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Deposition, Weathering, and Erosion. Weathering _767454.jpg What Caused This?

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Presentation on theme: "Deposition, Weathering, and Erosion. Weathering _767454.jpg What Caused This?"— Presentation transcript:

1 Deposition, Weathering, and Erosion

2 Weathering

3 http://commons.wikimedia.org/wiki/File:Toad_Rock_-_geograph.org.uk_- _767454.jpg What Caused This? http://en.wikipedia.org/wiki/File:KharazaArch.jpg

4 Effects of Weathering Weathering is a process that breaks down rock and other substances at Earth’s surfaceWeathering is a process that breaks down rock and other substances at Earth’s surface –creates soil –softer rock weathers faster –weathering is fastest in hot and wet climates

5 Types of Weathering Mechanical WeatheringMechanical Weathering Chemical WeatheringChemical Weathering

6 What is Mechanical Weathering? Breakdown of rock into smaller pieces without any change in the chemical composition of its minerals.Breakdown of rock into smaller pieces without any change in the chemical composition of its minerals. –Sometimes called “physical” weathering –Rock is torn apart by physical force, rather than by chemical breakdown.

7 Mechanical Weathering Works very slowlyWorks very slowly There are different typesThere are different types –ice wedging –exfoliation –thermal –biotic

8 Mechanical - Ice Wedging  Ice Wedging –Water fills joints of rocks and freezes –Freezing expands the water by 10% –Repeated freeze and thaw cycles over the years causes rock to break along joint

9 Mechanical - Exfoliation Exfoliation or unloadingExfoliation or unloading –Rock breaks off into leaves or sheets along joints which are parallel to the ground surface

10 Mechanical - Thermal Thermal expansionThermal expansion –Repeated daily heating and cooling of rock –Different minerals expand and contract at different rates causing the rock to split

11 Mechanical - Biotic Biotic – means lifeBiotic – means life –Weathering caused by living organisms –Plant roots, digging animals, microscopic plants and animals, algae and fungi.

12 Mechanical Weathering

13 What is Chemical Weathering? Breakdown of rock into smaller pieces because of change in the chemical composition of its minerals.Breakdown of rock into smaller pieces because of change in the chemical composition of its minerals. –Chemical reactions break down the bonds holding the rocks together, causing them to fall apart. –Chemical weathering occurs in all types of rock but smaller rocks are more susceptible because they have a greater amount of surface area.

14 Chemical Weathering Types of chemical weatheringTypes of chemical weathering Oxidation (oxygen)Oxidation (oxygen) Hydrolysis (water)Hydrolysis (water) Carbonation (carbon dioxide)Carbonation (carbon dioxide) Biotic (living organisms)Biotic (living organisms) Acid rainAcid rain

15 Chemical - Oxidation Oxidation - oxygen combines with other elements in rocks to form new types of rock.Oxidation - oxygen combines with other elements in rocks to form new types of rock. –Causes a “rusting” of the rock, often causes a color change in the rock

16 Chemical - Hydrolysis Hydrolysis - water combines with the substances in rocks to form new types of rockHydrolysis - water combines with the substances in rocks to form new types of rock –New substances are softer than the original rock types

17 Chemical - Carbonation Carbonation – Carbon dioxide is dissolved in water making carbonic acid, which eats away at the rockCarbonation – Carbon dioxide is dissolved in water making carbonic acid, which eats away at the rock –Weak acid is formed when carbon dioxide in the air mixes with rain. This is the same acid found in soft drinks. –Weak acid is formed when carbon dioxide in the air mixes with rain. This is the same acid found in soft drinks.

18 Chemical - Biotic Organisms - living organisms can cause changes in the chemistry of rock –Plants –Plants lower the local pH to make it more acidic –Bacteria –Bacteria act as catalysts in various geochemical processes

19 Chemical Weathering

20 Weathering by Water Most important agent of chemical weathering It can dissolve rock and minerals in rock

21 Weathering by Waves Waves weather the land: –Mechanical weathering Broken down into smaller pieces –Chemical weathering Dissolved in water

22 Weathering by Waves

23 Weathering by Wind Wind weathers the land by mechanical means –Abrasion Very slow process

24 Weathering by Wind

25

26 weathering The breaking down of rock into smaller pieces that remain next to each other. Weathering forms sediments ice wedging mechanical weatheringchemical weathering Physical breaking of rock without any change in the chemical composition of the rock. The breaking down of rock into smaller pieces because of chemical changes within the rock. hydrolysis carbonation biotic thermal biotic force oxidation exfoliation

27 Erosion

28 What Caused This? http://commons.wikimedia.org/wiki/File:Wind_erosion_ Seminole_Canyon.JPG http://commons.wikimedia.org/wiki/File:Bave ntian_Clay_Beds_-_geograph.org.uk_- _1776748.jpg http://commons.wikimedia.org/wiki/File:Water_erosion_ below_Hay_Bluff_-_geograph.org.uk_-_1074175.jpg

29 Erosion Movement of weathered rock and soil to a new location. –gravity –water –glaciers –waves –wind

30 What Is Gravitational Erosion? downward movement of rock and sediments, mainly due to the force of gravity.

31 Erosion by Gravity Gravity can erode landscapes –Landslides –Mudflow –Slump –Creep

32 Erosion by Water Moving water is the strongest agent of erosion that has shaped Earth’s land surface Erosion by water starts with rain. As the rain runs downhill, it carries soil rock and other material with it

33 Erosion by Water The rate depends on amount of rain, vegetation, type of soil, shape of land, and how people use the land As water moves fast, it picks up sediment As water slows down, it drops sediment

34 Water

35 What Is Glacial Erosion? moves and carries rocks, grinding the rocks beneath the glaciermoves and carries rocks, grinding the rocks beneath the glacier –Glaciers pluck and abrade to cause erosion

36 Erosion by Glaciers

37 What Is Wave Erosion? Waves - relentless pounding of waves that erodes the weaker, softer rock –Can take over 100 years to erode a rock to sand

38 Erosion by Waves When waves hit rocky coastlines, the impact can break off pieces of the rock The sand and sediment in the waves can also act like sandpaper and wear away rock

39 Waves

40 What Is Wind Erosion? wind picks up surface material and moves it, weakest agent of erosionwind picks up surface material and moves it, weakest agent of erosion –responsible for creating great deserts like the Sahara Desert and Gobi

41 Wind

42 erosion Movement of sediments from one place to another. wind gravity waves water glaciers

43 Deposition

44 laying down (dropping) of sediment carried by wind, water, or icelaying down (dropping) of sediment carried by wind, water, or ice

45 Deposition by Water Water is the strongest agent of deposition. Rivers deposit soil and sediment on their flood plains and deltas Good farmland is usually based on land where sediment was deposited by water

46 Water Deposition Deposition by Water

47 Deposition by Glaciers When a glacier melts, it deposits the sediment it eroded from the land This deposition can create new landforms and deposit sediment in new areas –Till – material deposited on the land’s surface –Moraine – ridge at the edge of a glacier

48 Glacier Deposition

49 Deposition by Waves Waves shape coastlines by depositing sand on the beach The type of sand is determined by the sediment on the ocean floor –White sand –Black sand

50 Deposition by Waves

51 Deposition by Wind Wind is the weakest agent of deposition When it drops the sediment it is carrying, it can form dunes or mounds

52 Deposition by Wind

53 deposition Laying down of sediment that was carried in from another place. water glacier waves wind

54 Wind, water, and waves work together in the processes of deposition, weathering, and erosion

55 What’s the Difference? WEATHERING - think weather wearing rock down EROSION - think of a road and traveling DEPOSITION – think of depositing money in a bank


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