Monte Cristo Range, Nevada magnitude 4.7 earthquake (1:16 PM, 15 February 2022) : 無料・フリー素材/写真
Monte Cristo Range, Nevada magnitude 4.7 earthquake (1:16 PM, 15 February 2022) / 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 Tinemaha seismic station in California. The noise was caused by a magnitude 4.7 earthquake that hit the Monte Cristo Range in western Nevada at 1:16 PM, local time, on 15 February 2022. The hypocenter was about 4 kilometers deep, which is a relatively shallow depth. Shaking resulted from strike-slip motion along a ~north-south trending fault zone or an east-northeast to west-southwest trending fault zone. This earthquake was part of ongoing seismic activity in the Monte Cristo Range-Candelaria Hills-Excelsior Mountains area of Nevada. A strong quake of magnitude 6.5 occurred in the Monte Cristo Range in mid-May 2020 (see: www.flickr.com/photos/jsjgeology/49898666476 ).--------------------------------Info. at:earthquake.usgs.gov/earthquakes/eventpage/nn00833903/exec...--------------------------------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 | 2022-02-16 03:35:48 |
| 撮影者 | James St. John |
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