Title: Unit 3: Rocks, Soil, & Minerals
1Unit 3 Rocks, Soil, Minerals
2Weathering
- Weathering
- the process that breaks down rock other
substances _at_ Earths surface. - Heat, cold, water, ice, oxygen, and carbon
dioxide contribute to weathering.
3Forces
- Forces of weathering break rocks into smaller
pieces - Forces of erosion carry these pieces away.
4Erosion
- Erosion
- the movement of rock particles by wind, water,
ice, or gravity. - Weathering and erosion work together to wear down
and carry away rocks at Earths surface.
5Concept Check
- What is the difference between weathering and
erosion?
62 Types of Weathering
- Mechanical Weathering
- Rocks are physically broken down into smaller
pieces. - Occurs slowly over time, but can wear away a
whole mountain. - Chemical weathering
- Breaks down rock through chemical changes.
- Agents include water, oxygen, carbon dioxide,
living organisms, and acid rain.
7Forces of Mechanical Weathering
- Release of Pressure
- As mass is removed, pressure is reduced and the
outside layer of rock flakes away. - Freezing and Thawing
- Deals with temperature changes
- Abrasion
- The grinding away of rock particles carried by
water, ice, wind, or gravity. - Plant growth
- Roots of plants enter cracks in rocks and causes
the rock to pry apart. - Animal actions
- When animals burrow into the ground it loosens up
soil and breaks apart rock.
8Agents of Chemical Weathering
- Water
- Most important
- Dissolves rock
- Oxygen
- Oxidation
- E.g. iron ? rust
- Carbon dioxide
- Forms carbonic acid when mixed with rain water on
the ground - Living organisms
- Produce acids that chemically weather rock
- Acid rain
- When the burning of fuels produces pollutants,
these harsh gases combine with rain and form
acids which weather very quickly.
9Mechanical Chemical Together
- Mechanical and chemical weathering often work
together - Mechanical breaks rocks down, exposing more of
the rock or mineral to chemical weathering. - Rate of weathering is determined by
- Type of rock
- More permeable weathers faster
- Temperature (remember the vinegar chalk)
- High temps high precipitation level faster
weathering
10As the surface area of this rock is increased by
mechanical weathering, it is more exposed to
agents of chemical weathering
11Climate
- Both types of weathering occur faster in hot, wet
climates. - Rainfall provides the water needed for chemical
changes as well as freezing and thawing. - Chemical reactions occur faster at higher
temperatures.
12Examples of the Effects of Weathering
- Look at the following examples of weathering.
Which type of weathering do you think occurred?
Why do you think that?
13Example 1
14Example 2
15Example 3
16Example 4
17Example 5
18Example 6
19Example 7
20Example 8
21Example 9
22Now you come up with your own example
23Soil
- Soil is the loose, weathered material on Earths
surface in which plants can grow. - It forms as a rock is broken down by weathering
and mixes with other materials on the surface.
24Soil Composition
- Soil
- mixture of rock particles, minerals, decayed
organic material, air, and water. - Type of rock particles and minerals in any given
soil depend on - The rock weathering
- Type of weathering that took place
25Soil Texture
- Depends on the size of individual soil particles
- E.g. sand vs. clay
- Particles are classified by size
- Gravel largest (2mm and above)
- Sand
- Silt
- Clay smallest
26Checkpoint
- Looking back at the particle size of different
types of soil, why do certain types have the
texture (feel) they do? Give an example.
27Soil Texture
- Important for plant growth.
- Clay is dense and heavy and typically holds a lot
of water. - Sand is coarse and water drains quickly.
- Loam is a type of soil that is an equal mix of
sand, clay, and silt. - Best for growing plants
28Soil Horizons
- 3 horizons
- Topsoil mix of humus, clay, other materials.
- Subsoil mix of clay and little humus
- Bedrock partly weathered rock
29Life in Soil
- Organisms mix the soil and make spaces in it for
air and water. Other soil organisms make humus,
the material that makes soil fertile.
30Soil Activity
- http//School.discoveryeducation.com/schooladventu
res/soil
31Soil Observations
- Explain your soils
- Color
- Texture
- Particle size (what do you think it has the most
of look back at your notes) - Original location
- Original depth (remember the horizons)
- What type of plant would grow the best in it
32Importance of Soil
- Soil is one of Earths most valuable resources
because everything that lives on land depends
directly or indirectly on soil. - Plants
- Animals
- Humans
33Importance of Soil
- Long time to form
- Limited supply of fertile soil
- Designates where farming can take place
34Soil Damage and Loss
- Can be lost to erosion by water and wind.
- Water where soil isnt protected by a plant
cover. - Wind occurs in dry climates (e.g. dust bowl)
35The Dust Bowl
- Plowing removed the grass from the Great Plains
and exposed the soil. - In times of drought, the topsoil quickly dried
out, turned to dust, and blew away.
36(No Transcript)
37Soil Conservation
- The management of soil to prevent its destruction
- 2 methods
- Contour plowing plowing along the curves of a
slope - Conservation plowing old crops and dead weeds
are left in the crop - Also, limiting herd grazing
38Diamond Formation
- At depths of 120 kilometers
- Under great pressure and heat
- This caused carbon atoms to change into diamonds
- Originated from a volcanic pipe
393 Main Ways Minerals Form
- As hot magma cools inside the crust or as lava
hardens on the surface - When the elements of a mineral dissolve in hot
water (forms a solution) - When solutions evaporate
40Processes of Mineral Formation
- Minerals have been forming since the beginning of
Earth - Minerals can form in 2 ways
- Through crystallization of materials dissolved in
water - Through crystallization of melted materials
41Uses of Minerals
- Minerals are the source of metals, gemstones, and
other materials used to make many products. - Ore
- A rock that contains a metal or economically
useful mineral - E.g. Copper comes from the ore chalcopyrite