Blanco Transform Fault magnitude 6.0 earthquake (11:15 AM, 30 October 2024) : 無料・フリー素材/写真
Blanco Transform Fault magnitude 6.0 earthquake (11:15 AM, 30 October 2024) / 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 is a seismogram from the Corvallis seismic station in Oregon, USA. The noise is from a magnitude 6.0 offshore earthquake west of Oregon. The quake hit at 11:15 AM, local time, on 30 October 2024. The epicenter was about 291 kilometers ~west of Oregon Dunes. Shaking resulted from right-lateral slip along a ~west-northwest to east-southeast striking fault zone.The quake occurred along the Blanco Transform Fault (often mis-referred to as the Blanco Fracture Zone - fracture zones are extensions of transform faults away from mid-ocean ridges). The Blanco Transform Fault forms part of the boundary between the Juan de Fuca Plate and the Pacific Plate. Transform plate boundaries involve two tectonic plates sliding past each other, usually in the form of sudden jolts.The quake occurred close to an Earth-Moon-Sun alignment.--------------------------------Info. at:earthquake.usgs.gov/earthquakes/eventpage/us7000np33/exec...anden.wikipedia.org/wiki/Blanco_Fracture_Zone--------------------------------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 | 2024-10-30 19:07:52 |
| 撮影者 | James St. John |
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