Chapter 8 - The Earth and it's Rocks Flashcards
The crust
30 - 50 km thick under continents
7km thick under oceans
Mantle
- Under crust
- 2900 km thick
- upper layer is called the asthenosphere
The Core
- dense
- iron and nickle
- Outercore : liquid
- Innercore : Solid
Weathering
Breaking or dissolving of rocks
Physical Weathering: Temperature change
Expand when heated, contract when cooled. Repeated expansion causes rocks to crack
Physical Weathering:
Water and Ice
Rivers flow making a V shape, and glaciers leave behind a U shape.
Physical Weathering:
Crystallization of Salts
Salt water can get in-between rocks and they evaporate, leaving salt crystals behind and expands, causing rocks to split and crack.
Chemical Weathering
A chemical reaction between rocks and substances in the soil or air. Can lead to crumbling or color change.
Biological Weathering
Breaking down of rocks by living organisms or their products. Can be physical or chemical.
Erosion
Movement of weathered rock, e.g. wind or water
Deposition
When weathered material carried by erosion is discarded somewhere.
Meandering
When river slows down it bends, where material is deposited.