Slika:Destructive plate margin.png
Sa Wikipedije, slobodne enciklopedije
Veličina umanjene slike: 800 × 545 piksela
Slika veće veličine (880 × 600 piksela, veličina: 65 KB, MIME vrsta: image/png)
| Ova datoteka postoji na Wikimedia Commons serveru. Detaljne informacije možete pronaći tamo. |
Destructive plate margin; oceanic crust is forced below the continental crust because oceanic crust is denser than continental crust. Friction between the moving plates causes earthquakes. The heat increase due to friction and being pushed into the asthenosphere causes the oceanic crust to melt, and reduced density forces the newly formed magma to rise. The magma rises up through weak areas in the continental crust, eventually erupting as one or more volcanoes.
Not to scale.
Image by Fredrik.
 |
This file has been released into the public domain by the copyright holder, its copyright has expired, or it is ineligible for copyright. This applies worldwide. |
 |
Note: This tag is obsolete! Don't use this generic template - please use instead:
العربية | česky | Deutsch | English | Español | Français | हिन्दी | Italiano | 日本語 | Norsk (nynorsk) | Português | Русский | Slovenčina | Slovenščina | Српски | Polski | Türkçe | 简体中文 | +/- |
Linkovi na sliku
Sljedeći članci vode na ovu sliku:
