Weathering, Erosion and Deposition

Slides:



Advertisements
Similar presentations
Weathering and Erosion
Advertisements

Weathering The breakdown do the materials of Earth’s crust into smaller pieces.
1. Why is water a major agent of chemical weathering. A
Weathering, and Soil Formation
Chemical Weathering.
Weathering and Erosion. Weathering The breakdown do the materials of Earth’s crust into smaller pieces.
Erosion and Deposition
Weathering, Erosion, and Deposition
Weathering And Erosion Weathering And Erosion.
As you observe the following pictures think about this… Have the landforms undergone changes? What do you think caused the changes? How long do you think.
Weathering and Erosion
The Earth’s Changing Surface
Weathering & Erosion.
8-1 Rocks and Weathering How do rocks and weathering affect Earth’s surface? What are the causes of mechanical weathering ands chemical weathering? What.
Aim: Weathering and Erosion. Weathering The breakdown of the materials of Earth’s crust into smaller pieces.
Weathering and Erosion. Student Expectation Analyze the effects of weathering, erosion, and deposition on the environment in ecoregions of Texas.
Weathering and Erosion. Weathering The breakdown of the materials of Earth’s crust into smaller pieces.
Weathering and Soil Formation
Constructive & Destructive Forces on Landforms
Weathering, Erosion and Deposition. Weathering The breakdown do the materials of Earth’s crust into smaller pieces.
Weathering and Erosion. Weathering The breakdown of rock material by physical and chemical processes.
Do you know the answers?  What is the salinity of water? the amount of salt dissolved in the water  Why is salinity important? if the salinity is too.
Weathering and Soil Erosion
Constructive and Destructive Forces
Weathering and Erosion. Weathering The breakdown do the materials of Earth’s crust into smaller pieces.
Weathering and Erosion
Weathering and Erosion
Weathering and Erosion. Weathering The breakdown of the materials of Earth’s crust into smaller pieces.
Weathering and Erosion NOTES
Weathering and Erosion Unit 3 Chapter 7. Weathering – the process by which rocks are broken up into smaller pieces by the action of water, the atmosphere.
What is the MAJOR agent of erosion that has shaped Earth’s land surface? Moving water Water moving over land’s surface is called runoff. This may cause.
Weathering and Erosion. Weathering Weathering is a set of physical, chemical and biological processes that change the physical and chemical properties.
Investigation 3: Rocks and Weathering. Key Question How do different types of rocks weather?
Bell Work Erosion is __________________________________ ___________________________________________ Sediment is _________________________________ Gravity.
Erosion & Deposition Ch 10 8 th grade. What processes wear down and build up Earth’s surface? Gravity, moving water, glaciers, waves, and wind are all.
Weathering The breakdown do the materials of Earth’s crust into smaller pieces. p?id=3204.
Weathering, Erosion , & Deposition –SEPT
WEATHERING, EROSION, & DEPOSITION
Investigation 3: Rocks and Weathering
Weathering – Physical and Chemical
6.5 Weathering & Erosion Review
Weathering and Erosion
Weathering and Erosion
External Forces.
Changing Earth’s Surface What Processes Break Down Rock?
T/F Wind, water, ice, and gravity continually shape Earth’s surface.
Weathering and Erosion
Weathering and Erosion
Weathering and Erosion
Weathering and Erosion
Weathering and Erosion
Weathering and Erosion
Weathering and Erosion
Weathering and Erosion
Weathering and Erosion
Weathering and Erosion
Weathering and Erosion
Weathering and Erosion
Weathering and Erosion
Weathering and Erosion
Weathering and Erosion
Weathering and Erosion
Weathering and Erosion
Weathering and Erosion
Weathering and Erosion
Weathering and Erosion
Weathering and Erosion pull out your HW
Weathering and Erosion
Weathering and Erosion
Weathering and Erosion
Presentation transcript:

Weathering, Erosion and Deposition

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.

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 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 by physical forces. Types of Mechanical weathering Ice wedging Plant roots Abrasion Burrowing of animals (animal action) Temperature changes (freezing and thawing)

Frost Wedging

Plant Roots

Abrasion

Animal Action (Burrowing)

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)

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.

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

Carbon Dioxide CO2 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 rock.

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 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 Located in rainy regions where there is limestone near the surface, characterized by sinkholes and caves.

View brainpop animation: http://www. brainpop

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 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 this beach in Costa Rica.

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

Waterfalls http://www.classzone.com/books/earth_science/terc/content/visualizations/es1305/es1305page01.cfm?chapter_no=visualization

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 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 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, 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_science/terc/content/visualizations/es1205/es1205page01.cfm?chapter_no=visualization

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

other examples of erosion control: silt fencing terracing

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 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/terc/content/visualizations/es1306/es1306page01.cfm?chapter_no=visualization formation of an oxbow lake: http://www.cleo.net.uk/resources/displayframe.php?src=309/consultants_resources%2F_files%2Fmeander4.swf

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 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 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

gullies

River System

Notes quiz 1. Examples of mechanical weathering are ice wedging, animal actions, oxidation plant growth, ice wedging, abrasion 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 the movement of sediment or rock the settling out of sediment or rock 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 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 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? (1st step in river formation)