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Earthquake environmental effects are divided into two main types: Coseismic surface faulting induced by the 1915 Fucino, Central Italy, earthquake. Primary effects: which are the surface expression of the seismogenic source (e.g., surface faulting), normally observed for crustal earthquakes above a given magnitude threshold (typically M w =5.5 ...
The aftermath of the 2011 Tōhoku earthquake and tsunami included both a humanitarian crisis and massive economic impacts. The tsunami created over 300,000 refugees in the Tōhoku region of Japan , and resulted in shortages of food, water, shelter, medicine and fuel for survivors. 15,900 deaths have been confirmed.
The 2004 Indian Ocean tsunami was a teletsunami.. A teletsunami (also called an ocean-wide tsunami, distant tsunami, distant-source tsunami, far-field tsunami, or trans-ocean tsunami) is a tsunami that originates from a distant source, defined as more than 1,000 km (620 mi) away or three hours' travel from the area of interest, [1] [2] sometimes travelling across an ocean.
The coastal town of Lhoknga was hit by tsunami waves of more than 20 to 25 meters with run-up heights of more than 30 meters in some places. Ten-meter tall waves passed the northern tip of the island to race south down the Straits of Malacca and strike along the northeast coast as far east as Lhokseumawe .
The effects of a 20° dipping fault along the top of the subducting plate was found to match both the observed seismic response and tsunami, but required a displacement of 10.4 m. [2] The displacement was reduced to a more reasonable value after the extra uplift caused by the deformation of sediments in the wedge and a shallower fault dip of 10 ...
The residents of the coastal towns and villages were taken completely by surprise because the tsunami had only been preceded by a relatively weak shock. The magnitude of the tsunami has been estimated as M t =8.2 while the earthquake shaking only indicated a magnitude of M s =7.2. This discrepancy in magnitude requires more than just a slow ...
Maximum recession of the sea at Kata Noi Beach at 10:25 a.m., prior to the third—and strongest—tsunami wave. The economic impact of the tsunami on Thailand was considerable, though not as great as in poorer countries such as Indonesia or Sri Lanka. Thailand has a liberalised, flexible and robust economy, which has shown powers of rapid ...
On 10 April 1815, an eruption of VEI 7 caused a localized tsunami. Tsunami of 4 metres (13 ft) in Sanggar, 1 to 2 m (3 ft 3 in to 6 ft 7 in) in Besuki, Java Island and 2 m (6 ft 7 in) in the Molucca Islands. 1819: Gujarat, India: 1819 Rann of Kutch earthquake: Earthquake: On 16 June 1819, a local tsunami inundated the Great Rann of Kutch: 1833