File:Oceanic.Stripe.Magnetic.Anomalies.Scheme.fr.gif
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Oceanic.Stripe.Magnetic.Anomalies.Scheme.fr.gif (260 × 190 pixels, file size: 17 KB, MIME type: image/gif)
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DescriptionOceanic.Stripe.Magnetic.Anomalies.Scheme.fr.gif | A theoretical model of the formation of magnetic striping. New oceanic crust forming continuously at the crest of the mid-ocean ridge cools and becomes increasingly older as it moves away from the ridge crest with seafloor spreading: * a. the spreading ridge about 5 million years ago. * b. about 2 to 3 million years ago. * c. present-day. |
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This is a retouched picture, which means that it has been digitally altered from its original version. The original can be viewed here: Oceanic.Stripe.Magnetic.Anomalies.Scheme.gif: .
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Permission is granted to copy, distribute and/or modify this document under the terms of the GNU Free Documentation License, Version 1.2 or any later version published by the Free Software Foundation; with no Invariant Sections, no Front-Cover Texts, and no Back-Cover Texts. A copy of the license is included in the section entitled GNU Free Documentation License. Subject to disclaimers.http://www.gnu.org/copyleft/fdl.htmlGFDLGNU Free Documentation Licensetruetrue |
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This image is in the public domain in the United States because it only contains materials that originally came from the United States Geological Survey, an agency of the United States Department of the Interior. For more information, see the official USGS copyright policy.
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[edit]This image is a derivative work of the following images:
- Image:Oceanic.Stripe.Magnetic.Anomalies.Scheme.gif licensed with GFDL-en, PD-USGov-USGS
- 2006-02-24T13:09:33Z Kurgus 255x187 (15567 Bytes) A theoretical model of the formation of magnetic striping. New [[oceanic crust]] forming continuously at the crest of the mid-ocean ridge cools and becomes increasingly older as it moves away from the ridge crest with seafloo
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Date/Time | Thumbnail | Dimensions | User | Comment | |
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current | 18:52, 7 July 2008 | 260 × 190 (17 KB) | Who killed Bambi ? (talk | contribs) | {{Information |Description=A theoretical model of the formation of magnetic striping. New oceanic crust forming continuously at the crest of the mid-ocean ridge cools and becomes increasingly older as it moves away from the ridge crest with seafloor s |
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