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Weathering, Erosion and Deposition

Across
Carry weathered rocks and sediment
When iron in rocks "rusts"
A vertical sequence of soil layers
Carve away at beaches, rocks and continents
The type of soil that is removed from its parent material
Needed to allow the weathering and erosion to work
Breaks larger rocks into smaller rocks of same type.
Promotes physical weathering, water freezes in rock cracks
Possibly the most powerful agent of weathering
The most significant factor controlling the development of soils
Pick up particles, dig into ground and building
The movement of air moving silt and other small particles
Down
When running water cuts small channels into the side of a slope.
Where weathered rock and soil stop moving
Water freezing and cracking rock over time.
The best place to promote chemical weathering, along with rain and lush vegetation
Can be compared to peeling the layers of an onion
The rocks that create soil by weathering
The loose covering of weathered rock particles and decaying rock particles.
The type of soil that is made from local bedrock
Causes "acid rain" and can interact as a chemical weatherring agent
Scrape and gouge out large sections of Earth's landscape
The process that breaks down and changes rocks and minerals
The removal of weathered rock and soil from its original location