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The Force of Geology-Part One
Endogenic and Exogenic Process
Widodo, S.T., M.T.
Mining Geology SMK N 1 Balikpapan
Plate Tectonic & Eartquake
Geology Process
 Endogenic
 Internal forces beneath or at Earth’s
surface
 Mountain building
 Earthquakes
 Exogenic
 External forces
 Erosion, water, wind, chemical
Endogenic Process
Plate Tectonics
 Fixed Earth Theory
 States that continents and oceans have
always been fixed in place
 Plate Tectonics Theory
 Proposed by Alfred Wegener, 1900s
 Became popular in the 1960s
 Pangaea Hypothesis
 First a supercontinent, and the tectonic
plates moved (see next slide – plate
boundaries)
Plate Boundaries
 Divergent
 Plates spreading apart, leading to:
 Seafloor spreading
 Rift Valleys in Africa
 Convergent
 Plates push together, leading to:
 Mountain building
 Volcanic eruptions as dense plates dive below
 Transform
 Grinding of plates past each other, leading to:
 Offset sidewalks
 E.g. along the San Andreas Fault, CA
Plate Boundaries
Earthquakes
 Focus
 Place of actual movement
 Epicenter
 Surface directly above focus
 See next slide – epicenters
 Seismic waves
 Recordable vibrations
 Seismograph
 Recording device for
seismic waves
 Richter Scale, 1935
Earthquakes
A 2.3 m coseismic displacement has distorted the railroad track near
the railway station Tepetarla in the region between Sapanca Lake and
Izmir Gulf, Turkey (www.geopages.co.uk/news/rev002.html).
Caused by Earthquakes
Earthquakes and the San Andreas Fault
India, Gujarat earthquake
Jan 26, 2001
Chapter 3 the force of geology 1 meeting

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Chapter 3 the force of geology 1 meeting

  • 1. The Force of Geology-Part One Endogenic and Exogenic Process Widodo, S.T., M.T. Mining Geology SMK N 1 Balikpapan Plate Tectonic & Eartquake
  • 2. Geology Process  Endogenic  Internal forces beneath or at Earth’s surface  Mountain building  Earthquakes  Exogenic  External forces  Erosion, water, wind, chemical
  • 3. Endogenic Process Plate Tectonics  Fixed Earth Theory  States that continents and oceans have always been fixed in place  Plate Tectonics Theory  Proposed by Alfred Wegener, 1900s  Became popular in the 1960s  Pangaea Hypothesis  First a supercontinent, and the tectonic plates moved (see next slide – plate boundaries)
  • 4. Plate Boundaries  Divergent  Plates spreading apart, leading to:  Seafloor spreading  Rift Valleys in Africa  Convergent  Plates push together, leading to:  Mountain building  Volcanic eruptions as dense plates dive below  Transform  Grinding of plates past each other, leading to:  Offset sidewalks  E.g. along the San Andreas Fault, CA
  • 6.
  • 7.
  • 8.
  • 9.
  • 10. Earthquakes  Focus  Place of actual movement  Epicenter  Surface directly above focus  See next slide – epicenters  Seismic waves  Recordable vibrations  Seismograph  Recording device for seismic waves  Richter Scale, 1935
  • 12. A 2.3 m coseismic displacement has distorted the railroad track near the railway station Tepetarla in the region between Sapanca Lake and Izmir Gulf, Turkey (www.geopages.co.uk/news/rev002.html). Caused by Earthquakes
  • 13. Earthquakes and the San Andreas Fault
  • 14.