Hazard Earth: Tectonics Flashcards
What are convection currents?
Tectonic plates are continually moving on the asthenosphere because of hot rising currents called convection currents.
Rock is heated by the lower mantle and rises.
After is slowly begins to cool.
When it reaches the asthenosphere it turns sideways.
Eventually it cools and sinks.
What is the asthenosphere?
Asthenosphere is the denser part of the upper mantle
Temperature is high (Above 1300 degrees)
What is the lithosphere?
This includes the crust and the top layer of the upper mantle.
It is broken up into tectonic plates.
What are convergent plate boundaries?
Plates move towards each other
Oceanic plate meets continental plate
Oceanic is more dense so it sinks under the continental plate (subduction)
Leading to a composite volcano
What are divergent plate boundaries?
Divergent plate boundaries is when the plate moves apart
The magma rises to fill the gap / rift valley
Forming a shield volcano
What are conservative plate boundaries?
Plates slide past one another
Pressure builds along the boundary causing an earthquake
What type of lava is erupted from composite volcanoes?
Andesitic lava which is more viscous (thick and sticky)
What type of lava flows from shield volcanoes?
Basaltic lava is erupted from shield volcanoes
Less viscous.
How are hotspots formed?
They are formed by a plume of superheated rock rising very slowly through the mantle.
How do you measure the size of an earthquake?
The size of an earthquake is recorded using a seismometer.
The magnitude is then given according to the Richter scale
What is the focus of an Earthquake?
The point of rupture - where the earthquake happens underground.
What happens at a conservative plate boundary?
In a conservate plate boundary, convection currents cause the plates to slide past each other which can cause earthquakes due to built up pressure.
What are the differences of basaltic and andesitic lava?
Andesitic is more viscous so that is flows more slowly.
Basaltic is less viscous which is more runny and flows faster.
Name 4 Primary impacts of the Pinatubo eruption.
Pinatubo Eruption, Philippines, 1991:
847 people were killed in the main eruption, many by pyroclastic flows and ash falls.
The ash cloud caused the region to become cold and dark, hampering rescue operations.
5000 homes destroyed. As well as Typhoon Yunya struck at the same time.
Many people were displaced to shanty towns.
Name 3 Secondary impacts of the Pinatubo eruption.
As winds dispersed the gas cloud, global temperatures dropped 0.5 degrees.
Hundreds of people died from disease in evacuation camps.
Crops were destroyed as ash covered 800km of rice fields.
800000 farm animals were killed costing around 1.5billion pesos.