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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
227,898 dead [5] [6] On 26 December 2004, at 07:58:53 local time ( UTC+7 ), a major earthquake with a magnitude of 9.2–9.3 Mw struck with an epicentre off the west coast of northern Sumatra, Indonesia. The undersea megathrust earthquake, known by the scientific community as the Sumatra–Andaman earthquake, [8] [9] was caused by a rupture ...
Dynaquad. Dynaquad, or DY, was a matrix decoder 4-channel quadraphonic sound system developed by Dynaco in 1969. [1] [2] [3] The system originally had four speakers that were arranged in a diamond shape (centre-front, centre-left, centre-rear, centre-right). [4] [5] Initially (first available in 1969 with th Dynaco SCA-80Q amplifier [6] ), it ...
1877 Iquique. On 10 May 1877 at 0:59 UTC, a magnitude 8.5 earthquake occurred near Iquique, Peru (now Chile). The resulting tsunami reached New Zealand's eastern coastline between 7 and 8 am NZDT on 11 May. The wave had a reported 1–2-metre height in most places and impacted the coast from the Bay of Islands to Bluff.
A megatsunami is a tsunami with an initial wave amplitude measured in many tens or hundreds of metres. A megatsunami is a separate class of event from an ordinary tsunami and is caused by different physical mechanisms. Normal tsunamis result from displacement of the sea floor due to movements in the Earth's crust (plate tectonics).
QS Regular Matrix. Quadraphonic Sound (originally called Quadphonic Synthesizer, and later incorrectly referred to as RM or Regular Matrix) was a phase amplitude matrix 4-channel quadraphonic sound system for phonograph records. The system was based on technology created by Peter Scheiber, but further developed by engineer Ryosuke Ito [1] [2 ...
Teletsunami. 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 ...
A meteotsunami or meteorological tsunami [1] is a tsunami -like sea wave of meteorological origin. Meteotsunamis are generated when rapid changes in barometric pressure cause the displacement of a body of water. In contrast to impulse-type tsunami sources, a traveling atmospheric disturbance normally interacts with the ocean over a limited ...
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