Geography

GEOLOGICAL HISTORY

The islands of Indonesia were formed in the Miocene age (12 million years BC); Palaeocene age (70 million years BC); Eocene age (30 million years BC); Oligacene age (25 million years BC). As people from Asia started to migrate, it is believed that Indonesia existed since the Pleistocene age (4 million years BC). The islands have a great effect on the change of the Australian and Pacific tectonic plate. The Australian plate changes slowly with an upward movement into the small plates of the Pacific plate that moves southward. Between these lines, the islands of Indonesia are stretched out.

This makes Indonesia as one of the most changing geological area in the world. There are 400 volcanic mountains – which 100 of them are active- that dot the islands of Indonesia. Every day Indonesia experiences three vibrations, at least one earthquake a day and one volcanic eruption in a year.