About: Gauss-Matuyama reversal   Sponge Permalink

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The Gauss-Matuyama Reversal was a geologic event approximately 2.588 million years ago when the Earth's magnetic field underwent reversal. This event, which separates the Piacenzian from the Gelasian and marks the start of the Quaternary, is useful in dating sediments.

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  • Gauss-Matuyama reversal
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  • The Gauss-Matuyama Reversal was a geologic event approximately 2.588 million years ago when the Earth's magnetic field underwent reversal. This event, which separates the Piacenzian from the Gelasian and marks the start of the Quaternary, is useful in dating sediments.
  • The Gauss/Matuyama Reversal was a geologic event approximately 2.588 million years ago when the Earth's magnetic field underwent reversal. This event which separates the Piacenzian from the Gelasian and marks the start of the Quaternary, is useful in dating sediments.
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dbkwik:fossil/prop...iPageUsesTemplate
dbkwik:paleontolog...iPageUsesTemplate
abstract
  • The Gauss-Matuyama Reversal was a geologic event approximately 2.588 million years ago when the Earth's magnetic field underwent reversal. This event, which separates the Piacenzian from the Gelasian and marks the start of the Quaternary, is useful in dating sediments.
  • The Gauss/Matuyama Reversal was a geologic event approximately 2.588 million years ago when the Earth's magnetic field underwent reversal. This event which separates the Piacenzian from the Gelasian and marks the start of the Quaternary, is useful in dating sediments.
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