weathering and climate 6.5 c, d weathering the break down of rocks, minerals, and soils at or near...
TRANSCRIPT
Weathering
The break down of rocks, minerals, and soils at or near the Earth's surface by wind, water, organisms and atmospheric conditions is called weathering.
Two types of weathering:Physical weathering Chemical weathering
Weathering is distinguished from erosion in that no transportation of material is involved.
Physical Weathering The break down of material by physical or
mechanical means. Physical weathering does not change the material into a new substance.
Examples of Physical Weathering Freezing water (ICE WEDGING) can break rock
without any change in the minerals that form the rock. This usually produces small particles and sand.
Tree roots Sand blasting (wind)
The breakdown of material by chemical reactions that changes the composition of the material is called chemical weathering.
Chemical Weathering
Oxidation = is the interaction between oxygen molecules and all the different substances they may contact, from metal to living tissue. (GOOD AND BAD)
Carbonation = is the term for the conversion of an organic substance into carbon
Examples of Chemical Weathering
Carbonization Some fossils are produced by carbonization First image is carbonized leaf from the Eocene Green River
Formation, Wyoming Second image is from the Cambrian Burgess Shale, Canadian
Rockies
Large bodies of water (like the ocean) play a big part in controlling and moderating our climate.
Climates around large bodies of water tend to be milder. In other words, the winters are less cold and the summers are less hot.
WHY?
WHY?Because water heats up more slowly and
cools down more slowly than land does thus making the winters less cold and the summers less hot.