Where the cataclysmic events of 73,000 years ago took place, there is now an idyllic landscape with a picturesque lake at its centre. The area has great beauty, friendly locals and many potential tourist attractions. Only the occasional slight tremor, or puff of smoke and a few hot springs give a tiny hint of the violence that is lurking below. In fact,
Toba is likely to have been the place where modern Homo sapiens most dangerous and fiercest struggle for survival began. Countless other species faced the same trial – and many did not make it. Our ancestors did.
Fig. 2-2. The eruption of 73,000 years ago left the Sibandung caldera. Lake Toba is surrounded by two small, active volcanos as well as several updomed areas and hot springs. These features indicate that there is activity below the surface today and that pressure is rising. Samosir island, too, is evidence for upthrust from below. From the record it seems that Toba produces major eruptions every 300-400,000 years and that it will erupt again – but not any time soon.
grey area Present-day topographic depression
green area Updomed areas
1 Sibandung caldera: made 73,000 years ago by the Toba YTT event (Young Toba Ash)
2 Haranggaol caldera: made 500,000 years ago by the Toba MTT event (Middle Toba Ash)
3 Sibandung caldera: made 800,000 years ago by the Toba OTT event (Old Toba Ash)
The MTT and OTT events were not as large as the YTT event of 73,000 years ago but were still major eruptions of at least VEI 7.
V1 Tandukbenua (Sipisopiso) – young dacit-andesite volcano
V2 Pusubukit volcano – young dacit-andesite volcano
D1 Pardepur dacite domes
D2 Tuk-tuk rhyolite dome
HS Hot springs