Forces of Geologic Change
A chart by Jim Barton
FORCES OF GEOLOGIC CHANGE
|
Forces Involved |
Energy Source |
Time Frame |
Examples of Physical Features |
Tectonics |
Gravity/Heat |
Tectonic movements of the
crust began shortly after Earth's crust formed 4.5 billion years ago,
and continue today with plate tectonics, earthquakes, volcanic
eruptions, and rising/falling landscapes. |
Earth's crustal plates, hot
spots, rising mountain ranges, sinking basins (large scale)
Volcanoes, faults, fractures, landslides (small scale) |
Water Erosion / Deposition |
Gravity/Heat |
The Hydrologic Cycle began
shortly after the formation of the oceans over 4 billion years
ago, is driven mainly by
energy of our Sun, and by heat within the earth. |
Rivers and stream channels,
flood plains, shoreline erosion of lakes and oceans, landslides,
glacial valleys and moraines, geyser mineral deposition |
Wind Erosion / Deposition |
Gravity/Heat |
Wind erosion began with the
formation of the
atmosphere and Earth's crust 4.5 billion years ago, is driven by the
energy of our Sun and
the rotational Force of the Earth. |
Desert landscapes |
Extra-terrestrial collision |
Gravity/Heat |
Extra-terrestrial collisions
from meteorites have continued to occur, with
lesser frequency, since the formation of Earth over 4.5 billion years
ago. |
Impact craters,
Cretaceous-Tertiary boundary (Iridium layer), Coesite (shocked quartz),
tektites (silica glass fragments), theoretical source of water on Earth. |
Chemical Erosion / Deposition |
Geochemical Reactions/ Gravity/Heat |
Geochemical reactions
beganwith the formation of the Earth over 4.5 billion years ago.
Chemical erosion/deposition is driven by gravity, the atomic structure
(minerals of rocks, the atmosphere, and water), energy (heat, light),
and conditions of the environment (pH, temperature, atmospheric
pressure. |
Caves in limestone, oxidation
of landscapes (rust, desert varnish), acid rain from air pollution, acid
rock drainage (sulfide) from abandoned mines, heap leaching of gold by
cyanide.
James Barton, RG, 2001
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