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Erosion,

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Title: Erosion,


1
Erosion, Types of Weathering
  • Chapter 10

2
Erosion
  • A process where water, wind, or gravity
    transports soil (sediment) from its source

3
  • The process by which rocks are broken down into
    smaller pieces
  • There are 2 main types, chemical Physical

Weathering
4
Mechanical Weathering
  • The break down of rock into smaller pieces due to
    physical means
  • Frost wedging (water freezing in rock cracks)
  • Abrasion (other rocks or sediment rubbing against
    rock.)

5
Chemical Weathering
  • Rocks break as a result of a chemical change
  • Acid rain
  • Chemical decomposition
  • Gases in the air (oxidation)

6
Deposition
  • Is the process where material lays to rest
  • Sediment is deposited in bodies of water and on
    land

7
Chapter 6
  • The Rock Record

? ? ?
8
  • Sedimentary Rock Layers
  • This is a normal record of rock. Layers are
    undisturbed. The Geologic Column is a model of
    what rock layers should look like.

9
Uniformitarianism
  • A principle or rule that states that events that
    happened in the past can be explained by current
    earth (geologic) processes
  • Earth Processes like erosion, weathering, and
    deposition remain uniformed and do not change.

10
Catastrophism
  • A principle that states that geologic changes
    happen suddenly. (natural disasters)
  • They believed the Earth was only a few thousand
    years old.
  • Catastrophic events formed the Earth, created
    volcanoes, mountains, oceans, etc.

11
Relative Dating
  • Determines which comes first. Determining if rock
    layers are older or younger
  • Compare them to undisturbed rock around the world

12
Principle of Superposition
  • A principle or rule that states that younger
    rocks lie above older rocks in un-disturbed
    sequences
  • As you move from top of rock layers to the bottom
    the rock layers get older

13
SUPERPOSITION
14
Uplift
  • movement within the Earth that moves rocks to the
    surface

15
Unconformities
  • Is a disturbance in the layer of a rock.
  • Represents thousands, to millions of years in
    missing time in the layers of a rock
  • Can be created through
  • Erosion and weathering (p159, figure 4)
  • Faulting- (earthquakes)
  • Folding (anticlines, synclines, and monoclines)
  • Tilting
  • intrusion

16
Rock Intrusion
  • A layer of molten rock (hardened magma) from the
    Earths interior that squeezes into existing rock
    and then cools.
  • Melts surrounding layers
  • Interrupts the rock time scale.

17
Types of Unconformities
  • Disconformity part of a parallel rock layer is
    missing. (Layers may be eroded away and deposited
    elsewhere)
  • Nonconformity- horizontal sedimentary rock
    layers lay on the eroded surface of intrusive
    igneous rocks or metamorphic rocks
  • Angular unconformity- rocks are tilted or folded
    due to earthquakes or uplift (p 160)

18
Terms
  • Erosion
  • Weathering
  • Uplift
  • Deforestation
  • Mechanical weathering
  • Chemical weathering
  • Relative dating
  • Uniformitarianism
  • Superposition
  • Intrusion
  • Catastrophism
  • Un-conformity
  • Strip Mining
  • Frost Wedging
  • Abrasion
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