Structure of the Lithosphere, Plate Tectonics and Rock Formation Flashcards
Crust
The outer layer with a thickness of 70 km.
Two types of crust: oceanic and continental.
Mantle
This is a very thick layer extending 2900 km. Mostly dense and solid although there is a densely thin-semi-liquid layer in the upper mantle.
Core
Can be divided into the liquid outer core and an iron-rich solid inner core. Temperatures here reach 5500 C. The centre of the Earth’s core is 4600 km below the surface.
What is the earths crust made up of?
Several large sections called Plates about 100 km thick.
Where are these plates located?
The crust and the upper part mantle. The plates rest on the semi-liquid layer in the upper mantle which helps them to move
Name the plates
Adriatic
Aegean
Turkish
Juan de Fuca
Cocos
Caribbean Plate
Philippines
Iranian
Arabian
Where are earthquakes concentrated?
At the edges of the plates (boundaries) pressure is built up and suddenly released causing earthquakes.
The four types of plate margins?
Divergent
Convergent
Collision
Transform
What causes plates to move?
Convection currents. This occurs when heat spreads out and flows towards the surface, forming large convection (heat) cells.
Evidence of plate tectonics?
Evidence to support continental drift?
- Identical rocks in South America and West Africa
- Continents fit together like a jigsaw puzzle
- Identical species of land-based fossils found in continents that are today separated by wide oceans
- Patterns of earthquakes, volcanoes, mountain ranges and deep ocean trenches provide evidence of the precise location of active plate boundaries.
Divergent boundary or Constructive margin
Two plates moving from each other
*Volcanoes
*Underwater volcanoes
*Range of mountains called mid-oceanic ridge
Convergent boundary or Destructive margin
Two plates moving towards each other
One of the plates is made of dense oceanic crust causing it to dive underneath the other plate to form a subduction zone. Immense heat destroys the subducting plate.
*Earthqaukes
*Volcanoes
*Fold mountains
Collision margin
Plates of the same density collide with no subduction
*Earthquakes
*Fold mountain
*No volcanoes
Transform boundary
Sliding alongside each other.
*Earthquakes
The types of plate margins and landforms associated with the Caribbean plate
On the northern edge of the Caribbean plate, there is a transform boundary between the Caribbean plate and the North American plate.
At the western boundary of the Caribbean plate, oceanic crust making up the Cocos plates is subducting beneath the Caribbean plate forming a zone of volcanoes, earthquakes and fold mountains in South America
The southern boundary of the Caribbean plate is part convergent and part transform. Earthquakes do not occur here as often as in the other Caribbean plate boundaries.
To the east of the Caribbean plate, an active convergent boundary exists between the south american plate and the Caribbean plate. The subducting south american plate is responsible for a chain of mostly volcanic islands known as the lesser Antilles