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The Force of Geology-Part Three
Endogenic and Exogenic Process
Widodo, S.T., M.T.
Mining Geology SMK N 1 Balikpapan
Weathering, Material Movement & Erosion
Rock Formation
 Igneous
 Cooled molten crustal material (magma)
 E.g. Basalt, granite
 Sedimentary
 Sediments laid down in layers and from high pressure
 E.g. Sandstone, shale, limestone
 Metamorphic
 The 2 rocks above can be later compacted again, by
heat & pressure, and so undergo further change
 E.g. Marble derived from limestone
Weathering
 Process of breaking rock into pieces
 The first step in the formation of soil
 Mechanical weathering
 Process of rocks breaking down by physical force, e.g. tree
roots, freezing & thawing - pot holes. See next slide.
 Chemical weathering
 Process of breaking down rock by:
 Exposure to air and water
 Acids released by decaying vegetation
 Oxidation (rust due to iron content)
 Leaching (nutrients being washed downwards beyond plant
roots)
 Decomposition of calcium carbonate
Mechanical
 Frost Wedging: the most important type of mechanical weathering;
freeze-thaw repetition. Also responsible for city pot-holes.
 Personal home experiment
Frost Wedging
Frost Heaving
Plant Root
Friction & Repeated Impact
Burrowing of Animals
Temperature Changes
Chemical
 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
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
Karst Topography
 A type of landscape in rainy regions where
there is limestone near the surface,
characterized by caves, sinkholes, and
disappearing streams.
 Created by chemical weathering of limestone
Features of Karst: Sinkholes
Features of Karst: Cave
Movement of Weathered Material
 Mass movement could be:
 Slow gradual movement occurring near the surface, like
soil creep
 Or in dramatic movements such as rock slides, landslides
and mudflows
Glaciers
 Slow moving “rivers of ice” flowing from colder to
warmer regions. They move only a few feet per year.
 They act like conveyor belts, picking up sediment and
dropping it in depositional areas
 These glacial sediments are called, Moraines
 Terminal moraines – found at the very end of
glacier
 Lateral moraines – found along the sides
 Medial moraines – found in the middle
 See next slide
Moraines
Impact of Past Glaciations
 Soils & Landforms
 Advance and retreat of glaciers leave behind highly
fertile soil and various landforms (see next slide).
 Water supply & Transportation routes
 Retreating glaciers left sand and gravel deposits
yielding large supplies of ground water
 Also, water transport is heavily influenced by
glacial melt water channels left behind by receding
glaciers. E.g. Great Lakes, Hudson Bay, etc. See
pg 117.
U-shaped valleys
& jagged/rugged
landscapes
Erosion
 The process by which water, ice, wind or
gravity moves fragments of rock and soil.
Coastal Erosion
 Longshore currents:
 Currents traveling parallel to the shore, caused by
repeated breaking of waves. Capable of carrying
enormous amounts of sediment, and changing the form
of beaches.
Coastal Erosion
Effects of longshore currents:
Water Erosion
 Rivers, streams, and runoff
Ice Erosion
 Glaciers
Wind Erosion
Chapter 5 the force of geology 1 meeting

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Chapter 5 the force of geology 1 meeting

  • 1. The Force of Geology-Part Three Endogenic and Exogenic Process Widodo, S.T., M.T. Mining Geology SMK N 1 Balikpapan Weathering, Material Movement & Erosion
  • 2. Rock Formation  Igneous  Cooled molten crustal material (magma)  E.g. Basalt, granite  Sedimentary  Sediments laid down in layers and from high pressure  E.g. Sandstone, shale, limestone  Metamorphic  The 2 rocks above can be later compacted again, by heat & pressure, and so undergo further change  E.g. Marble derived from limestone
  • 3. Weathering  Process of breaking rock into pieces  The first step in the formation of soil  Mechanical weathering  Process of rocks breaking down by physical force, e.g. tree roots, freezing & thawing - pot holes. See next slide.  Chemical weathering  Process of breaking down rock by:  Exposure to air and water  Acids released by decaying vegetation  Oxidation (rust due to iron content)  Leaching (nutrients being washed downwards beyond plant roots)  Decomposition of calcium carbonate
  • 4. Mechanical  Frost Wedging: the most important type of mechanical weathering; freeze-thaw repetition. Also responsible for city pot-holes.  Personal home experiment
  • 5.
  • 12. Chemical  Water weathers rock by dissolving it
  • 13. Oxygen  Iron combines with oxygen in the presence of water in a processes called oxidation  The product of oxidation is rust
  • 14. Living Organisms  Lichens that grow on rocks produce weak acids that chemically weather rock
  • 15. Acid Rain  Compounds from burning coal, oil and gas react chemically with water forming acids.  Acid rain causes very rapid chemical weathering
  • 16. Karst Topography  A type of landscape in rainy regions where there is limestone near the surface, characterized by caves, sinkholes, and disappearing streams.  Created by chemical weathering of limestone
  • 17. Features of Karst: Sinkholes
  • 19. Movement of Weathered Material  Mass movement could be:  Slow gradual movement occurring near the surface, like soil creep  Or in dramatic movements such as rock slides, landslides and mudflows
  • 20.
  • 21. Glaciers  Slow moving “rivers of ice” flowing from colder to warmer regions. They move only a few feet per year.  They act like conveyor belts, picking up sediment and dropping it in depositional areas  These glacial sediments are called, Moraines  Terminal moraines – found at the very end of glacier  Lateral moraines – found along the sides  Medial moraines – found in the middle  See next slide
  • 23.
  • 24. Impact of Past Glaciations  Soils & Landforms  Advance and retreat of glaciers leave behind highly fertile soil and various landforms (see next slide).  Water supply & Transportation routes  Retreating glaciers left sand and gravel deposits yielding large supplies of ground water  Also, water transport is heavily influenced by glacial melt water channels left behind by receding glaciers. E.g. Great Lakes, Hudson Bay, etc. See pg 117.
  • 26.
  • 27. Erosion  The process by which water, ice, wind or gravity moves fragments of rock and soil.
  • 28.
  • 29. Coastal Erosion  Longshore currents:  Currents traveling parallel to the shore, caused by repeated breaking of waves. Capable of carrying enormous amounts of sediment, and changing the form of beaches.
  • 30. Coastal Erosion Effects of longshore currents:
  • 31. Water Erosion  Rivers, streams, and runoff