File:Flux of crustal material in the mantle.jpg
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Summary
| Description |
English: The pale blue arrows indicate the ultimate destiny of crustal material that is subducted into the mantle. The material may be incorporated into mantle plumes, recycled into overlying volcanic arcs, descend wholly to the core-mantle boundary (a proposed "slab graveyard") or absorbed into the mantle proper, mingling with the "crystal mush" and eventually being incorporated into mantle-characterized igneous rocks (like those at a mid-ocean ridge).
Español: Las flechas en azul claro indican el destino final del material de la corteza que es subducido hacia dentro del manto. El material puede incorporarse a plumas del manto, reciclarse en un arco volcánico, descender completamente al margen manto-núcleo (sugerido como "cementerio de losas") o ser absorbido hacia el manto, mezclándose con la "pasta de cristal" e incorporándose finalmente a las rocas ígneas características del manto (como las de las dorsales oceánicas). |
| Date | 20 October 2011 (original upload date) |
| Source | Transferred from en.wikipedia to Commons. |
| Author | Erin Walde |
| Permission (Reusing this file) |
Creative Commons Attribution-ShareAlike 3.0 |
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Original upload log
The original description page was here. All following user names refer to en.wikipedia.
- 21:17, October 20, 2011 Ewalde1 talk contribs block 534 bytes +534 The pale blue arrows indicate the ultimate destiny of crustal material that is subducted into the mantle. The material may be incorporated into mantle plumes, recycled into overlying volcanic arcs or absorbed into the mantle proper, mingling with the "cry
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File history
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 14:27, 22 January 2020 | | 1,942 × 1,112 (654 KB) | Izmir2 | {{Information |description ={{en|1=The pale blue arrows indicate the ultimate destiny of crustal material that is subducted into the mantle. The material may be incorporated into mantle plumes, recycled into overlying volcanic arcs, descend wholly to the core-mantle boundary (a proposed "slab graveyard") or absorbed into the mantle proper, mingling with the "crystal mush" and eventually being incorporated into mantle-characterized igneous rocks (like those at a mid-ocean ridge).}} {{es|1=La... |
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