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2000 Banggai Islands Earthquake
On 4 May 2000 at 12:21 WITA (04:21 UTC), Banggai Islands Regency was hit by an earthquake of magnitude 7.5 , followed by a tsunami. The Banggai Islands, an archipelago located at the far eastern end of Central Sulawesi, Indonesia, was the worst affected by the earthquake. Eighty percent of Banggai's buildings were destroyed. Damage also occurred on Peleng. The earthquake triggered a local tsunami of up to 6 m in height that caused significant damage east of Luwuk on the mainland and on Peleng. Tectonic setting The Banggai region of Sulawesi lies within the complex area of interaction between the Pacific, Philippine Sea, Australian and Eurasian Plates. The Banggai Islands themselves form part of the Banggai-Sula microcontinent, which collided with eastern Sulawesi during the Neogene, with a thrust fault boundary along the southeastern edge of the Eastern arm. The northern margin of the Banggai-Sula block has been interpreted as a continuous southward moving thrust zone, but ...
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Time In Indonesia
The Indonesian Archipelago geographically stretches across four time zones from UTC+06:00 in Aceh to UTC+09:00 in Papua. However, the Indonesian government recognises only three time zones in its territory, namely: *Western Indonesia Time (WIB) — seven hours ahead ( UTC+07:00) of the Coordinated Universal Time (UTC); *Central Indonesia Time (WITA) — eight hours ahead ( UTC+08:00) of UTC; *Eastern Indonesia Time (WIT) — nine hours ahead ( UTC+09:00) of UTC. The boundary between the Western and Central time zones was established as a line running north between Java and Bali through the provincial boundaries of West and Central Kalimantan. The border between the Central and Eastern time zones runs north from the eastern tip of Indonesian Timor to the eastern tip of Sulawesi. Daylight saving time (DST) is no longer observed anywhere in Indonesia. Current usage In Indonesia Indonesia, officially the Republic of Indonesia, is a country in Southeast Asia and Oceania b ...
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Reflection Seismology
Reflection seismology (or seismic reflection) is a method of exploration geophysics that uses the principles of seismology to estimate the properties of the Earth's subsurface from reflected seismic waves. The method requires a controlled seismic source of energy, such as dynamite or Tovex blast, a specialized air gun or a seismic vibrator. Reflection seismology is similar to sonar and echolocation. This article is about surface seismic surveys; for vertical seismic profiles, see VSP. History Reflections and refractions of seismic waves at geologic interfaces within the Earth were first observed on recordings of earthquake-generated seismic waves. The basic model of the Earth's deep interior is based on observations of earthquake-generated seismic waves transmitted through the Earth's interior (e.g., Mohorovičić, 1910). The use of human-generated seismic waves to map in detail the geology of the upper few kilometers of the Earth's crust followed shortly thereafter and h ...
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May 2000 Events In Asia
May is the fifth month of the year in the Julian and Gregorian calendars and is the third of seven months to have a length of 31 days. May is a month of spring in the Northern Hemisphere, and autumn in the Southern Hemisphere. Therefore, May in the Southern Hemisphere is the seasonal equivalent of November in the Northern Hemisphere and vice versa. Late May typically marks the start of the summer vacation season in the United States ( Memorial Day) and Canada (Victoria Day) that ends on Labor Day, the first Monday of September. May (in Latin, ''Maius'') was named for the Greek goddess Maia, who was identified with the Roman era goddess of fertility, Bona Dea, whose festival was held in May. Conversely, the Roman poet Ovid provides a second etymology, in which he says that the month of May is named for the ''maiores,'' Latin for "elders," and that the following month (June) is named for the ''iuniores,'' or "young people" (''Fasti VI.88''). Eta Aquariids meteor shower ap ...
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Earthquakes In Indonesia
__NOTOC__ This is an incomplete list of more recent recorded major earthquakes that have occurred within the boundaries of Indonesia. The determinants of the activity are indicated by the geology of the region, and the volcanic activity. Large numbers of earthquakes of smaller magnitude occur very regularly due to the meeting of major tectonic plates in the region. Based on the records of the USGS, Indonesia has had more than 150 earthquakes with magnitude > 7 in the period 1901–2019. Earthquakes 2000–present 1900-1999 1629-1899 See also * Eurasian Plate * Geology of Indonesia * Indo-Australian Plate * Krakatoa * List of faults in Indonesia * List of historical earthquakes * List of natural disasters in Indonesia * List of tsunamis affecting Indonesia * List of volcanoes in Indonesia * Seismicity of the Sumatra coast References Sources * Further reading * External links * Hayes, G.P. ''et al.'' 2013Seismicity of the Earth 1900–2012 Sumatr ...
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2000 In Indonesia
The following lists events that happened during 2000 in Indonesia Incumbents Events * Indonesia 2000 census May * May 28: 2000 Walisongo school massacre June * June 4: The 7.9 Enggano earthquake shakes southwestern Sumatra with a maximum Mercalli intensity of VI (''Strong''). One-hundred and three people were killed and 2,174–2,585 were injured. August * August 1: 2000 Philippine consulate bombing September * September 8: United Nations Security Council Resolution 1319 * September 14: Jakarta Stock Exchange bombing December * December 24: Christmas Eve 2000 Indonesia bombings Births * July 1: Lalu Muhammad Zohri, Indonesian sprinter References Indonesia Years of the 20th century in Indonesia 2000s in Indonesia Indonesia Indonesia, officially the Republic of Indonesia, is a country in Southeast Asia and Oceania between the Indian and Pacific oceans. It consists of over 17,000 islands, including Sumatra, Java, Sulawesi, and parts of Borneo and Ne ...
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List Of Earthquakes In Indonesia
__NOTOC__ This is an incomplete list of more recent recorded major earthquakes that have occurred within the boundaries of Indonesia. The determinants of the activity are indicated by the geology of the region, and the volcanic activity. Large numbers of earthquakes of smaller magnitude occur very regularly due to the meeting of major tectonic plates in the region. Based on the records of the USGS, Indonesia has had more than 150 earthquakes with magnitude > 7 in the period 1901–2019. Earthquakes 2000–present 1900-1999 1629-1899 See also * Eurasian Plate * Geology of Indonesia * Indo-Australian Plate * Krakatoa * List of faults in Indonesia * List of historical earthquakes * List of natural disasters in Indonesia * List of tsunamis affecting Indonesia * List of volcanoes in Indonesia * Seismicity of the Sumatra coast References Sources * Further reading * External links * Hayes, G.P. ''et al.'' 2013Seismicity of the Earth 1900–2012 Sumatr ...
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2018 Sulawesi Earthquake And Tsunami
On 28 September 2018, a shallow, large earthquake struck in the neck of the Minahasa Peninsula, Indonesia, with its epicentre located in the mountainous Donggala Regency, Central Sulawesi. The magnitude 7.5 quake was located away from the provincial capital Palu and was felt as far away as Samarinda on East Kalimantan and also in Tawau, Malaysia. This event was preceded by a sequence of foreshocks, the largest of which was a magnitude 6.1 tremor that occurred earlier that day. Following the mainshock, a tsunami alert was issued for the nearby Makassar Strait. A localised tsunami struck Palu, sweeping shore-lying houses and buildings on its way. The combined effects of the earthquake and tsunami led to the deaths of an estimated 4,340 people. This makes it the deadliest earthquake to strike the country since the 2006 Yogyakarta earthquake, as well as the deadliest earthquake worldwide in 2018, surpassing the previous earthquake that struck Lombok nearly 2 months earlier, k ...
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1968 Sulawesi Earthquake
The 1968 Sulawesi earthquake struck Indonesia on August 14. It had a Richter magnitude scale, Richter magnitude of 7.4, spawned a large tsunami, and killed roughly 200 people. Damage and casualties The earthquake had a Richter magnitude of 7.4. It created a tsunami with wave heights of to , which soon traveled onto Sulawesi. The most extensive waves reached inland, destroying 700 homes and killing around 200 people. Geology The earthquake ruptured along Palu-Koro fault in Manimbaja Bay. It caused subsidence that decreased elevations by as much as to along the coast. It also appeared to tectonic uplift, uplift at least one of the Togian Islands. The earthquake was near the Celebes Sea; it sank the island of Tuguan. See also *2018 Sulawesi earthquake and tsunami *List of earthquakes in 1968 *List of earthquakes in Indonesia References External links

* 1968 tsunamis 1968 earthquakes 1968 in Indonesia 1968 disasters in Indonesia Earthquakes in Indonesia ...
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Indonesian Rupiah
The rupiah (Currency symbol, symbol: Rp; ISO 4217, currency code: IDR) is the official currency of Indonesia. It is issued and controlled by Bank Indonesia. The name "Rupee, rupiah" is derived from the Sanskrit word for silver, (). Sometimes, Indonesians also informally use the word ("silver" in Indonesian language, Indonesian) in referring to rupiah in coins. The rupiah is divided into 100 ''cent (currency), sen'', although high inflation has rendered all coins and banknotes denominated in obsolete. Introduced in 1946 by Indonesian nationalists Indonesian National Revolution, fighting for independence, the currency replaced Japanese government-issued currency in the Dutch East Indies, a version of the Netherlands Indies gulden, which had been introduced during the Japanese occupation of the Dutch East Indies, Japanese occupation in World War II. In its early years, the rupiah was used in conjunction with other currencies, including a new version of the gulden introduced by th ...
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United Nations Office For The Coordination Of Humanitarian Affairs
The United Nations Office for the Coordination of Humanitarian Affairs (OCHA) is a United Nations (UN) body established in December 1991 by the General Assembly to strengthen the international response to complex emergencies and natural disasters. It is the successor to the Office of the United Nations Disaster Relief Coordinator (UNDRO). The Department of Humanitarian Affairs (DHA) was established shortly thereafter by the Secretary-General, but in 1998 was merged into OCHA, which became the UN's main focal point on major disasters. OCHA's mandate was subsequently broadened to include coordinating humanitarian response, policy development and humanitarian advocacy. Its activities include organizing and monitoring humanitarian funding, advocacy, policy-making, and information exchange to facilitate rapid-response teams for emergency relief. OCHA is led by the Under-Secretary-General for Humanitarian Affairs and Emergency Relief Coordinator (USG/ERC), appointed for a five-year t ...
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