Michoacán State, Mexico magnitude 6.8 earthquake (1:16 AM, 22 September 2022) 3 : 無料・フリー素材/写真
Michoacán State, Mexico magnitude 6.8 earthquake (1:16 AM, 22 September 2022) 3 / James St. John
| ライセンス | クリエイティブ・コモンズ 表示 2.1 |
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| 説明 | This seismogram is from the Tegucigalpa seismic station in Honduras. The noise is from a strong, magnitude 6.8 earthquake that hit southwestern coastal Mexico at 1:16 AM, local time, on 22 September 2022. The epicenter was about 45 kilometers ~east of the town of Maruata, Michoacán State, Mexico. The hypocenter was about 24 kilometers deep. Shaking resulted from thrust faulting along a west-northwest to east-southeast striking fault zone. A much stronger quake of magnitude 7.6 occurred ~west of here about 2.5 days earlier.The quake occurred along a subduction zone - such settings experience the most powerful tectonic quakes in the world. In the far-eastern Pacific Ocean, the Cocos Plate, composed of oceanic lithosphere, subducts beneath continental lithosphere of the North American Plate. The subduction zone's surface expression is a deep seafloor trough called the Middle America Trench.--------------------------------Info. at:earthquake.usgs.gov/earthquakes/eventpage/us7000ia36/exec...anden.wikipedia.org/wiki/Cocos_Plateanden.wikipedia.org/wiki/Middle_America_Trench--------------------------------An earthquake is a natural shaking or vibrating of the Earth caused by sudden fault movement and a rapid release of energy. Earthquake activity is called "seismicity". The study of earthquakes is called "seismology". The actual underground location of an earthquake is the hypocenter, or focus. The site at the Earth's surface, directly above the hypocenter, is the epicenter. Minor earthquakes may occur before a major event - such small quakes are called foreshocks. Minor to major quakes after a major event are aftershocks.Most earthquakes occur at or near tectonic plate boundaries, such as subduction zones, mid-ocean ridges, collision zones, and transform plate boundaries. They also occur at hotspots - large subsurface mantle plumes (Examples: Hawaii, Yellowstone, Iceland, Afar).Earthquakes generate four types of shock waves: P-waves, S-waves, Love waves, and Rayleigh waves. P-waves and S-waves are body waves - they travel through solid rocks. Love waves and Rayleigh waves travel only at the surface - they are surface waves. P-waves are push-pull waves that travel quickly and cause little damage. S-waves are up-and-down waves (like flicking a rope) that travel slowly and cause significant damage. Love waves are side-to-side surface waves, like a slithering snake. Rayleigh waves are rotational surface waves, somewhat like ripples from tossing a pebble into a pond.Earthquakes are associated with many specific hazards, such as ground shaking, ground rupturing, subsidence (sinking), uplift (rising), tsunamis, landslides, fires, and liquefaction.Some famous major earthquakes in history include: Shensi, China in 1556; Lisbon, Portugal in 1755; New Madrid, Missouri in 1811-1812; San Francisco, California in 1906; Anchorage, Alaska in 1964; and Loma Prieta, California in 1989. |
| 撮影日 | 2022-09-23 12:36:41 |
| 撮影者 | James St. John |
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