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The Force of Geology-Part Two
Endogenic and Exogenic Process
Widodo, S.T., M.T.
Mining Geology SMK N 1 Balikpapan
Volcanic
Volcanic Activity
 Magma
 Molten rock underneath the earth
 Lava
 Molten rock reaching Earth’s surface
 Volcano
 Surface vent for lava
Volcano Types
 Shield volcanoes
 Sedate
 Runny lava
 The Hawaiian Islands: Mauna Loa, Hawaii (still
active, but not explosive)
 Composite cone volcanoes
 Explosive
 Pyroclasts – this explosive material includes sticky
lava, hot ash, sulfurous gas, rock bombs, etc – e.g.
Pompei
 Krakatau in Indonesia, largest recorded eruption.
Tectonic-Volcanic
Volcanic Product
 Three factors effect the explosivity of a volcano
 Temperature of magma
 High-temperature, less explosive
 Composition of magma
 Less silica, less explosive
 Gas content of magma
 Less gas, less explosive
fluidity
Volcanic Eruption
Product of Effusive Eruption
low viscosity, low gas content
Hawaiian type
Smooth Ropey
pahoehoe surfacerough rubbly
surfaces A’a
med - high viscosity, high gas content
pumice Volcanic ash
Names for pyroclastic
rocks based on clast size
or tephra
Pumice is formed as pyroclastic
material is ejected into the air as a
froth containing masses of gas
bubbles or vessicles, the lava
solidifies quickly and the vessicles
are contained in the rock.
Product of Explosive Eruption
Chapter 4 the force of geology 1 meeting

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Chapter 4 the force of geology 1 meeting

  • 1. The Force of Geology-Part Two Endogenic and Exogenic Process Widodo, S.T., M.T. Mining Geology SMK N 1 Balikpapan Volcanic
  • 2. Volcanic Activity  Magma  Molten rock underneath the earth  Lava  Molten rock reaching Earth’s surface  Volcano  Surface vent for lava
  • 3. Volcano Types  Shield volcanoes  Sedate  Runny lava  The Hawaiian Islands: Mauna Loa, Hawaii (still active, but not explosive)  Composite cone volcanoes  Explosive  Pyroclasts – this explosive material includes sticky lava, hot ash, sulfurous gas, rock bombs, etc – e.g. Pompei  Krakatau in Indonesia, largest recorded eruption.
  • 4.
  • 5.
  • 8.  Three factors effect the explosivity of a volcano  Temperature of magma  High-temperature, less explosive  Composition of magma  Less silica, less explosive  Gas content of magma  Less gas, less explosive fluidity Volcanic Eruption
  • 9.
  • 10. Product of Effusive Eruption low viscosity, low gas content Hawaiian type Smooth Ropey pahoehoe surfacerough rubbly surfaces A’a
  • 11. med - high viscosity, high gas content pumice Volcanic ash Names for pyroclastic rocks based on clast size or tephra Pumice is formed as pyroclastic material is ejected into the air as a froth containing masses of gas bubbles or vessicles, the lava solidifies quickly and the vessicles are contained in the rock. Product of Explosive Eruption