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Weathering, Erosion, and
         Soil
         CHAPTER 7
Weathering
  SECTION 7.1
Introduction
Introduction

weathering -the process by which rocks on
or near earth’s surface break down and
change
Introduction

weathering -the process by which rocks on
or near earth’s surface break down and
change

erosion - the removal and transport of
weathered materials from one location to
another
Mechanical Weathering
Mechanical Weathering

 mechanical weathering (physical weathering)
 - the process by which rocks and minerals
 break down into smaller pieces
Mechanical Weathering

 mechanical weathering (physical weathering)
 - the process by which rocks and minerals
 break down into smaller pieces

   no change in rocks composition
Mechanical Weathering

 mechanical weathering (physical weathering)
 - the process by which rocks and minerals
 break down into smaller pieces

   no change in rocks composition

   only changes size and sometimes shape
Temperature
Temperature
when water freezes it expands and increases
in volume
Temperature
when water freezes it expands and increases
in volume

  water in rocks freezes, expands, exerts
  pressure on rocks and causes to split
Temperature
when water freezes it expands and increases
in volume

  water in rocks freezes, expands, exerts
  pressure on rocks and causes to split

    frost wedging - the repeated thawing
    and freezing of water in the cracks of
    rocks
Temperature
when water freezes it expands and increases
in volume

  water in rocks freezes, expands, exerts
  pressure on rocks and causes to split

    frost wedging - the repeated thawing
    and freezing of water in the cracks of
    rocks

       responsible for formation of potholes
       in rocks
Pressure
Pressure
bedrock @ great depths is under pressure
from overlaying rock
Pressure
bedrock @ great depths is under pressure
from overlaying rock

  when layers removed, former layers
  buried can now expand (cracks form)
Pressure
bedrock @ great depths is under pressure
from overlaying rock

  when layers removed, former layers
  buried can now expand (cracks form)

exfoliation - the process by which outer rock
layers are stripped away
Pressure
bedrock @ great depths is under pressure
from overlaying rock

  when layers removed, former layers
  buried can now expand (cracks form)

exfoliation - the process by which outer rock
layers are stripped away

  roots of trees can grow in cracks and
  further split rocks
Chemical Weathering
Chemical Weathering
chemical weathering
- the process by
which minerals
undergo changes in
their composition as
the result of
chemical reactions
Chemical Weathering
chemical weathering
- the process by
which minerals
undergo changes in
their composition as
the result of
chemical reactions
Chemical Weathering
chemical weathering
- the process by
which minerals
undergo changes in
their composition as
the result of
chemical reactions
Chemical Weathering
chemical weathering    5 significant agents:
- the process by
which minerals
undergo changes in
their composition as
the result of
chemical reactions
Chemical Weathering
chemical weathering    5 significant agents:
- the process by
which minerals           water
undergo changes in
their composition as
the result of
chemical reactions
Chemical Weathering
chemical weathering    5 significant agents:
- the process by
which minerals           water
undergo changes in
their composition as     oxygen
the result of
chemical reactions
Chemical Weathering
chemical weathering    5 significant agents:
- the process by
which minerals           water
undergo changes in
their composition as     oxygen
the result of
chemical reactions       carbon dioxide
Chemical Weathering
chemical weathering    5 significant agents:
- the process by
which minerals           water
undergo changes in
their composition as     oxygen
the result of
chemical reactions       carbon dioxide

                         acids
Chemical Weathering
chemical weathering    5 significant agents:
- the process by
which minerals           water
undergo changes in
their composition as     oxygen
the result of
chemical reactions       carbon dioxide

                         acids

                         temperature
Water
Water

can dissolve many kinds of minerals and
rocks
Water

can dissolve many kinds of minerals and
rocks

  has active role in some reactions
Water

can dissolve many kinds of minerals and
rocks

  has active role in some reactions

  serves as medium through which other
  reactions occur
Water

can dissolve many kinds of minerals and
rocks

  has active role in some reactions

  serves as medium through which other
  reactions occur

     hydrolysis - the reaction of water w/
     other substances
Oxygen
Oxygen

can combine w/ other substances
Oxygen

can combine w/ other substances

oxidation - the chemical reaction of oxygen
w/ other substances
Oxygen

can combine w/ other substances

oxidation - the chemical reaction of oxygen
w/ other substances

  ex. iron readily combines w/ oxygen in
  atmosphere to form minerals w/ oxidized
  form of iron
Carbon Dioxide
Carbon Dioxide

produced by living organisms during
respiration
Carbon Dioxide

produced by living organisms during
respiration

when combined w/ water in air, it forms
weak carbonic acid that falls to earth’s
surface as precipitation
Carbon Dioxide

produced by living organisms during
respiration

when combined w/ water in air, it forms
weak carbonic acid that falls to earth’s
surface as precipitation

  carbonic acid reacts w/ minerals to
  dissolve rock
Acid Rain
Acid Rain

caused mainly by oxidation of sulfur dioxide
and nitrogen oxides released into air by
human activities
Acid Rain

caused mainly by oxidation of sulfur dioxide
and nitrogen oxides released into air by
human activities

  2 gases combine w/ oxygen and water in
  air to form sulfuric and nitric acid
Acid Rain

caused mainly by oxidation of sulfur dioxide
and nitrogen oxides released into air by
human activities

  2 gases combine w/ oxygen and water in
  air to form sulfuric and nitric acid

     pH = 5.6 or lower
Acid Rain

caused mainly by oxidation of sulfur dioxide
and nitrogen oxides released into air by
human activities

  2 gases combine w/ oxygen and water in
  air to form sulfuric and nitric acid

     pH = 5.6 or lower

       precipitation affects wildlife
What Affects the Rate
   of Weathering?
What Affects the Rate
   of Weathering?
 natural weathering occurs very slowly
What Affects the Rate
   of Weathering?
 natural weathering occurs very slowly

 certain conditions and interactions can
 accelerate or slow weathering
What Affects the Rate
   of Weathering?
 natural weathering occurs very slowly

 certain conditions and interactions can
 accelerate or slow weathering

   climate
What Affects the Rate
   of Weathering?
 natural weathering occurs very slowly

 certain conditions and interactions can
 accelerate or slow weathering

   climate

   rock type
What Affects the Rate
   of Weathering?
 natural weathering occurs very slowly

 certain conditions and interactions can
 accelerate or slow weathering

   climate

   rock type

   surface area
What Affects the Rate
   of Weathering?
 natural weathering occurs very slowly

 certain conditions and interactions can
 accelerate or slow weathering

   climate

   rock type

   surface area

   topography
Climate
Climate

major influence on rate of chemical
weathering
Climate

major influence on rate of chemical
weathering

variables of climate:
Climate

major influence on rate of chemical
weathering

variables of climate:

  precipitation
Climate

major influence on rate of chemical
weathering

variables of climate:

  precipitation

  temperature
Climate

major influence on rate of chemical
weathering

variables of climate:

  precipitation

  temperature

  evaporation
Climate cont...
Climate cont...

interaction b/c temperature and precipitation
has greatest effect
Climate cont...

interaction b/c temperature and precipitation
has greatest effect

  chemical weathering occurs readily in
  climates of warm temperatures
Climate cont...

interaction b/c temperature and precipitation
has greatest effect

  chemical weathering occurs readily in
  climates of warm temperatures

physical weathering occurs readily in cool,
dry climates
Rock Type and
 Composition
Rock Type and
       Composition

how hard or resistant rocks are to be broken
down, depends on their type an composition
Rock Type and
       Composition

how hard or resistant rocks are to be broken
down, depends on their type an composition

  sedimentary rocks more easily weathered
  than harder igneous and metamorphic
  rocks
Surface Area
Surface Area


as pieces get smaller, surface areas increase
Surface Area


as pieces get smaller, surface areas increase

  the higher the total surface area, the
  more weathering that occurs
Topography and Other
      Variables
Topography and Other
        Variables
materials on level areas likely to remain in place as
they undergo changes
Topography and Other
        Variables
materials on level areas likely to remain in place as
they undergo changes

materials on slopes have greater tendency to move as
result of gravity
Topography and Other
        Variables
materials on level areas likely to remain in place as
they undergo changes

materials on slopes have greater tendency to move as
result of gravity

  as move down slope, exposes underlying rock
  surfaces and provides more opportunities for
  weathering to occur
Topography and Other
        Variables
materials on level areas likely to remain in place as
they undergo changes

materials on slopes have greater tendency to move as
result of gravity

  as move down slope, exposes underlying rock
  surfaces and provides more opportunities for
  weathering to occur

organisms affect weathering
Topography and Other
        Variables
materials on level areas likely to remain in place as
they undergo changes

materials on slopes have greater tendency to move as
result of gravity

  as move down slope, exposes underlying rock
  surfaces and provides more opportunities for
  weathering to occur

organisms affect weathering

  decaying organic matter
Topography and Other
        Variables
materials on level areas likely to remain in place as
they undergo changes

materials on slopes have greater tendency to move as
result of gravity

  as move down slope, exposes underlying rock
  surfaces and provides more opportunities for
  weathering to occur

organisms affect weathering

  decaying organic matter

  living plant roots
Erosion and Deposition
       SECTION 7.2
Intro
Intro

erosion process that transports earth’s
minerals from one location to another
Intro

erosion process that transports earth’s
minerals from one location to another

  running water, glaciers, wind, and ocean
  currents
Intro

erosion process that transports earth’s
minerals from one location to another

  running water, glaciers, wind, and ocean
  currents

     deposition - minerals are dropped in
     another location
Gravity’s Role in Erosion
Gravity’s Role in Erosion


 force gravity pulls materials down slope
Gravity’s Role in Erosion


 force gravity pulls materials down slope

   w/out gravity, glaciers would not move
   downslope and streams would not flow
Erosion by Running
      Water
Erosion by Running
           Water
water has a lot of power to move large particles
Erosion by Running
           Water
water has a lot of power to move large particles

  great potential to erode materials b/c steeper
  slope, faster water flows
Erosion by Running
           Water
water has a lot of power to move large particles

  great potential to erode materials b/c steeper
  slope, faster water flows

small streams join into larger streams (watershed)
Erosion by Running
           Water
water has a lot of power to move large particles

  great potential to erode materials b/c steeper
  slope, faster water flows

small streams join into larger streams (watershed)

rill erosion - erosion by running water in small
channels, on side of slope
Erosion by Running
           Water
water has a lot of power to move large particles

  great potential to erode materials b/c steeper
  slope, faster water flows

small streams join into larger streams (watershed)

rill erosion - erosion by running water in small
channels, on side of slope

gully erosion - when channels becomes steep and
wide
Erosion by Running
           Water
water has a lot of power to move large particles

  great potential to erode materials b/c steeper
  slope, faster water flows

small streams join into larger streams (watershed)

rill erosion - erosion by running water in small
channels, on side of slope

gully erosion - when channels becomes steep and
wide

  problem in farming and grazing areas
Costal Deposition and
       Erosion
Costal Deposition and
       Erosion

weathering process continue in ocean
Costal Deposition and
       Erosion

weathering process continue in ocean

  ocean currents, waves, and tides carve
  out cliffs, arches, and edges of continents
Costal Deposition and
       Erosion

weathering process continue in ocean

  ocean currents, waves, and tides carve
  out cliffs, arches, and edges of continents

     sand particles accumulate on shorelines
     forming dunes and beaches
Costal Deposition and
    Erosion cont...
Costal Deposition and
    Erosion cont...
erosion occurs
Costal Deposition and
    Erosion cont...
erosion occurs

  constant movement of water
Costal Deposition and
    Erosion cont...
erosion occurs

  constant movement of water

     sand repeatedly picked up and moved
Costal Deposition and
    Erosion cont...
erosion occurs

  constant movement of water

     sand repeatedly picked up and moved

       sandbars form
Costal Deposition and
    Erosion cont...
erosion occurs

  constant movement of water

     sand repeatedly picked up and moved

       sandbars form

          can turn into barrier islands
Glacier Erosion
Glacier Erosion
erosional effects large-scale and dramatic
Glacier Erosion
erosional effects large-scale and dramatic

  scrape and gorge out large sections
Glacier Erosion
erosional effects large-scale and dramatic

  scrape and gorge out large sections

     can carry huge rocks and piles of debris over
     great distance
Glacier Erosion
erosional effects large-scale and dramatic

  scrape and gorge out large sections

     can carry huge rocks and piles of debris over
     great distance

       features left in wake of glacier movement:
Glacier Erosion
erosional effects large-scale and dramatic

  scrape and gorge out large sections

     can carry huge rocks and piles of debris over
     great distance

       features left in wake of glacier movement:

          valleys, majestic water falls, lakes,
          deposits of sediment
Wind Erosion
Wind Erosion


major erosional agent in areas that
experience limited rain and high
temperatures
Wind Erosion


major erosional agent in areas that
experience limited rain and high
temperatures

  areas have little vegetation to hold
  sediments in place
Wind Barriers
Wind Barriers


reduces effect of wind erosion
Wind Barriers


reduces effect of wind erosion

  trees and other vegetation planted
  perpendicular to direction of wind
Erosion by Plants,
Animals, and Humans
Erosion by Plants,
Animals, and Humans

as plants and animals carry on life process
they move materials from one place to
another
Erosion by Plants,
Animals, and Humans

as plants and animals carry on life process
they move materials from one place to
another

humans excavate areas

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Chpater 7 Presentation (Cp)

  • 1. Weathering, Erosion, and Soil CHAPTER 7
  • 3.
  • 5. Introduction weathering -the process by which rocks on or near earth’s surface break down and change
  • 6. Introduction weathering -the process by which rocks on or near earth’s surface break down and change erosion - the removal and transport of weathered materials from one location to another
  • 8. Mechanical Weathering mechanical weathering (physical weathering) - the process by which rocks and minerals break down into smaller pieces
  • 9. Mechanical Weathering mechanical weathering (physical weathering) - the process by which rocks and minerals break down into smaller pieces no change in rocks composition
  • 10. Mechanical Weathering mechanical weathering (physical weathering) - the process by which rocks and minerals break down into smaller pieces no change in rocks composition only changes size and sometimes shape
  • 12. Temperature when water freezes it expands and increases in volume
  • 13. Temperature when water freezes it expands and increases in volume water in rocks freezes, expands, exerts pressure on rocks and causes to split
  • 14. Temperature when water freezes it expands and increases in volume water in rocks freezes, expands, exerts pressure on rocks and causes to split frost wedging - the repeated thawing and freezing of water in the cracks of rocks
  • 15. Temperature when water freezes it expands and increases in volume water in rocks freezes, expands, exerts pressure on rocks and causes to split frost wedging - the repeated thawing and freezing of water in the cracks of rocks responsible for formation of potholes in rocks
  • 16.
  • 18. Pressure bedrock @ great depths is under pressure from overlaying rock
  • 19. Pressure bedrock @ great depths is under pressure from overlaying rock when layers removed, former layers buried can now expand (cracks form)
  • 20. Pressure bedrock @ great depths is under pressure from overlaying rock when layers removed, former layers buried can now expand (cracks form) exfoliation - the process by which outer rock layers are stripped away
  • 21. Pressure bedrock @ great depths is under pressure from overlaying rock when layers removed, former layers buried can now expand (cracks form) exfoliation - the process by which outer rock layers are stripped away roots of trees can grow in cracks and further split rocks
  • 22.
  • 24. Chemical Weathering chemical weathering - the process by which minerals undergo changes in their composition as the result of chemical reactions
  • 25. Chemical Weathering chemical weathering - the process by which minerals undergo changes in their composition as the result of chemical reactions
  • 26. Chemical Weathering chemical weathering - the process by which minerals undergo changes in their composition as the result of chemical reactions
  • 27. Chemical Weathering chemical weathering 5 significant agents: - the process by which minerals undergo changes in their composition as the result of chemical reactions
  • 28. Chemical Weathering chemical weathering 5 significant agents: - the process by which minerals water undergo changes in their composition as the result of chemical reactions
  • 29. Chemical Weathering chemical weathering 5 significant agents: - the process by which minerals water undergo changes in their composition as oxygen the result of chemical reactions
  • 30. Chemical Weathering chemical weathering 5 significant agents: - the process by which minerals water undergo changes in their composition as oxygen the result of chemical reactions carbon dioxide
  • 31. Chemical Weathering chemical weathering 5 significant agents: - the process by which minerals water undergo changes in their composition as oxygen the result of chemical reactions carbon dioxide acids
  • 32. Chemical Weathering chemical weathering 5 significant agents: - the process by which minerals water undergo changes in their composition as oxygen the result of chemical reactions carbon dioxide acids temperature
  • 33. Water
  • 34. Water can dissolve many kinds of minerals and rocks
  • 35. Water can dissolve many kinds of minerals and rocks has active role in some reactions
  • 36. Water can dissolve many kinds of minerals and rocks has active role in some reactions serves as medium through which other reactions occur
  • 37. Water can dissolve many kinds of minerals and rocks has active role in some reactions serves as medium through which other reactions occur hydrolysis - the reaction of water w/ other substances
  • 39. Oxygen can combine w/ other substances
  • 40. Oxygen can combine w/ other substances oxidation - the chemical reaction of oxygen w/ other substances
  • 41. Oxygen can combine w/ other substances oxidation - the chemical reaction of oxygen w/ other substances ex. iron readily combines w/ oxygen in atmosphere to form minerals w/ oxidized form of iron
  • 43. Carbon Dioxide produced by living organisms during respiration
  • 44. Carbon Dioxide produced by living organisms during respiration when combined w/ water in air, it forms weak carbonic acid that falls to earth’s surface as precipitation
  • 45. Carbon Dioxide produced by living organisms during respiration when combined w/ water in air, it forms weak carbonic acid that falls to earth’s surface as precipitation carbonic acid reacts w/ minerals to dissolve rock
  • 47. Acid Rain caused mainly by oxidation of sulfur dioxide and nitrogen oxides released into air by human activities
  • 48. Acid Rain caused mainly by oxidation of sulfur dioxide and nitrogen oxides released into air by human activities 2 gases combine w/ oxygen and water in air to form sulfuric and nitric acid
  • 49. Acid Rain caused mainly by oxidation of sulfur dioxide and nitrogen oxides released into air by human activities 2 gases combine w/ oxygen and water in air to form sulfuric and nitric acid pH = 5.6 or lower
  • 50. Acid Rain caused mainly by oxidation of sulfur dioxide and nitrogen oxides released into air by human activities 2 gases combine w/ oxygen and water in air to form sulfuric and nitric acid pH = 5.6 or lower precipitation affects wildlife
  • 51. What Affects the Rate of Weathering?
  • 52. What Affects the Rate of Weathering? natural weathering occurs very slowly
  • 53. What Affects the Rate of Weathering? natural weathering occurs very slowly certain conditions and interactions can accelerate or slow weathering
  • 54. What Affects the Rate of Weathering? natural weathering occurs very slowly certain conditions and interactions can accelerate or slow weathering climate
  • 55. What Affects the Rate of Weathering? natural weathering occurs very slowly certain conditions and interactions can accelerate or slow weathering climate rock type
  • 56. What Affects the Rate of Weathering? natural weathering occurs very slowly certain conditions and interactions can accelerate or slow weathering climate rock type surface area
  • 57. What Affects the Rate of Weathering? natural weathering occurs very slowly certain conditions and interactions can accelerate or slow weathering climate rock type surface area topography
  • 59. Climate major influence on rate of chemical weathering
  • 60. Climate major influence on rate of chemical weathering variables of climate:
  • 61. Climate major influence on rate of chemical weathering variables of climate: precipitation
  • 62. Climate major influence on rate of chemical weathering variables of climate: precipitation temperature
  • 63. Climate major influence on rate of chemical weathering variables of climate: precipitation temperature evaporation
  • 65. Climate cont... interaction b/c temperature and precipitation has greatest effect
  • 66. Climate cont... interaction b/c temperature and precipitation has greatest effect chemical weathering occurs readily in climates of warm temperatures
  • 67. Climate cont... interaction b/c temperature and precipitation has greatest effect chemical weathering occurs readily in climates of warm temperatures physical weathering occurs readily in cool, dry climates
  • 68. Rock Type and Composition
  • 69. Rock Type and Composition how hard or resistant rocks are to be broken down, depends on their type an composition
  • 70. Rock Type and Composition how hard or resistant rocks are to be broken down, depends on their type an composition sedimentary rocks more easily weathered than harder igneous and metamorphic rocks
  • 71.
  • 73. Surface Area as pieces get smaller, surface areas increase
  • 74. Surface Area as pieces get smaller, surface areas increase the higher the total surface area, the more weathering that occurs
  • 75.
  • 76. Topography and Other Variables
  • 77. Topography and Other Variables materials on level areas likely to remain in place as they undergo changes
  • 78. Topography and Other Variables materials on level areas likely to remain in place as they undergo changes materials on slopes have greater tendency to move as result of gravity
  • 79. Topography and Other Variables materials on level areas likely to remain in place as they undergo changes materials on slopes have greater tendency to move as result of gravity as move down slope, exposes underlying rock surfaces and provides more opportunities for weathering to occur
  • 80. Topography and Other Variables materials on level areas likely to remain in place as they undergo changes materials on slopes have greater tendency to move as result of gravity as move down slope, exposes underlying rock surfaces and provides more opportunities for weathering to occur organisms affect weathering
  • 81. Topography and Other Variables materials on level areas likely to remain in place as they undergo changes materials on slopes have greater tendency to move as result of gravity as move down slope, exposes underlying rock surfaces and provides more opportunities for weathering to occur organisms affect weathering decaying organic matter
  • 82. Topography and Other Variables materials on level areas likely to remain in place as they undergo changes materials on slopes have greater tendency to move as result of gravity as move down slope, exposes underlying rock surfaces and provides more opportunities for weathering to occur organisms affect weathering decaying organic matter living plant roots
  • 83. Erosion and Deposition SECTION 7.2
  • 84. Intro
  • 85. Intro erosion process that transports earth’s minerals from one location to another
  • 86. Intro erosion process that transports earth’s minerals from one location to another running water, glaciers, wind, and ocean currents
  • 87. Intro erosion process that transports earth’s minerals from one location to another running water, glaciers, wind, and ocean currents deposition - minerals are dropped in another location
  • 89. Gravity’s Role in Erosion force gravity pulls materials down slope
  • 90. Gravity’s Role in Erosion force gravity pulls materials down slope w/out gravity, glaciers would not move downslope and streams would not flow
  • 92. Erosion by Running Water water has a lot of power to move large particles
  • 93. Erosion by Running Water water has a lot of power to move large particles great potential to erode materials b/c steeper slope, faster water flows
  • 94. Erosion by Running Water water has a lot of power to move large particles great potential to erode materials b/c steeper slope, faster water flows small streams join into larger streams (watershed)
  • 95. Erosion by Running Water water has a lot of power to move large particles great potential to erode materials b/c steeper slope, faster water flows small streams join into larger streams (watershed) rill erosion - erosion by running water in small channels, on side of slope
  • 96. Erosion by Running Water water has a lot of power to move large particles great potential to erode materials b/c steeper slope, faster water flows small streams join into larger streams (watershed) rill erosion - erosion by running water in small channels, on side of slope gully erosion - when channels becomes steep and wide
  • 97. Erosion by Running Water water has a lot of power to move large particles great potential to erode materials b/c steeper slope, faster water flows small streams join into larger streams (watershed) rill erosion - erosion by running water in small channels, on side of slope gully erosion - when channels becomes steep and wide problem in farming and grazing areas
  • 99. Costal Deposition and Erosion weathering process continue in ocean
  • 100. Costal Deposition and Erosion weathering process continue in ocean ocean currents, waves, and tides carve out cliffs, arches, and edges of continents
  • 101. Costal Deposition and Erosion weathering process continue in ocean ocean currents, waves, and tides carve out cliffs, arches, and edges of continents sand particles accumulate on shorelines forming dunes and beaches
  • 102. Costal Deposition and Erosion cont...
  • 103. Costal Deposition and Erosion cont... erosion occurs
  • 104. Costal Deposition and Erosion cont... erosion occurs constant movement of water
  • 105. Costal Deposition and Erosion cont... erosion occurs constant movement of water sand repeatedly picked up and moved
  • 106. Costal Deposition and Erosion cont... erosion occurs constant movement of water sand repeatedly picked up and moved sandbars form
  • 107. Costal Deposition and Erosion cont... erosion occurs constant movement of water sand repeatedly picked up and moved sandbars form can turn into barrier islands
  • 109. Glacier Erosion erosional effects large-scale and dramatic
  • 110. Glacier Erosion erosional effects large-scale and dramatic scrape and gorge out large sections
  • 111. Glacier Erosion erosional effects large-scale and dramatic scrape and gorge out large sections can carry huge rocks and piles of debris over great distance
  • 112. Glacier Erosion erosional effects large-scale and dramatic scrape and gorge out large sections can carry huge rocks and piles of debris over great distance features left in wake of glacier movement:
  • 113. Glacier Erosion erosional effects large-scale and dramatic scrape and gorge out large sections can carry huge rocks and piles of debris over great distance features left in wake of glacier movement: valleys, majestic water falls, lakes, deposits of sediment
  • 115. Wind Erosion major erosional agent in areas that experience limited rain and high temperatures
  • 116. Wind Erosion major erosional agent in areas that experience limited rain and high temperatures areas have little vegetation to hold sediments in place
  • 118. Wind Barriers reduces effect of wind erosion
  • 119. Wind Barriers reduces effect of wind erosion trees and other vegetation planted perpendicular to direction of wind
  • 121. Erosion by Plants, Animals, and Humans as plants and animals carry on life process they move materials from one place to another
  • 122. Erosion by Plants, Animals, and Humans as plants and animals carry on life process they move materials from one place to another humans excavate areas