HAZARDS : Plate Tectonics Flashcards
Before the development of the plate tectonic theory, how did scientists divide the interior of the Earth?
Into three different sections:
- Crust
- Mantle
- Core
What is the core?
The centre of the Earth, made of dense rocks containing iron and nickel alloys.
Name and explain the two parts of core:
- Inner - solid ball
- Outer - semi-molten
Both contain iron and nickel alloys.
What is the mantle?
The layer around the core, made up of molten and sem-molten silicate rocks.
What are silicate rocks?
Rocks made of lighter elements such as silicon and oxygen.
Describe the differences in the layers of the mantle:
- Part nearest the core is rigid.
- Asthenosphere (layer above this) is semi-molten.
- Very top layer is rigid.
What does semi-molten mean?
The substance can flow.
Describe the layers of the mantle:
- Nearest the core is quite rigid.
- Layer above this is semi molten - asthenosphere.
- Very top is rigid.
What is the asthenosphere?
The highly viscous, mechanically weak and ductile region of the upper mantle of the Earth.
It lies below the lithosphere.
What is the crust?
The outermost layer of the earth.
What does the lithosphere consist of?
The crust and the rigid upper section of the mantle.
It is the section of Earth that is divided into tectonic plates.
What are the two types of crust?
Oceanic and continental.
Compare the thickness of oceanic and continental plates:
Continental crusts are thicker.
Continental = 30-70km.
Oceanic = 6-10 km.
Compare the density of oceanic and continental plates:
Continental plates are lighter.
2.6 compared to 3.0.
What are continental plates composed of?
Continental plates are mainly made of granite, silicon, aluminium and oxygen.
SIAL.