcanoes
- constructive plate margins
- wide base
- gentle sloping sides
- lava is runny, flows a long way, basic (opposite acidic)
- frequent eruptions
- not violent
why do people live near volcanoes
- geothermal energy
- tourism
- mining
- farming
geothermal energy - volcanoes
- energy created by using steam from underground
- steam drives turbines in stations
- energy for domestic and industrial use.
- cheap and environmentally friendly