cyanic-selkie/wikianc huggingface dataset:
Téori kaputusan
Complex decisions
Other aréas of decision théory are concerned with decisions that are difficult simply because of their complexity, or the complexity of the organisation that has to take them. In such cases the issue is not the deviation between réal and optimal behaviour, but the difficulty of determining the optimal behaviour in the first place.
2015 YV20
Bebentukan
Kawas sakumna astéroid, ieu astéroid kabentuk tina nébula panonpoé primordial minangka beubeulahan planétisimal, objék di nébula marcapada ngora nu teu cukup badag pikeun robah jadi planét.
(450263) 2003 WD158
Ari 2003 WD158 mangrupa hiji astéroid. Ieu asteroid téh bagéan tina astéroid Apollo, anu nganjrek deukeut jeung marcapada. Ékséntrisitas orbit ieu astéroid kacatet gedéna 0.409, sedengkeun magnitudo mutlakna 18.8. Ari nu jadi référénsina mah nyaéta MPO�373404.
Bebentukan
Kawas sakumna astéroid, ieu astéroid kabentuk tina nébula panonpoé primordial minangka beubeulahan planétisimal, objék di nébula marcapada ngora nu teu cukup badag pikeun robah jadi planét.
2012 HM8
Ari 2012 HM8 mangrupa hiji astéroid. Ieu asteroid téh bagéan tina astéroid Amor, anu nganjrek deukeut jeung marcapada. Ékséntrisitas orbit ieu astéroid kacatet gedéna 0.640, sedengkeun magnitudo mutlakna 24.0. Ari nu jadi référénsina mah nyaéta MPO 235400.
Bebentukan
Kawas sakumna astéroid, ieu astéroid kabentuk tina nébula panonpoé primordial minangka beubeulahan planétisimal, objék di nébula marcapada ngora nu teu cukup badag pikeun robah jadi planét.
Sukamukti, Sukawening, Garut
Sukamukti nyaéta salah sahiji désa di kacamatan Sukawening, Kabupatén Garut, Propinsi Jawa Barat, Indonésia.
Tanjung Kurung, Wonosobo, Tanggamus
Tanjung Kurung nyaéta salah sahiji Désa di kacamatan Wonosobo, Kabupatén Tanggamus, Propinsi Sumatra Kalér, Indonésia.
2016 GE2
Bebentukan
Kawas sakumna astéroid, ieu astéroid kabentuk tina nébula panonpoé primordial minangka beubeulahan planétisimal, objék di nébula marcapada ngora nu teu cukup badag pikeun robah jadi planét.
131
Taun ka-131 Maséhi dina Kalénder Grégorian.
Pedes
Pedes atawa Marica (Piper nigrum) nyaéta salah sahiji tutuwuhan ngarambat tina kulawarga Piperaceae. Tutuwuhan ieu miboga buah nu sok dimanfaatkeun salaku bumbu dapur jeung mangrupa tutuwuhan pertanian nu miboga prospék usaha nu luhur. Tutuwuhan ieu sumebar di loba wilayah indonésia jeung miboga loba ngaran daérah, misalna Sa'ang (Madura), Sahang (Bangka Belitung) jeung sajabana.
Bungbu
Pedes atawa sahang dipikawanoh ogé minangka salah sahiji bungbu dapur atawa panyedep kaolahan. Jaman baheula loba jalma nu daragang pikeun néangan asal mula atawa tempat ayana pedes nepikeun ka bisana ngarojong kana padagangan jeung pelayaran dunya.
Botani
Salian ti India, lada hideung loba dibudidayakeun di Indonésia, Malaysia, Brazil, Sri Lanka, Vietnam jeung Cina. Tangkal pedes miboga daun anu lega, héjo ngagurilap, kalayan gagang anu rapih selang-seling, ogé miboga kembang leutik bodas, rengkep, teu boga gagang, cucukan ipis, sarta dina hiji kelompok aya kira-kira 50. Sedengkeun buahna buleud kira-kira diaméter 05-1,0 cm siki tunggal. Pedes jadi beureum konéng asak jeung sast ngandung hiji. Seungitna kuat jeung rada lada.
Gagang
Gagang tangkal pedes jadi ngarambat dina sahiji tiang, sakapeung ogé ngajalar dina luhur taneuh.Panjang gagang bisa nepika 15 meter, tapi dina gagang tangkal pedes, biasanya sok dipotong jeung disésakeun kira-kira 275–300 cm. Bentuk gagangna kabagi-bagi jiga tangkal tiwu jeung panjang bukuna kira-kira 4–7 cm, hal éta gumantung kana tingkat kasuburan. Panjang buku dina pangkal biasana lebih pendék dibanding jeung ruas nu aya dina tengah-tengah atawa tungtung, sedengkeun ukuran diameter rata-rata 6–25 mm.
Akar
Akar anu dipiboga ku tangkal pedes nyaéta akar tunggang tapi mirip jeung akar serat. Ukuranna leutik teu sapanjang akar tunggang biasa. Nurutkeun jenisna, akar tutuwuhan ieu dibagi jadi dua, nyaéta akar napel jeung akar taneuh. Akar napel nyaéta akar anu tumuwuh dina unggal titik dina taneuh jeung panjangna rata-rata 2,5-3,5 cm. Dina hiji ruas buku bisa tumuwuh saloba 10-25 untaian akar. Saterusna akar taneuh nyaéta akar anu tumuwuh dina batang tangkal pedes anu aya dina taneuh. Ti hiji suku gagang bisa tumuwuh kira-kira 10-20 untaian akar.
Dahan
Tangkal pedes miboga dua rupa pedes, nyaéta dahan ortotropik jeung dahan pang plagiatrop. Dahan ortotropik nyaéta dahan anu tumuwuh tina axils daun dina buku gagang, boh dina luhur cai atawa dina taneuh. Saterusna, cabang plagiatrop mangrupa dahan anu tumuwuh tina buku dahan, biasana dahanna bakal tumuwuh saenggeus tangkal pedes ngabuahan dua kali. Beuki loba buku dahanna, beuki loba buahna.
Rantau Limau Kapas, Tiang Pumpung, Merangin
Rantau Limau Kapas nyaéta salah sahiji désa di kacamatan Tiang Pumpung, Kabupatén Merangin, Propinsi Jambi, Indonésia.
Histogram
Dina statistik, histogram nyaéta tampilan grafis tina tabulasi frékuénsi. Dina hal ieu, histogram nyaéta versi grafis tina tabel nu nembongkeun babandingan kasus kana sababaraha atawa lobana kategori husus. Kategori ieu ilahar mangrupa hal nu husus saperti taya interval nu tumpang tindih dina sababaraha variabel.
Aya dua cara keur nembongkeun tabel nu sarua, sarta dua rupa histogram saperti ditembongkeun di handap ieu. Hiji nemobongkeun jumlah kasus per satuan interval, mangka legana wewengkon di handapeun kurva sarua jeung jumlah sakabéh kasus. Nu séjénna nembongkeun jumlah kasus per satuan interval dibagi ku total jumlah kasus, mangka legana wewengkon di handapeun kurva sarua jeung 1.
Dina conto ieu, data nu dipaké dikumpulkeun ku Biro Sensus Amérika, nyaéta data waktu nu diperlukeun keur indit gawe (sensus 2000,, Table 5). Sensus nyatet yén aya 124 juta urang digawe di luar imahna. Nu di sensus nyebutkeun sabaraha lila waktu nu diperlukeun nepi ka tempat gawe, hasilna dibagi kana lima bagéan nyaéta: kurang ti 5 menit, leuwih ti 5 menit kurang ti sapuluh menit, leuwih ti sapuluh menit kurang ti 15 menit jeung saterusna. Tabel di handap nembongkeun hasil sensus dina rebuan, upamana 4.180 hartina 4.180.000.
Data nu aya dina tabel di luhur digambarkeun sacara grafik dina gambar di handap ieu. Aréa unggal "bar" sarua jeung sakabéh nu di sensus dina éta kategori, mangka sakabéh legana "bar" sarua jeung jumlah nu disurvey (124) juta.
Aya nu matak kataji dina éta diagram nyaéta naekna sacara ngadadak dina kategori 30 nepi ka 35 menit. Bentukna saperti artefak: satengah jam mangrupa waktu ukuran ilahar, mangka nu disensus ngarepkeun waktu indit gawena kurang ti atawa leuwih leutik ti 30 menit, bisa ogé méré jawaban ampir "30 menit".
Histogram waktu indit gawe, sensus 2000 Amérika. Legana sahandapeun kurva sarua jeung lobana kasus.
Ayeuna data nu sarua digambarkeun ku cara nu béda. Aréa unggal bar sarua jeung babandingan nu disurvey tina nu sakabéh disurvey aya dina kategori ieu. Mangka total legana "bar" sarua jeung 1.
Tabel di luhur digambarkeun sacara grafis dina gambar di handap. Gambar kadua béda jeung gambar mimiti ngan dina skala nangtung. Gambar ieu bisa dipaké gumantung kana kaperluan histogram; lamun jumlah absolut penting, mangka bentuk mimiti leuwih hadé dipaké, sarta bentuk kadua leuwih hadé dipaké lamun babandingan leuwih penting.
Histogram waktu indit gawe, sensus 2000. Legana handapeun kurva sarua jeung 1.
Sei Tuan, Pantai Labu, Deli Serdang
Sei Tuan nyaéta salah sahiji Désa di kacamatan Pantai Labu, Kabupatén Deli Serdang, Propinsi Sumatra Kalér, Indonésia.
Sakuy, Sungai Mas, Aceh Barat
Sakuy nyaéta salah sahiji Gampong di kacamatan Sungai Mas, Kabupatén Aceh Barat, Propinsi Acéh, Indonésia.
Mekarsari, Bojong, Pandéglang
Mekarsari nyaéta salasahiji désa di Kacamatan Bojong, Pandéglang, Propinsi Banten, Indonésia.
Banda Alam, Acéh Wétan
Banda Alam nyaéta salah sahiji kacamatan di Kabupatén Acéh Wétan, Propinsi Acéh, Indonésia.
Bungong, Syamtalira Bayu, Aceh Utara
Bungong nyaéta salah sahiji Gampong di kacamatan Syamtalira Bayu, Kabupatén Aceh Utara, Propinsi Acéh, Indonésia.
Sunami
Sunami (éjahan  atawa ) hartina runtuyan galura / gelombang nu dihasilkeun nalika awak cai, misalna sagara ngalir sacara gancang dina jumlah/skala anu badag. Sunami ieu biasana mangrupa balukar ayana lini, longsor, gunung bitu, atawa tabrakan météorit. Anapon balukarna rupa-rupa, bisa sama sakali teu mangaruhan manusa, tapi bisa ogé ngabalukarkeun musibah anu nelasan ratusan rébu jalma.
Istilah sunami asalna tina basa Jepang nu hartina labuan ("tsu", 津) jeung gelombang ("nami", 波). Sunami téh lain kajadian sub-beungeut di jero sagara; jangkung gelombang caina (amplitudo) teu sabaraha, tapi panjang pisan (bisa nepi ka ratusan kilo), sahingga kadang di sagara mah teu pati kabireungeuh. <!--
Causes
Tsunamis can be generated when the sea floor abruptly deforms and vertically displaces the overlying water. Such large vertical movements of the Earth’s crust can occur at plate boundaries. Subduction earthquakes are particularly effective in generating tsunamis. As an Oceanic Plate is subducted beneath a Continental Plate, it sometimes brings down the lip of the Continental with it. Eventually, too much stress is put on the lip and it snaps back, sending shockwaves through the Earth’s crust, causing a tremor under the sea, known as an Undersea Earthquake.
Sub-marine landslides (which are sometimes triggered by large earthquakes) as well as collapses of volcanic edifices may also disturb the overlying water column as sediment and rocks slide downslope and are redistributed across the sea floor. Similarly, a violent submarine volcanic eruption can uplift the water column and form a tsunami.
In the 1950s it was discovered that larger tsunamis than previously believed possible could be caused by landslides, explosive volcanic action and impact events. These phenomena rapidly displace large volumes of water, as energy from falling debris or expansion is transferred to the water into which the debris falls. Tsunamis caused by these mechanisms, unlike the ocean-wide tsunamis caused by some earthquakes, generally dissipate quickly and rarely affect coastlines distant from the source due to the small area of sea affected. These events can give rise to much larger local shock waves (solitons), such as the landslide at the head of Lituya Bay which produced a water wave estimated at 50 – 150 m and reached 524 m up local mountains. However, an extremely large landslide could generate a megatsunami that might have ocean-wide impacts.
Characteristics
Often referred to as "tidal waves", a tsunami does not look like the popular impression of "a normal wave only much bigger". Instead it looks rather like an endlessly onrushing tide which forces its way around and through any obstacle. Most of the damage is caused by the huge mass of water behind the initial wave front, as the height of the sea keeps rising fast and floods powerfully into the coastal area. The sheer weight of water is enough to pulverise objects in its path, often reducing buildings to their foundations and scouring exposed ground to the bedrock. Large objects such as ships and boulders can be carried several miles inland before the tsunami subsides.
Tsunamis act very differently from typical surf swells: they contain immense energy, propagate at high speeds and can travel great trans-oceanic distances with little overall energy loss. A tsunami can cause damage thousands of kilometres from its origin, so there may be several hours between its creation and its impact on a coast, arriving long after the seismic wave generated by the originating event arrives. Although the total or overall loss of energy is small, the total energy is spread over a larger and larger circumference as the wave travels. The energy per linear metre in the wave is proportional to the inverse of the distance from the source. (In other words, it decreases linearly with distance.) This is the two-dimensional equivalent of the inverse square law, which is followed by waves which propagate in three dimensions (in a sphere instead of a circle).
A single tsunami event may involve a series of waves of varying heights; the set of waves is called a train. In open water, tsunamis have extremely long periods (the time for the next wave top to pass a point after the previous one), from minutes to hours, and long wavelengths of up to several hundred kilometres. This is very different from typical wind-generated swells on the ocean, which might have a period of about 10 seconds and a wavelength of 150 metres.
The actual height of a tsunami wave in open water is often less than one metre. This is often practically unnoticeable to people on ships. Because it has such a large wavelength, the energy of a tsunami mobilizes the entire water column, down to the sea bed. Ocean waves in deep water typically cause water motion to a depth approximately equal to half their wavelength. This means, ocean surface wave motion will only reach down to a depth of a few 100 m or less. Tsunamis, by contrast behave as shallow water waves in the deep ocean (provided their length is at least 20 times the local depth), for which little attenuation of water motion occurs with depth.
The wave travels across open ocean at an average speed of 500 mph(). As the wave approaches land, the sea shallows and the wave no longer travels as quickly, so it begins to 'pile-up'; the wave-front becomes steeper and taller, and there is less distance between crests. While a person at the surface of deep water would probably not even notice the tsunami, the wave can increase to a height of six stories or more as it approaches the coastline and compresses. The steepening process is analogous to the cracking of a tapered whip. As a wave goes down the whip from handle to tip, the same energy is deposited in less and less material, which then moves more violently as it receives this energy.
A wave becomes a 'shallow-water wave' when the ratio between the water depth and its wavelength gets very small, and since a tsunami has an extremely large wavelength (hundreds of kilometres), tsunamis act as a shallow-water wave even in deep oceanic water. Shallow-water waves move at a speed that is equal to the square root of the product of the acceleration of gravity (9.8 m/s2) and the water depth. For example, in the Pacific Ocean, where the typical water depth is about 4000 m, a tsunami travels at about 200 m/s (720 km/h or 450 mi/h) with little energy loss, even over long distances. At a water depth of 40 m, the speed would be 20 m/s (about 72 km/h or 45 mi/h), which is much slower than the speed in the open ocean but the wave would still be difficult to outrun.
Tsunamis propagate outward from their source, so coasts in the "shadow" of affected land masses are usually fairly safe. However, tsunami waves can diffract around land masses (as shown in this Indian Ocean tsunami animation as the waves reach southern Sri Lanka and India). It's also not necessary that they are symmetrical; tsunami waves may be much stronger in one direction than another, depending on the nature of the source and the surrounding geography.
Local geographic peculiarities can lead to seiche or standing waves forming, which can amplify the onshore damage. For instance, the tsunami that hit Hawaii on April 1, 1946 had a fifteen-minute interval between wave fronts. The natural resonant period of Hilo Bay is about thirty minutes. That meant that every second wave was in phase with the motion of Hilo Bay, creating a seiche in the bay. As a result, Hilo suffered worse damage than any other place in Hawaii, with the tsunami/seiche reaching a height of 14 m and killing 159 inhabitants.
Tsunami wave
Ocean waves are normally divided into 3 groups, characterized by depth:
Even though a tsunami is generated in deep water (around 4000 m below mean sea level), tsunami waves are considered shallow-water waves. As the tsunami wave approaches the shallow waters of shore, its time period remains the same, but its wavelength decreases rapidly, thus causing the water to pile up to form tremendous crests, in an effect known as "shoaling".
Etymology
The word "tsunami" is Japanese for "harbor wave", because tsunamis cause little or no visible effect in deep sea, and often Japanese fishermen would be out at sea fishing in deep sea when a tsunami came, and in the evening they came home and found their home village devastated by the tsunami, and thus they theorized that tsunamis only happen in harbors and elsewhere close inshore.
Warnings and prevention
Tsunamis cannot be prevented or precisely predicted, but there are some warning signs of an impending tsunami, and there are many systems being developed and in use to reduce the damage from tsunamis.
In instances where the leading edge of the tsunami wave is its trough, the sea will recede from the coast half of the wave's period before the wave's arrival. If the slope is shallow, this recession can exceed many hundreds of metres. People unaware of the danger may remain at the shore due to curiosity, or for collecting fish from the exposed sea bed.
In instances where the leading edge of the tsunami is its first peak, succeeding waves can lead to further flooding. Again, being educated about a tsunami is important, to realize that when the water level drops the first time, the danger is not yet over. In a low-lying coastal area, a strong earthquake is a major warning sign that a tsunami may be produced.
Regions with a high risk of tsunamis may use tsunami warning systems to detect tsunamis and warn the general population before the wave reaches land. In some communities on the west coast of the United States, which is prone to Pacific Ocean tsunamis, warning signs advise people where to run in the event of an incoming tsunami. Computer models can roughly predict tsunami arrival and impact based on information about the event that triggered it and the shape of the seafloor (bathymetry) and coastal land (topography).
One of the early warnings comes from nearby animals. Many animals sense danger and flee to higher ground before the water arrives. The Lisbon quake is the first documented case of such a phenomenon in Europe. The phenomenon was also noted in Sri Lanka in the 2004 Indian Ocean earthquake (). Some scientists speculate that animals may have an ability to sense subsonic Rayleigh waves from an earthquake minutes or hours before a tsunami strikes shore (Kenneally, '').
While it is not possible to prevent a tsunami, in some particularly tsunami-prone countries some measures have been taken to reduce the damage caused on shore. Japan has implemented an extensive programme of building tsunami walls of up to 4.5 m (13.5 ft) high in front of populated coastal areas. Other localities have built floodgates and channels to redirect the water from incoming tsunamis. However, their effectiveness has been questioned, as tsunamis are often higher than the barriers. For instance, the tsunami which hit the island of Hokkaido on July 12, 1993 created waves as much as 30 m (100 ft) tall - as high as a 10-story building. The port town of Aonae was completely surrounded by a tsunami wall, but the waves washed right over the wall and destroyed all the wood-framed structures in the area. The wall may have succeeded in slowing down and moderating the height of the tsunami but it did not prevent major destruction and loss of life.
The effects of a tsunami can be mitigated by natural factors such as tree cover on the shoreline. Some locations in the path of the 2004 Indian Ocean tsunami escaped almost unscathed as a result of the tsunami's energy being sapped by a belt of trees such as coconut palms and mangroves. In one striking example, the village of Naluvedapathy in India's Tamil Nadu region suffered minimal damage and few deaths as the wave broke up on a forest of 80,244 trees planted along the shoreline in 2002 in a bid to enter the Guinness Book of Records. Environmentalists have suggested tree planting along stretches of sea coast which are prone to tsunami risks. While it would take some years for the trees to grow to a useful size, such plantations could offer a much cheaper and longer-lasting means of tsunami mitigation than the costly and environmentally destructive method of erecting artificial barriers.
Historical tsunamis
See also List of historic tsunamis by death toll.
Tsunamis occur most frequently in the Pacific Ocean, but are a global phenomenon; they are possible wherever large bodies of water are found, including inland lakes, where they can be caused by landslides. Very small tsunamis, non-destructive and undetectable without specialized equipment, occur frequently as a result of minor earthquakes and other events.
Circa 65 million years B.C
In theory, a meteor impact created the Chicxulub Crater about 65 million years ago. This impact may also have caused the Cretaceous-Tertiary extinction event. There is clear evidence for a tsunami more than one kilometre high. (See Discovery of the Chicxulub Crater.) The tsunami disturbed and transported sediments over a huge distance. This is the most popular theory as to the extinction of the dinosaurs, however it has not been proven as fact.
Circa 1,500 B.C.
The eruption of the Santorini volcano about 3,500 years ago generated a megatsunami estimated at 600 feet. The effects of this megatsunami disturbing sediment at the bottom of the Mediterranean have been found. It has been theorised that the story of The Passage of the Red Sea as described in the Torah may have been due to this. Proponents suggest that the tsunami could have caused waters to recede temporarily and then drowned the Egyptian army when they later returned, however this is purely speculative. The Tsunami was nonetheless a real event that has been proved by geologists. (See Cause of the Passage of the Red Sea.)
1607 - Bristol Channel, England and Wales
In 2002 it was suggested that the Bristol Channel floods of 1607 in England and Wales, UK, may have been caused by a tsunami.
1755 - Lisbon, Portugal
Tens of thousands of Portuguese who survived the great 1755 Lisbon earthquake were killed by a tsunami which followed a half hour later. Many townspeople fled to the waterfront, believing the area safe from fires and from falling debris from aftershocks. Before the great wall of water hit the harbour, waters retreated, revealing lost cargo and forgotten shipwrecks.
The earthquake, tsunami, and subsequent fires killed more than a third of Lisbon's pre-quake population of 275,000. Historical records of explorations by Vasco da Gama and other early navigators were lost, and countless buildings were destroyed (including most examples of Portugal's Manueline architecture). Europeans of the 18th century struggled to understand the disaster within religious and rational belief systems. Philosophers of the Enlightenment, notably Voltaire, wrote about the event. The philosophical concept of the sublime, as described by philosopher Immanuel Kant in the Observations on the Feeling of the Beautiful and Sublime, took inspiration in part from attempts to comprehend the enormity of the Lisbon quake and tsunami.
1883 - Krakatoa explosive eruption
The island volcano of Krakatoa in Indonesia exploded with devastating fury in 1883, blowing its underground magma chamber partly empty so that much overlying land and seabed collapsed into it. A series of large tsunami waves was generated from the explosion, some reaching a height of over 40 metres above sea level. Tsunami waves were observed throughout the Indian Ocean, the Pacific Ocean, the American West Coast, South America, and even as far away as the English Channel. On the facing coasts of Java and Sumatra the sea flood went many miles inland and caused such vast loss of life that one area was never resettled but went back to the jungle and is now the Ujung Kulon nature reserve.
1929 - Newfoundland tsunami
On November 18, 1929, an earthquake of magnitude 7.2 occurred beneath the Laurentian Slope on the Grand Banks. The quake was felt throughout the Atlantic Provinces of Canada and as far west as Ottawa, Ontario and as far south as Claymont, Delaware. The resulting tsunami measured over 7 metres in height and took about 2½ hours to reach the Burin Peninsula on the south coast of Newfoundland, where 28 people lost their lives in various communities.
1946 - Pacific tsunami
The April 1 Aleutian Island earthquake tsunami that killed 165 people on Hawaii and Alaska resulted in the creation of a tsunami warning system (specifically The Pacific Tsunami Warning Center), established in 1949 for Pacific Ocean area countries. The tsunami is locally known in Hawaii as the April Fools Day Tsunami in Hawaii due to people thinking the warnings were an April Fools prank.
1960 - Chilean tsunami
The magnitude-9.5 Great Chilean Earthquake was the strongest earthquake ever recorded. Its epicentre off the coast of South Central Chile, generated one of the most destructive tsunamis of the 20th century.
It spread across the entire Pacific Ocean, with waves measuring up to 25 metres high. The first tsunami arrived at Hilo, Hawaii approximately 14.8 hrs after it originated off the coast of South Central Chile.
The highest wave at Hilo Bay was measured at around 10.7 m (35 ft.). 61 lives were lost allegedly due to people's failure to heed warning sirens. When the tsunami hit Onagawa, Japan, almost 22 hours after the quake, the wave height was 3 m above high tide. The number of people killed by the earthquake and subsequent tsunami is estimated to be between 490 and 2,290.
1963 - Vajont Dam disaster
The reservoir behind the Vajont Dam in northern Italy was struck by an enormous landslide. A tsunami was triggered which swept over the top of the dam (without bursting it) and into the valley below. Nearly 2,000 people were killed.
1964 - Good Friday tsunami
After the magnitude 9.2 Good Friday Earthquake, tsunamis struck Alaska, British Columbia, California and coastal Pacific Northwest towns, killing 121 people. The tsunamis were up to 6 m tall, and killed 11 people as far away as Crescent City, California.
1976 - Moro Gulf tsunami
On August 16, 1976 at 12:11 A.M., a devastating earthquake of 7.9 hit the island of Mindanao, Philippines. It created a tsunami that devastated more than 700 km of coastline bordering Moro Gulf in the North Celebes Sea. An estimated number of victims for this tragedy left 5,000 dead, 2,200 missing or presumed dead, more than 9,500 injured and a total of 93,500 people were left homeless. It devastated the cities and provinces of Pagadian City, Zamboanga del Sur, Zamboanga City, Basilan, Sulu, Sultan Kudarat, Maguindanao, Cotabato City, Lanao del Sur and Lanao del Norte.
1979 - Tumaco tsunami
A magnitude-7.9 earthquake occurred on December 12, 1979 at 7:59:4.3 (UTC) along the Pacific coast of Colombia and Ecuador. The earthquake and the resulting tsunami caused the destruction of at least six fishing villages and the death of hundreds of people in the Colombian province of Nariño. The earthquake was felt in Bogotá, Cali, Popayán, Buenaventura and several other cities and towns in Colombia and in Guayaquil, Esmeraldas, Quito and other parts of Ecuador. When the Tumaco Tsunami hit the coast, it caused huge destruction in the city of Tumaco, as well as in the small towns of El Charco, San Juan, Mosquera and Salahonda on the Pacific Coast of Colombia. The total number of victims of this tragedy was 259 dead, 798 wounded and 95 missing or presumed dead.
1993 - Okushiri tsunami
A devastating tsunami occurred off the coast of Hokkaido in Japan as a result of an earthquake on July 12, 1993. As a result, 202 people on the small island of Okushiri were killed, and hundreds more were missing or injured. In addition, millions of pet birds, cats and dogs lost their lives.
2004 - Indian Ocean tsunami
The 2004 Indian Ocean earthquake, which had a magnitude of 9.15, triggered a series of lethal tsunamis on December 26, 2004 that killed approximately 230,000 people (including 168,000 in Indonesia alone), making it the deadliest tsunami in recorded history. The tsunami killed people over an area ranging from the immediate vicinity of the quake in Indonesia, Thailand and the north-western coast of Malaysia to thousands of kilometres away in Bangladesh, India, Sri Lanka, the Maldives, and even as far as Somalia, Kenya and Tanzania in eastern Africa. The disaster prompted a huge worldwide effort to help victims of the tragedy, with billions of dollars being raised for disaster relief.
Unlike in the Pacific Ocean, there was no organized alert service covering the Indian Ocean. This was in part due to the absence of major tsunami events between 1883 (the Krakatoa eruption, which killed 36,000 people) and 2004. In light of the 2004 Indian Ocean tsunami, UNESCO and other world bodies have called for a global tsunami monitoring system.
Other historical tsunamis
Other tsunamis that have occurred include the following:
North American and Caribbean tsunamis
Possible tsunamis
Source: NOAA National Weather Service Forecast Office
Gambar jeung video
Tempo oge: Images and video, 2004 Indian Ocean earthquake Bahaya tsunamis
Tanjungmekar, Pakisjaya, Karawang
Tanjungmekar nyaéta salasahiji désa di kacamatan Pakisjaya, Kabupatén Karawang, Propinsi Jawa Barat, Indonésia.
SMAN 47 Jakarta
SMAN 47 Jakarta nyaéta Sakola Menengah Atas Negeri anu aya di Kota Jakarta Selatan. Alamat lengkepna di Jalan Delman Utama I Rt.001/011, Kalurahan/Désa Kebayoran Lama Utara Kacamatan Kebayoran Lama, Jakarta Selatan, DKI Jakarta, kalawan nomor NPSN 20102193.
2005 NB56
Ari 2005 NB56 mangrupa hiji astéroid. Ieu asteroid téh bagéan tina astéroid Apollo, anu nganjrek deukeut jeung marcapada. Ékséntrisitas orbit ieu astéroid kacatet gedéna 0.473, sedengkeun magnitudo mutlakna 22.9. Ari nu jadi référénsina mah nyaéta MPO87705.
Bebentukan
Kawas sakumna astéroid, ieu astéroid kabentuk tina nébula panonpoé primordial minangka beubeulahan planétisimal, objék di nébula marcapada ngora nu teu cukup badag pikeun robah jadi planét.
Baledog
balédog nyaéta kécap anu hartina miceun jauh pisan atawa dina bahasa Indonesia nyaéta lempar.
Conto kalimat:kuring dibalédog ku senda ku andi artina saya dilempar oleh andi.
130
Taun ka-130 Maséhi dina Kalénder Grégorian.
Bale-bale, Pulau-pulau Batu Barat, Nias Kidul
Bale-bale nyaéta salah sahiji Désa di kacamatan Pulau-pulau Batu Barat, Kabupatén Nias Kidul, Propinsi Sumatra Kalér, Indonésia.
Kajeung, Sungai Mas, Aceh Barat
Kajeung nyaéta salah sahiji Gampong di kacamatan Sungai Mas, Kabupatén Aceh Barat, Propinsi Acéh, Indonésia.
Sukasono, Sukawening, Garut
Sukasono nyaéta salah sahiji désa di kacamatan Sukawening, Kabupatén Garut, Propinsi Jawa Barat, Indonésia.
2014 ST1
Ari 2014 ST1 mangrupa hiji astéroid. Ieu asteroid téh bagéan tina astéroid Amor, anu nganjrek deukeut jeung marcapada. Ékséntrisitas orbit ieu astéroid kacatet gedéna 0.593, sedengkeun magnitudo mutlakna 26.0. Ari nu jadi référénsina mah nyaéta MPO 309119.
Bebentukan
Kawas sakumna astéroid, ieu astéroid kabentuk tina nébula panonpoé primordial minangka beubeulahan planétisimal, objék di nébula marcapada ngora nu teu cukup badag pikeun robah jadi planét.
Padang Manis, Wonosobo, Tanggamus
Padang Manis nyaéta salah sahiji Désa di kacamatan Wonosobo, Kabupatén Tanggamus, Propinsi Sumatra Kalér, Indonésia.
Baru Sungai Sakai, Tiang Pumpung, Merangin
Baru Sungai Sakai nyaéta salah sahiji désa di kacamatan Tiang Pumpung, Kabupatén Merangin, Propinsi Jambi, Indonésia.
2009 LE
Bebentukan
Kawas sakumna astéroid, ieu astéroid kabentuk tina nébula panonpoé primordial minangka beubeulahan planétisimal, objék di nébula marcapada ngora nu teu cukup badag pikeun robah jadi planét.
Teluk Limo, Pulau-pulau Batu Barat, Nias Kidul
Teluk Limo nyaéta salah sahiji Désa di kacamatan Pulau-pulau Batu Barat, Kabupatén Nias Kidul, Propinsi Sumatra Kalér, Indonésia.
Hudangna Yésus
Numutkeun Pasubayaan Énggal, utamina Injil, Yésus Kristus, ngalampahan kasangsawisan atanapi kasawat miwah teras perlaya disalibkeun di sahandapeun gupernur Yudéa, Pontius Pilatus, dina kaping 14 Nisan (~sasih April) kinten-kinten warsih 30-33 M. Numutkeun murid-murid-Mantenna sareng sawatawis catetan sanésna, Mantenna gugah deui tina pupusna dina dinten anu katiga, yaktos saparantos kaping 17 Nisan. Dinten éta mangrupi dinten munggaran dina saminggon. Pajaratan geusan Mantenna dikumurebkeun saparantos ngantunkeun kabuka seweng. Kinten-kinten 500 jalmi ningali Mantenna jumeneng deui saparantos Palastra-Na sareng sawatawis ti aranjeunna ningali Mantenna kaangkat munggah ka jomantara dugi ka ical kapambengan ku méga.
Kasang Pengker
Peristiwa ieu disebat dina términologi Karésten minangka gugahna Yésus Kristus, anu dipiémut sareng dirayakeun ku sadaya umat Karésten unggal warsih anu disebat Paskah. Seuseueurna umat Kristen, nampi Pasubayaan Énggal minangka peristiwa sajarah tina kajantenan leres anu mangrupi puseur tina kapercantenan aranjeunna, sanaos kitu kasondong sawatawis Karésten liberal anu henteu nampi gugahna sarira. Sanaos sapertos éta, limbrahna henteu aya umat Kristen anu nyawang cariosan ieu minangka legénda atanapi alégori.
Kitab Mazmur
Pangganepan: Yésus henteu teterasan linggih dina lebet pajaratan, nanging gugah ti dunya geusan jalmi anu perlaya.
Kitab Yesaya
Pangganepan: Yésus teras iasa ningali jalmi-jalmi anu diwilujengkeun ku Mantenna, margi Mantenna parantos gugah tina palastra miwah henteu pupus deui sapapaosna.
Kronologi Gugahna
Opat Injil nyatet sapertos manten murid-murid-Mantenna sareng jalmi-jalmi anu sanésna mendak wiréh lalayon Yésus henteu nyondong deui dina Pajaratan geusan Mantenna dikumurebkeun saparantos ngantunkeun.
2014 JW79
Ari 2014 JW79 mangrupa hiji astéroid. Ieu asteroid téh bagéan tina astéroid Apollo, anu nganjrek deukeut jeung marcapada. Ékséntrisitas orbit ieu astéroid kacatet gedéna 0.369, sedengkeun magnitudo mutlakna 26.6. Ari nu jadi référénsina mah nyaéta MPO�317897.
Bebentukan
Kawas sakumna astéroid, ieu astéroid kabentuk tina nébula panonpoé primordial minangka beubeulahan planétisimal, objék di nébula marcapada ngora nu teu cukup badag pikeun robah jadi planét.
SMAN 74 Jakarta
SMAN 74 Jakarta nyaéta Sakola Menengah Atas Negeri anu aya di Kota Jakarta Selatan. Alamat lengkepna di Jl. Dharma Putra Xi, Kalurahan/Désa Kebayoran Lama Selatan Kacamatan Kebayoran Lama, Jakarta Selatan, DKI Jakarta, kalawan nomor NPSN 20102569.
Kalibrasi (statistik)
Kalibrasi dina statistik nyaéta sabalikna tina prosés régrési. Masalah kalibrasi (en:Calibration problem) nyaéta digunakeunana data nu dipikanyaho dina hubungan observasi antara variabel terikat jeung variabel bébas keur nyieun estimasi nilai variabel bébas séjénna tina observasi anyar dina variabel terikat.
Masalah dina maké ieu kalibrasi nyaéta perlu modél keur ngahubungkeun umur nu diobservasi keur ngaminimalkeun kasalahan dina observasi atawa ngaminimalkeun kasalahan dina nangtukeun umur. Dua cara pamarekanbakal méré hasil nu béda, sarta ieu béda bakal ngagedéan lamun maké dipaké keur ekstrapolasi dina sababaraha jauh tina hasil nu dipikanyaho.
Natal, Mandailing Natal
Natal nyaéta salah sahiji kacamatan di Kabupatén Mandailing Natal, Propinsi Sumatra Kalér, Indonésia.
2008 YP2
Ari 2008 YP2 mangrupa hiji astéroid. Ieu asteroid téh bagéan tina astéroid Amor, anu nganjrek deukeut jeung marcapada. Ékséntrisitas orbit ieu astéroid kacatet gedéna 0.326, sedengkeun magnitudo mutlakna 23.3. Ari nu jadi référénsina mah nyaéta MPO 151120.
2002 XO40
Bebentukan
Kawas sakumna astéroid, ieu astéroid kabentuk tina nébula panonpoé primordial minangka beubeulahan planétisimal, objék di nébula marcapada ngora nu teu cukup badag pikeun robah jadi planét.
2008 YP2
Bebentukan
Kawas sakumna astéroid, ieu astéroid kabentuk tina nébula panonpoé primordial minangka beubeulahan planétisimal, objék di nébula marcapada ngora nu teu cukup badag pikeun robah jadi planét.
Banda Baro, Acéh Kalér
Banda Baro nyaéta salah sahiji kacamatan di Kabupatén Acéh Kalér, Propinsi Acéh, Indonésia.
Baroh Blang Rimueng, Syamtalira Bayu, Aceh Utara
Baroh Blang Rimueng nyaéta salah sahiji Gampong di kacamatan Syamtalira Bayu, Kabupatén Aceh Utara, Propinsi Acéh, Indonésia.
Burni Pase, Permata, Bener Meriah
Burni Pase nyaéta salah sahiji Gampong di kacamatan Permata, Kabupatén Bener Meriah, Propinsi Acéh, Indonésia.
Tengah, Pantai Labu, Deli Serdang
Tengah nyaéta salah sahiji Désa di kacamatan Pantai Labu, Kabupatén Deli Serdang, Propinsi Sumatra Kalér, Indonésia.
Consistency (statistics)
Dina statistik, éstimator konsisten nyaéta estimator nu converges in probability kana lobana nu geus diestimasi salaku ukuran sampel nu tumuwuh.
éstimator tn (di mana n mangrupa ukuran sampel) mangrupa éstimator konsisten keur parameter θ lamun jeung ngan lamun, keur sakabéh ε > 0, teu nempo sakumaha leutikna, urang mibanda
Propinsi Kabul
Kābul (کابل Kābəl, ) nyaéta salah sahiji ti 34 propinsi di Apganistan. Propinsi ieu aya di beulah wétan nagara. Ibu kota propinsi ieu nyaéta Kota Kabul, nu mangrupa ibu kota Apganistan. Populasi propinsi ieu nyaéta 3,5 yuta jiwa sakumaha dina 2009, nu méh 80 persén hirup di wewengkon pakotaan.
Geudong, Sungai Mas, Aceh Barat
Geudong nyaéta salah sahiji Gampong di kacamatan Sungai Mas, Kabupatén Aceh Barat, Propinsi Acéh, Indonésia.
Tambak Ratu, Batang Asai, Sarolangun
Tambak Ratu nyaéta salah sahiji désa di kacamatan Batang Asai, Kabupatén Sarolangun, Propinsi Jambi, Indonésia.
Tanjungpakis, Pakisjaya, Karawang
Tanjungpakis nyaéta salah sahiji désa di kacamatan Pakisjaya, Kabupatén Karawang, Propinsi Jawa Barat, Indonésia.
129
Taun ka-129 Maséhi dina Kalénder Grégorian.
2012 HL8
Ari 2012 HL8 mangrupa hiji astéroid. Ieu asteroid téh bagéan tina astéroid Amor, anu nganjrek deukeut jeung marcapada. Ékséntrisitas orbit ieu astéroid kacatet gedéna 0.538, sedengkeun magnitudo mutlakna 23.7. Ari nu jadi référénsina mah nyaéta MPO 234430.
Bebentukan
Kawas sakumna astéroid, ieu astéroid kabentuk tina nébula panonpoé primordial minangka beubeulahan planétisimal, objék di nébula marcapada ngora nu teu cukup badag pikeun robah jadi planét.
2012 DW60
Ari 2012 DW60 mangrupa hiji astéroid. Ieu asteroid téh bagéan tina astéroid Apollo, anu nganjrek deukeut jeung marcapada. Ékséntrisitas orbit ieu astéroid kacatet gedéna 0.168, sedengkeun magnitudo mutlakna 26.5. Ari nu jadi référénsina mah nyaéta MPO�227524.
Wayne Sermon
Daniel Wayne Sermon mangripa musisi, panulis lagu, ogé produser rékaman ti Amérika. Anjeunna mangrupikeun gitaris tina band pop rock namina Imagine Dragons.
2012 DW60
Bebentukan
Kawas sakumna astéroid, ieu astéroid kabentuk tina nébula panonpoé primordial minangka beubeulahan planétisimal, objék di nébula marcapada ngora nu teu cukup badag pikeun robah jadi planét.
Odading
Odading atawa kuéh bantal nyaéta sabangsa roti anu asakna digoréng tur mibanda rasa amis wujudna aya anu lonyod aya ogé rada masagi kawas bantal dijieun tina adonan tarigu jeung gula, Kuéh odading biasana sok digédéngkeun jeung cakué atawa youtiao. Odading mangrupa kuéh jajanan anu kasohor tur loba anu mikaresep umumna urang Jawa Kulon utamana urang Bandung. Odading ilaharna dipaké nyarap atawa ngopi isuk-isuk dibaturan ku cikopi atawa citéh haneut.
Sajarah
Baheula ieu kuéh téh tacan mibanda ngaran, ngan saukur kuéh basajan tina adonan tarigu jeung gula anu diguluntung-guluntung sagedé indung suku tuluy baé digoréng. Hiji mangsa aya budak keur dagang éta kuéh diwadahan kana nyiru anu dituruban ku daun cau, teu kungsi lila jol aya sinyo Walanda ngaliwat jeung indungna ninggali éta dagangan téh sinyo ngarenghik ka indungna mun urang mah “uing hayang meuli éta”, pokna téh “Mammie, koop dat voor mij". Tuluy éta simami téh ngageroan budak anu dagang téa, nitah nyingkabkeun turub kuéh tina daun cau. Pok si mamih téh ngomong “O, dat ding?” maksud namah nanya “O, anu iéu?”, ari budak anu dagang ku lataran teu ngarti basa Walanda téa ngagerentes dina haténa ”geuning ieu kuéh téh ngarana odading”. Tempona balik ka imahna ieu budak hariweusweus ka indungna ngabéjaan cenah kuéh anu sok didagangkeun ku manéhna téh ngarna odading, nya ti waktu harita ngaran odading téh dipaké pikeun nyebut kueh beunang ngagoréng tina adonan tarigu anu di guluntung-guluntung.
Kejadian, Wonosobo, Tanggamus
Kejadian nyaéta salah sahiji Désa di kacamatan Wonosobo, Kabupatén Tanggamus, Propinsi Sumatra Kalér, Indonésia.
Bale Musara, Permata, Bener Meriah
Bale Musara nyaéta salah sahiji Gampong di kacamatan Permata, Kabupatén Bener Meriah, Propinsi Acéh, Indonésia.
SMAS Bakti Mulya 400
SMAS Bakti Mulya 400 nyaéta Sakola Menengah Atas Swasta anu aya di Kota Jakarta Selatan. Alamat lengkepna di Jl.Lingkar Selatan, Kalurahan/Désa Pondok Pinang Kacamatan Kebayoran Lama, Jakarta Selatan, DKI Jakarta, kalawan nomor NPSN 20107281.
Bagan Serdang, Pantai Labu, Deli Serdang
Bagan Serdang nyaéta salah sahiji Désa di kacamatan Pantai Labu, Kabupatén Deli Serdang, Propinsi Sumatra Kalér, Indonésia.
Sukawening, Sukawening, Garut
Sukawening nyaéta salah sahiji désa di kacamatan Sukawening, Kabupatén Garut, Propinsi Jawa Barat, Indonésia.
Ar-Rum
Surat Ar-Rum (basa Arab: الروم) nyaéta surat ka-30 dina Al-Qur'an. Ieu surat téh aya 60 ayat, kaasup kana golongan surat-surat Makkiyah nu turun di Mekkah. Judul Ar-Rum hartina Bangsa Erum (Romawi).
(164214) 2004 LZ11
Bebentukan
Kawas sakumna astéroid, ieu astéroid kabentuk tina nébula panonpoé primordial minangka beubeulahan planétisimal, objék di nébula marcapada ngora nu teu cukup badag pikeun robah jadi planét.
2017 DP109
Ari 2017 DP109 mangrupa hiji astéroid. Ieu asteroid téh bagéan tina astéroid Apollo, anu nganjrek deukeut jeung marcapada. Ékséntrisitas orbit ieu astéroid kacatet gedéna 0.614, sedengkeun magnitudo mutlakna 26.9. Ari nu jadi référénsina mah nyaéta MPO�399984.
Bebentukan
Kawas sakumna astéroid, ieu astéroid kabentuk tina nébula panonpoé primordial minangka beubeulahan planétisimal, objék di nébula marcapada ngora nu teu cukup badag pikeun robah jadi planét.
2014 JV79
Bebentukan
Kawas sakumna astéroid, ieu astéroid kabentuk tina nébula panonpoé primordial minangka beubeulahan planétisimal, objék di nébula marcapada ngora nu teu cukup badag pikeun robah jadi planét.
Muara Batang Gadis, Mandailing Natal
Muara Batang Gadis nyaéta salah sahiji kacamatan di Kabupatén Mandailing Natal, Propinsi Sumatra Kalér, Indonésia.
Ciinjuk, Cadasari, Pandéglang
Ciinjuk nyaéta salasahiji désa di Kacamatan Bojong, Pandéglang, Propinsi Banten, Indonésia.
Banda Mulia, Acéh Tamiang
Banda Mulia nyaéta salah sahiji kacamatan di Kabupatén Acéh Tamiang, Propinsi Acéh, Indonésia.
2005 NX55
Ari 2005 NX55 mangrupa hiji astéroid. Ieu asteroid téh bagéan tina astéroid Apollo, anu nganjrek deukeut jeung marcapada. Ékséntrisitas orbit ieu astéroid kacatet gedéna 0.594, sedengkeun magnitudo mutlakna 22.1. Ari nu jadi référénsina mah nyaéta MPO87705.
Bebentukan
Kawas sakumna astéroid, ieu astéroid kabentuk tina nébula panonpoé primordial minangka beubeulahan planétisimal, objék di nébula marcapada ngora nu teu cukup badag pikeun robah jadi planét.
Cécé Somantri
Radén Tjétjé Somantri. Ngarana basa gumelar nyaéta R. Rusdi Somantridiputra (Roesdi Somantridiputra), ngan sabab emangna anu ngagedékeunna miboga ngaran kanyaah atawa landian Cécé, nu ngajadikeun ngaran Cécé nu sok dipakéna. (Subang, 1891- Bandung, 30 April 1963). Penari, guru jeung pencipta tari sarta nu mawa parobahan tari sunda. Ramana, R.Somantri Kusumah (Koesoemah),patih Purwakarta, ngantunkeun anjeunna basa Cécé dina jero kakandungan kénéh. Matak ti oorok geus di gedékeun ku emangna, R. Karta Kusumah (Koesoemah), wedana Subang. Sanggeus tamat HIS jeung MULO dilajeng ka MOSVIA, tapi teu nepi tamat sabab kaburu resep kanu nari.
Lalampahan Karir
Anu mimiti ngajarkeun anjeunna nari nyaéta R.Gandakusumah (Gandakoesoemah) nu kasohor ku landian Aom Doyot nu sok dianggap tokoh di tukangeun layar lahirna Ibing Keurseus. Cécé diajar nari ka anjeuna di kabupaten (tempat cicing bupati) Purwakarta 1911. Cécé ogé diajar penca ka R. Kartaatmaja (Kartaatmadja), tokoh aliran Timbangan. Cécé diajar tari wayang di Bandung nu matak anjeunna kasohor penri wayang wong priyayi. Guruna Aom Menim. Anjeunna ogé diajar tari topéng ka dua dalang topéng Palimanan, nyaéta Wentar jeung Koncar nu dina sakitaran tahun 1918 didatagkeun ku pangusaha nu resep kana tari nagarana Asép Berlian jang ngajar salila sabulan. Cécé neuleuman tari topéng Cirebon ti dalang lain nu ngarana Kamsi jeung Resna, ogé ti É lang Oto Dendakusumah (Dendakoesoemah)-anjeunna baraya Keraton Kanoman, Cirebon. Dina taun 1926, Cécé maén jadi Baladéwa dina paméntasan wayang wong priyayi pimpinan R. Ardiputra (Ardipoetra) nu diayakeun ku bupati Bandung R.A.A Wiranatakusumah.
DIna taun 1935, Cécé jadi anggota "Sekar Pakuan" jeung iwal aktip nari, ogé ngajar ka wanoja-wanoja budak pajabat (Ménak). Salian ti Cta écé ogé ngajar tari ka murid-murid HIK jeung MOSVIA. Dina waktu "Sekar Pakuan" meunang ondangan jang ngeusian acara ngareuah-reuah ulang taun Keraton Surakarta Adiningrat nu ka-200 (1939), Cécé tampil nari, salianti acara séjénna.
Taun 1942, sanggeus "Sekar Pakuan", dibubarkeun ku Balatentara Jepang, Cécé diajak ku TB. O. Martakusuma jang ngajar tari di Keimin Bunka Shidosho. Gawé bareng duanana nepi tauhn 1958, teu saukur nyieun tarian anyar, tapi ogé neundeun dasar-dasar jang kamekaran seni tari sunda moderen. Tb. O.Martakusuma mineng jadi nu nyiptakeun raksukan tari jieunan Cécé. Mangsa Keimin Bunka Shidoso bubar jeung revolusi ngagolak, Cécé ngungsi ka Garut. Di ditu anjeunna gabung jeung Tb. O. Martakusuma, R. Barnas Prawiradiningrat, dkk. Nu ngajieun Badan Kebudayaan Jawa Barat (BKDB). Di DItu ogé, Cécé ngajar tari sunda (1946-1948). Anjeunna jeung murid-muridna méntaskeun tatarian dina resépsi Konférénsi Pamongpraja sa-Indonésia nu dihadiran ogé ku Presiden Sukarno (1947).
Dina waktu éta anjeunna nyiptakeun a.l. tari "Dewi" (1946), "Anjasmara" I jeung II (1946), "Puragabaya" (1947), "Kendit Birayung" (1947), "Dewi Sérang" (1948) jeung "Sulintang" (1948). Sanggeus balik deui ka Bandung dina pangungsian, (1948), Cécé nuluykeun gawé barengna jeung Tb. O. Martakusuma jeung R. Barnas nu ngabentuk Badan Kasenian Indonésia (BKI). Ogé ngajar nari bari ngajieun tatarian anu anyar, nu utamana jang di pentaskeun ku wanoja., a.I. "Komala Gilang Kusumah" (1949),"Ratu Graéni" (1949), "Topéng Koncaran" (1950), "Srigati" (1950), "Golék Purwokertoan" (1952), "Sekar Putri" (1952-1954), "Merak" (1955), "Golék Rinéka" (1957), "Nusantara" (1958), "Anjasmara" III (1958), "Sekar Arum" (1958), jeung "Renggarini" (1958).
Sarah Perlak, Sungai Mas, Aceh Barat
Sarah Perlak nyaéta salah sahiji Gampong di kacamatan Sungai Mas, Kabupatén Aceh Barat, Propinsi Acéh, Indonésia.
SMAS Hang Tuah 1 Jakarta
SMAS Hang Tuah 1 Jakarta nyaéta Sakola Menengah Atas Swasta anu aya di Kota Jakarta Selatan. Alamat lengkepna di Jl. Cileduk Raya Komp. Seskoal, Kalurahan/Désa Cipulir Kacamatan Kebayoran Lama, Jakarta Selatan, DKI Jakarta, kalawan nomor NPSN 20107300.
Tutut, Sungai Mas, Aceh Barat
Tutut nyaéta salah sahiji Gampong di kacamatan Sungai Mas, Kabupatén Aceh Barat, Propinsi Acéh, Indonésia.
2016 GC2
Bebentukan
Kawas sakumna astéroid, ieu astéroid kabentuk tina nébula panonpoé primordial minangka beubeulahan planétisimal, objék di nébula marcapada ngora nu teu cukup badag pikeun robah jadi planét.
Marit Baru, Pulau-pulau Batu Barat, Nias Kidul
Marit Baru nyaéta salah sahiji Désa di kacamatan Pulau-pulau Batu Barat, Kabupatén Nias Kidul, Propinsi Sumatra Kalér, Indonésia.
(450259) 2003 WQ7
Ari 2003 WQ7 mangrupa hiji astéroid. Ieu asteroid téh bagéan tina astéroid Apollo, anu nganjrek deukeut jeung marcapada. Ékséntrisitas orbit ieu astéroid kacatet gedéna 0.454, sedengkeun magnitudo mutlakna 19.6. Ari nu jadi référénsina mah nyaéta MPO�353839.