1899 Ceram earthquake

Last updated

1899 Ceram earthquake
Indonesia Maluku location map.svg
Bullseye1.png
Local date30 September 1899 (1899-09-30)
Local time01:42.2 AM
Magnitude7.8 Ms
Epicenter 3°17′S128°39′E / 3.29°S 128.65°E / -3.29; 128.65
Max. intensity VIII (Heavily damaging) [1]
Tsunami10 m (33 ft)

On 30 September 1899 the island of Ceram, Dutch East Indies, was struck by an Ms 7.8 earthquake which was accompanied by a 10-meter landslide-induced tsunami. [2] According to the Batavian Magnetic and Meteorological Observatory, the shock occurred at 01:42.2 AM Amahei local time. [3] The study about the quake and its effects was published by Dr. R. D. M. Verbeek in an article named Short Report about the earth- and sea-quake in Ceram, the 30th September 1899, which serves as the only extensive source on this earthquake.

Contents

Earthquake and tsunamis

The Ceram earthquake is ranked among the tectonic quakes. The epicenter of the quake is shown in Figure 1. [3] From there the quake spread in all directions. The most forceful spread went west and east, presumably through an old crack or tear in the Earth's crust. [3]

The 1899 Ceram earthquake had nothing to do with the 1898 Ambon earthquake. The first-mentioned took place along one of the many concentric cracks, the latter one took place along a radial crack. [3] The earthquake was especially heavy in the Elpaputih-bay. Presumably because, as calculations suggest, the epicenter of the shock was located in the mountains west of the bay. These calculations were confirmed by visual inspection of the mountain rocks, which showed signs of fracture and breaking due to the quake. [3] The earthquake itself would not have been responsible for a lot of damage, were it not that the several parts of the shore broke off due to the quake and fell into the sea, creating a severe tsunami that flooded the shores and the nearby located villages. [3]

Effects

Figure 1. A map that shows the epicenter of the Ceram earthquake. 1899 Seram Earthquake map.jpg
Figure 1. A map that shows the epicenter of the Ceram earthquake.

The devastating tsunami took 3,864 lives and swept away several villages completely. [3] The areas that were struck hardest were all located on, or near, the Ceram fracture line and included Hatusua (Piru-bay area), Paulohy-Samasuru and Makariki (Elpaputih-bay area), Tehoru, Wolu and Laimu (Taluti-bay area). [3]

Piru-bay area

Only the east side suffered damage from a single-wave tsunami which destroyed village of Hatusua. A 2.4-meter tall wave which travelled 203 metres (666 ft) inland swept away the village in its entirety. [3]

Elpaputih-bay area

Like at Piru-bay, the most severe damage was suffered on the east-side of the bay (Paulohy-Samasuru and Mani were the only west-side villages that were struck). Here, the shore broke off, creating a 9-meter wave flooding land inward for 170 m. 2400 people's lives were taken by the tsunami in this area. [3]

Taluti-bay area

Here, the west side of the bay suffered the greatest impact. At the Tehoru shore, a 'land-sliding' occurred, which created a flood that flooded the entire Tehoru village as well as parts of the nearby Wolu and Laimu villages. [3]

Dr. R. D. M. Verbeek's study

Rogier Verbeek was a Dutch geologist and natural scientist, located in the Dutch Indies due to his work for the Royal Dutch Geography Society. Therefore, his work is part of a broader scholarly effort to get a better understanding of the geography of the Dutch colonies. [4] In that time, the focus was mainly on the micro-geography of certain Dutch areas. This case study tries to give an overview of the cause and impact of the 1899 earthquake and tsunami, indexing the specifics of the natural disaster for the entire Ceram area. However, Verbeek's presence in the Dutch Indies was not merely scholarly in nature. There was also an imperialistic incentive to have Dutch scholars located in Dutch colonies. As the first president of the Royal Dutch Geography Society, P.J. Veth, stated, it was also a matter of pursuing and maintaining the Dutch glory, in a cultural-nationalistic sense. Dutch scholarly presence in the Indies was therefore not merely scientific, but also part of a colonial effort based on the idea of a 'Greater Holland'. [4]

See also

Related Research Articles

<span class="mw-page-title-main">1960 Valdivia earthquake</span> 9.4–9.6 magnitude earthquake in Chile

The 1960 Valdivia earthquake and tsunami or the Great Chilean earthquake on 22 May 1960 was the most powerful earthquake ever recorded. Various studies have placed it at 9.4–9.6 on the moment magnitude scale. It occurred in the afternoon, and lasted for approximately 10 minutes. The resulting tsunamis affected southern Chile, Hawaii, Japan, the Philippines, eastern New Zealand, southeast Australia, and the Aleutian Islands.

<span class="mw-page-title-main">Simeulue Regency</span> Regency in Sumatra, Indonesia

Simeulue Regency is a regency in the Aceh special region of Indonesia. It occupies the whole island of Simeulue, 150 km off the west coast of Sumatra, with an area of 1,838.10 square kilometres. It had a population of 80,674 at the 2010 census and 92,865 at the 2020 census; the official estimate as at mid 2023 was 97,118.

<span class="mw-page-title-main">Kamchatka earthquakes</span> Earthquakes in the Kamchatka Peninsula, far eastern Russia

Many major earthquakes have occurred in the region of the Kamchatka Peninsula in far eastern Russia. Events in 1737, 1923 and 1952, were megathrust earthquakes and caused tsunamis. There are many more earthquakes and tsunamis originating from the region.

<span class="mw-page-title-main">2005 Fukuoka earthquake</span> Earthquake in Japan

The Fukuoka earthquake struck Fukuoka Prefecture, Japan at 10:53 am JST on March 20, 2005, and lasted for approximately 1 minute. The Japan Meteorological Agency (JMA) measured it as peaking at a magnitude of 7.0, whereas the United States Geological Survey (USGS) reported a magnitude of 6.6. The quake occurred along a previously unknown fault in the Genkai Sea, North of Fukuoka city, and the residents of Genkai Island were forced to evacuate as houses collapsed and landslides occurred in places. Investigations subsequent to the earthquake determined that the new fault was most likely an extension of the known Kego fault that runs through the centre of the city.

<span class="mw-page-title-main">Seismicity of the Sanriku coast</span>

The seismicity of the Sanriku coast identifies and describes the seismic activity of an area of Japan. Seismicity refers to the frequency, type and size of earthquakes experienced over a period of time. The Sanriku Coast is a descriptive term referring to the coastal areas of the former provinces of Rikuō in Aomori, Rikuchū in Aomori, and Rikuzen in Miyagi.

<span class="mw-page-title-main">September 2007 Sumatra earthquakes</span> Earthquakes affecting Indonesia

The September 2007 Sumatra earthquakes were a series of megathrust earthquakes that struck the Sunda Trench off the coast of Sumatra, Indonesia, with three of magnitude 7 or greater. A series of tsunami bulletins was issued for the area. The most powerful of the series had a magnitude of 8.5, which makes it in the top 20 of the largest earthquakes ever recorded on a seismograph.

<span class="mw-page-title-main">Mount Breakenridge</span> Mountain in British Columbia, Canada

Mount Breakenridge, 2,395 m or 7,858 ft, is a mountain in the Lillooet Ranges of southwestern British Columbia, Canada, located on the east side of upper Harrison Lake in the angle of mountains formed by that lake and the Big Silver River.

<span class="mw-page-title-main">1958 Lituya Bay earthquake and megatsunami</span> Geologic events off the Alaska coast

The 1958 Lituya Bay earthquake occurred on July 9, 1958 at 22:15:58 PST with a moment magnitude of 7.8 to 8.3 and a maximum Mercalli intensity of XI (Extreme). The strike-slip earthquake took place on the Fairweather Fault and triggered a rockslide of 30 million cubic meters and about 90 million tons into the narrow inlet of Lituya Bay, Alaska. The impact was heard 80 kilometers (50 mi) away, and the sudden displacement of water resulted in a megatsunami that washed out trees to a maximum elevation of 524 meters at the entrance of Gilbert Inlet. This is the largest and most significant megatsunami in modern times; it forced a re-evaluation of large-wave events and the recognition of impact events, rockfalls, and landslides as causes of very large waves.

<span class="mw-page-title-main">2010 Chile earthquake</span> Magnitude 8.8 earthquake in Chile on 27 February 2010

The 2010 Chile earthquake and tsunami occurred off the coast of central Chile on Saturday, 27 February at 03:34:12 local time, having a magnitude of 8.8 on the moment magnitude scale, with intense shaking lasting for about three minutes. It was felt strongly in six Chilean regions that together make up about 80 percent of the country's population. According to the United States Geological Survey (USGS) the cities experiencing the strongest shaking—VIII (Severe) on the Mercalli intensity scale (MM)—were Concepción, Arauco, and Coronel. According to Chile's Seismological Service, Concepción experienced the strongest shaking at MM IX (Violent). The earthquake was felt in the capital Santiago at MM VII or MM VIII. Tremors were felt in many Argentine cities, including Buenos Aires, Córdoba, Mendoza, and La Rioja. Tremors were felt as far north as the city of Ica in southern Peru. It is the largest earthquake to hit Chile since the 1960 Valdivia earthquake.

The 1965 Ceram Sea earthquake occurred on January 24 at 00:11 UTC with a moment magnitude of 8.2 and its epicenter was located just off the southwestern coast of Sanana Island in eastern Indonesia. The event occurred at a depth of 28 kilometers under the Ceram Sea, and a tsunami was generated which caused damage in Sanana, Buru, and Mangole. During the tsunami three consecutive run-ups were reported in Seram Island, and a four-meter run-up was reported at Buru Island.

<span class="mw-page-title-main">2011 Tōhoku earthquake and tsunami</span> Megathrust earthquake off Japans east coast

On 11 March 2011, at 14:46 JST, a Mw 9.0–9.1 undersea megathrust earthquake occurred in the Pacific Ocean, 72 km (45 mi) east of the Oshika Peninsula of the Tōhoku region. It lasted approximately six minutes, causing a tsunami. It is sometimes known in Japan as the "Great East Japan Earthquake", among other names. The disaster is often referred to by its numerical date, 3.11.

The 1932 Jalisco earthquakes began on June 3 at 10:36 UTC with a megathrust event that registered 8.1 on the moment magnitude scale. With a maximum perceived intensity of X (Extreme) on the Mercalli intensity scale, at least 400 deaths were caused in Mexico and neighboring Guatemala. It was the first of a series of seismic events that affected parts of western Mexico during the month of June 1932, all reaching magnitude 7 or greater.

The 1989 Irian Jaya earthquake struck Kurima District, Yahukimo Regency, Highland Papua, Indonesia – then Irian Jaya province – on August 1 with a moment magnitude of 6.0 and a maximum Mercalli intensity of VIII (Severe). Around 120 people were killed, mainly due to landslides and mudslides.

<span class="mw-page-title-main">2016 Sumatra earthquake</span> Earthquake off the coast of Sumatra, Indonesia

The 2016 Sumatra earthquake was a 7.8 magnitude earthquake which struck on 2 March 2016 in the Indian Ocean, approximately 800 kilometers southwest of Sumatra in Indonesia. Tsunami warnings were issued for Indonesia and Australia, but were withdrawn two hours later. There were no deaths directly related to the earthquake.

<span class="mw-page-title-main">2016 Solomon Islands earthquakes</span> Seismic events

On 9 December 2016 at 4:38 a.m. local time, the Solomon Islands region was rocked by an Mww 7.8 earthquake, centered 30 km off San Cristobal Island, about 61 km southwest of Kirakira, the capital of Makira-Ulawa Province. Initially registering magnitude 8.0, later downgraded to 7.8, the temblor prompted tsunami warnings that kept countries surrounding the Coral, Tasman and Solomon Sea on high alert, but was later cancelled. A large aftershock of magnitude 6.9 occurred shortly afterwards. This earthquake was largely felt, waking many residents who later ran to high ground for fears of a potential tsunami. The earthquake killed a child and affected some 34,000 people in Makira, South Malaita and Guadalcanal Island where many had lost their homes or had no access to basic needs. Earthquakes are common in this region, with little or no fatalities. This earthquake is tied with three other magnitude 7.8 earthquakes for the second largest earthquake of 2016. On 17 December, the Solomon Islands would be rattled again by a 7.9 magnitude earthquake, this time 54 km east of Taron, Papua New Guinea.

<span class="mw-page-title-main">2013 Craig, Alaska earthquake</span> Earthquake in Alaska and British Columbia

The 2013 Craig, Alaska earthquake struck on January 5, at 12:58 am (UTC–7) near the city of Craig and Hydaburg, on Prince of Wales Island. The Mw 7.5 earthquake came nearly three months after an Mw  7.8 quake struck Haida Gwaii on October 28, in 2012. The quake prompted a regional tsunami warning to British Columbia and Alaska, but it was later cancelled. Due to the remote location of the quake, there were no reports of casualties or damage.

<span class="mw-page-title-main">2008 Simeulue earthquake</span> Earthquake in Indonesia

On February 20, 2008, an earthquake with a moment magnitude of 7.4 struck off the coast of Sumatra at a hypocentre depth of 26 km. The earthquake had an epicenter located on the island of Simeulue, northwest from Sinabang, a small town on the island. Three people were killed and an additional 25 seriously injured as a result of the earthquake.

The 1852 Banda Sea earthquake struck on 26 November at 07:40 local time, affecting coastal communities on the Banda Islands. It caused violent shaking lasting five minutes, and was assigned XI on the Modified Mercalli intensity scale in the Maluku Islands. A tsunami measuring up to 8 m (26 ft) slammed into the islands of Banda Neira, Saparua, Haruku and Ceram. The tsunami caused major damage, washing away many villages, ships and residents. At least 60 people were killed in the earthquake and tsunami. The earthquake had an estimated moment magnitude of 7.5 or 8.4–8.8, according to various academic studies.

The 1889 Chilik earthquake occurred on July 11 on the Gregorian calendar, or June 30 on the Julian calendar at 15:14 local time in the Tien Shan mountains. The earthquake measured an estimated Mw  7.9–8.0 on the moment magnitude scale and was assigned a maximum intensity of X (Devastating) on the MSK 64 and Rossi-Forel scales. Over 92 people across Kazakhstan, Kyrgyzstan and China were killed.

The 1657 Concepción earthquake occurred on March 15 at 20:00 local time off the coast of Concepción, Biobío Region in the Spanish Empire. The earthquake caused severe damage along the coast, and generated a large tsunami in the Bay of Concepción. At least 40 people were killed, the majority due to drowning from the tsunami. The town of Concepción was the hardest hit, with the earthquake and tsunami totally destroying it.

References

  1. Martin, S. S.; Cummins, P. R.; Meltzner, A. J. (2022), "Gempa Nusantara: A Database of 7380 Macroseismic Observations for 1200 Historical Earthquakes in Indonesia from 1546 to 1950", Bulletin of the Seismological Society of America, 112 (6): 2958–2980, doi:10.1785/0120220047, hdl: 10356/166257 , ISSN   0037-1106
  2. Yung-Chun Liu, Z.; Harris, R. A. (2013). "Discovery of possible mega-thrust earthquake along the Seram Trough from records of 1629 tsunami in eastern Indonesian region" (PDF). Natural Hazards. 72 (3): 1324. doi: 10.1007/s11069-013-0597-y . Archived from the original (PDF) on 25 November 2021. Retrieved 5 June 2016.
  3. 1 2 3 4 5 6 7 8 9 10 11 Dr. R. D. M. Verbeek, Kort verslag over de aard- en zeebeving op Ceram, den 30sten september 1899 (Batavia Landsdrukkerij, 1900) p. 1–11. (in Dutch)
  4. 1 2 KNAG Expedities, URL: http://www.knag-expedities.nl/pages/tijdgeest/tijdgeest1.php (in Dutch)