1888 Ritter Island eruption and tsunami

1888 Ritter Island eruption and tsunami
1888 Ritter Island eruption and tsunami
Volcano	Ritter Island
Start date	March 13, 1888
End date	March 13, 1888
Type	Phreatic or phreatomagmatic
Location	Bismarck Sea ; (German New Guinea); 5°31′12″S148°06′54″E / 5.520°S 148.115°E
VEI	2
Impact	Volcanic summit collapsed resulting in a tsunami
Deaths	1,500–3,000 (estimated)
	Ritter Island

Last updated January 12, 2025

On 13 March 1888, a section of Ritter Island, a small volcanic island off the coast of New Guinea, collapsed into the sea in a sector collapse. The collapse triggered tsunami waves that struck nearby and distant islands such as New Guinea, Umboi, Sakar and New Britain. It caused heavy damage and deaths in coastal settlements. While no confirmed death toll exists, it is estimated that between 1,500 and 3,000 people died.

Background

Ritter Island in the Bismarck Archipelago is an active stratovolcano located off the northeast coast of Papua New Guinea. It is one of the many active volcanoes in Papua New Guinea as a result of subduction of the Solomon Sea plate beneath the Bismarck Plate along the New Britain Trench.^[2] Before the eruption of 1888, the island was described as a steep-sided and almost-circular volcanic cone and was a notable feature to sailors passing through the Dampier Strait. It had an estimated height of 780 m (2,560 ft).^[2] Based on sketches from the 1830s, the sides of the volcano had an average angle of 45°, with the western flank probably steeper as it had experienced minor landslides.^[1] In other illustrations, these slopes were measured at up to 50°, though they were likely exaggerated. Earlier signs of activity were recorded in 1699 and 1793, demonstrating Strombolian eruptions. Smoke and steam were observed in 1835 and 1848.^[3]^[4]^[1] The eruptions of 1887 and 1878 remain uncertain, with various sources supporting or denying their existence.^[3] An anonymous report stated that ashfall and tremors were recorded at Finschhafen in February 1887 and may have originated from Ritter Island.^[5]

Eruption and collapse

There were no direct observations of the sector collapse on Ritter Island.^[1]^[6] After the collapse, only a crescent-shaped island and islet near its southern tip remained of the former volcanic cone. The height of the island was reduced from 780 to 140 m (2,560 to 460 ft).^[2]^[1] An amphitheater-shaped scar representing the landslide scarp extends approximately north–south. The steep scarp rises 100–200 m (330–660 ft) from the sea, and extends towards the western base of the cone, at 900 m (3,000 ft) beneath sea level, where it also spreads out to 4 km (2.5 mi) across.^[7] The volume of material lost to the collapse remains a contentious topic with various figures estimated. Ritter Island remains active; minor eruptions occurred for the first time since the collapse in 1972.^[2]

Witnesses at Hatzfeldthaven, 350 km (220 mi) west of the volcano, reported plausible phreatic activity, while a thunder-like sound was heard at Finschhafen, 100 km (62 mi) in the south. About 20 km (12 mi) away, fragmented pumice fell on New Guinea's western rainforest while pumice swept onto the northern coastline. These reports might suggest a magmatic eruption, however, an alternative explanation is a phreatic explosion caused by seawater entering the conduit system exposed by the landslide.^[1] This process was similar to Mount Bandai's eruption the same year.^[8]

A 2019 study published Earth and Planetary Science Letters estimated that 2.4 km³ (0.58 cu mi) of the western edifice collapsed based on based on seafloor bathymetry analysis. This estimate is slightly smaller than the sector collapse involved in the 1980 eruption of Mount St. Helens (2.7 km³ (0.65 cu mi)),^[1] but larger than other sector collapses involving Oshima-Oshima in 1741 (0.4 km³ (0.096 cu mi)); Unzen in 1792 (0.34 km³ (0.082 cu mi)) and Anak Krakatoa in 2018 (0.3 km³ (0.072 cu mi)).^[3] The collapse was preceded by gradual, intermittent lateral spreading of the volcanic edifice, as evidenced by compressional structures in seismic profiles. This phenomenon extended into the basement, destabalizing the edifice and contributed to the eventual collapse. The collapse mobilised more than 13 km³ (3.1 cu mi) of material; a large portion (11.2 km³ (2.7 cu mi)) comprised the deformed seafloor, eroded sediments and pre-collapse edifice affected by the gradual spreading. The dramatic collapse which generated the tsunami only represented 2.4 km³ (0.58 cu mi) of the total volume. Edifice spreading also continued after the collapse.^[1]

Published in Marine and Petroleum Geology , a 2015 study estimated that Ritter Island lost 4.2 km³ (1.0 cu mi) of its volume by comparing a reconstructed topographic map of the volcano before and after its collapse. This analysis revealed that the failure also involved part of the volcano’s base, which was constructed above weak marine sediments. This structural weakness directed the collapse at the base. Reports of a single wave train supported the hypothesis of a single landslide event generating the tsunami. The collapsing mass shattered into several blocks that moved together. About 71 percent of the landslide debris was deposited near the valley between Sakar and Umboi.^[7]

Tsunami

Some places located 350 to 500 km (220 to 310 mi) from the volcano were damaged by the tsunami.^[8] There are no exact tally for the death toll but at least 1,500 to about 3,000 people may have died. Every village along the Dampier Strait between Sakar and Umboi were demolished. Many died on Umboi and villages along the northern coast were destroyed,^[9]^[10] but there were no detailed studies to document the losses. According to a local leader, several hundred were killed and the village of Lutherhafen on northwestern Umboi was abandoned. In a survey of Umboi one year after the tsunami, several villages along the eastern shore were missing.^[5]^[3]

On Umboi and Sakar, run-ups of 10 to 15 m (33 to 49 ft) were measured while at Hatzfeldhafen and Rabaul, the run-ups were 10 m (33 ft) and 5 m (16 ft), respectively.^[11] In Arica, Chile, newspapers reported that a series of strong waves smashed and capsized ships. Tide gauges in Sydney, Australia, recorded abnormal readings ruled out as tidal floods and attributed it to a possible tsunami.^[10]

Eighteen people; 2 Germans, 4 Malays, and 12 Melanesians from the Duke of York Islands, were on New Britain at the time as part of a New Guinea Company group syrveying possible for coffee plantations areas.^[5] They were located along the coast near a cliff when the waves washed away some of the expedition members. It left a 1.2 meters (3.9 ft) thick layer of organic debris composed of sand, debris and dead fish, onto the coast.^[10] A search party was sent out to rescue the two Germans missing, but found only five Melanesians workers. They were caught by the wave but survived by clutching onto tree branches before it retreated back to sea.^[5] The tsunami had a maximum wave height of 12–15 metres (39–49 ft) based on tidemarks on the trees.^[6]

At Finschhafen a witness recalled the shore receding after thunderous noises. The water level at the town was so low that it posed dangers to ships at the harbor, and a reef near Madang was exposed some 1.5–1.8 metres (5–6 ft). The tsunami destroyed some homes and canoes belonging to the Melanesian people.^[5] At Hatzfeldhaven, the tsunami arrived at 06:40; the first wave was estimated to be 2 m (6 ft 7 in) taller than the tallest flood marking. The highest wave struck at 09:00, measuring about 8 m (26 ft).^[3] It destroyed a yam store and boat shelter. It also carried some lumber that was to be used for a bridge. Some poorly constructed houses in Kelana village were swept away.^[12]

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References

1 2 3 4 5 6 7 8 Karstens, Jens; Berndt, Christian; Urlaub, Morelia; Watt, Sebastian F.L.; Micallef, Aaron; Ray, Melanie; Klaucke, Ingo (2019). "From gradual spreading to catastrophic collapse – Reconstruction of the 1888 Ritter Island volcanic sector collapse from high-resolution 3D seismic data". Earth and Planetary Science Letters. 517: 1–13. Bibcode:2019E&PSL.517....1K. doi:10.1016/j.epsl.2019.04.009. ISSN 0012-821X. S2CID 150016618.
1 2 3 4 "Ritter Island". Global Volcanism Program . Smithsonian Institution . Retrieved 2021-02-06.
1 2 3 4 5 Karstens, J.; Kelfoun, K.; Watt, S.F.L. (2020). "Combining 3D seismics, eyewitness accounts and numerical simulations to reconstruct the 1888 Ritter Island sector collapse and tsunami". International Journal of Earth Sciences. 109 (8): 2659–2677. Bibcode:2020IJEaS.109.2659K. doi: 10.1007/s00531-020-01854-4 .
↑ Micallef, Aaron; Watt, Sebastian F. L.; Berndt, Christian; Urlaub, Morelia; Brune, Sascha; Klaucke, Ingo; Böttner, Christoph; Karstens, Jens; Elger, Judith (2017). "An 1888 Volcanic Collapse Becomes a Benchmark for Tsunami Models". eos.org. Archived from the original on 2019-08-30. Retrieved 2021-02-06.
1 2 3 4 5 Johnson, R. Wally (2013). Fire Mountains of the Islands: A History of Volcanic Eruptions and Disaster Management in Papua New Guinea and the Solomon Islands. Australia: Australian National University E Press. pp. 65–70. ISBN 9781922144232.
1 2 Ward, Steven N.; Day, Simon (2003). "Ritter Island Volcano—lateral collapse and the tsunami of 1888". Geophysical Journal International. 154 (3): 891–902. Bibcode:2003GeoJI.154..891W. doi: 10.1046/j.1365-246X.2003.02016.x .
1 2 Day, Simon; Llanes, Pilar; Silver, Eli; Hoffmann, Gary; Ward, Steve; Driscoll, Neal (2015). "Submarine landslide deposits of the historical lateral collapse of Ritter Island, Papua New Guinea". Marine and Petroleum Geology. 67: 419–438. Bibcode:2015MarPG..67..419D. doi: 10.1016/j.marpetgeo.2015.05.017 . ISSN 0264-8172.
1 2 Siebert, Lee; Glicken, Harry; Ui, Tadahide (1987). "Volcanic hazards from Bezymianny- and Bandai-type eruptions" (PDF). Bulletin of Volcanology. 49 (1): 435–459. Bibcode:1987BVol...49..435S. doi:10.1007/BF01046635. S2CID 55499424.
↑ "Significant Volcanic Eruption". National Geophysical Data Center / World Data Service (NGDC/WDS): NCEI/WDS Global Significant Volcanic Eruptions Database. NOAA National Centers for Environmental Information. doi:10.7289/V5JW8BSH . Retrieved 2021-02-06.
1 2 3 "Tsunami Event Information". National Geophysical Data Center / World Data Service: NCEI/WDS Global Historical Tsunami Database. NOAA National Centers for Environmental Information. doi:10.7289/V5PN93H7.
↑ Paris, Raphael (2015). "Source mechanisms of volcanic tsunamis". Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences. 373 (2053). Bibcode:2015RSPTA.37340380P. doi:10.1098/rsta.2014.0380. PMID 26392617.
↑ Blong, R. J. (1984). Volcanic Hazards: A Sourcebook on the Effects of Eruptions. Australia: Academic Press Australia. pp. 237–238. ISBN 9781483288208.

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[Karstens19-1] 1 2 3 4 5 6 7 8 Karstens, Jens; Berndt, Christian; Urlaub, Morelia; Watt, Sebastian F.L.; Micallef, Aaron; Ray, Melanie; Klaucke, Ingo (2019). "From gradual spreading to catastrophic collapse – Reconstruction of the 1888 Ritter Island volcanic sector collapse from high-resolution 3D seismic data". Earth and Planetary Science Letters. 517: 1–13. Bibcode:2019E&PSL.517....1K. doi:10.1016/j.epsl.2019.04.009. ISSN 0012-821X. S2CID 150016618.

[gvp1-2] 1 2 3 4 "Ritter Island". Global Volcanism Program . Smithsonian Institution . Retrieved 2021-02-06.

[Karstens20-3] 1 2 3 4 5 Karstens, J.; Kelfoun, K.; Watt, S.F.L. (2020). "Combining 3D seismics, eyewitness accounts and numerical simulations to reconstruct the 1888 Ritter Island sector collapse and tsunami". International Journal of Earth Sciences. 109 (8): 2659–2677. Bibcode:2020IJEaS.109.2659K. doi: 10.1007/s00531-020-01854-4 .

[4] Micallef, Aaron; Watt, Sebastian F. L.; Berndt, Christian; Urlaub, Morelia; Brune, Sascha; Klaucke, Ingo; Böttner, Christoph; Karstens, Jens; Elger, Judith (2017). "An 1888 Volcanic Collapse Becomes a Benchmark for Tsunami Models". eos.org. Archived from the original on 2019-08-30. Retrieved 2021-02-06.

[Johnson13-5] 1 2 3 4 5 Johnson, R. Wally (2013). Fire Mountains of the Islands: A History of Volcanic Eruptions and Disaster Management in Papua New Guinea and the Solomon Islands. Australia: Australian National University E Press. pp. 65–70. ISBN 9781922144232.

[Ward03-6] 1 2 Ward, Steven N.; Day, Simon (2003). "Ritter Island Volcano—lateral collapse and the tsunami of 1888". Geophysical Journal International. 154 (3): 891–902. Bibcode:2003GeoJI.154..891W. doi: 10.1046/j.1365-246X.2003.02016.x .

[Simon15-7] 1 2 Day, Simon; Llanes, Pilar; Silver, Eli; Hoffmann, Gary; Ward, Steve; Driscoll, Neal (2015). "Submarine landslide deposits of the historical lateral collapse of Ritter Island, Papua New Guinea". Marine and Petroleum Geology. 67: 419–438. Bibcode:2015MarPG..67..419D. doi: 10.1016/j.marpetgeo.2015.05.017 . ISSN 0264-8172.

[Siebert87-8] 1 2 Siebert, Lee; Glicken, Harry; Ui, Tadahide (1987). "Volcanic hazards from Bezymianny- and Bandai-type eruptions" (PDF). Bulletin of Volcanology. 49 (1): 435–459. Bibcode:1987BVol...49..435S. doi:10.1007/BF01046635. S2CID 55499424.

[ngdcVO-9] "Significant Volcanic Eruption". National Geophysical Data Center / World Data Service (NGDC/WDS): NCEI/WDS Global Significant Volcanic Eruptions Database. NOAA National Centers for Environmental Information. doi:10.7289/V5JW8BSH . Retrieved 2021-02-06.

[tsunamiNGDC-10] 1 2 3 "Tsunami Event Information". National Geophysical Data Center / World Data Service: NCEI/WDS Global Historical Tsunami Database. NOAA National Centers for Environmental Information. doi:10.7289/V5PN93H7.

[Paris15-11] Paris, Raphael (2015). "Source mechanisms of volcanic tsunamis". Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences. 373 (2053). Bibcode:2015RSPTA.37340380P. doi:10.1098/rsta.2014.0380. PMID 26392617.

[12] Blong, R. J. (1984). Volcanic Hazards: A Sourcebook on the Effects of Eruptions. Australia: Academic Press Australia. pp. 237–238. ISBN 9781483288208.

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