File:Isotopic stages hg.png: Difference between revisions

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{{Image_Details
== Summary ==
|description  = The short term climatic changes of the Quaternary are induced by the Milankovitch cycles of earth's orbit. Stable oxygen isotope record of the last 300,000 years. The image shows the last three glacial/interglacial cycles of the Quaternary.
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|author      = Hannes Grobe. (Creative Commons CC-BY-SA-2.5)
|copyright    = This file is licensed under the Creative Commons Attribution ShareAlike 2.5 License.
|source      = http://commons.wikimedia.org/wiki/Image:Isotopic_stages_hg.png
|date-created = 2006-09-12
|pub-country  = Bremerhaven, Germany
|notes        =
|versions    =
}}

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current19:56, 11 March 2022Thumbnail for version as of 19:56, 11 March 2022800 × 556 (130 KB)Maintenance script (talk | contribs)== Summary == Importing file

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