Mount Tandikat

Stratovolcano in Sumatra, Indonesia
Tandikat
The Tandikat (left) - Singgalang (right) twin volcano as seen from Marapi.
Highest point
Elevation2,438 m (7,999 ft)
Coordinates0°25′57.30″S 100°19′1.69″E / 0.4325833°S 100.3171361°E / -0.4325833; 100.3171361
Geography
Tandikat is located in Sumatra
Tandikat
Tandikat
West Sumatra, Indonesia
Parent rangeBarisan Mountains
Geology
Mountain typeStratovolcano
Rock typeAndesite
Volcanic arcSunda Arc
Last eruptionApril 1924

Tandikat is an active stratovolcano in West Sumatra, Indonesia. Its elevation is 2,438 m (7,999 ft). It is a twin volcano with Mount Singgalang, which is located to the north-north-east of Tandikat. However, only Tandikat has had historical volcanic activity. The city of Padang Panjang is located at the foot of the mountain.

Geology

Mount Tandikat is part of the greater Sunda Arc subduction zone. Volcanism here is caused by the Indo-Australian plate subducting under the Sunda plate.[1] As the Indo-Australian plate subducts into the mantle, it carries with it vast amounts of seawater. At ~20 kilometers (12.5 miles) water start to dehydrate from the subducted slab, which lowers the melting point of the surrounding mantle. This generates magma which is more buoyant than the surrounding mantle. This makes it's way to the surface and erupts as a volcano, which is how Mount Tandikat operates.[2]

Mount Tandikat sits about 285 km (177 miles) from the Java trench. Melt begins at around 130 km (80 miles) directly below the volcano.[3]

Quaternary-aged rocks from early eruptions are made up of hornblende hypersthene pumiceous tuff which occurred around 52 ka. Most of Mount Tandikat's eruptions are made of andesite lava's, which are intermediate in silica content. It is thought that Mount Tandikat has two separate magma chambers. The shallow magma chamber is around 5 km (3 miles) deep, and there is also a deeper magma chamber of an unknown depth.[4]

2009 landslide

On April 30, 2009 at 17:16 local time, a powerful 7.6 magnitude earthquake triggered a large debris avalanche at Mount Tandikat. This was the most extensive of many landslides caused by the earthquake. Due to heavy rainfall in the area, 30-50 degree slopes, and loose pumice weakened the slopes of the volcano. The earthquake caused the side of the mountain to "flow" downhill which killed hundreds of people.[5][6]

See also

References

  1. ^ Brett Israel (26 October 2010). "Indonesia's Explosive Geology Explained". Live Science. Retrieved 25 November 2025.
  2. ^ Cerpa, Nestor G.; Wada, Ikuko (June 2025). "Hydration State and Updip Fluid Migration in the Slab Mantle". Journal of Geophysical Research: Solid Earth. 130 (6) e2024JB030609. Bibcode:2025JGRB..13030609C. doi:10.1029/2024JB030609. Retrieved 25 November 2025.
  3. ^ Acocella, Valerio; Bellier, Olivier; Sandri, Laura; Sébrier, Michel; Pramumijoyo, Subagyo (9 February 2018). "Weak Tectono-Magmatic Relationships along an Obliquely Convergent Plate Boundary: Sumatra, Indonesia". Frontiers in Earth Science. 6 3. Bibcode:2018FrEaS...6....3A. doi:10.3389/feart.2018.00003.
  4. ^ Dahrin, Darharta; Amir, Harman; Suryanata, Putu Billy; Bijaksana, Satria; Fajar, Silvia Jannatul; Ibrahim, Khalil; Harlianti, Ulvienin; Arisbaya, Ilham; Pebrian, Mutiara Qalbi; Rahman, Adinda Aisyah; Kasendri, Adibbian (3 November 2022). "Subsurface structures of Sianok Segment in the GSF (Great Sumatran Fault) inferred from magnetic and gravity modeling". Frontiers in Earth Science. 10 1012286. Bibcode:2022FrEaS..1012286D. doi:10.3389/feart.2022.1012286.
  5. ^ Faris, Fikri; Fawu, Wang (December 2014). "Investigation of the initiation mechanism of an earthquake- induced landslide during rainfall: a case study of the Tandikat landslide, West Sumatra, Indonesia". Geoenvironmental Disasters. 1 (1) 4. Bibcode:2014GeoDi...1....4F. doi:10.1186/s40677-014-0004-3.
  6. ^ Faris, Fikri; Wang, Fawu (December 2014). "Stochastic analysis of rainfall effect on earthquake induced shallow landslide of Tandikat, West Sumatra, Indonesia". Geoenvironmental Disasters. 1 (1) 12. Bibcode:2014GeoDi...1...12F. doi:10.1186/s40677-014-0012-3.


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