Weathering and Erosion Basics

Sean Fisher-Rohde
11 Feb 201307:38

Summary

TLDRThis educational video explores the concepts of weathering and erosion, distinguishing between the two processes with a practical demonstration using a graham cracker and a rolling pin. It delves into the agents of weathering and erosion, such as wind, water, gravity, and ice, and explains four types of mechanical weathering: frost wedging, abrasion, exfoliation, and organic action. The video promises a follow-up on chemical weathering and encourages students to take notes for an upcoming quiz.

Takeaways

  • πŸ“š The video discusses the difference between weathering and erosion, highlighting that weathering is the process of breaking down materials into smaller pieces, while erosion involves the movement of these materials.
  • πŸ”¨ Mechanical or physical weathering is demonstrated using a graham cracker and a rolling pin, showing how materials can be broken into smaller pieces through physical force.
  • πŸ§ͺ Chemical weathering is introduced with a baking soda and vinegar experiment, illustrating how a chemical reaction can change the substance permanently, unlike physical weathering.
  • 🌬 Agents of weathering and erosion include wind, water, gravity, and ice, each causing breakdown and movement of materials in different ways.
  • ❄️ Frost wedging or ice wedging is a type of mechanical weathering where water in fractures of rocks expands upon freezing, causing the rock to break apart.
  • πŸ” Abrasion is identified as the process where earth materials collide, often caused by glaciers, rivers, gravity, or wind, leading to the wearing down of rocks.
  • 🦡 Exfoliation is a type of mechanical weathering where rocks peel away in layers due to the release of pressure, often after the overlying softer rock has been eroded away.
  • 🌳 Organic action is another form of mechanical weathering, where living organisms like trees, animals, or insects physically break up rocks.
  • πŸ“ The video script emphasizes the importance of taking good notes for an upcoming quiz on the mechanical agents of weathering.
  • πŸ“š The next video will cover chemical weathering and erosion, expanding on the concepts introduced in the current video.
  • πŸ’¬ The instructor encourages students to ask questions via Edmodo or email, indicating an open line of communication for further clarification.

Q & A

  • What is the main difference between weathering and erosion?

    -Weathering is the process of breaking down rocks and minerals into smaller pieces without necessarily moving them, while erosion is the process of transporting these broken-down materials from one place to another by agents like wind, water, or ice.

  • What are the two main types of weathering mentioned in the script?

    -The two main types of weathering mentioned are mechanical (or physical) weathering and chemical weathering.

  • Can you explain the concept of mechanical weathering using the example given in the script?

    -Mechanical weathering is demonstrated by smashing a graham cracker into smaller pieces using a rolling pin. This represents the process of physical breakdown of earth materials into smaller pieces.

  • What is an example of chemical weathering provided in the script?

    -An example of chemical weathering is the reaction between baking soda and vinegar, which causes the baking soda to chemically change and produce bubbles, indicating a permanent transformation.

  • What are the agents of weathering and erosion as mentioned in the script?

    -The agents of weathering and erosion include wind, water, gravity, and ice (such as glaciers).

  • What is the process called when water freezes in rock fractures and causes the rock to break apart?

    -This process is called frost wedging or ice wedging, where the expansion of water upon freezing causes the rock fractures to enlarge and the rock to break up.

  • How does abrasion contribute to both weathering and erosion?

    -Abrasion occurs when earth materials, such as rocks, collide with each other. This can happen due to the movement of glaciers, running water in rivers, or even gravity causing rocks to roll down a hill, leading to the breakdown and transportation of materials.

  • What is exfoliation in the context of mechanical weathering?

    -Exfoliation is a type of mechanical weathering where layers of rock peel away due to the release of pressure, often occurring when a magma chamber is exposed and expands after the overlying rock has been worn away.

  • What is organic action in relation to weathering?

    -Organic action refers to the physical breakdown of rocks by living organisms, such as tree roots growing between rocks, animals walking over them, or even insects like ants digging tunnels.

  • Why is it important to take good notes on the types of mechanical weathering discussed in the script?

    -Taking good notes on the types of mechanical weathering is important because it helps in understanding the different processes that break down rocks and minerals, and these concepts will be tested in an upcoming quiz.

Outlines

00:00

πŸŒͺ️ Weathering vs. Erosion: Fundamental Concepts

This paragraph introduces the video's focus on weathering and erosion, explaining the distinction between the two geological processes. Weathering is described as the process of breaking down earth materials into smaller pieces, illustrated by physically crushing a graham cracker. Erosion, on the other hand, is the movement of these materials, exemplified by wind or water transport. The paragraph also touches on chemical weathering, using a baking soda and vinegar reaction to demonstrate a chemical change that cannot be reversed. The agents of weathering and erosion are mentioned, including wind, water, gravity, and ice, setting the stage for a deeper dive into the types of mechanical weathering in subsequent content.

05:02

πŸ”οΈ Mechanical Weathering: Processes and Examples

This paragraph delves into the specifics of mechanical or physical weathering, detailing four primary types: frost wedging/ice wedging, abrasion, exfoliation, and organic action. Frost wedging is explained as the expansion of water when it freezes, causing rocks to crack. Abrasion is described as the collision of earth materials, such as rocks, which can be caused by glaciers, rivers, gravity, or wind. Exfoliation is depicted as the peeling away of rock layers due to the release of pressure in geological formations. Organic action refers to the physical breakdown of rocks by living organisms, like tree roots or burrowing animals. The paragraph provides examples to illustrate each type, emphasizing the relevance of these processes in various environments, not just in mountainous or glacial regions.

Mindmap

Keywords

πŸ’‘Weathering

Weathering is the process where rocks and minerals are broken down into smaller pieces by natural forces. In the video, it is differentiated from erosion by explaining that weathering involves the breakdown without the displacement of material. An example given is mechanical or physical weathering, where a grand cracker is smashed into smaller pieces using a rolling pin, illustrating how rocks can be broken down by forces like wind or ice.

πŸ’‘Erosion

Erosion is the process of moving weathered rock and soil from one place to another by natural agents such as wind, water, or ice. The video script uses the analogy of moving the crushed grand cracker crumbs to explain how erosion works. It's distinguished from weathering by the movement of material, not just its breakdown.

πŸ’‘Mechanical Weathering

Mechanical weathering, also referred to as physical weathering in the script, involves the breakdown of rocks into smaller pieces without changing their chemical composition. The video demonstrates this with the grand cracker example, where the cracker is physically smashed. It's a key concept in understanding how rocks are broken down by natural forces like temperature changes, water, or abrasion.

πŸ’‘Chemical Weathering

Chemical weathering is the process where the chemical composition of rocks is altered by reactions with substances like water or acids. The video script introduces this concept by showing a chemical reaction between baking soda and vinegar, which causes the baking soda to change chemically and cannot be reversed, illustrating how rocks can be chemically altered over time.

πŸ’‘Agents of Weathering and Erosion

The agents of weathering and erosion are the forces that cause these processes to occur. The script mentions wind, water, gravity, and ice as the primary agents. For instance, wind can move rocks and cause abrasion, while water can cause both weathering through chemical reactions and erosion by moving sediment.

πŸ’‘Frost Wedging

Frost wedging, also known as ice wedging, is a type of mechanical weathering where water that has seeped into cracks in rocks freezes, expands, and causes the rock to break apart. The video script describes this process using the example of water in rock fractures that expands upon freezing, leading to the rock breaking up.

πŸ’‘Abrasion

Abrasion is the process by which rocks and sediments are worn down through friction and collision with other rocks or sediments. The video script explains that glaciers can cause abrasion as they move downhill, carrying rocks that grind against the mountain's rocks. Additionally, running water and wind can also cause abrasion by moving earth materials that collide with each other.

πŸ’‘Exfoliation

Exfoliation is a type of mechanical weathering where rocks peel away in layers due to the release of pressure. The video script uses the analogy of a skin peeling away to describe how rocks can exfoliate when the pressure from overlying rock is removed, such as when a magma chamber expands outward after the softer rock above it has eroded away.

πŸ’‘Organic Action

Organic action refers to the role of living organisms in breaking down rocks. In the video, examples include tree roots growing between rocks, animals walking over rocks, or even ants digging tunnels. This concept is important as it shows how biological processes can contribute to the physical breakdown of rock material.

πŸ’‘Glaciers

Glaciers are massive bodies of ice that move slowly across land and are significant agents of both weathering and erosion. The script mentions glaciers as a cause of frost wedging and abrasion, highlighting their role in shaping landscapes through the movement of large amounts of rock and sediment.

Highlights

Introduction to the topic of weathering and erosion, discussing the differences between the two processes.

Demonstration of mechanical or physical weathering using a graham cracker and a rolling pin to illustrate the concept.

Explanation of erosion as the movement of broken materials, differentiated from weathering which involves breaking down.

Introduction to chemical weathering with a baking soda and vinegar experiment to show a chemical reaction.

Differentiation between physical and chemical weathering based on whether the substance's chemical composition changes.

Listing of the agents of weathering and erosion, including wind, water, gravity, and ice.

Discussion of the specific type of mechanical weathering called frost wedging or ice wedging, using water freezing in rock fractures as an example.

Illustration of how ice wedging contributes to the formation of pointed and jagged mountain peaks and potholes in roads.

Explanation of abrasion as the collision of earth materials, with examples of how glaciers, water, and gravity can cause this type of weathering.

Introduction to exfoliation as a type of mechanical weathering caused by the release of pressure and expansion of rock layers.

Description of organic action as a form of mechanical weathering caused by living organisms that physically break up rocks.

Emphasis on the importance of taking good notes for an upcoming quiz on the mechanical agents of weathering.

Announcement of a follow-up video that will cover chemical weathering and erosion.

Invitation for students to ask questions via Edmodo or email, encouraging interaction and clarification of concepts.

Highlighting the practical application of the concepts discussed in class and the importance of understanding the agents of weathering and erosion.

Reinforcement of the distinction between physical and chemical weathering processes and their outcomes.

Transcripts

play00:14

you

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alright guys this video is going to get

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into weathering and erosion we'll talk

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about the difference between weathering

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and erosion we'll talk about what the

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agents are of weathering and erosion and

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what that means is what causes them to

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happen and we'll also get into the types

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of mechanical or physical weather and

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mechanical and physical mean the same

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thing in the next video we'll get into

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chemical weathering and erosion make

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sure you take good notes on this one or

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the quiz on in class also a couple of

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activities that we're going to do follow

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up with this video as well I'll check

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your notes in class for a stamp let me

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know if you have any questions alright

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guys so what is the difference between

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weathering and erosion

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let's go ahead and take a look at this

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graham-cracker here and let's take this

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rolling pin and let's smash it up so as

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I do this I'm taking the big Grand

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cracker and I'm breaking it up into

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smaller pieces little tiny crumbs that

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what weathering is now this type of

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weathering is specifically what's called

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mechanical weathering or physical

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weathering it's taking earth material

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and it's smashing it up into little

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pieces now what's the difference between

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this and erosion erosion is when you

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take it and you move it somehow either

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by wind like that or maybe water will

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wash it away or maybe a glacier will

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wash it away really the big difference

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is that weathering is when something

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gets smashed like this and erosion is

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when something moves it now weathering

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doesn't need to be just be a physical

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process here I have another substance

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this is baking soda I'm going to add a

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little bit of vinegar here and you're

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going to notice

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hopefully that it bubbles this is a

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chemical reaction this chemical reaction

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is chemical weathering I'm chemically

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changing the substance the baking soda

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is changing forever it chemically cannot

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be changed back to what it was when it

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first started so what's a big difference

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one is a chemical one's a physical

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process where at the end it's chemically

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the same and the other is a chemical

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process where at the end its chemically

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different and it can't be undone alright

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so what are the agents of weathering and

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erosion and what I mean by agents is

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what are the things that

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caused it to happen first thing is the

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wind the wind not necessarily the wind

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itself but when the winds blow rocks

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across a desert environment then rocks

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can smash and rocks and they break up

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then there's the water now water can

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cause weathering and erosion in a number

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of different ways but primarily caused

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something called abrasion we'll get into

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that in just a little bit but water

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carrying rocks and those rocks then

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smashing into one another there's also

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gravity rocks just rolling down a hill

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and then there's ice and again there's a

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couple different ways that ice can cause

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weathering and erosion to happen so to

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understand these better let's get into

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some more specific details and talk

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about the types of mechanical or

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physical weathering okay so the first

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type of mechanical weathering that we're

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going to talk about is I sweating or

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frost wedging they both mean the same

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thing here we have a rock that has some

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fractures in it filled with water and if

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we lower the temperature of that water

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and we freeze it that water is going to

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cool down turn into ice and when it does

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water expands when it freezes and it's

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going to make those fractures much

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larger and it will be it will break up

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those rocks let's go ahead and see that

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again here's the water we freeze it it

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expands notice that the fractions and

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rock it bigger and then it breaks up the

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rocks this is called frost wedging or

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ice watching same thing ice white dreams

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going to be really important when we

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start to talk about glaciers take a look

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at this picture here notice how pointed

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and how jagged that mountain looks that

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all formed because of erosion due to ice

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wedging and if you take a look at the

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bottom picture here there's this big

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pothole in the middle of the road this

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pothole formed because of ice washing so

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just because we don't live in the

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mountains near glaciers doesn't mean

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we're not affected by ice why dang

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alright so next we have abrasion which

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simply means the collision of earth

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material remember earth material can be

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rocks minerals anything like that and if

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we can begin up here in the mountains

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and we can go ahead and take a look at a

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glacier glaciers can certainly cause

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abrasion house also because glaciers

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hold in a lot of rocks and as those

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glaciers move downhill because of

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gravity the rocks within the glacier

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grind up against the rocks of the

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mountains

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and it causes those rocks to smash up so

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glaciers can absolutely cause abrasion

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the let's say the glacier melts or some

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rain comes down and we get a little

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river that forms down the side of the

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mountain and that running water that

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running water can cause rocks to slam

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into one another why because as that

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water cascades down the mountain it's

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going to carry earth material with it

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and as that earth material gets carried

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in the water the rocks within it will

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smash up against one another then we

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also simply have gravity we have a

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hillside here and gravity can run rocks

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on down the side of the mountain which

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can cause them to smash up into one

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another so gravity is also a cause of

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abrasion and we also have wind if

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there's wind blown across the land here

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that can cause rocks to smash into one

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another and then as rocks fall into the

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ocean we have water again that can cause

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these rocks to smash up so one of the

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big things that cause abrasion to happen

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we have wind water gravity and ice like

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in glaciers okay our third type of

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mechanical weathering is called

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exfoliation you may have heard of

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exfoliation before like the peeling away

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of layers of skin or dead skin so

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exfoliation happens because of a release

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of pressure and here's what I mean by

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that over here we have this big igneous

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formation underneath the ground maybe a

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batholith or a laccolith or something we

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learned about that back with volcanoes

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and then something washes away all these

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softer rocks up on top and exposes that

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hardened magma chamber

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well this heart of mammoth chambers been

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compressed over a very long period of

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time and eventually once enough of that

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softer Rock is worn away and the

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pressure from the overlying Rock is gone

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that hardened magma chamber is going to

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expand outward and cause these rocks to

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peel away in layers and that's what

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causes exfoliation and lastly we have

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organic action what that means is

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anything living that can break up rocks

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here we have a tree that's growing

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between rocks but it's not necessarily

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just a tree it could be an animal that's

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walking over the rocks that breaks them

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up it could be

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an ant digging a tunnel it could be a

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snake burrowing through the ground

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basically anything living that can break

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up rocks physically and we call that

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organic action alright so in this video

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we discussed the differences between

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weathering and erosion we talked about

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the causes of weathering and erosion or

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the agents of weathering and erosion and

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we got into the four types of mechanical

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or physical weathering but we got a

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video coming that's going to discuss

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chemical weathering but make sure you

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took really good notes on the mechanical

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agents of weathering your never quiz on

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it pretty soon and we're also going to

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apply it in lecture I'm going to check

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your notes for a stamp please feel free

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to send me a message on Edmodo with any

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questions or you can send me an email

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Related Tags
WeatheringErosionMechanicalChemicalFrost WedgingAbrasionExfoliationOrganic ActionEducationalGeologyScience Class