File:Oceanic magnetic striping example sk.gif

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Oceanic_magnetic_striping_example_sk.gif ‎(285 × 190 pixels, file size: 15 KB, MIME type: image/gif)

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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 spreading: a. the spreading ridge about 5 million years ago. b. about 2 to 3 million years ago. c. present-day. This picture is Slovak version of image fom commons.
Date
Source http://commons.wikimedia.org/wiki/Image:Oceanic_magnetic_striping_example.gif self-made
Author Pelex

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I, Pelex, the copyright holder of this work, hereby publishes it under the following licenses:
GNU head 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.
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attribution share alike 		This file is licensed under the Creative Commons Attribution-Share Alike 3.0 Unported license.
Attribution: I, Pelex
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Date/TimeThumbnailDimensionsUserComment
current12:56, 22 July 2007Thumbnail for version as of 12:56, 22 July 2007285 × 190 (15 KB)Pelex (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 sprea
22:41, 21 July 2007Thumbnail for version as of 22:41, 21 July 2007255 × 187 (15 KB)Pelex (talk | contribs)Obnovené na skoršiu verziu
22:34, 21 July 2007Thumbnail for version as of 22:34, 21 July 2007283 × 187 (15 KB)Pelex (talk | contribs)== Opis súboru == {{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
16:55, 21 July 2007Thumbnail for version as of 16:55, 21 July 2007255 × 187 (15 KB)Pelex (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 sprea

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