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  2. Tsunami - Wikipedia

    en.wikipedia.org/wiki/Tsunami

    The reason for the Japanese name "harbour wave" is that sometimes a village's fishermen would sail out, and encounter no unusual waves while out at sea fishing, and come back to land to find their village devastated by a huge wave. As the tsunami approaches the coast and the waters become shallow, wave shoaling compresses the wave and its speed ...

  3. Airy wave theory - Wikipedia

    en.wikipedia.org/wiki/Airy_wave_theory

    Airy wave theory is also a good approximation for tsunami waves in the ... the phase speed of the waves is only dependent ... decimeters in case of a water–air ...

  4. Megatsunami - Wikipedia

    en.wikipedia.org/wiki/Megatsunami

    An example of this was the 17 July 1998, Papua New Guinean landslide tsunami where waves up to 15 m high impacted a 20 km section of the coast killing 2,200 people, yet at greater distances the tsunami was not a major hazard. This is due to the comparatively small source area of most landslide tsunami (relative to the area affected by large ...

  5. A ‘non-destructive’ tsunami was spotted after California’s ...

    www.aol.com/non-destructive-tsunami-spotted...

    A simulation shows tsunami wave behavior along the central California coastline. For visualization purposes, 70 minutes of elapse time were compressed into 20 seconds and the tsunami wave’s ...

  6. Seismic wave - Wikipedia

    en.wikipedia.org/wiki/Seismic_wave

    These waves can travel through any type of material, including fluids, and can travel nearly 1.7 times faster than the S waves. In air, they take the form of sound waves, hence they travel at the speed of sound. Typical speeds are 330 m/s in air, 1450 m/s in water and about 5000 m/s in granite.

  7. Meteotsunami - Wikipedia

    en.wikipedia.org/wiki/Meteotsunami

    Only about 3% of historical tsunami events (from 2000 BC through 2014) are known to have meteorological origins, although their true prevalence may be considerably higher than this because 10% of historical tsunamis have unknown origins, tsunami events in the past are often difficult to validate, and meteotsunamis may have previously been ...

  8. 1946 Aleutian Islands earthquake - Wikipedia

    en.wikipedia.org/wiki/1946_Aleutian_Islands...

    UTC time: 1946-04-01 12:29:01: ISC event: 898313: USGS-ANSSComCat: Local date: April 1, 1946 (): Local time: 02:29: Magnitude: 7.4 M s, 8.6 M w, 9.3 M t: Depth: 15 km (9.3 mi) [1] Epicenter: 1]: Type: Megathrust: Areas affected: Hawaii, Alaska United States: Max. intensity: MMI VI (Strong): Tsunami: Up to 42 m (138 ft) at Unimak Island: Casualties: 165–173 [2]: The 1946 Aleutian Islands ...

  9. 1958 Lituya Bay earthquake and megatsunami - Wikipedia

    en.wikipedia.org/wiki/1958_Lituya_Bay_earthquake...

    The wave came out of the lower part, and looked like the smallest part of the whole thing. The wave did not go up 1,800 feet, the water splashed there. [11] The wave made its way to his boat 2–3 minutes after he saw it and carried the Edrie down to the southern shore and then back near the center of the bay. Ulrich was able to control the ...