Weathering Erosion and Deposition Weathering Weathering is the

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Weathering, Erosion and Deposition

Weathering, Erosion and Deposition

Weathering • Weathering is the wearing away of rock and can be chemical or

Weathering • Weathering is the wearing away of rock and can be chemical or mechanical These mountains in Costa Rica were mechanically weathered by abrasion. • Abrasion is weathering by grinding action.

These mountains in Salt Lake City, Utah, were also weathered by abrasion.

These mountains in Salt Lake City, Utah, were also weathered by abrasion.

More examples of weathering on the Pacific Coast of Costa Rica are shown by

More examples of weathering on the Pacific Coast of Costa Rica are shown by these sea stacks out in the ocean. They were formed as ocean waves weathered away part of the rocks seen here.

Another example of how weathering forms landscapes is the creation of a horn. This

Another example of how weathering forms landscapes is the creation of a horn. This is a peak of a mountain that has been formed by the weathering away of rock by glaciers.

1. Mechanical Weathering • Process by which rocks are broken down into smaller pieces

1. Mechanical Weathering • Process by which rocks are broken down into smaller pieces by physical forces. • Types of Mechanical weathering – Ice wedging – Plant roots – Abrasion – Burrowing of animals (animal action) – Temperature changes (freezing and thawing)

Frost Wedging

Frost Wedging

PLANT ROOTS

PLANT ROOTS

Abrasion

Abrasion

Animal Action (Burrowing)

Animal Action (Burrowing)

How decomposers enrich soil and make it fertile: mechanical weathering. Chipmunks live in dens

How decomposers enrich soil and make it fertile: mechanical weathering. Chipmunks live in dens in the soil and search the litter for seeds and nuts. Plant roots break up the soil and hold it in place. Earthworms break up the soil, making it easier for plant roots to spread and for air and water to enter the soil. They create waste which makes soil more fertile by adding nitrogen. Bacteria are decomposers that break down animal and plant remains and wastes.

Freezing and Thawing (temperature changes)

Freezing and Thawing (temperature changes)

Chemical Weathering • the process that breaks down rock through chemical changes. • The

Chemical Weathering • the process that breaks down rock through chemical changes. • The agents of chemical weathering: – water- water dissolves rock over time – oxygen- combines with iron to form rust (oxidation) – carbon dioxide- dissolves in water to form carbonic acid – living organisms- plant roots secrete acids – acid rain- from the burning of fossil fuels

Water • Water weathers rock by dissolving it.

Water • Water weathers rock by dissolving it.

Oxygen • Iron combines with oxygen in the presence of water in a processes

Oxygen • Iron combines with oxygen in the presence of water in a processes called oxidation. • The product of oxidation is rust.

Carbon Dioxide • CO 2 dissolves in rain water and creates carbonic acid. •

Carbon Dioxide • CO 2 dissolves in rain water and creates carbonic acid. • Carbonic acid easily weathers limestone and marble.

Living Organisms • Lichens that grow on rocks produce weak acids that chemically weather

Living Organisms • Lichens that grow on rocks produce weak acids that chemically weather rock.

Acid Rain • Compounds from burning coal, oil and gas react chemically with water

Acid Rain • Compounds from burning coal, oil and gas react chemically with water forming acids. • Acid rain causes very rapid chemical weathering.

2 factors that determine the rate of weathering: • rock type- Rock that is

2 factors that determine the rate of weathering: • rock type- Rock that is permeable (has holes that let water in), weathers faster than rock that is impermeable. The mineral content of rock also determines how fast a rock weathers. • climate- Rock weathers faster in warm, humid climates.

Karst Topography • A type of landscape created by chemical weathering of limestone •

Karst Topography • A type of landscape created by chemical weathering of limestone • Located in rainy regions where there is limestone near the surface, characterized by sinkholes and caves.

View brainpop animation: http: //www. brainpop. com/science/weathering/

View brainpop animation: http: //www. brainpop. com/science/weathering/

Erosion • Erosion is the movement of sediment by water, wind or ice. •

Erosion • Erosion is the movement of sediment by water, wind or ice. • In this picture taken in Oregon, a gully has been created by a stream that has cut a path through soft sediment after a strong rainfall.

Erosion • Erosion has caused this bank in Squaw Creek to be cut away

Erosion • Erosion has caused this bank in Squaw Creek to be cut away by the weathering of the river, forming a landform that simulates a partial cave on the left side of this picture.

Erosion • Here, erosion by longshore drift, has caused a lagoon to form along

Erosion • Here, erosion by longshore drift, has caused a lagoon to form along this beach in Costa Rica.

Mass Movement • http: //www. phschool. com/atschool/phsciexp /active_art/mass_movement/index. html

Mass Movement • http: //www. phschool. com/atschool/phsciexp /active_art/mass_movement/index. html

Waterfalls • http: //www. classzone. com/books/earth_scie nce/terc/content/visualizations/es 1305/es 130 5 page 01. cfm? chapter_no=visualization

Waterfalls • http: //www. classzone. com/books/earth_scie nce/terc/content/visualizations/es 1305/es 130 5 page 01. cfm? chapter_no=visualization

View brainpop video and name 3 types of erosion and how they change land:

View brainpop video and name 3 types of erosion and how they change land: http: //www. brainpop. com/science/earthsystem/erosion/

Deposition • Definition: deposition is the settling out of sediment that has been eroded.

Deposition • Definition: deposition is the settling out of sediment that has been eroded.

Deposition is the adding of sediment in an area as it settles out and

Deposition is the adding of sediment in an area as it settles out and forms new landforms. In this picture, taken in Squaw Creek, near Sisters, Oregon, rocks have been deposited along the bank of the river after heavy rains.

Deposition • In this picture, also taken in Squaw Creek, a sandbar has been

Deposition • In this picture, also taken in Squaw Creek, a sandbar has been formed by sediment that has been washed down the river. This might also be considered a spit.

Deposition • In this picture, salt has been deposited in the Great Salt Lake,

Deposition • In this picture, salt has been deposited in the Great Salt Lake, Utah. You can see the salt deposits. They appear as white areas on the edge of the water.

Landforms • http: //www. classzone. com/books/earth_scie nce/terc/content/visualizations/es 1205/es 120 5 page 01. cfm? chapter_no=visualization

Landforms • http: //www. classzone. com/books/earth_scie nce/terc/content/visualizations/es 1205/es 120 5 page 01. cfm? chapter_no=visualization

Erosion Control Methods: • These native plants were left undisturbed on the beach in

Erosion Control Methods: • These native plants were left undisturbed on the beach in Costa Rica, so that they would hold in the sand prevent erosion on the beach. This is an example of permanent erosion control.

other examples of erosion control: silt fencing terracing

other examples of erosion control: silt fencing terracing

River Formation • A river is a natural stream of freshwater that is larger

River Formation • A river is a natural stream of freshwater that is larger than a brook or creek. Rivers are normally the main channels or largest tributaries of drainage systems. Typical rivers begin with a flow from headwater areas made up of small tributaries, such as springs. They then travel in meandering paths at various speeds. Finally, they discharge or flow out into desert basins, into major lakes, or most likely, into oceans.

Erosion and Deposition • Meanders are formed by the weathering of one bank of

Erosion and Deposition • Meanders are formed by the weathering of one bank of a river and the deposition of the weathered sediment on the opposite bank of the river. This creates a loop-like bend in a river, such as this one. This view was taken from an airplane over a mountain range in the midwest.

 • changes in a meandering river • http: //www. classzone. com/books/earth_science/t erc/content/visualizations/es 1306

• changes in a meandering river • http: //www. classzone. com/books/earth_science/t erc/content/visualizations/es 1306 page 01. cfm? chapter_no=visualization • formation of an oxbow lake: • http: //www. cleo. net. uk/resources/d isplayframe. php? src=309/consultant s_resources%2 F_files%2 Fmeander 4. swf

The world's longest river is the Nile River in Africa, which runs 4, 187

The world's longest river is the Nile River in Africa, which runs 4, 187 miles (6, 739 kilometers) from its source in Burundi to the Mediterranean Sea. •

 • Every river has a point of origin- it is the highest point

• Every river has a point of origin- it is the highest point in the water basin. • Gravity- is important; rivers almost always flow downhill watercourse. • Some rivers start from springs, especially in humid climates. Springs occur as groundwater rises to Earth's surface and flows away. • Other rivers originate from lakes, marshes, or runoff from melting glaciers located high in the mountains. Some rivers have their beginnings in huge glaciers.

Steps to River Formation 1) Precipitation (rainwater or snow ) is the source of

Steps to River Formation 1) Precipitation (rainwater or snow ) is the source of the water for most rivers. 2)When a heavy rain falls on ground that is steeply sloped or is already saturated with water, water runoff trickles down Earth's surface rather than being absorbed- this is called surface runoff. 3) After it travels a short distance, the water begins to run in small parallel rivulets called rills. 4) As these rills pass over fine soil or silt, they begin to dig shallow channels, called gullies. This is the first stage of erosion. A gully only has water in it when it rains. 5) A stream is formed when gullies join together. It is a channel along which water is continually flowing down a slope. Streams rarely dry up. 6) A stream grows larger as it gets water from tributaries. A tributary is a stream that flows into a larger stream.

Visual steps to river formation Rills

Visual steps to river formation Rills

gullies

gullies

River System

River System

Notes quiz 1. Examples of mechanical weathering are a) ice wedging, animal actions, oxidation

Notes quiz 1. Examples of mechanical weathering are a) ice wedging, animal actions, oxidation b) plant growth, ice wedging, abrasion c) freezing and thawing, burrowing, acid rain 2. Examples of chemical weathering are • a) acid rain, oxidation, living organism • b) freezing and thawing, animal actions, oxidation • c) burrowing, carbon dioxide, abrasion

3. Deposition is a) the movement of sediment or rock b) the settling out

3. Deposition is a) the movement of sediment or rock b) the settling out of sediment or rock c) the breaking down of sediment or rock 4. A meander is • a) a small river that runs into a larger river • b) a loop-like bend in a river • c) a lake that has been cut off from a river

 • • 5) Name 3 methods of erosion control a) b) c) •

• • 5) Name 3 methods of erosion control a) b) c) • 6) What are 2 factors that affect the rate of weathering? • a) ___________ • b) ___________ • 7) What is surface run-off?

 • 8) Rills in soil run together to form _____ that only have

• 8) Rills in soil run together to form _____ that only have water in them when it rains. • • 9) What forms when gullies join together? a) a rill b) a stream c) a tributary • 10) What is the original source of water of most rivers? (1 st step in river formation)