1. Science Starter Please get your binder and your data folder
Add any returned notes to the notes section, daily work to the daily work section, and homework to the homework section of your binder
The next entry on your green data sheet is titled Unit 2.1 and grid in your test score.

2. Weathering, Erosion, Deposition

3. Weathering - the process of rock breaking down into smaller pieces.

4. Chemical Weathering - changes the chemical makeup of rocks or minerals.
Carbonation
Oxidation
Plant Acids
Acid Rain

5. Carbonation
Carbon dioxide in the soil mixes with water to form carbonic acid which dissolves calcium carbonate in limestone rocks.
Example: Cave Formations

6. Oxidation Oxygen in the air joins chemically with metals. Example:
Iron turning red (rusting)
Copper turning green (tarnishing)

7. Plant Acids
Plant roots produce acids (humic acids) which can dissolve rocks.
Example:
Lichens (fungus/algae) growing on rocks

8. Acid Rain
Water in the air reacts chemically with excess carbon, sulfur, and nitrogen compounds to form acids.

9. Acid Rain
1908
1969
Dissolving of statues 9

10. Mechanical Weathering
Abrasion
Root Pry
Ice Wedging
Exfoliation
Animal Actions

11. Abrasion
Sand and other rock particles that are carried by wind, water, or ice can wear exposed rock surfaces, like sand paper on wood.
Wind abrasion

12. Root Pry Roots of trees and other plants enter cracks in rocks,
forcing the cracks
farther apart.

13. Ice Wedging
When water freezes in a crack in a rock, it expands and makes the crack bigger.

14. Exfoliation
Extreme high temperatures cause the outside of the rock to crack and flake off, like layers of an onion.

15. Animal Actions
Animals that burrow in the ground loosen and break apart rocks in the soil. Other animals erode landscape by walking on it.

16. Soil Formation
Soil forms as rock is broken down by weathering and mixes with other materials on the surface.

17. Soil Composition
Soil is a mixture of rock particles, minerals, decayed organic material, air and water
Humus – decayed organic material in the soil that creates spaces for air and water and also provides necessary nutrients for plants to grow.
Soil color is determined by the mineral content of the soil.

18. Soil Texture
Soil texture is determined by the size of the individual particles, which is directly related to the amount of pore spaces where water can be stored.
Gravel or rock 2 mm and larger
Sand <2 mm
Silt <1/16th mm
Clay <1/256th mm
Loam – soil that is made up of equal parts of sand, silt, and clay

19. Soil Profiles
The arrangement of soil layers in an area, made up of individual layers or horizons.
Soil horizon- An individual layer of soil that differs in
color or texture from the layers above or below it.

20. Rate of soil formation
The rate at which soil forms (weathering) depends on the climate and type of rock.
Most rapid weathering occurs in warm, rainy climates.
Limestone weathers faster than granite.

21. Life in soil
Soil is one of Earth’s most valuable resources, because everything that lives on land depends directly or indirectly on soil.
Billions of organisms live in every cubic meter of soil.
All organisms that live in soil enrich humus with their remains or waste.
Animals and plant roots break up the soil, opening up spaces for air and water.

22. Agents of Erosion
Moving Water
Wind
Gravity
Glaciers 22

23. Moving Water
The major agent of erosion that shaped Earth’s land surface.
Rain water carries away sediment leaving tiny grooves in its path.
Streams and rivers carve large channels into the landscape. 23

24. Wind Dust Storms Blowing away of exposed sediments.
Fast moving winds can carry sand and dust that scour and weather the surfaces they strike. Wind is considered the weakest form of erosion.
Dust Storms
Blowing away
of exposed
sediments. 24

25. Gravity
The force that moves rock and other materials down hill, causing mass movement.
Landslide
Mudslide 25

26. Glaciers
A large mass of ice moving slowly over the land gathering rocks and soil as it erodes the land in its path. 26

27. Deposition
The settling of eroded particles or sediment wherever they are transported by wind or water.
Sediments on ocean and lake floors
Sand dunes
New beach sand
River deltas 27