earthquakes and volcanoes Flashcards
What are earthquakes
Earthquakes are a sudden violent shaking of the ground, as a result of movements within the Earth’s crust or volcanic action
What are the causes of earthquakes
Earthquakes are caused by all types of plate boundaries
Sometimes, because of friction, plates try to move and become stuck. Pressure builds up because the plates are still trying to move. When the pressure is released, it sends out huge amounts of energy causing the Earth’s surface to shake violently.
What is the focus
The point inside the Earth’s crust where the earthquake originates from is known as the focus.
What are seismic waves
The earthquake’s energy is released in seismic waves and they spread out from the focus.
what is the epicentre
The seismic waves are most powerful at the epicentre.
The epicentre is the point on the Earth’s surface directly above the focus.
What are the factors affecting level of damage earthquake
- Distance from the epicentre - the effects of an earthquake are more severe at its centre.
- The higher on the Richter scale, the more severe the earthquake is.
- Level of development (MEDC or LEDC) - MEDCs are more likely to have the resources and technology for monitoring, prediction and response.
- Population density (rural or urban area). The more densely populated an area, the more likely there are to be deaths and casualties.
- Communication - accessibility for rescue teams.
- Time of day influences whether people are in their homes, at work or travelling. A severe earthquake at rush hour in a densely populated urban area could have devastating effects.
- The time of year and climate will influence survival rates and the rate at which disease can spread.
how to measure earthquakes
The power of an earthquake is measured using a seismometer. A seismometer detects the vibrations caused by an earthquake. It plots these vibrations on a seismograph.
We use the Richter Scale to categorize the intensity of different magnitudes
What are the 4 types of plate boundaries
Constructive
Destructive
Conservative
Collision
What are constructive plate boundaries + characteristics
At constructive boundaries two plates are moving apart. Molten magma rises to the surface, cools and solidifies to form new oceanic crust.
The magma is hot and runny (non viscous) so volcanic eruptions are gentle and non explosive
Destructive plate boundaries + characteristics
Destructive boundaries are when dense (heavy) oceanic crust are subducted beneath less dense continental crust.
Intense heat and pressure in the subduction zone creates molten magma which rises to the surface to form explosive volcanoes.
Powerful earthquakes also occur.
Conservative plate boundaries + characteristics
At conservative boundaries two plates are grinding slowly past each other horizontally.
There is no volcanic activity but powerful earthquakes occur.
Collision plate boundaries + characteristics
Collision margins are where two continental plates collide. The continental crust is too thick to allow subduction.
Instead sedimentary rock is forced upwards to form huge mountain ranges like the Himalayas.
There is no volcanic activity.
What are hotspots
Hot spots cause volcanic activity away from plate margins. As the plate moves over the stationary hot spot, a series of volcanoes are formed. The most famous example is the Hawaiian Islands.
How are fold mountains formed
by Collison plate boundaries
What is the crust
a layer of sand and rock varying from 5-50 km thick
What is the mantle
A rock layer about 2850 km thick that reaches about half the distance to the centre of the earth. Parts of this layer become hot enough to liquify and become slow moving molten rock or magma
Outer core
a mass of molten iron about 2200 km thick that surrounds the solid inner core
Inner core
a mass of iron with a temperature of 3870. Normally iron would melt at this temperature, but its immense pressure keeps it solid. Its 2400 km in diamaeter