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Prehistoric Indonesia

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Through Prehistory, Megalith and Java

Geology

Geologically, the area of modern Indonesia appeared from under the Southeast Asian seas as the result of the Indian and Australian plates colliding and slipping under the Sunda Plate, sometime in the early Cenozoic era around 63 million years ago. This tectonic collision created the Sunda volcanic Arc that has produced the chains of islands of Sumatra, Java and the Lesser Sunda Islands. The active volcanic arc creating supervolcano that today become Lake Toba in Sumatra. The massive eruption of the Toba supervolcano that occurred some time between 69,000 and 77,000 years ago (72,000 BCE) instigated the Toba catastrophe theory, a global volcanic winter that caused a bottleneck in human evolution. Other notable volcanoes in Sunda Arc are Mount Tambora (erupted in 1815) and Krakatau (erupted in 1883). The region is known for its instability due to volcano formations and other volcanic and tectonic activities as well as climate changes; resulted in lowlands drowned occasionally under shallow seas, the formation of islands, the connection and disconnection of islands through narrow land-bridges, etc.

The Indonesian archipelago nearly reached its present form in the Pleistocene period. For some periods, the Sundaland was still linked with Asian mainland, creating the landmass extension of Southeast Asia that enabled the migrations of some Asian animals and hominid species. Geologically the New Guinea island and the shallow seas of Arafura is the northern part of Australia tectonic plate and once connected as a land bridge identified as Sahulland. During the end of the last ice age (around 20,000–10,000 years ago), earth experienced global climate change; a global warming with the rising of average temperature caused the melting of polar ice caps and contributed to the rising of sea surface. Sundaland was submerged under shallow sea, creating Malacca Strait, South China Sea, Karimata Strait and Java Sea. During that period, Malay Peninsula, Sumatra, Java, Borneo and the islands around them were formed. On the east, New Guinea and Aru Islands were separated from the Australia mainland. The rise of sea surface created isolated areas that separated plants, animals and hominid species, causing further evolution and speciation.

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