UTC time | 1882-11-08 19:30:00 |
---|---|
USGS-ANSS | ComCat |
Local date | November 7, 1882 |
Magnitude | Mfa 6.2, Mw 6.6±0.6 |
Epicenter | 40°30′N105°30′W / 40.5°N 105.5°W |
Areas affected | Northern Colorado United States |
Max. intensity | MMI VII (Very strong) |
The 1882 Fort Collins earthquake or Front Range earthquake measured Mw 6.6 and struck near Fort Collins, Colorado at 1:30 UTC on November 8, which was 18:30 on the November 7. [1] The earthquake occurred as the result of deformation within the Front Range and caused shaking as strong as Modified Mercalli intensity (MMI) VII (Very Strong). Shaking was felt as far away as Salt Lake City, Utah and Salina, Kansas. An aftershock struck locally at 04:45 on November 8 and was felt as far as Laramie, Wyoming and Meeker, Colorado. It is the largest earthquake in Colorado's history.
The Southern Rocky Mountains are still actively growing due to the Laramide orogeny. The Front Range accommodates some of this as a deformation front of the orogeny. Stresses in this region are generally northwest–southeast oriented. The causative fault of this specific earthquake is unknown, but other earthquakes such as the 1984 Wyoming earthquake struck at a depth of 20 km (12 mi). [2] [3]
The Mw 6.6 [a] earthquake struck at 01:30 on November 8 in UTC time, or 18:30 on November 7. The earthquake caused Modified Mercalli intensity (MMI) VII (Very Strong) shaking in various localities near in the Front Range urban corridor and was felt over an area of 470,000 km2 (180,000 sq mi). [2] Due to the sparseness of the epicentral region, very little is known about where exactly the earthquake occurred. [2] An aftershock of magnitude 4.5 to 5.0 was also felt in the urban corridor. [5] This earthquake is the largest known to have occurred in the state of Colorado. [4]
At the University of Colorado Boulder, plaster fell from the ceiling. In Denver, some bolts snapped and bent at an electric light plant. In La Porte, a wooden house suffered cracking. At Thompson, a house's walls were severely cracked and the plaster on some walls came off. Glass windows broke in Laramie. [4]
The Modified Mercalli intensity scale measures the effects of an earthquake at a given location. This is in contrast with the seismic magnitude usually reported for an earthquake.
The Laramide orogeny was a time period of mountain building in western North America, which started in the Late Cretaceous, 80 to 70 million years ago, and ended 55 to 35 million years ago. The exact duration and ages of beginning and end of the orogeny are in dispute. The Laramide orogeny occurred in a series of pulses, with quiescent phases intervening. The major feature that was created by this orogeny was deep-seated, thick-skinned deformation, with evidence of this orogeny found from Canada to northern Mexico, with the easternmost extent of the mountain-building represented by the Black Hills of South Dakota. The phenomenon is named for the Laramie Mountains of eastern Wyoming. The Laramide orogeny is sometimes confused with the Sevier orogeny, which partially overlapped in time and space.
The Laramie Mountains are a range of moderately high peaks on the eastern edge of the Rocky Mountains in the U.S states of Wyoming and Colorado. The range is the northernmost extension of the line of the ranges along the eastern side of the Rockies, and in particular of the higher peaks of the Front Range directly to the south. North of the range, the gap between the Laramie range and the Bighorn Mountains provided the route for historical trails, such as the Oregon Trail, the Mormon Trail, and the Pony Express.
The Sevier orogeny was a mountain-building event that affected western North America from northern Canada to the north to Mexico to the south.
The geology of the Rocky Mountains is that of a discontinuous series of mountain ranges with distinct geological origins. Collectively these make up the Rocky Mountains, a mountain system that stretches from Northern British Columbia through central New Mexico and which is part of the great mountain system known as the North American Cordillera.
The 1976 Guatemala earthquake struck on February 4 at 03:01:43 local time with a moment magnitude of 7.5. The shock was centered on the Motagua Fault, about 160 km northeast of Guatemala City at a depth of 5 kilometers (3.1 mi) near the town of Los Amates in the department of Izabal.
The Wyoming Craton is a craton in the west-central United States and western Canada – more specifically, in Montana, Wyoming, southern Alberta, southern Saskatchewan, and parts of northern Utah. Also called the Wyoming Province, it is the initial core of the continental crust of North America.
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On February 7, 2021, at 12:22 PM PST, an earthquake measuring Mww 6.0 struck Davao del Sur and Cotabato. The event registered a Modified Mercalli Intensity Scale (MMI) of VIII (Severe) with VII on the PHIVOLCS Earthquake Intensity Scale (PEIS).
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