Weathering, Erosion, & Deposition part 1
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Transcript of Weathering, Erosion, & Deposition part 1
Weathering, Erosion, & Deposition
part 1
Part I. WeatheringA. Weathering is the physical or chemical break-
down of rocks or minerals at or near the earth’s surface - Breaking rock into pieces
B. ONLY rocks at the surface can weatherC. Types
A. Physical – breaking rocks w/o changing composition
B. Chemical – breaking rocks by chemically changing the minerals
Chemical Weathering Agents
A. Water – dissolves certain rocks (salt)B. Air
a) Oxidation (rusting) – O2 combines w/ water and reacts with minerals containing iron
b) CO2 – combines w/ water to make carbonic acid, dissolves limestone
c) Plants – lichens make acid that dissolves rock
Chemical Weathering Agents
Lichens
Oxidation
Carbonic Acid
Oxidation
Oxidized rocks in Utah
Carbonic acid at work!
Hydrolysis of feldspar
Feldspar
Clay forming
from hydrolysis
of feldspar
Acid rain at work!
Review of chemical weathering• Oxidation (rust)• Acid rain• Carbonic acid
Water + Carbon dioxide Carbonic acid• Water dissolving rocks with acids mixed in it• Hydrolysis-water reacting with rock causing chemical
changefeldspar + water = clay
Physical WeatheringA. Frost action
1. Water enters cracks in rocks, as it freezes it expands breaking the rock
Physical WeatheringB. Abrasion
1. Grinding, rolling & scraping of rocks together. Breaks off sharp edges, rounding the rock
2. Caused by running water, waves, wind and glaciers
Physical WeatheringC. Plant action
1. Plant roots work into rocks breaking the rock apart as it grows
Physical WeatheringD. Exfoliation
1. Peeling off the outer layers of rock.2. Caused by repeated heating or cooling
Review of physical weathering
• Frost action-alternating temperatures above and below freezing causes rock to crumble
• Abrasion-the physical grinding of rocks along a surface
• Root action -roots break a part land as they grow into the ground
• Burrowing animals• Exfoliation-peeling of rock layers due to crustal
unloading
Exfoliation examples
Abrasion
Frost action at work!
Root action
Burrowing animals
Factors Affecting WeatheringA. Climate
1. Hot, dry climate – very little weathering
2. Warm, moist climate – rapid chemical
3. Cold, moist climate – strong frost action
Factors Affecting Weathering
B. Type of Rock1. Igneous and Metamorphic – react
SLOWLY, more dense2. Sedimentary – weather rapidly
Factors Affecting WeatheringC. Particle Size
1. As rocks break into smaller pieces, it weathers faster (more surface area exposed)
0
5
10
15
20
25
30
35
1 2 3 4 5
Particle Size
Rate
of W
eath
erin
g
Review Factors affecting rate of weathering
• Exposure to the elementsThe closer a rock is to the earth’s surface, the more weathering will occur
• Particle sizeWhen the rock particles are smaller, the rate of weathering increases
• Mineral compositionSome minerals are more resistant to weathering than others
• ClimateWarm, moist climates chemicalCold, dry climates physical
SOILS• Soils are a mixture of rocks, minerals and
organic material
SoilA. Final product of weatheringB. Soil composition
1. Inorganic material – pieces of weathered rock
2. Humus – organic material from decayed plants and animals; provides nutrients for growth
Classes of Soil
A. Soil Types1. Residual Soil
a. Soils that stay where they are formedb. Soil composition matches the rocks
underneath, granite rock = granite in soil
2. Transported Soila. Soils that were carried to other locationsb. Soil does NOT match, granite rock = NO
granite in soil
Soil development depends on…
• Climate• Biological activity• Slope of the land • Time
Soil profile
Know this profile!Know this profile!
Porosity and permeability of soils
• Porosity- amount of open spaces within soil particles
• Permeability- amount of water that passes through a soil
Weathering, Erosion, & Deposition
part 2
Part 2 - Erosion
A. Carries away pieces from weatheringB. Most soils are different from bedrock
under them (transported soils)C. Gravity is MAIN force behind erosion
What does erosion mean?
• Transport of weathered material.
• Agents of erosion are: wind, water, ice (glaciers) and gravity.
• Water is the most common erosional agent
Mass movement notes
What comes up, must come down!
What is mass movement?
• Mass movement: When gravity pulls geologic materials down slope
• Driving force gravity
• Resisting force friction
Soil creep
Velocity: Less than 1 cm/year
Debris flow
Velocity:1 mm/day to 1 km/hour
Mud flowVelocity:1-5 Km/hour
Rock fallsVelocity: Greater than 4 km/hour
Conclusion
• Mass movement is the downward movement of rock, snow, soil and ice as a result of gravity.
• When the driving force>resisting force slope failure occurs
• Order of increasing speed: soil creepdebris flowmud flowrock fall
Agents of Erosion
A. Gravity (Review)1. Landslides – rapid movement of rock
material down hill2. Slumping – small landslides3. Creep – VERY slow mvmt of material4. Talus – piles of rock found at base of
very steep slopes
Agents of ErosionSlumpingLandslide
Agents of ErosionTalus
Creep
Agents of ErosionB. Wind
1. Carries fine grained sediments about 1 meter above ground
2. Grains are lifted and bounced along
3. Wears away rocks at the base
4. Dunes – piles of wind blown sand
Agents of Erosion
Agents of Erosion
Agents of ErosionC. Glaciers
1. Masses of frozen water on ground2. Valley (alpine) glaciers
a. “rivers of ice”b. Found at high altitudes in mountains
Agents of Erosion
3. Continental glaciersa. Large sheets of ice covering large areas of
surface (Greenland, Antarctica)
Agents of Erosion
4. Formed in areas where snow does not melt, keeps building up and is compacted into ice
5. As Ice builds up, pressure increases at bottom, causing ice to flow (cm to m per day)
Agents of Erosion
6. As glaciers move, they carry materials of ALL sizes (sand to boulders)
7. Materials carried cause bedrock under glacier to be gouged and scraped
VIII. Agents of Erosion
Agents of Erosion
8. Glacier Landscapesa. U-shaped valleysb. UNSORTED rock material when glacier melts
(till)c. Drumlins – groups of long oval hillsd. Eskers – winding ridges formed in tunnels
under icee. Kettles – large piece of ice breaks off glacier
making a hole, ice melts leaving the hole. Kettle lake – hole is filled with water (Beaver Lake)
Agents of Erosion
VIII. Agents of Erosion
Kettle Lake
DrumlinGlacial Till
The Hydrologic (Water) Cycle
Water table
Agents of Erosion
D. Running Water1. MOST important (moves most material)2. Ways of carrying sediments
a. Solution – dissolved materials (salt)b. Suspension – very fine particles (silt)
suspended in water, looks muddyc. Bouncing – pebbles bounced along streamd. Rolling and sliding – largest particles moved
without being liftedParticle Transport
Agents of Erosion
3. Velocitya. Speed of the water flowb. Depends on slope and volume (stream
discharge)c. Greater slope = greater velocityd. Greater volume = greater velocity
Agents of Erosion
4. Sediments Carrieda. Size
1) FAST streams can carry LARGER sediments
b. Quantity (amount)1) MORE volume carries MORE sediment2) Even though a fast moving stream can carry larger
rocks, a slow moving stream with greater volume can carry more sediment (Mississippi River)
How fast does a stream need to be flowing to carry a cobble?
About 190 cm/sec
What kind of particle can a stream carry if it is going 400 cm/sec?
Boulder
How fast does a stream need to be flowing to carry a 1.0 cm particle?
50 cm/sec
Agents of Erosion
5. Effects of moving streamsa. Carry sedimentsb. Deepen and widen stream bed as it drags
and carries its sedimentsc. Abrasion happens (rocks becoming rounded)
Agents of Erosion6. Stages of Stream Development
a. Youth1) Steep gradients2) Rapid downcutting (carries rocks and pebbles)3) V shaped valley4) Has waterfalls or rapids5) Straight path
Agents of Erosionb. Mature
1) Less steep, less velocity2) Wind around obstructions forming loops3) Carries silt and clay (no rocks)4) Larger volume = more sediment than youth
Agents of Erosionc. Old
1) Very small gradient2) Only carries finest sediments3) Can flood4) Makes Oxbow Lakes
Agents of Erosion
Agents of Erosiond. Old streams can
become young again if the area is uplifted and gradient becomes steeper
e. Most streams have youth at source, mature in middle and old age at their mouth (where river dumps into a lake/ocean)
Weathering, Erosion, & Deposition
part 3
Part 3 - Deposition
A. Sediments are released or dropped from the agent of erosion
Factors Affecting Deposition
A. Size1. Large particles settle the fastest
Settling Time
Particle Size
Tim
e
Particle Size
Rat
e
Settling Rate
Factors Affecting Deposition
B. Shape1. Round particles settle faster than flat
particles
C. Density1. More dense particles settle faster
Sorting of SedimentsA. Graded bedding (vertical sorting)
1. Happens at ocean bottoms or landslides
Sorting of Sediments
B. Horizontal Sorting1. Large particles settle first as a stream
enters a body of water
Glacial Deposits
A. Till1. Dropped from glacier.2. UNSORTED!!!!! (all sizes mixed)
B. Outwash material1. Deposited from meltwater2. SORTED
Energy Changes
A. Kinetic Energy – energy of movementB. Potential Energy – stored energyC. High velocity = High KE = erosionD. Low velocity = Low KE = deposition
1. Streams slow when:a. Slope or volume decreasesb. Moves into a body of waterc. On the inside of a curve
Energy Changes
E. Streams have GREATEST PE at their source (highest point)
1. Loses PE as it turns to KE on the way down
Greatest PE, Less KE
Greater KE, Less PE
KE
PE
Erosion – Deposition System
A. Side View (profile)Erosion Dominates – water moving fast
Delta can form
Source
Mouth
A
B
C
Ocean
Deposition – river slows down
Erosion – Deposition System
B. Top ViewInside of curve, water moves SLOWER, deposition, shallow
Outside of curve, water moves FASTER, erosion, deeper water
OCEAN
A B C
Delta
Velocity within a Stream
A. Water moves fastest in the middle towards the top of the stream (less friction)
Stream Cross Section
AB
CD
D – Water moves fastest, smallest friction
Velocity within a Stream
B. Cross Section of a Stream Corner
Outside = Faster = More Erosion = Deep
Inside = Slower = More Deposition = Shallow
Velocity within a Stream
Effects of Climate on Landscape
A. Humid (wet)1. Worn down and rounded (more
weathering)
B. Arid (dry)1. More angled, sharper edges
Effects of Climate on Landscape
Humid Arid
Drainage PatternsA. Arrangement of
streams draining water in an area
B. Determined by type of bedrock