List of volcanoes in Indonesia

Last updated

Mahameru (Semeru) above Mount Bromo, East Java. Mahameru-volcano.jpeg
Mahameru (Semeru) above Mount Bromo, East Java.
East Indonesia Islands from ISS. Seven active volcanoes are visible: 5 in East Java, Agung in Bali and Rinjani in Lombok. East Indonesia Island Chain from ISS.jpg
East Indonesia Islands from ISS. Seven active volcanoes are visible: 5 in East Java, Agung in Bali and Rinjani in Lombok.

The geography of Indonesia is dominated by volcanoes that are formed due to subduction zones between the Eurasian plate and the Indo-Australian plate. Some of the volcanoes are notable for their eruptions, for instance, Krakatoa for its global effects in 1883, [1] the Lake Toba Caldera for its supervolcanic eruption estimated to have occurred 74,000 years before present which was responsible for six years of volcanic winter, [2] and Mount Tambora for the most violent eruption in recorded history in 1815. [3]

Contents

Volcanoes in Indonesia are part of the alpida belt and Pacific Ring of Fire. The 150 entries in the list below are grouped into six geographical regions, four of which belong to the volcanoes of the Sunda Arc trench system. The remaining two groups are volcanoes of Halmahera, including its surrounding volcanic islands, and volcanoes of Sulawesi and the Sangihe Islands. The latter group is in one volcanic arc together with the Philippine volcanoes.

The most active volcano is Mount Merapi on Java. Since AD 1000, Kelut has erupted more than 30 times, of which the largest eruption was at scale 5 on the volcanic explosivity index (VEI), [4] while Mount Merapi has erupted more than 80 times. [5] The International Association of Volcanology and Chemistry of the Earth's Interior has named Mount Merapi as a Decade Volcano since 1995 because of its high volcanic activity.

As of 2012, Indonesia has 127 active volcanoes and about 5 million people live within the danger zones. It has been conjectured that the earthquake and tsunami event of 26 December 2004 could trigger eruptions, with Mount Sinabung (dormant since the 1600s) erupting in 2010 as a possible example. [6]

The word for Mount in Indonesian and many regional languages of the country is Gunung. Thus, Mount Merapi may be referred to as Gunung Merapi.

Scope

Major volcanoes in Indonesia Map indonesia volcanoes.gif
Major volcanoes in Indonesia

There is no single standard definition of a volcano. It can be defined as individual vents, volcanic edifices, or volcanic fields. The interior of ancient volcanoes may have been eroded, creating a new subsurface magma chamber as a separate volcano. Many contemporary active volcanoes rise as young parasitic cones from flank vents or at a central crater. Some volcanic cones are grouped into one volcano name, for instance, the Tengger caldera complex, whereas, individual vents are named by local people. The status of a volcano, either active or dormant, cannot be defined precisely. An indication of a volcano is determined by either its historical records, radiocarbon dating, or geothermal activities.

The primary source of the list below is taken from the Volcanoes of the World book, compiled by two volcanologists Tom Simkin and Lee Siebert, [a] in which active volcanoes in the past 10,000 years (Holocene) are listed. [7] Particularly for Indonesia, Simkin and Siebert used a catalogue of active volcanoes from the International Association of Volcanology and Chemistry of the Earth's Interior publication series. [b] The Simkin and Siebert list is the most complete list of volcanoes in Indonesia, but the accuracy of the record varies from one region to another in terms of contemporary activities and fatalities in recent eruptions. Complementary sources for the latest volcanic data are taken from the Volcanological Survey of Indonesia, a governmental institution which is responsible for volcanic activities and geological hazard mitigation in Indonesia, [8] and some academic resources.

Geographical groups

Sumatra

Map showing the location of volcanoes and geological fault lines of Sumatra Sumatra Volcanoes.png
Map showing the location of volcanoes and geological fault lines of Sumatra

The geography of Sumatra is dominated by a mountain range called Bukit Barisan (lit: "a row of hills"). The mountain range spans nearly 1,700 km (1,100 mi) from the north to the south of the island, and it was formed by movement of the Australian tectonic plate. [9] The plate moves with a convergence rate of 5.5 cm/year which has created major earthquakes on the western side of Sumatra including the 2004 Sumatra–Andaman earthquake. [10] [11] The tectonic movement has been responsible not only for earthquakes, but also for the formation of magma chambers beneath the island. [9]

Only one of the 35 active volcanoes, Weh, is separated from the Sumatran mainland. The separation was caused by a large eruption that filled the lowland between Weh and the rest of the mainland with sea water in the Pleistocene epoch. The largest volcano of Sumatra is the supervolcano Toba within the 100 km (62 mi) × 30 km (19 mi) Lake Toba, which was created after a caldera collapse (est. in 74,000 Before Present). [2] The eruption is estimated to have been at level eight on the VEI scale, the highest level for a volcanic eruption. The highest peak of the mountain range is Mount Kerinci with an elevation of 3,800 m (12,467 ft).

NameShapeElevationLast eruption (VEI)Coordinates
Weh stratovolcano 617 metres (2,024 ft) Pleistocene 5°49′N95°17′E / 5.82°N 95.28°E / 5.82; 95.28
Seulawah Agam stratovolcano1,810 metres (5,940 ft)1839 (2) 5°26′53″N95°39′29″E / 5.448°N 95.658°E / 5.448; 95.658
Peuet Sague complex volcano 2,801 metres (9,190 ft)25 December 2000 (2) 4°54′50″N96°19′44″E / 4.914°N 96.329°E / 4.914; 96.329
Geureudong stratovolcano2,885 metres (9,465 ft)1937 4°48′47″N96°49′12″E / 4.813°N 96.82°E / 4.813; 96.82
Kembar shield volcano 2,245 metres (7,365 ft)Pleistocene 3°51′00″N97°39′50″E / 3.850°N 97.664°E / 3.850; 97.664
Sibayak stratovolcano2,212 metres (7,257 ft)1881 3°14′N98°31′E / 3.23°N 98.52°E / 3.23; 98.52
Sinabung stratovolcano2,460 metres (8,070 ft)2 March 2021 [12] 3°10′12″N98°23′31″E / 3.17°N 98.392°E / 3.17; 98.392
Toba supervolcano 2,157 metres (7,077 ft)75000 BC (8) 2°35′N98°50′E / 2.58°N 98.83°E / 2.58; 98.83
Helatoba-Tarutung fumarole field1,100 metres (3,600 ft) Pleistocene 2°02′N98°56′E / 2.03°N 98.93°E / 2.03; 98.93
Imun unknown1,505 metres (4,938 ft)unknown 2°09′29″N98°55′48″E / 2.158°N 98.93°E / 2.158; 98.93
Sibualbuali stratovolcano1,819 metres (5,968 ft)unknown 1°33′22″N99°15′18″E / 1.556°N 99.255°E / 1.556; 99.255
Lubukraya stratovolcano1,862 metres (6,109 ft)unknown 1°28′41″N99°12′32″E / 1.478°N 99.209°E / 1.478; 99.209
Sorikmarapi stratovolcano2,145 metres (7,037 ft)1986 (1) 0°41′10″N99°32′20″E / 0.686°N 99.539°E / 0.686; 99.539
Talakmau complex volcano2,919 metres (9,577 ft)unknown 0°04′44″N99°58′48″E / 0.079°N 99.98°E / 0.079; 99.98
Sarik-Gajah volcanic cone unknownunknown 0°00′29″N100°12′00″E / 0.008°N 100.20°E / 0.008; 100.20
Marapi complex volcano2,885 metres (9,465 ft)2024 0°22′52″S100°28′23″E / 0.381°S 100.473°E / -0.381; 100.473
Tandikat stratovolcano2,438 metres (7,999 ft)1924 (1) 0°25′59″S100°19′01″E / 0.433°S 100.317°E / -0.433; 100.317
Talang stratovolcano2,597 metres (8,520 ft)27 November 2007 (2) 0°58′41″S100°40′44″E / 0.978°S 100.679°E / -0.978; 100.679
Kerinci stratovolcano3,800 metres (12,500 ft)2019 (on going) 1°41′49″S101°15′50″E / 1.697°S 101.264°E / -1.697; 101.264
Hutapanjang stratovolcano2,021 metres (6,631 ft)unknown 2°20′S101°36′E / 2.33°S 101.60°E / -2.33; 101.60
Sumbing stratovolcano2,507 metres (8,225 ft)23 May 1921 (2) 2°24′50″S101°43′41″E / 2.414°S 101.728°E / -2.414; 101.728
Masurai stratovolcano2,916 metres (9,567 ft) Pleistocene [13] 2°30′11″S101°43′41″E / 2.503°S 101.728°E / -2.503; 101.728
Kunyit stratovolcano2,151 metres (7,057 ft)unknown 2°35′31″S101°51′00″E / 2.592°S 101.85°E / -2.592; 101.85
Pendan unknownunknownunknown 2°49′S102°01′E / 2.82°S 102.02°E / -2.82; 102.02
Belirang-Beriti complex volcano1,958 metres (6,424 ft)unknown 2°49′S102°11′E / 2.82°S 102.18°E / -2.82; 102.18
Bukit Daun stratovolcano2,467 metres (8,094 ft)unknown 3°23′S102°22′E / 3.38°S 102.37°E / -3.38; 102.37
Kaba stratovolcano1,952 metres (6,404 ft)22 August 2000 (1) 3°31′S102°37′E / 3.52°S 102.62°E / -3.52; 102.62
Dempo stratovolcano3,173 metres (10,410 ft)2023 4°02′S103°08′E / 4.03°S 103.13°E / -4.03; 103.13
Patah unknown2,817 metres (9,242 ft)unknown 4°16′S103°18′E / 4.27°S 103.30°E / -4.27; 103.30
Bukit Lumut Balai stratovolcano2,055 metres (6,742 ft)unknown 4°14′S103°37′E / 4.23°S 103.62°E / -4.23; 103.62
Besar stratovolcano1,899 metres (6,230 ft)April 1940 (1) 4°26′S103°40′E / 4.43°S 103.67°E / -4.43; 103.67
Ranau caldera 1,881 metres (6,171 ft)unknown 4°50′S103°55′E / 4.83°S 103.92°E / -4.83; 103.92
Sekincau Belirang caldera1,719 metres (5,640 ft)unknown 5°07′S104°19′E / 5.12°S 104.32°E / -5.12; 104.32
Suoh caldera1,000 metres (3,300 ft)24 May 2024 5°15′S104°16′E / 5.25°S 104.27°E / -5.25; 104.27
Hulubelu caldera1,040 metres (3,410 ft)1836 5°21′S104°36′E / 5.35°S 104.60°E / -5.35; 104.60
Rajabasa stratovolcano1,281 metres (4,203 ft)1798 5°46′48″S105°37′30″E / 5.78°S 105.625°E / -5.78; 105.625

Sunda Strait and Java

The Sunda Strait separates the islands of Sumatra and Java with the volcanic island Krakatoa lying between them. Krakatau erupted violently in 1883, destroying two-thirds of the island and leaving a large caldera under the sea. This cataclysmic explosion was heard as far away as the island of Rodrigues near Mauritius (approx. 4,800 kilometres (3,000 mi) away). [1] A new parasitic cone, called Anak Krakatau (or the child of Krakatau), rose from the sea at the centre of the caldera in 1930. [14] The other Krakatau islets from the 1883 eruptions are known as Sertung, Panjang and Rakata.

Java is a relatively small island compared to Sumatra, but it has a higher concentration of active volcanoes. There are 45 active volcanoes on the island excluding 20 small craters and cones in the Dieng volcanic complex and the young cones in the Tengger caldera complex. Some volcanoes are grouped together in the list below because of their close location. Mount Merapi, Semeru and Kelud are the most active volcanoes in Java. Mount Semeru has been continuously erupting since 1967. [15] Mount Merapi has been named as one of the Decade Volcanoes since 1995. [16] Ijen has a unique colourful caldera lake which is an extremely acidic natural reservoir (pH<0.3). [17] There are sulfur mining activities at Ijen, where miners collect highly concentrated sulfur rocks by hand.

NameShapeElevationLast eruption (VEI)Coordinates
Krakatau caldera 813 metres (2,667 ft)2022 (ongoing) 6°06′07″S105°25′23″E / 6.102°S 105.423°E / -6.102; 105.423
Pulosari stratovolcano 1,346 metres (4,416 ft)unknown 6°20′31″S105°58′30″E / 6.342°S 105.975°E / -6.342; 105.975
Gunung Karang stratovolcano1,778 metres (5,833 ft)unknown 6°16′12″S106°02′31″E / 6.27°S 106.042°E / -6.27; 106.042
Salak stratovolcano2,211 metres (7,254 ft)31 January 1938 (2) 6°43′S106°44′E / 6.72°S 106.73°E / -6.72; 106.73
Kiaraberes-Gagak stratovolcano1,511 metres (4,957 ft)6 April 1939 (1) 6°44′S106°39′E / 6.73°S 106.65°E / -6.73; 106.65
Perbakti stratovolcano1,699 metres (5,574 ft)unknown 6°45′S106°41′E / 6.75°S 106.68°E / -6.75; 106.68
Kendeng stratovolcano1,732 metres (5,682 ft) Pleistocene 6°46′05″S106°31′34″E / 6.768°S 106.526°E / -6.768; 106.526
Gede stratovolcano2,958 metres (9,705 ft)13 March 1957 (2) 6°47′S106°59′E / 6.78°S 106.98°E / -6.78; 106.98
Patuha stratovolcano2,434 metres (7,986 ft)unknown 7°09′36″S107°24′00″E / 7.160°S 107.40°E / -7.160; 107.40
Wayang-Windu lava dome 2,182 metres (7,159 ft)unknown 7°12′29″S107°37′48″E / 7.208°S 107.63°E / -7.208; 107.63
Malabar stratovolcano2,343 metres (7,687 ft)unknown 7°08′S107°39′E / 7.13°S 107.65°E / -7.13; 107.65
Tangkuban Perahu stratovolcano2,084 metres (6,837 ft)26 June 2019 (1) 6°46′S107°36′E / 6.77°S 107.60°E / -6.77; 107.60
Papandayan stratovolcano2,665 metres (8,743 ft)11 November 2002 (2) 7°19′S107°44′E / 7.32°S 107.73°E / -7.32; 107.73
Kendang stratovolcano2,608 metres (8,556 ft)unknown 7°14′S107°43′E / 7.23°S 107.72°E / -7.23; 107.72
Kamojang stratovolcano1,730 metres (5,680 ft) Pleistocene 7°07′30″S107°48′00″E / 7.125°S 107.80°E / -7.125; 107.80
Guntur complex volcano 2,249 metres (7,379 ft)16 October 1847 (2) 7°08′35″S107°50′24″E / 7.143°S 107.840°E / -7.143; 107.840
Tampomas stratovolcano1,684 metres (5,525 ft)unknown 6°46′S107°57′E / 6.77°S 107.95°E / -6.77; 107.95
Galunggung stratovolcano2,168 metres (7,113 ft)9 January 1984 (1) 7°15′00″S108°03′29″E / 7.25°S 108.058°E / -7.25; 108.058
Talagabodas stratovolcano2,201 metres (7,221 ft)unknown 7°12′29″S108°04′12″E / 7.208°S 108.07°E / -7.208; 108.07
Karaha fumarole 1,155 metres (3,789 ft)unknown 7°07′S108°05′E / 7.12°S 108.08°E / -7.12; 108.08
Cereme stratovolcano3,078 metres (10,098 ft)1951 6°53′31″S108°24′00″E / 6.892°S 108.40°E / -6.892; 108.40
Slamet stratovolcano3,432 metres (11,260 ft)2014 7°14′31″S109°12′29″E / 7.242°S 109.208°E / -7.242; 109.208
Dieng complex volcano2,565 metres (8,415 ft)29 April 2021 (?) 7°12′S109°55′E / 7.20°S 109.92°E / -7.20; 109.92
Sundoro stratovolcano3,136 metres (10,289 ft)29 October 1971 (2) 7°18′00″S109°59′31″E / 7.30°S 109.992°E / -7.30; 109.992
Sumbing stratovolcano3,371 metres (11,060 ft)1730 (?) 7°23′02″S110°04′12″E / 7.384°S 110.070°E / -7.384; 110.070
Ungaran stratovolcano2,050 metres (6,730 ft)unknown 7°11′S110°20′E / 7.18°S 110.33°E / -7.18; 110.33
Telomoyo stratovolcano1,894 metres (6,214 ft)unknown 7°22′S110°24′E / 7.37°S 110.40°E / -7.37; 110.40
Merbabu stratovolcano3,145 metres (10,318 ft)1797 (2) 7°27′S110°26′E / 7.45°S 110.43°E / -7.45; 110.43
Merapi stratovolcano2,968 metres (9,738 ft)2019 (ongoing) 7°32′31″S110°26′31″E / 7.542°S 110.442°E / -7.542; 110.442
Muria stratovolcano1,625 metres (5,331 ft)160 BC ± 30 years 6°37′S110°53′E / 6.62°S 110.88°E / -6.62; 110.88
Lawu stratovolcano3,265 metres (10,712 ft)28 November 1885 (1) 7°37′30″S111°11′31″E / 7.625°S 111.192°E / -7.625; 111.192
Wilis stratovolcano2,563 metres (8,409 ft)unknown 7°48′29″S111°45′29″E / 7.808°S 111.758°E / -7.808; 111.758
Kelud stratovolcano1,731 metres (5,679 ft)13 February 2014 (4) 7°55′48″S112°18′29″E / 7.93°S 112.308°E / -7.93; 112.308
KawiButak stratovolcano2,651 metres (8,698 ft)unknown 7°55′S112°27′E / 7.92°S 112.45°E / -7.92; 112.45
ArjunoWelirang stratovolcano3,339 metres (10,955 ft)15 August 1952 (0) 7°43′30″S112°34′48″E / 7.725°S 112.58°E / -7.725; 112.58
Penanggungan stratovolcano1,653 metres (5,423 ft)unknown 7°37′S112°38′E / 7.62°S 112.63°E / -7.62; 112.63
Malang Plain maar 680 metres (2,230 ft)unknown 8°01′S112°41′E / 8.02°S 112.68°E / -8.02; 112.68
Semeru stratovolcano3,676 metres (12,060 ft)2024 (ongoing) 8°06′29″S112°55′12″E / 8.108°S 112.92°E / -8.108; 112.92
Bromo stratovolcano2,329 metres (7,641 ft)2023 7°56′31″S112°57′00″E / 7.942°S 112.95°E / -7.942; 112.95
Lamongan stratovolcano1,651 metres (5,417 ft)5 February 1898 (2) 7°58′44″S113°20′31″E / 7.979°S 113.342°E / -7.979; 113.342
Lurus complex volcano539 metres (1,768 ft)unknown 7°44′S113°35′E / 7.73°S 113.58°E / -7.73; 113.58
Iyang-Argapura complex volcano3,088 metres (10,131 ft)unknown 7°58′S113°34′E / 7.97°S 113.57°E / -7.97; 113.57
Raung stratovolcano3,332 metres (10,932 ft)2022 (?) 8°07′30″S114°02′31″E / 8.125°S 114.042°E / -8.125; 114.042
Ijen stratovolcano2,799 metres (9,183 ft)28 June 1999 (1) 8°03′29″S114°14′31″E / 8.058°S 114.242°E / -8.058; 114.242
Baluran stratovolcano1,247 metres (4,091 ft)unknown 7°51′S114°22′E / 7.85°S 114.37°E / -7.85; 114.37

Note: Height of Krakatau is of Rakata, not of the active Anak Krakatau

Lesser Sunda Islands

The Lesser Sunda Islands is a small archipelago which, from west to east, consists of Bali, Lombok, Sumbawa, Flores, Sumba and the Timor islands; all are located at the edge of the Australian continental shelf. Volcanoes in the area are formed because of oceanic crusts and the movement of the shelf itself. [18] Some volcanoes completely form an island, for instance, the Sangeang Api island. Mount Tambora, on Sumbawa island, erupted on 5 April 1815, with a scale 7 on the VEI and is considered the most violent eruption in recorded history. [3]

NameIslandShapeElevationLast eruption (VEI)Coordinates
Merbuk Baliunknown1,386 metres (4,547 ft)unknown 8°13′S114°39′E / 8.22°S 114.65°E / -8.22; 114.65
Bratan Bali caldera 2,276 metres (7,467 ft)unknown 8°17′S115°08′E / 8.28°S 115.13°E / -8.28; 115.13
Batur Balicaldera1,717 metres (5,633 ft)2000 (1) 8°14′31″S115°22′30″E / 8.242°S 115.375°E / -8.242; 115.375
Agung Bali stratovolcano 3,031 metres (9,944 ft)2019 8°20′31″S115°30′29″E / 8.342°S 115.508°E / -8.342; 115.508
Samalas Lombokstratovolcano2,867 metres (9,406 ft)1257 (7) 8°25′S116°24′E / 8.41°S 116.40°E / -8.41; 116.40
Rinjani Lombokstratovolcano3,726 metres (12,224 ft)2016 (2) 8°25′S116°28′E / 8.42°S 116.47°E / -8.42; 116.47
Tambora Sumbawastratovolcano2,722 metres (8,930 ft)1967 ± 20 years (0) 8°15′S118°00′E / 8.25°S 118.00°E / -8.25; 118.00
Sangeang Api Sangeang complex volcano 1,949 metres (6,394 ft)2019 (ongoing) 8°12′S119°04′E / 8.20°S 119.07°E / -8.20; 119.07
Wai Sano Florescaldera903 metres (2,963 ft)unknown 8°43′S120°01′E / 8.72°S 120.02°E / -8.72; 120.02
Poco Leok Floresunknown1,675 metres (5,495 ft)unknown 8°41′S120°29′E / 8.68°S 120.48°E / -8.68; 120.48
Ranakah Flores lava dome 2,100 metres (6,900 ft)March 1991 (1) 8°37′S120°31′E / 8.62°S 120.52°E / -8.62; 120.52
Inierie Floresstratovolcano2,245 metres (7,365 ft)8050 BC 8°52′30″S120°57′00″E / 8.875°S 120.95°E / -8.875; 120.95
Inielika Florescomplex volcano1,559 metres (5,115 ft)11 January 2001 (2) 8°44′S120°59′E / 8.73°S 120.98°E / -8.73; 120.98
Ebulobo Floresstratovolcano2,124 metres (6,969 ft)27 February 1969 (2) 8°49′S121°11′E / 8.82°S 121.18°E / -8.82; 121.18
Iya Floresstratovolcano637 metres (2,090 ft)27 January 1969 (3) 8°53′49″S121°38′42″E / 8.897°S 121.645°E / -8.897; 121.645
Sukaria Florescaldera1,500 metres (4,900 ft)unknown 8°47′31″S121°46′12″E / 8.792°S 121.77°E / -8.792; 121.77
Ndete Napu Flores fumarole 750 metres (2,460 ft)unknown 8°43′S121°47′E / 8.72°S 121.78°E / -8.72; 121.78
Kelimutu Florescomplex volcano1,639 metres (5,377 ft)3 June 1968 (1) 8°46′S121°49′E / 8.77°S 121.82°E / -8.77; 121.82
Paluweh Palu'e stratovolcano875 metres (2,871 ft)3 February 1985 (1) 8°19′12″S121°42′29″E / 8.32°S 121.708°E / -8.32; 121.708
Egon Floresstratovolcano1,703 metres (5,587 ft)2008 8°40′S122°27′E / 8.67°S 122.45°E / -8.67; 122.45
Ilimuda Floresstratovolcano1,100 metres (3,600 ft)unknown 8°28′41″S122°40′16″E / 8.478°S 122.671°E / -8.478; 122.671
Lewotobi Floresstratovolcano1,703 metres (5,587 ft)2024 8°32′31″S122°46′30″E / 8.542°S 122.775°E / -8.542; 122.775
Leroboleng Florescomplex volcano1,117 metres (3,665 ft)26 June 2003 (3) 8°21′29″S122°50′31″E / 8.358°S 122.842°E / -8.358; 122.842
Riang Kotang Floresfumarole200 metres (660 ft)unknown 8°18′00″S122°53′31″E / 8.30°S 122.892°E / -8.30; 122.892
Iliboleng Adonara Island stratovolcano1,659 metres (5,443 ft)June 1993 (1) 8°20′31″S123°15′29″E / 8.342°S 123.258°E / -8.342; 123.258
Lewotolo Lembata stratovolcano1,423 metres (4,669 ft)2020 (ongoing) 8°16′19″S123°30′18″E / 8.272°S 123.505°E / -8.272; 123.505
Ililabalekan Lembata stratovolcano1,018 metres (3,340 ft)unknown 8°33′S123°23′E / 8.55°S 123.38°E / -8.55; 123.38
Iliwerung Lembata complex volcano1,018 metres (3,340 ft)29 November 2021 8°32′S123°34′E / 8.53°S 123.57°E / -8.53; 123.57
Batu Tara Komba islandstratovolcano748 metres (2,454 ft)2007–2015 (2) 7°47′31″S123°34′44″E / 7.792°S 123.579°E / -7.792; 123.579
Sirung Pantar Island complex volcano862 metres (2,828 ft)2021 8°30′29″S124°07′48″E / 8.508°S 124.13°E / -8.508; 124.13
Yersey submarine −3,800 metres (−12,500 ft)unknown 7°32′S123°57′E / 7.53°S 123.95°E / -7.53; 123.95

Banda Sea

The Banda Sea in the south of the Molucca archipelago includes a small group of islands. Three major tectonic plates beneath the sea, the Eurasian plate, Pacific plate and Indo-Australian plate, have been converging since the Mesozoic epoch. [19] Volcanoes in the Banda Sea are mainly islands, but some are submarine volcanoes.

NameShapeElevationLast eruption (VEI)Coordinates
Emperor of China submarine −2,850 metres (−9,350 ft)unknown 6°37′S124°13′E / 6.62°S 124.22°E / -6.62; 124.22
Nieuwerkerk submarine−2,285 metres (−7,497 ft)unknown 6°36′00″S124°40′30″E / 6.60°S 124.675°E / -6.60; 124.675
Gunungapi Wetar stratovolcano 282 metres (925 ft)1699 (3) 6°38′31″S126°39′00″E / 6.642°S 126.65°E / -6.642; 126.65
Wurlali stratovolcano868 metres (2,848 ft)3 June 1892 (2) 7°07′30″S128°40′30″E / 7.125°S 128.675°E / -7.125; 128.675
Teon stratovolcano655 metres (2,149 ft)3 June 1904 (2) 6°55′12″S129°07′30″E / 6.92°S 129.125°E / -6.92; 129.125
Nila stratovolcano781 metres (2,562 ft)7 May 1968 (1) 6°44′S129°30′E / 6.73°S 129.50°E / -6.73; 129.50
Serua stratovolcano641 metres (2,103 ft)18 September 1921 (2) 6°18′S130°00′E / 6.30°S 130.00°E / -6.30; 130.00
Manuk stratovolcano282 metres (925 ft)unknown 5°31′48″S130°17′31″E / 5.53°S 130.292°E / -5.53; 130.292
Banda Api caldera 640 metres (2,100 ft)9 May 1988 (3) 4°31′30″S129°52′16″E / 4.525°S 129.871°E / -4.525; 129.871

Sulawesi and Sangihe Islands

Four peninsulas dominate the shape of Sulawesi island (formerly known as Celebes). The central part is a high mountainous area, but mostly non-volcanic. Active volcanoes are found in the northern peninsula and continuously stretch to the north to Sangihe Islands. The Sangihe Islands mark the border with the Philippines.

NameShapeElevationLast eruption (VEI)Coordinates
Colo stratovolcano 507 metres (1,663 ft)18 July 1983 (4) 0°10′12″S121°36′29″E / 0.17°S 121.608°E / -0.17; 121.608
Ambang complex volcano 1,795 metres (5,889 ft)1845 ± 5 years 0°45′N124°25′E / 0.75°N 124.42°E / 0.75; 124.42
Soputan stratovolcano1,784 metres (5,853 ft)December 2018 1°06′29″N124°43′48″E / 1.108°N 124.73°E / 1.108; 124.73
Sempu caldera 1,549 metres (5,082 ft)unknown 1°07′48″N124°45′29″E / 1.13°N 124.758°E / 1.13; 124.758
Tondano caldera1,202 metres (3,944 ft)unknown 1°14′N124°50′E / 1.23°N 124.83°E / 1.23; 124.83
LokonEmpung stratovolcano1,580 metres (5,180 ft)2015 1°21′29″N124°47′31″E / 1.358°N 124.792°E / 1.358; 124.792
Mahawu stratovolcano1,324 metres (4,344 ft)16 November 1977 (0) 1°21′29″N124°51′29″E / 1.358°N 124.858°E / 1.358; 124.858
Klabat stratovolcano1,995 metres (6,545 ft)unknown 1°28′N125°02′E / 1.47°N 125.03°E / 1.47; 125.03
Tongkoko stratovolcano1,149 metres (3,770 ft)1880 (1) 1°31′N125°12′E / 1.52°N 125.20°E / 1.52; 125.20
Ruang stratovolcano725 metres (2,379 ft)April 2024 (ongoing) 2°18′N125°22′E / 2.30°N 125.37°E / 2.30; 125.37
Karangetang stratovolcano1,784 metres (5,853 ft)2019 (ongoing) 2°47′N125°24′E / 2.78°N 125.40°E / 2.78; 125.40
Banua Wuhu submarine −5 metres (−16 ft)18 July 1919 (3) 3°08′17″N125°29′28″E / 3.138°N 125.491°E / 3.138; 125.491
Awu stratovolcano1,320 metres (4,330 ft)2 June 2004 (2) 3°40′N125°30′E / 3.67°N 125.50°E / 3.67; 125.50
Submarine 1922 submarine−5,000 metres (−16,000 ft)unknown 3°58′N125°10′E / 3.97°N 125.17°E / 3.97; 125.17
Vuurberg (Dutch: fire mountain, Gunung Api) in Bandanaira COLLECTIE TROPENMUSEUM Kustgezicht met vissersboot met op de achtergrond de Vuurberg Bandanaira TMnr 10021959.jpg
Vuurberg (Dutch: fire mountain, Gunung Api) in Bandanaira

Halmahera

Halmahera island in the north of Molucca archipelago has been formed by the movement of three tectonic plates resulting in two intersecting mountain ranges, which form four rocky peninsulas separated by three deep bays. A volcanic arc stretches from north to south in the west side of Halmahera, some of which are volcanic islands, for instance, Gamalama and Tidore. Gamalama's island name is Ternate and it has been the centre for spice trading since the Portuguese Empire opened a fort in 1512. Due to its location as the centre for spice trading during the Age of Discovery, historical records of volcanic eruptions in Halmahera have been available as far back as the early 16th century.

NameShapeElevationLast eruption (VEI)Coordinates
Tarakan pyroclastic cone 318 metres (1,043 ft)unknown 1°50′N127°50′E / 1.83°N 127.83°E / 1.83; 127.83
Dukono complex volcano 1,335 metres (4,380 ft)1933–2021 (ongoing) 1°41′N127°53′E / 1.68°N 127.88°E / 1.68; 127.88
Tobaru unknown1,035 metres (3,396 ft)unknown 1°38′N127°40′E / 1.63°N 127.67°E / 1.63; 127.67
Ibu stratovolcano 1,325 metres (4,347 ft)2024 1°29′17″N127°37′48″E / 1.488°N 127.63°E / 1.488; 127.63
Gamkonora stratovolcano1,635 metres (5,364 ft)9 July 2007 (?) 1°23′N127°32′E / 1.38°N 127.53°E / 1.38; 127.53
Todoko-Ranu caldera 979 metres (3,212 ft)unknown 1°15′N127°28′E / 1.25°N 127.47°E / 1.25; 127.47
Jailolo stratovolcano1,130 metres (3,710 ft)unknown 1°05′N127°25′E / 1.08°N 127.42°E / 1.08; 127.42
Hiri stratovolcano630 metres (2,070 ft)unknown 0°54′N127°19′E / 0.90°N 127.32°E / 0.90; 127.32
Gamalama stratovolcano1,715 metres (5,627 ft)2018 0°48′N127°20′E / 0.80°N 127.33°E / 0.80; 127.33
Tidore stratovolcano1,730 metres (5,680 ft)unknown 0°39′29″N127°24′00″E / 0.658°N 127.40°E / 0.658; 127.40
Mare stratovolcano308 metres (1,010 ft)unknown 0°34′N127°24′E / 0.57°N 127.40°E / 0.57; 127.40
Moti stratovolcano950 metres (3,120 ft)unknown 0°27′N127°24′E / 0.45°N 127.40°E / 0.45; 127.40
Makian stratovolcano1,357 metres (4,452 ft)29 July 1988 (3) 0°19′N127°24′E / 0.32°N 127.40°E / 0.32; 127.40
Tigalalu stratovolcano422 metres (1,385 ft)unknown 0°04′N127°25′E / 0.07°N 127.42°E / 0.07; 127.42
Amasing stratovolcano1,030 metres (3,380 ft)unknown 0°32′S127°29′E / 0.53°S 127.48°E / -0.53; 127.48
Bibinoi stratovolcano900 metres (3,000 ft)unknown 0°46′S127°43′E / 0.77°S 127.72°E / -0.77; 127.72
Depiction of Gamalama erupting in the early 1700s with a Portuguese fort shown Ternate.JPG
Depiction of Gamalama erupting in the early 1700s with a Portuguese fort shown

Major eruptions

Below is a list of selected major eruptions of volcanoes in Indonesia, sorted chronologically by the starting date of the eruption. Only eruptions with scale 3 or above on VEI are given with known sources and fatalities, except if smaller scale eruptions resulted in some fatalities.

Eruption dateVolcanoCessation date VEI Characteristics Tsunami Tephra volumeFatalitySources
3 November 2024Lewotobi Laki LakiOngoing?cv,pf,fa,lmnoN/A10
3 December 2023 Marapi 8 December 20233cv,pf,fa,lmnoN/A24
4 December 2021 Semeru 5 December 20214cv,pf,fa,lmnoN/A69
21 December 2018 Anak Krakatoa 10 January 20193cv,se,pf,fa,lm,cc12 mN/A437 [20] [21]
13 February 2014 Kelut 15 February 20144cv,cl,pf,ph,ld,lmno0.16 km34 [22]
3 November 2010 Merapi 8 November 20104cv,pf,ld,lmnoN/A353 [5]
10 February 1990 Kelut March 19904cv,cl,pf,ph,ld,lmno0.13 km335 [23]
18 July 1983 Colo December 19834cv,pf,phnoN/A0 [23]
5 April 1982 Galunggung 8 January 19834cv,pf,lf,lmno0.37 km3 +68 [24] [25]
6 October 1972MerapiMarch 19852cv,pf,lf,ld,lmno0.021 km329 [5]
26 April 1966Kelut27 April 19664cv,cl,pf,lmno0.089 km3212 [23]
17 March 1963 Agung 27 January 19645cv,pf,lf,lmno1 km31,148 [26]
31 August 1951Kelut31 August 19514cv,cl,pf,lmno0.2 km37 [23]
25 November 1930MerapiSeptember 19313cv,rf,pf,lf,ld,lmno0.0017 km31,369 [5]
19 May 1919Kelut20 May 19194cv,cl,pf,lmno0.19 km35,110 [23]
7 June 1892 Awu 12 June 18923cv,pf,lmyesN/A1,532 [27]
26 August 1883 Krakatoa February 18846cv,se,pf,fa,lm,cc1542 m58.5 km336,600 [1] [26] [28]
15 April 1872Merapi21 April 18724cv,pfno0.33 km3200 [5]
2 March 1856Awu17 March 18563cv,pf,lmyes0.51±0.50 km32,806 [27]
8 October 1822 Galunggung December 18225cv,pf,ld,lmno1 km3 +4,011 [23]
10 April 1815 Mount Tambora 15 July 18157cv,pf,cc12 m160 km371,000+ [3] [29]
6 August 1812Awu8 August 18124cv,pf,lmno0.55±0.50 km3963 [27]
12 August 1772 Papandayan 12 August 17723cv,phnoN/A2,957 [30]
4 August 1672Merapiunknown3cv,pf,lmnoN/A3,000 [5]
1586Kelutunknown5cf,cl,lmno1 km3 +10,000 [23]
September 1257 Samalas unknown7 [31]
≈ 74,000 BP Toba unknown8pf,lf,cclikely2,800 km3 Possible near extinction of all the human population [2]
Notes: cv=central vent eruption, pf=pyroclastic flows, lf=lava flows, lm=lahar mudflows, cl=crater lake eruption, ph=phreatic eruption, ld=lava dome extrusion, cc=caldera collapse, se=submarine eruption, fa=fumarole activity, rf=radial fissure eruption.

See also

Related Research Articles

A caldera is a large cauldron-like hollow that forms shortly after the emptying of a magma chamber in a volcanic eruption. An eruption that ejects large volumes of magma over a short period of time can cause significant detriment to the structural integrity of such a chamber, greatly diminishing its capacity to support its own roof, and any substrate or rock resting above. The ground surface then collapses into the emptied or partially emptied magma chamber, leaving a large depression at the surface. Although sometimes described as a crater, the feature is actually a type of sinkhole, as it is formed through subsidence and collapse rather than an explosion or impact. Compared to the thousands of volcanic eruptions that occur over the course of a century, the formation of a caldera is a rare event, occurring only a few times within a given window of 100 years. Only eight caldera-forming collapses are known to have occurred between 1911 and 2018, with a caldera collapse at Kīlauea, Hawaii in 2018. Volcanoes that have formed a caldera are sometimes described as "caldera volcanoes".

<span class="mw-page-title-main">Krakatoa</span> Volcanic caldera in the Sunda Strait

Krakatoa, also transcribed Krakatau, is a caldera in the Sunda Strait between the islands of Java and Sumatra in the Indonesian province of Lampung. The caldera is part of a volcanic island group comprising four islands. Two of them are known as Lang and Verlaten; another, Rakata, is the only remnant of an island mostly destroyed by an eruption in 1883 which created the caldera.

<span class="mw-page-title-main">Lake Toba</span> Volcanic lake located in North Sumatra Province, Indonesia

Lake 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 2.88°N 98.52°E to 2.35°N 99.1°E. The lake is about 100 kilometres 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.

<span class="mw-page-title-main">Volcano</span> Rupture in a planets crust where material escapes

A volcano is a rupture in the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape from a magma chamber below the surface. The process that forms volcanoes is called volcanism.

<span class="mw-page-title-main">Mount Tambora</span> Active stratovolcano in Sumbawa in Indonesia

Mount Tambora, or Tomboro, is an active stratovolcano in West Nusa Tenggara, Indonesia. Located on Sumbawa in the Lesser Sunda Islands, it was formed by the active subduction zones beneath it. Before 1815, its elevation reached more than 4,300 metres high, making it one of the tallest peaks in the Indonesian archipelago.

<span class="mw-page-title-main">Stratovolcano</span> Type of conical volcano composed of layers of lava and tephra

A stratovolcano, also known as a composite volcano, is a conical volcano built up by many alternating layers (strata) of hardened lava and tephra. Unlike shield volcanoes, stratovolcanoes are characterized by a steep profile with a summit crater and explosive eruptions. Some have collapsed summit craters called calderas. The lava flowing from stratovolcanoes typically cools and solidifies before spreading far, due to high viscosity. The magma forming this lava is often felsic, having high to intermediate levels of silica, with lesser amounts of less viscous mafic magma. Extensive felsic lava flows are uncommon, but can travel as far as 8 km (5 mi).

<span class="mw-page-title-main">Ring of Fire</span> Region around the rim of the Pacific Ocean where many volcanic eruptions and earthquakes occur

The Ring of Fire is a tectonic belt of volcanoes and earthquakes.

<span class="mw-page-title-main">Novarupta</span> Volcano in Katmai National Park, Alaska, US

Novarupta is a volcano that was formed in 1912, located on the Alaska Peninsula on a slope of Trident Volcano in Katmai National Park and Preserve, about 290 miles (470 km) southwest of Anchorage. Formed during the largest volcanic eruption of the 20th century, Novarupta released 30 times the volume of magma of the 1980 eruption of Mount St. Helens.

<span class="mw-page-title-main">Phreatic eruption</span> Volcanic eruption caused by an explosion of steam

A phreatic eruption, also called a phreatic explosion, ultravulcanian eruption or steam-blast eruption, occurs when magma heats ground water or surface water. The extreme temperature of the magma causes near-instantaneous evaporation of water to steam, resulting in an explosion of steam, water, ash, rock, and volcanic bombs. At Mount St. Helens in Washington state, hundreds of steam explosions preceded the 1980 Plinian eruption of the volcano. A less intense geothermal event may result in a mud volcano.

<span class="mw-page-title-main">Sunda Arc</span> Volcanic island arc in Indonesia

The Sunda Arc is a volcanic arc that produced the volcanoes that form the topographic spine of the islands of Sumatra, Nusa Tenggara, Java, the Sunda Strait, and the Lesser Sunda Islands. The Sunda Arc begins at Sumatra and ends at Flores, and is adjacent to the Banda Arc. The Sunda Arc is formed via the subduction of the Indo-Australian Plate beneath the Sunda and Burma plates at a velocity of 63–70 mm/year.

<span class="mw-page-title-main">Mount Rinjani</span> Volcano in Lombok, Indonesia

Mount Rinjani is an active volcano in Indonesia on the island of Lombok. Administratively the mountain is in the Regency of North Lombok, West Nusa Tenggara. It rises to 3,726 metres (12,224 ft), making it the second highest volcano in Indonesia. It is also the highest point in the Indonesian province of West Nusa Tenggara. Adjacent to the volcano is a 6-by-8.5-kilometre caldera, which is filled partially by the crater lake known as Segara Anak or Anak Laut, due to the color of its water, as blue as the sea (laut). This lake is approximately 2,000 metres (6,600 ft) above sea level and estimated to be about 200 metres (660 ft) deep; the caldera also contains hot springs. The lake and mountain are sacred to the Sasak people and Hindus, and are the site of religious rituals. UNESCO made Mount Rinjani Caldera a part of the Global Geoparks Network in April 2018. Mount Rinjani or Samalas are the largest volcanic eruption in the last 2000 years.

<span class="mw-page-title-main">Anak Krakatoa</span> Volcanic island in the Sunda Strait, Indonesia

Anak Krakatau is a volcanic island in Indonesia. On 29 December 1927, Anak Krakatau first emerged from the caldera formed in 1883 by the explosive volcanic eruption that destroyed the island of Krakatoa. There has been sporadic eruptive activity at the site since the late 20th century, culminating in a large underwater collapse of the volcano, which caused a deadly tsunami in December 2018. There has been subsequent activity since. Owing to its young age the island is one of several in the area that are of interest to, and the subject of extensive study by volcanologists.

<span class="mw-page-title-main">Mount Merbabu</span> Stratovolcano in Central Java, Indonesia

Mount Merbabu is a dormant stratovolcano in Central Java province on the Indonesian island of Java. The name Merbabu could be loosely translated as 'Mountain of Ash' from the Javanese combined words; Meru means "mountain" and awu or abu means "ash".

<span class="mw-page-title-main">Volcanism of Indonesia</span>

Indonesia is a volcanically active country, containing numerous major volcanoes. It has the most volcanoes of any country in the world, with 76 volcanoes that have erupted at least 1,171 times in total within historical times. The Smithsonian Institution has 141 Indonesian entries in its volcano database. Indonesia has around 130 active volcanoes that are part of the Pacific Ring of Fire, and it has suffered the highest numbers of eruptions resulting in fatalities, damage to arable land, debris flows, tsunamis, lava domes, and pyroclastic flows. Indonesia's most active volcanoes are Kelut and Mount Merapi on the island of Java. The majority of Indonesia's volcano are located on a 3,000 km long chain called the Sunda Arc. Here, the subduction of the Indian Ocean crust underneath the Asian Plate produced most of these volcanoes.

<span class="mw-page-title-main">Timeline of volcanism on Earth</span>

This timeline of volcanism on Earth includes a list of major volcanic eruptions of approximately at least magnitude 6 on the Volcanic explosivity index (VEI) or equivalent sulfur dioxide emission during the Quaternary period. Other volcanic eruptions are also listed.

The Deep Earth Carbon Degassing (DECADE) project is an initiative to unite scientists around the world to make tangible advances towards quantifying the amount of carbon outgassed from the Earth's deep interior into the surface environment through naturally occurring processes. DECADE is an initiative within the Deep Carbon Observatory (DCO).

References

Notes

  1. 1 2 3 Winchester, Simon (2003). Krakatoa: The Day the World Exploded: August 27, 1883. HarperCollins. ISBN   978-0-06-621285-2.
  2. 1 2 3 Oppenheimer, C. (2002). "Limited global change due to the largest known Quaternary eruption, Toba ≈74 kyr BP?". Quaternary Science Reviews. 21 (14–15): 1593–1609. Bibcode:2002QSRv...21.1593O. doi:10.1016/S0277-3791(01)00154-8.
  3. 1 2 3 Stothers, Richard B. (1984). "The Great Tambora Eruption in 1815 and Its Aftermath". Science . 224 (4654): 1191–1198. Bibcode:1984Sci...224.1191S. doi:10.1126/science.224.4654.1191. PMID   17819476. S2CID   23649251.
  4. "Kelut Eruptive History". Global Volcanism Program. Smithsonian Institution . Retrieved 19 December 2006.
  5. 1 2 3 4 5 6 "Merapi Eruptive History". Global Volcanism Program. Smithsonian Institution . Retrieved 19 December 2006.
  6. "Indonesia Miliki 127 Gunung Api Aktif". 2 May 2012.
  7. "Volcano Data Criteria". Global Volcanism Program. Smithsonian Institution . Retrieved 14 June 2015.
  8. "Centre of Volcanology & Geological Hazard Mitigation". Volcanological Survey of Indonesia. Archived from the original on 16 December 2006. Retrieved 31 December 2006.
  9. 1 2 Simoes, M.; Avouac, J.P.; Cattin, R.; Henry, P. (2004). "The Sumatra subduction zone: A case for a locked fault zone extending into the mantle" (PDF). Journal of Geophysical Research. 109 (B10): B10402. Bibcode:2004JGRB..10910402S. doi: 10.1029/2003JB002958 . Archived (PDF) from the original on 9 September 2006.
  10. Subarya, C.; Chlieh, M.; Prawirodirdjo, L.; Avouac, J.P.; Bock, Y.; Sieh, K.; Meltzner, A.; Natawidjaja, D.H.; McCaffrey, R. (2006). "Plate-boundary deformation associated with the great Sumatra-Andaman earthquake" (PDF). Nature . 440 (7080): 46–51. Bibcode:2006Natur.440...46S. doi:10.1038/nature04522. hdl:10356/94250. PMID   16511486. S2CID   4429816. Archived (PDF) from the original on 9 September 2006.
  11. Lay, T.; Kanamori, H.; Ammon, C.; Nettles, M.; Ward, S.; Aster, R.; Beck, S.; Bilek, S.; Brudzinski, M.; Butler, R.; DeShon, H.; Ekstrom, G. (2005). "The Great Sumatra-Andaman Earthquake of 26 December 2004" (PDF). Science . 308 (5725): 1127–1133. Bibcode:2005Sci...308.1127L. doi:10.1126/science.1112250. PMID   15905392. S2CID   43739943. Archived (PDF) from the original on 11 September 2006.
  12. "Smithsonian / USGS Weekly Volcanic Activity Report". Smithsonian Institution. 15 August 2020. Retrieved 15 August 2020.
  13. "Masurai". Global Volcanism Program . Smithsonian Institution.
  14. Whittaker, R. J.; Bush, M. B. (1993). "Anak Krakatau and old Krakatau: a reply". GeoJournal . 29 (4): 417–420. doi:10.1007/BF00807545. S2CID   155054596.
  15. "Semeru Weekly Reports". Global Volcanism Program. Smithsonian Institution . Retrieved 7 December 2006.
  16. International Association of Volcanology and Chemistry of the Earth's Interior (1995). "Decade Volcano Update". Bulletin of Volcanology. 57 (1): 82–83. Bibcode:1995BVol...57...76.. doi:10.1007/BF00298711. S2CID   195243529.
  17. Ansje Löhr; Thom Bogaard; Alex Heikens; Martin Hendriks; Sri Sumarti; Manfred van Bergen; Kees C.A.M. van Gestel; Nico van Straalen; Pieter Vroonand & Budi Widianarko (2005). "Natural Pollution Caused by the Extremely Acid Crater Lake Kawah Ijen, East Java, Indonesia". Environmental Science and Pollution Research. 12 (2): 89–95. Bibcode:2005ESPR...12...89L. doi:10.1065/espr2004.09.118. PMID   15859115. S2CID   128470417.
  18. H. A. Brouwer (July 1939). "Exploration in the Lesser Sunda Islands". The Geographical Journal. 94 (1): 1–10. Bibcode:1939GeogJ..94....1B. doi:10.2307/1788584. JSTOR   1788584.
  19. Christian Honthaasa; Jean-Pierre Réhaulta; René C. Maurya; Hervé Bellona; Christophe Hémonda; Jacques-André Maloda; Jean-Jacques Cornéeb; Michel Villeneuveb; Joseph Cottena; Safri Burhanuddinc; Hervé Guilloud; Nicolas Arnaud (1998). "A Neogene back-arc origin for the Banda Sea basins: geochemical and geochronological constraints from the Banda ridges (East Indonesia)". Tectonophysics. 298 (4): 297–317. Bibcode:1998Tectp.298..297H. doi:10.1016/S0040-1951(98)00190-5.
  20. Albert (4 January 2019). "The rise and fall of Anak Krakatau". VolcanoCafe. Retrieved 13 June 2019.
  21. "Krakatau". Global Volcanism Program. Retrieved 13 June 2019.
  22. "Kelut Eruptive History". Global Volcanism Program. Retrieved 13 June 2019.
  23. 1 2 3 4 5 6 7 "Large Holocene Eruptions". Global Volcanism Program. Smithsonian Institution. Archived from the original on 30 December 2006. Retrieved 18 December 2006.
  24. Katili, J.A. & Sudradjat, A. (1984). "Galunggung: the 1982-1983 eruption". Volcanology Survei Indonesia: 102.
  25. "Galunggung, Java, Indonesia". Volcano World. Department of Geosciences at Oregon State University. Archived from the original on 16 June 2008. Retrieved 30 December 2006.
  26. 1 2 Michael R. Rampino & Stephen Self (1982). "Historic eruptions of Tambora (1815), Krakatau (1883), and Agung (1963), their stratospheric aerosols, and climatic impact". Quaternary Research. 18 (2): 127–143. Bibcode:1982QuRes..18..127R. doi:10.1016/0033-5894(82)90065-5. S2CID   140594715.
  27. 1 2 3 "Awu's Eruptive History". Global Volcanism Program. Smithsonian Institution . Retrieved 31 December 2006.
  28. B.H. Choi; E. Pelinovsky; K.O. Kim; J.S. Lee (2003). "Simulation of the trans-oceanic tsunami propagation due to the 1883 Krakatau volcanic eruption". Natural Hazards and Earth System Sciences. 3 (5): 321–332. Bibcode:2003NHESS...3..321C. doi: 10.5194/nhess-3-321-2003 .
  29. Oppenheimer, Clive (2003). "Climatic, environmental and human consequences of the largest known historic eruption: Tambora volcano (Indonesia) 1815". Progress in Physical Geography. 27 (2): 230–259. Bibcode:2003PrPG...27..230O. doi:10.1191/0309133303pp379ra. S2CID   131663534.
  30. "The Deadliest Eruptions". Volcano World. Department of Geosciences at Oregon State University. Archived from the original on 25 January 2009. Retrieved 15 March 2009.
  31. Vidal, Céline M.; Komorowski, Jean-Christophe; Métrich, Nicole; Pratomo, Indyo; Kartadinata, Nugraha; Prambada, Oktory; Michel, Agnès; Carazzo, Guillaume; Lavigne, Franck; Rodysill, Jessica; Fontijn, Karen; Surono (8 August 2015). "Dynamics of the major plinian eruption of Samalas in 1257 A.D. (Lombok, Indonesia)". Bulletin of Volcanology. 77 (9): 73. Bibcode:2015BVol...77...73V. doi:10.1007/s00445-015-0960-9. S2CID   127929333.

Sources

  1. Tom Simkin & Lee Siebert (1994). Volcanoes of the World: A Regional Directory, Gazetteer, and Chronology of Volcanism During the Last 10,000 Years (2nd ed.). Geoscience Press. ISBN   978-0-945005-12-4.
  2. M. Neumann van Padang (1951). "Indonesia". Catalog of Active Volcanoes of the World and Solfatara Fields (1 ed.). Rome: IAVCEI. pp. 1–271.