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PHYS 0106 (Spring, 2001) Earth History Timeline |
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| Phanerozoic Eon: Cenozoic Era: Quaternary Period | |||
Timeline Links Phanerozoic Neoproterozoic Mesoproterozoic Paleoproterozoic Archean Other Links Historical Geology Page Physical Geology Page Mike's Home Page |
Writer/Researcher: Jason Pease Editor: Crystal Venturo Web Page Builder: Jason Pease Throughout history there have been several periods Of glaciations. These cycles are often referred to as the Milankovich cycles. Many of the glacial periods took place within the last billion years. Over twenty glacial advances have taken place over the last two million years.
Changes in the earths orbit through time causes
changes in the amount of sunlight that reaches earth.
There are also three different things that are thought
to have an important role in causing ice sheets. These
things are changes in the eccentricity of the earths
orbit, changes in the tilt of the earthÕs axis, and the
procession of the equinoxes. Changes in the tilt of
the earths orbit cause changes in the distribution of
radiation at high latitude and the length of dark
periods at the poles. Differences in radiation of this level, is one of the biggest factors that influences the making and melting of these ice sheets. Today the tilt is approximately twenty-three point five degrees. The tilt varies from between twenty-one point six and twenty-four point five.
The Earths orbit around the sun is an ellipse not a circle, which is measured by eccentricity, that fluctuates from between one and five percent through time. This affects the amount of radiation the earths surface receives at aphelion and perihelion. Even thought the amount of change in radiation is very small it is apparently important in the making and melting of the ice sheets. |