Andesgebergte

Source: NASA World Wind - Publiek Domein

Description

De Andes zijn geologisch gezien een jong systeem. Het gebergte ontstond tijdens het Krijt en de Tertiaire periode. Het ontstaan van de bergketen in Zuid-Amerika is het gevolg van de platentektoniek. De oceanische Nazcaplaat duikt weg onder de continentale Zuid-Amerikaanse plaat (subductie), met een snelheid van ongeveer 8 cm per jaar. Hierdoor nemen de bergen steeds meer in hoogte toe. Vulkanen en aardbevingen komen er dikwijls voor.

Source

Source: Wikipedia

| Public

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Source: NASA World Wind - Publiek Domein

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Source: NASA World Wind - Publiek Domein

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