Unit 2 - The natural environment Flashcards
Structure of the earth
- Crust - 100km thick - oceanic & continental crust
- upper mantle - 400km deep 100-1300˚C
- Lower mantle - 700km deep 200-2500˚C
- Outer core - 2900km deep 2500-3000˚C
- Inner core - 5150km deep 4000-5000˚C
Oceanic crust
Thin but very dense
Continental crust
Thick but less dense
4 types of plate boundaries
- Divergent
- Convergent
- Collision
- Transform
Divergent plate boundary
- Two plates move apart
- Magma rises and fills gap - erupts as Laval and solidifies to make new crust
- Also known as a constructive boundary
- Example: Mid-Atlantic ridge - North American and Eurasian plate
Convergent plate boundary
- Plates move towards each other
- When continental and oceanic plates come together - denser oceanic sinks and continental rises - forms subduction zone
- Friction between plates and the mantle melts oceanic crust
- Magma rises and erupts as a volcano
- Also known as a destructive boundary
- volcanoes and earthquakes occur
- Example: Nazca plate subjects under South American plate
Collision plate boundary
- When two continental plates of similar densities move towards each other
- Crust pushed up and forms fold mountains
- Only earthquakes occur
- Example: Himalayas growing with Indian & Eurasian plate
Transform plate boundary
- Plates move pas each other in opposite directions or in same direction at different speeds
- Also known as a conservative boundary
- Volcanoes and earthquakes occur
- Example: San Andreas Fault - USA
Convection currents in the mantle
Hotter less dense material due to outer core rises and colder denser material sinks
Cause of earthquakes
- Convection currents cause movement of plates
- Plates can get stuck and build up pressure
- When pressure is too high the boundary suddenly moves
- All stored energy is released in seismic waves
- Waves move through the crust and cause shaking
Focus
The point underground where the release of seismic energy happens
Epicentre
The point above the focus on the surface of the crust
Scales of earthquake magnitude
- Richter scale - energy released
- Moment magnitude scale - distance the fault line has moves
- Mercalli scale - visible damage
Causes of volcanoes
- Formed when ruptures on the crust allow lava, volcanic ash and hot gases to erupt
Features of volcanoes
- Magma chamber
- Layers of ash and lava
- vent
- Crater
- Lava flow
- Ash cloud
Places where volcanoes occur
- Divergent plate boundaries
- Convergent plate boundaries
- Hot-spots - areas of super-heated plumes of magma under the crust
Active volcano
Erupts regularly
Dormant volcano
Potential to become active, gap of eruptions from less than a year to over 10000
Extinct volcano
No activity detected in human history - will not erupt again
4 types of Volcanoes
- Stratovolcano/composite
- Shield volcano
- Cinder cone
- Fissure vent
Stratovolcano/composite
- Forms at convergent boundaries
- Erupts violently and unpredictably
- Lava is thick and slow moving
- Steep sides and classic cone shape
Shield volcanoes
- Forms at divergent boundaries and hot-spots
- Eruptions are less explosive and more predictable
- Lava is runny and flows for long distances
- Gently sloping sides
Cinder cone
- Hot lava and ash blasts into the air
- Substances cool, fall and stick to the cone’s slope as opposed to flowing
Fissure vent
- Linear volcanic vent where lava erupts
- Often few meters wide and kilometers long