Sakurajima
Stratovolcano in Kagoshima Prefecture, Japan
From Wikipedia, the free encyclopedia
Sakurajima (Japanese: 桜島, lit. 'Cherry Blossom Island') is an active stratovolcano, formerly an island and now a peninsula, in Kagoshima Prefecture in Kyushu, Japan.[2] It is the most active volcano in Japan.[3]
| Sakurajima | |
|---|---|
View of Sakurajima from mainland Kagoshima, 2009 | |
| Highest point | |
| Elevation | 1,117 m (3,665 ft) |
| Coordinates | 31°34′50″N 130°39′29″E |
| Geography | |
Kagoshima Prefecture, Japan | |
| Geology | |
| Mountain type | Somma-stratovolcano |
| Last eruption | April 11, 2026[1] |
As of November 2025[update], the volcanic activity continues,[4][5] dropping volcanic ash on the surroundings. Earlier eruptions built the white sand highlands in the region. On September 13, 2016, a team of experts from Bristol University and the Sakurajima Volcano Research Centre in Japan suggested that the volcano could have a major eruption within 30 years; since then many eruptions have occurred.[6][5]
Sakurajima has a population of a few thousand residents, formerly incorporated as Sakurajima town, with a number of schools, shrines, and shops on the island. It is serviced by the Sakurajima Ferry which runs 24/7. It is a tourist destination known for its onsen, local pottery made from volcanic ash, and produce such as the Sakurajima daikon radish and Sakurajima komikan orange which grow in the immensely fertile volcanic soil.
Sakurajima has many different natural areas due to its eruptive history and the ecosystems where recent eruptions have taken place have been researched as an example of ecological succession.
Geography
Sakurajima is a stratovolcano. Its summit has three peaks, Kita-dake (northern peak), Naka-dake (central peak) and Minami-dake (southern peak) which has been recently active.
Kita-dake is Sakurajima's highest peak, rising to 1,117 m (3,665 ft) above sea level. The mountain is in a part of Kagoshima Bay known as Kinkō-wan. The lava flows of the 1914 eruption connected it with the Ōsumi Peninsula.[7] The former island is part of the city of Kagoshima which is only 4 km (2.5 mi) across the bay.[8] The surface of this volcanic peninsula is about 77 km2 (30 sq mi).

Sakurajima is part of the Kirishima-Kinkowan National Park, and its lava flows are a major tourist attraction. The area around Sakurajima contains several hot spring resorts. One of the main agricultural products of Sakurajima is a huge basketball-sized white radish (Sakurajima daikon).[9]
Geology
Sakurajima is in the 25 km (16 mi)-wide Aira caldera, which formed in an enormous "blow-out-and-cave-in" eruption around 28,000 years ago.[10] Several hundred cubic kilometres of ash and pumice were ejected, causing the magma chamber underneath the erupting vents to collapse. Tephra fell as far as 1,000 km (620 mi) from the volcano. Sakurajima is an active vent of the same Aira caldera volcano.
Sakurajima was initially formed about 3000 years later and has had 17 large-scale pumice eruptions since.[10] It is about 8 km (5 mi) south of the centre of the caldera, on its rim.[10] Most of the lavas and tephra erupted have an andesitic-dacitic composition but there are some rhyolite composition eruptives.[11]
Volcanic activity at Kita-dake ended around 4,900 years ago: later eruptions. have been centered on Minami-dake.[12] Initially since 2006, activity was centred on Showa crater, to the east of the summit of Minami-dake,[13] but by 2025 had moved to the summit crater.[5]
History
Prehistoric eruptions
After the volcano formed about 26,000 years ago BP, until recorded history times only the largest eruptions can be identified.[10] Pumice layers P4 to P17 include the P14 vary thick layer from a VEI 6 eruption over 10,000 years ago.[10]
Historic eruptions
Its first eruption in recorded history was in 963 AD.[14] Most of its eruptions are Strombolian,[14] affecting only the summit areas, but larger Plinian eruptions have occurred in 1471–1476, 1779–1782 and 1914.[15]
1914 eruption
The 1914 eruption (also known as Sakura-Jima eruption[7] or Taisho eruption[17]) began on January 11 and was the most powerful in twentieth-century Japan. The volcano had been dormant for over a century until 1914.[18] Almost all residents had left the island in the previous days; several large earthquakes had warned them that an eruption was imminent.
Initially, the eruption was very explosive, generating eruption columns and pyroclastic flows, but after a very large earthquake on January 12, and another the day after, it became effusive, generating a large lava flow.[18] Ash fall occurred as far as the north of Honshu.[17] The January 12 earthquake killed 35, and in total, 58 people died.[16][18] Lava flows filled the narrow strait between the island and the mainland, turning it into a peninsula. It transpired that about 90% of the total magma volume in dense-rock equivalent was lava.[19]
Lava flows are rare in Japan—because the silica content of the magmas is high, explosive eruptions are far more common[20]—but the lava flows at Sakurajima continued for months.[18] The island grew, engulfing several smaller islands nearby, and eventually became connected to the mainland by a narrow isthmus. Parts of Kagoshima Bay became significantly shallower, and it made tides higher.[18]
During the last stages of the eruption, emptying of the underlying magma chamber sank the centre of the Aira Caldera by about 60 cm (24 in).[18] This showed that Sakurajima draws its magma from the same magma reservoir that fed the ancient caldera-forming eruption.[18] The eruption partly inspired a 1914 movie, The Wrath of the Gods, centering on a family curse that ostensibly causes the eruption.
Recent activity

Sakurajima's activity became more prominent in 1955, and the volcano has been erupting almost constantly ever since. Thousands of small explosions happen each year, throwing ash to heights of up to a few kilometers above the mountain. The Sakurajima Volcano Observatory was set up in 1960 to monitor these eruptions.[14] Between 1955 and 2024, 15,057 eruptions from the Minamidake and the Showa craters were observed.[19]
Monitoring of the volcano and predictions of large eruptions are particularly important because it is in a densely populated area, with the city of Kagoshima's 680,000 residents just a few kilometers from the volcano. The city conducts regular evacuation drills, and a number of shelters have been built where people can take refuge from falling volcanic debris.[21]
In light of the dangers it presents to nearby populations, Sakurajima was designated a Decade Volcano in 1991, identifying it as worthy of particular study as part of the United Nations' International Decade for Natural Disaster Reduction.[22]

On March 10, 2009, Sakurajima erupted, sending debris up to 2 km (1.2 mi). An eruption had been expected following a series of smaller explosions over the weekend. It is not thought there was any damage caused.[23] An eruption occurred from the Minami-dake summit crater at 5:38 on Sunday, August 9, 2010, sending debris up to 5000 m (16,000 ft).[24] In 2011 and 2012, Sakurajima experienced several significant eruptions; volcanic activity continued into 2013.[25] On August 18, 2013, the volcano erupted from Showa crater and produced its highest recorded plume of ash since 2006, rising 5,000 metres high and causing darkness and significant ash falls on the central part of Kagoshima city. The eruption occurred at 16:31 and was the 500th eruption of the year.[26] In August 2015, Japan's meteorological agency issued a level 4 emergency warning, which urges residents to prepare to evacuate.[27]
Scientists warned that a major eruption could soon take place at the volcano;[28] it eventually did erupt around 20:00 on February 5, 2016.[29] After a long pause of eruptions at the vent, the eruptions abruptly stopped there and returned to the Showa crater, on April 4, 2016, some 8–9 days preceding major earthquakes on the Median Tectonic Line near Kumamoto, Japan.[30] Then, three months later, on July 26, it spewed volcanic ash 5,000 m (16,000 ft) into the air.[31]
On October 3, 2020, at 07:35 UTC, the volcano erupted once again, this time from the Aira caldera. A volcanic ash advisory for aviation was issued by the Volcanic Ash Advisory Center Tokyo (VAAC) at 07:43 UTC, showing the ash cloud to be stationary and reaching FL100 (10,000 feet).[32] On July 24, 2022, at 20:05 JST, an explosive eruption occurred at the summit crater of the volcano, and cinders scattered up to 2.5 km (1.6 mi) from the crater.[33][34] Following this eruption, at 20:50 JST, the Japan Meteorological Agency raised the eruption alert level from Level 3 to Level 5, the highest level, and urged maximum precaution and evacuation.[33] This was the first time an eruption alert level 5 has been issued for Sakurajima.[35]
On February 9, 2023, an eruption occurred at the Showa crater on Sakurajima at 10:52 JST.[36] The plumes had risen to 1,000 metres (3,300 feet) at 11:10 JST, according to the Kagoshima Meteorological Office.[36] People in a 2 km (1.2 mi) radius were sent a warning by the local weather observatory against pyroclastic flows and falling rocks.[37] On February 14, 2024, an eruption occurred at the southern peak's Minamidake crater on Sakurajima at 18:33 JST, emitting plumes of over 5 kilometres (3.1 miles) in height and spewing rocks as far as 1.3 km (0.81 mi) away.[38] Minamidake crater again erupted on October 18, 2024 with a plume above 4 km (2.5 mi).[5] Between May 15 and May 16, 2025 multiple small eruptions with volcanic plumes up to 3 km (1.9 mi) high occurred disturbing local air travel.[39] On November 16, 2025, Minamidake crater erupted at 00:57 JST with an eruption plume that reached 4,400 m (14,400 ft) high.[5] Volcanic rocks from the eruption reached as far as the fifth station, some 1.2 km (0.75 mi) from the crater and a level 3 alert was issued.[40] On April 11, 2026, another eruption occurred at the Minamidake crater at 12:04 JST. The plume reached a height of 3,400 m (11,200 ft) with large volcanic rocks reaching the volcano's 7th station ejected. Alert level 3 remains in effect.[1]
Summary of eruptive history
| Start Date[41] | Years before 1950 (BP)[41] | VEI[41] | Lava volume (km3) |
Tephra volume (km3) |
Comment |
|---|---|---|---|---|---|
| March 25, 2017 | - | 3 | - | - | Explosive with effusive eruption continuing.[41] Minamidake crater M3 phase.[10] |
| October 13, 1955 | - | 3 | - | - | Explosive with effusive eruption continuing until August 22, 2016.[41] Contains Minamidake crater M1 phase until 1971 and M2 phase from 1972, and from 2006 to 2017 eruptions at Showa crater.[10] |
| November 16, 1954 ± 15 | - | - | - | - | Uncertain details December 16, 1954± 15.[41] |
| June 29, 1950 | 0 | 1 | - | - | Explosive with effusive eruption continuing until September 9, 1950.[41] |
| July 27, 1948 | 2 | 1 | - | - | Explosive with effusive eruption on single day.[41] |
| January 1946 | 4 | 2 | 0.18[10] | - | Eruption ended November 1946.[41] |
| July 1, 1942 | 8 | 1 | - | - | Explosive with effusive eruption on single day.[41] |
| April 1941 | 9 | 2 | - | - | Explosive with effusive eruption ended 26 August 1941[41] |
| April 24, 1940 | 10 | 2 | - | - | Explosive with effusive eruption ended 9 July 1940.[41] |
| November 26, 1939 | 11 | 2 | - | - | Explosive with effusive eruption ended about 12 November 1939.[41] |
| February 25, 1938 | 12 | 2 | - | - | Explosive with effusive eruption ended 31 March 1938.[41] |
| September 20, 1935 | 15 | 1 | - | - | Explosive with effusive eruption ended 24 September 1935.[41] |
| January 12, 1914 | 36 | 4 | 1.34[10] | 0.5[10] | Explosive (P1 tephra) with effusive eruption of Taisho lava ended in May 1915.[41][11] |
| September 24, 1899 | 51 | - | - | - | Uncertain details, ended September 25, 1899.[41] |
| 1860 | 90 | 1 | - | - | Explosive with effusive eruption.[41] |
| March 27, 1799 | 151 | 2 | - | - | Explosive with effusive eruption.[41] |
| 1797 | 153 | 2 | - | - | Explosive with effusive eruption.[41] |
| 1794 | 156 | 2 | - | - | Explosive with effusive eruption[41] |
| September 11, 1791 | 159 | 2 | - | - | Explosive with effusive eruption.[41] |
| July 29, 1790 | 160 | 2 | - | - | Explosive with effusive eruption.[41] |
| November 20, 1785 | 165 | 2 | - | - | Explosive with effusive eruption.[41] |
| September 3, 1783 | 167 | 3 | Explosive with effusive eruption continuing until August 22, 2016.[41] | ||
| January 18, 1782 | 168 | 2 | - | - | Explosive with effusive eruption may have VEI less than 2.[41] |
| November 8, 1779 | 171 | 4 | 1.7[11] | 0.22[11] | Explosive (P2 tephra) with effusive eruption of An-ei lava ended in May 1781.[41][11] |
| September 9, 1756 | 194 | 2 | - | - | Explosive with effusive eruption.[41] |
| September 1749 | 201 | 2 | - | - | Explosive with effusive eruption.[41] |
| April 6, 1742 | 208 | 2 | - | - | Explosive with effusive eruption possibly less than VEI 2.[41] |
| January 1706 | 244 | 2 | - | - | Explosive with effusive eruption possibly less than VEI 2.[41] |
| March 1, 1678 | 272 | 2 | - | - | Explosive with effusive eruption possibly less than VEI 2.[41] |
| April 6, 1642 | 308 | 2 | - | - | Explosive with effusive eruption possibly less than VEI 2.[41] |
| September 23, 1478 | 472 | 2 | - | - | Explosive with effusive eruption possibly less than VEI 2.[41] |
| November 3, 1471 | 479 | 5 | 0.53[11] | 0.49[11] | Explosive (P3 tephra) with effusive eruption of Bunmei lava possibly less than VEI 5 ending on or after October 8, 1476.[41][11] |
| 1468 | 482 | 2 | - | - | Explosive with effusive eruption.[41] |
| 778 | 1172 | 0 | - | - | Explosive with effusive eruption.[41] |
| July 20, 766 | 1184 | 3 | Explosive with effusive eruption.[41] | ||
| January 764 | 1186 | 4 | - | - | Explosive with effusive eruption.[41] First recorded large–scale historical eruption.[10] |
| 716 | 1234 | 3 | Explosive with effusive eruption continued until 718.[41] | ||
| 708 | 1242 | 3 | Explosive with effusive eruption.[41] | ||
| 650 BCE | 2600 | - | - | - | Explosive with effusive eruption.[41] |
| 1050 BCE | 3000 | - | - | - | Explosive with effusive eruption.[41] |
| 2050 BCE | 4000 | - | - | - | Explosive with effusive eruption[41] |
| 2900 BCE | 4850 | 4 | - | 0.18[11] | Explosive (P5 tephra)[11] with effusive eruption.[41] |
| 3500 BCE | 5450 | - | - | - | Explosive with effusive eruption.[41] |
| 4800 BCE | 6750 | - | - | - | Explosive with effusive eruption,[41] Minami-dak activity.[10] |
| 5400 BCE | 7350 | - | - | - | Explosive with effusive eruption.[41] |
| 5950 BCE | 7900 | - | - | - | Explosive with effusive eruption.[41] |
| 6050 BCE | 8000 | 5 | - | - | Explosive with effusive eruption.[41] |
| 6350 BCE | 8300 | - | - | - | Explosive (P11 tephra) with effusive eruption of Gongenyam lava.[41][11] |
| 7750 BCE | 9700 | - | - | - | Explosive (P12 tephra) with effusive eruption of Harutayama lava[41][11] |
| 8050 ± 1000 BCE | 10000 | 6 | - | - | P13 tephra and Kitadake lava (Warishizaki lava)[11] |
Eruptive risk
A monitoring system with formalised warnings since 2007 is in place, and evacuation drills have been held in the Sakurajima immediate area since 1970.[10] Since 2024 a predictive model based on local ground inflation has been in place at the local volcanic observatory that may give short term warning of eruption and ash fall distribution from contemporary minor eruptions.[19] An impact assessment of a eruption of the scale of the 1914 eruption predicts the disruption with damage multiple critical infrastructure features, including airports, roads, power networks, and buildings up to a Japanese national level.[17] The volcano is predicted to accumulate sufficient magma in 130 years to allow a repeat of this scale eruption.[17] The ash fall thickness of such an eruption would have about a 5% probability of temporarily closing the six largest airports in Japan and above a 80% probability of closing the major Kyushu airports of Miyazaki and Kagoshima.[17] Road and rail transport disruption would be limited to Kyushu and electricity supply disruption to souther Kyushu.[17] The combination of an eruption and a high rainfall weather event would be particularity problematical due to electrical arc flash events.[17] The ash fall would be most disruptive to local property and people if an eruption occurred in winter or during a has the local ash fall is likely to be heavier then.[17]
Culture

Sakurajima is a novella written in 1946 by the Japanese writer Haruo Umezaki, about a disillusioned Navy officer stationed on the island towards the end of World War II as American planes bomb Japan. The story is one of Umezaki's most famous works. It is based on his own experience; during World War II, he was stationed at a military cipher base in the nearby city of Kagoshima.
"Sakurajima" is also the name of a song by Japanese singer Tsuyoshi Nagabuchi. In 2004, Nagabuchi held an all night concert at a quarry of Sakurajima that attracted an audience of 75,000. Afterwards, a statue showing Nagabuchi screaming with a guitar was installed on the site of the concert.[42]
See also
- List of volcanoes in Japan
- Flag of Kagoshima Prefecture, which features Sakurajima