Lake Toba in the context of "Volcanic lake"

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⭐ Core Definition: Lake Toba

Lake Toba (Indonesian: Danau Toba, Toba Batak: ᯖᯀᯬ ᯖᯬᯅ; romanized: Tao Toba) is a large natural lake in North Sumatra, Indonesia, occupying the caldera of the Toba supervolcano. The lake is located in the middle of the northern part of the island of Sumatra, with a surface elevation of about 900 metres (2,953 ft), the lake stretches from 2°53′N 98°31′E / 2.88°N 98.52°E / 2.88; 98.52 to 2°21′N 99°06′E / 2.35°N 99.1°E / 2.35; 99.1. The lake is about 100 kilometres (62 miles) long, 30 kilometres (19 mi) wide, and up to 505 metres (1,657 ft) deep. It is the largest lake in Indonesia and the largest volcanic lake in the world. Toba Caldera is one of twenty geoparks in Indonesia, and was recognised in July 2020 as one of the UNESCO Global Geoparks.

Lake Toba is the site of a supervolcanic eruption estimated at VEI 8 that occurred 69,000 to 77,000 years ago, representing a climate-changing event. Recent advances in dating methods suggest a more accurate eruption date of 74,000 years ago. It is the largest-known explosive eruption on Earth in the last 25 million years. According to the Toba catastrophe theory, the eruption had global consequences for human populations as it killed most humans living at that time and is believed to have created a population bottleneck in central east Africa and India, which affects the genetic make-up of the human worldwide population to the present. A recent study has cast doubt on this theory and found no evidence of substantial changes in global population.

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👉 Lake Toba in the context of Volcanic lake

A volcanogenic lake is a lake formed as a result of volcanic activity. They are generally a body of water inside an inactive volcanic crater (crater lakes) but can also be large volumes of molten lava within an active volcanic crater (lava lakes) and waterbodies constrained by lava flows, pyroclastic flows or lahars in valley systems. The term volcanic lake is also used to describe volcanogenic lakes, although it is more commonly assigned to those inside volcanic craters.

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Lake Toba in the context of Supervolcanic eruption

A supervolcano is a volcano that has had an eruption with a volcanic explosivity index (VEI) of 8, the largest recorded value on the index. This means the volume of deposits for such an eruption is greater than 1,000 cubic kilometers (240 cubic miles).

Supervolcanoes occur when magma in the mantle rises into the crust but is unable to break through it. Pressure builds in a large and growing magma pool until the crust is unable to contain the pressure and ruptures. This can occur at hotspots (for example, Yellowstone Caldera) or at subduction zones (for example, Toba).

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Lake Toba in the context of Toba Batak people

The Toba (also known as Toba Batak) people (Batak Toba: ᯅᯖᯂ᯲ ᯖᯬᯅ) are one of the sub-ethnic groups of the Batak people, found mainly in North Sumatra, Indonesia. The general term "Batak" is sometimes used to refer to the Batak Toba people, for one thing because the Toba people are the largest sub-group of the Batak ethnicity, for another because they tend to self-identify as merely Batak instead of "Toba" or "Toba Batak", contrary to the habit of the Mandailing, Angkola, Karo, Simalungun and Pakpak communities who commonly self-identify with their respective sub-groups. Religiously, they predominantly adhere to Protestantism of Christianity.

The Toba people are found in Toba Regency, Humbang Hasundutan Regency, Samosir Regency, North Tapanuli Regency, Central Tapanuli Regency (with Sibolga and its surrounding regions), and part of Dairi Regency. The Batak Toba people speak the Toba Batak language and are centered on Lake Toba and Samosir Island within the lake. Batak Toba people frequently build in traditional Batak architecture styles which are common in Samosir. Cultural demonstrations, performances, and festivities such as Sigale Gale are often held for tourists.

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