File:Platse tect2 nl.svg

From Wikimedia Commons, the free media repository

Jump to: navigation, search

Platse_tect2_nl.svg(SVG file, nominally 4,217 × 3,169 pixels, file size: 451 KB)

Description

The key principle of plate tectonics is that the lithosphere exists as separate and distinct tectonic plates, which float on the fluid-like (visco-elastic solid) asthenosphere. The relative fluidity of the asthenosphere allows the tectonic plates to undergo motion in different directions. Note: That the Indian and Australian plate aren't separated; they are together forming the Indo-Australian Plate * 1 Synopsis on development * 2 Key principles * 3 Types of plate boundaries o 3.1 Transform (conservative) boundaries o 3.2 Divergent (constructive) boundaries o 3.3 Convergent (destructive) boundaries * 4 Driving forces of plate motion o 4.1 Friction o 4.2 Gravitation o 4.3 External forces o 4.4 Relative significance of each mechanism * 5 Major plates o 5.1 Continental drift o 5.2 Floating continents o 5.3 Plate tectonic theory + 5.3.1 Explanation of magnetic striping + 5.3.2 Subduction discovered + 5.3.3 Mapping with earthquakes o 5.4 Geological paradigm shift * 6 Biogeographic implications on fauna and flora * 7 Plate tectonics on other planets * 8 Metaphoric uses * 9 See also * 10 References * 11 External links

Date

2008-09-18 09:30 (UTC)

Source
Author
Permission
(Reusing this image)

see below


Nuvola apps kolourpaint.png This is a retouched picture, which means that it has been digitally altered from its original version. Modifications: translated English words into Dutch. The original can be viewed here: Plates_tect2_en.svg‎. Modifications made by Lies Van Rompaey.


I, the copyright holder of this work, hereby publish it under the following license:
Public domain I, the copyright holder of this work, hereby release it into the public domain. This applies worldwide.

In case this is not legally possible:
I grant anyone the right to use this work for any purpose, without any conditions, unless such conditions are required by law.


Afrikaans | Alemannisch | Aragonés | العربية | Asturianu | Azərbaycan | Беларуская (тарашкевіца) | Български | Català | Cebuano | Soranî / کوردی | Česky | Cymraeg | Dansk | Deutsch | Ελληνικά | English | Esperanto | Español | Eesti | Euskara | Estremeñu | فارسی | Suomi | Français | Galego | עברית | हिन्दी | Hrvatski | Magyar | Հայերեն | Bahasa Indonesia | Ido | Íslenska | Italiano | 日本語 | ქართული | ភាសាខ្មែរ | 한국어 | Ripoarisch | Kurdî / كوردی | Latina | Lietuvių | Latviešu | 文言 | Македонски | Bahasa Melayu | Plattdüütsch | Nederlands | ‪Norsk (nynorsk)‬ | ‪Norsk (bokmål)‬ | Polski | Português | Română | Русский | Slovenčina | Slovenščina | Shqip | Српски / Srpski | Svenska | ไทย | Tagalog | Türkçe | Українська | Vèneto | Tiếng Việt | Walon | 吴语 | 中文 | ‪中文(简体)‬ | ‪中文(繁體)‬ | 粵語 | +/−

[edit] Original upload log

This image is a derivative work of the following images:

  • Image:Plates_tect2_en.svg‎ licensed with PD-self
    • 2006-12-26T21:54:44Z AzaToth 4217x3169 (460986 Bytes) if it's small, and it's an svg, lets then resize it :)
    • 2006-01-26T00:42:41Z Scott Nash 682x462 (461282 Bytes) Tectonic plate map with its relative movements. Translated from [[Image:Placas_tect2_pt_BR.svg]].

Uploaded with derivativeFX

File history

Click on a date/time to view the file as it appeared at that time.

Date/TimeThumbnailDimensionsUserComment
current09:33, 18 September 2008Thumbnail for version as of 09:33, 18 September 20084,217×3,169 (451 KB)Lies Van Rompaey (talk | contribs) ({{Information |Description=The key principle of plate tectonics is that the lithosphere exists as separate and distinct tectonic plates, which float on the fluid-like (visco-elastic solid) asthenosphere. The relative fluidity of the asthenosphere allows t)

There are no pages that link to this file.