Tsunami in hindi wikipedia


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2004 Indian Ocean earthquake and tsunami




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Further analysis of seismic waveforms suggests that a fault trending north-south gives a better fit. The strongest shaking was felt in Donggala Regency where a maximum intensity of IX violent was recorded. According to the Indonesian Agency for the Assessment and Application for Technology BPPTenergy released by the quake was times to that released in the nuclear bombing of Hiroshima. Analysis also showed that the shoreline which was located near the rupture in Palu and Donggala had a decrease on its height. Height drops of 0. The tsunami, however, struck higher than expected. Residents of Palu reported waves with heights of more than 2 metres while several others stated that the waves managed to reach the second floor.

Calculations suggested that the tsunami would arrive in Palu approximately 20 minutes after the earthquake. Around A tsunami warning was issued, and later lifted. The BMKG claimed the warning was lifted after the tsunami had struck, but the timing is unclear, and the agency was criticized on social media. The Palu Nomoni Festival in Talise Beach continued and most of the festival attendees did not realize that there was a possibility of a tsunami.

Eyewitnesses even stated that some people were still strolling on the beach when the tsunami struck. It was estimated that hundreds were caught off guard and swept away by the waves. The shaking was violent enough to damage the tsunami detectors in Palu, as further examination revealed that none of the detectors were able to send signals to alert residents. Since the earthquake was a strike-slip earthquakethe tsunami was expected to be at a low height, with a maximum height of approximately 2 metres. During a strike-slip earthquake, the movements of the crusts were largely in horizontal motion while most tsunamis occurred in earthquakes with vertical motion.

One explanation is that the earthquake triggered underwater landslides, causing the tsunami. Palu's Tatura Mall, one of the oldest shopping centres in Palu, collapsed, trapping dozens of people. At the time of the earthquake, 76 of the 80 bedrooms of the hotel were occupied. Airport officials confirmed that the navigation system was damaged and the control tower of the airport collapsed. However, an extremely large landslide could generate a megatsunami that might have ocean-wide impacts. In fact, a tsunami is better understood as a new and suddenly higher sea level, which manifests as a shelf or shelves of water. The leading edge of a tsunami superficially resembles a breaking wave but behaves differently: Although 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 are phenomena which move the entire depth of the ocean often several kilometres deep rather than just the surface, so they contain immense energy, propagate at high speeds and can travel great transoceanic distances with little overall energy loss.

Nairobiwhich many at the northern end of the Bay of Chicagohad few times despite being a low-lying sole badly beyond the epicenter. Methodical outlet, confidence, medicine and aids labour of hearthstone theaters were also qualified to Palu and Donggala.

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. However, like tsunami, seismic sea wave is not a completely accurate term, as forces other than earthquakes — including underwater landslidesvolcanic eruptions, underwater explosions, land or ice slumping into the ocean, meteorite impacts, and the weather when the atmospheric pressure changes very rapidly — can generate such waves by displacing water. While Japan may have the longest recorded history of tsunamis, the sheer destruction caused by the Indian Ocean earthquake and tsunami event mark it as the most devastating of its kind in modern times, killing aroundpeople.

Of historical and current with regard to risk assumptions importance are the Lisbon earthquake and tsunami which was caused by the Azores—Gibraltar Transform Faultthe Calabrian earthquakeseach causing several tens of thousands of deaths and the Messina earthquake and tsunami. The tsunami claimed more thanlives in Sicily and Calabria and is among the most deadly natural disasters in modern Europe. The Storegga Slide in the Norwegian Sea and some examples of tsunamis affecting the British Isles refer to landslide and meteotsunamis predominantly and less to earthquake-induced waves. As early as BC the Greek historian Thucydides inquired in his book History of the Peloponnesian War about the causes of tsunami, and was the first to argue that ocean earthquakes must be the cause.

At the point where its shock has been the most violent the sea is driven back, and suddenly recoiling with redoubled force, causes the inundation. Without an earthquake I do not see how such an accident could happen. Tectonic earthquakes are a particular kind of earthquake that are associated with the Earth's crustal deformation; when these earthquakes occur beneath the sea, the water above the deformed area is displaced from its equilibrium position. Movement on normal extensional faults can also cause displacement of the seabed, but only the largest of such events typically related to flexure in the outer trench swell cause enough displacement to give rise to a significant tsunami, such as the Sumba and Sanriku events.

Plate slips, causing subsidence and releasing energy into water. The energy released produces tsunami waves. They grow in height when they reach shallower water, in a wave shoaling process described below. A tsunami can occur in any tidal state and even at low tide can still inundate coastal areas.

Hindi wikipedia in Tsunami

On April 1,the 8. Between and were killed. The waves travel at a great speed across an ocean with little energy loss. They can Tsunami in hindi wikipedia sand from beachesdestroy treestoss and drag vehicleshouses and even destroy whole towns. Tsunamis can even be wikipexia when a meteorite strikes the earths surface, though it is very rare. Yindi tsunami normally occurs in the Pacific Ocean, especially in what is called the ring of firebut can occur in any large body of wikipediw. The water often draws back from the seacoast half of the wave period prior to the wave getting to the coast. Each of these megathrust earthquakes also spawned tsunamis in the Pacific Ocean.

However, in comparison to the Indian Ocean earthquake, the death toll from these earthquakes was significantly lower, primarily because of the lower population density along the coasts near affected areas, the much greater distances to more populated coasts, and the superior infrastructure and warning systems in MEDCs More Economically Developed Countries such as Japan. All of them are believed to be greater than magnitude 9, but no accurate measurements were available at the time. Tectonic plates Main article: Plate tectonics Epicenter and associated aftershocks The Indian Ocean earthquake was unusually large in geographical and geological extent. The slip did not happen instantaneously but took place in two phases over several minutes: The rupture proceeded at about 2.

However, the northern rupture occurred more slowly than in the south, at about 2. The Indian Plate is part of the great Indo-Australian Platewhich underlies the Indian Ocean and Bay of Bengaland is moving north-east at an average of 6 centimetres per year 2.

The India Plate sinks deeper and deeper beneath the Burma Plate until the increasing temperature and pressure drive volatiles out of the subducting plate. These volatiles rise into the overlying plate, causing partial melting and the formation of magma. The rising magma intrudes into the crust above and exits the Earth's crust through volcanoes in the form of a volcanic arc. As well as the sideways movement between the plates, the Indian Ocean earthquake resulted in a rise of the sea floor by several metres, displacing an estimated 30 cubic kilometres 7. This greatly increased the geographical area over which the waves were observed, reaching as far as Mexico, Chile, and the Arctic.

The raising of the sea floor significantly reduced the capacity of the Indian Ocean, producing a permanent rise in the global sea level by an estimated 0. List of earthquakes in Indonesia and List of earthquakes in Initial earthquake and aftershocks measuring greater than 4. The magnitude 8. Other aftershocks of up to magnitude 6. A week after the earthquake, its reverberations could still be measured, providing valuable scientific data about the Earth's interior.


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