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• Internal Structure of Earth and Plate Tectonics • Chapter 2 The
• Internal Structure of Earth and Plate Tectonics • Chapter 2 The

...  Understanding Plate Tectonics helped to clear up two geological problems:  How did fossils of the same animals and plants end up in both South America and Africa  Evidence of ancient glaciation on several continents with inferred directions of ice flow were the same as if there was only one cont ...
baumgardner`s modeling of rapid plate tectonic motion
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Geological Catastrophes
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Mineralogy, Geochemistry, and Chronology of the Caballo and
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... constrained to be older than late Cambrian as episyenite clasts occur in the C-O Bliss Sandstone that unconformably overlies metasomatised basement. Direct dating of the metasomatism using the 40Ar/39Ar method on sub-milligram fragments of metasomatic K-feldspar yield complex and intriguing age resu ...
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Chapter 34: The Changing Face of the Earth
Chapter 34: The Changing Face of the Earth

... itself abrade the land but it also carries embedded rocks of all sizes, and thus acts very much like sandpaper. Valley glaciers gouge and scoop out the valleys they occupy, modifying them into U-shaped troughs. The topography between adjacent glaciated valleys is often angular and sharp. Continental ...
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Age of the Earth



The age of the Earth is 4.54 ± 0.05 billion years (4.54 × 109 years ± 1%). This age is based on evidence from radiometric age dating of meteorite material and is consistent with the radiometric ages of the oldest-known terrestrial and lunar samples.Following the development of radiometric age dating in the early 20th century, measurements of lead in uranium-rich minerals showed that some were in excess of a billion years old.The oldest such minerals analyzed to date—small crystals of zircon from the Jack Hills of Western Australia—are at least 4.404 billion years old. Comparing the mass and luminosity of the Sun to those of other stars, it appears that the Solar System cannot be much older than those rocks. Calcium-aluminium-rich inclusions – the oldest known solid constituents within meteorites that are formed within the Solar System – are 4.567 billion years old, giving an age for the solar system and an upper limit for the age of Earth.It is hypothesised that the accretion of Earth began soon after the formation of the calcium-aluminium-rich inclusions and the meteorites. Because the exact amount of time this accretion process took is not yet known, and the predictions from different accretion models range from a few millions up to about 100 million years, the exact age of Earth is difficult to determine. It is also difficult to determine the exact age of the oldest rocks on Earth, exposed at the surface, as they are aggregates of minerals of possibly different ages.
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