weathering is the breakdown of rocks at the Earth's surface by natural processes
mechanical weathering is caused by the effects of changing temperature on rocks, causing the rocks to break apart
Frost wedging is when water enters the cracks of a rocks, freezes, and expands, causing the rock to break
Salt Crystal Growth is when saltwater comes in the pores of rocks. when it evaporates, salt remains in the pores
Abrasion - gasgas = deformed rocks
Biologicalweathering is the breakdown of rocks by living organisms.
Chemicalweathering caused by slightly acidic water or minerals
dissolution = crystallization
oxidation = takla, reddish thingy
Hydrolysis - clay-like
Areas that are cold and dry tend to have slow rates of chemical weathering and weathering is mostly physical; chemical weathering is most active in areas with high temperature and rainfall.
Factors that affect the rate at which weathering takes place
Climate
Rock Type
Rock Structure
Topography
Time
Time
Length of exposure to agents of weather determines the degree of weathering of a rock
weathering is focused on abrasion while erosion is more with transportation
Erosion is the incorporation and transportation of material by a mobile agent such as water, wind, or ice
Deposition is the geological process in which sediments, soil, and rocks are added to a landform or land mass
Running water encompasses both overland flow and stream flow
Discharge is the volume of water passing through a cross-section of a stream during a given time
Ocean/sea waves caused by wind moving across the surface of water. The friction between the air molecules and the water molecules causes energy
A glacier is a moving body of ice on land that moves downslope or outward from an area of accumulation
Wind - the flow of gases on a large scale
The main erosional process associated with groundwater is solution
Gravity is responsible for erosion by flowing water and glaciers but also causes erosion directly