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  2. Earthquake environmental effects - Wikipedia

    en.wikipedia.org/wiki/Earthquake_environmental...

    Earthquake environmental effects are divided into two main types: Coseismic surface faulting induced by the 1915 Fucino, Central Italy, earthquake. Primary effects: which are the surface expression of the seismogenic source (e.g., surface faulting), normally observed for crustal earthquakes above a given magnitude threshold (typically M w =5.5 ...

  3. Modified Mercalli intensity scale - Wikipedia

    en.wikipedia.org/wiki/Modified_Mercalli...

    The Modified Mercalli intensity scale (MM, MMI, or MCS) measures the effects of an earthquake at a given location. This is in contrast with the seismic magnitude usually reported for an earthquake. Magnitude scales measure the inherent force or strength of an earthquake – an event occurring at greater or lesser depth. (The "M w" scale is ...

  4. Environmental Seismic Intensity scale - Wikipedia

    en.wikipedia.org/wiki/Environmental_Seismic...

    Seismically induced ground effects of the 1805, 1930 and 1980 earthquakes in the Southern Apennines (Italy). Ital .J. Geosci., 126, 2, 333–346. Serva L., E. Esposito, L. Guerrieri, S. Porfido, E. Vittori, V. Comerci (2007) Environmental effects from five historical earthquakes in southern Apennines (Italy) and macroseismic intensity ...

  5. Earthquakes happen all the time, you just can't feel them. A ...

    www.aol.com/earthquakes-happen-time-just-cant...

    About 55 earthquakes a day – 20,000 a year – are recorded by the National Earthquake Information Center.Most are tiny and barely noticed by people living where they happen. But some are strong ...

  6. What causes earthquakes? The science behind why seismic ... - AOL

    www.aol.com/causes-earthquakes-science-behind...

    Moderately damaging earthquakes strike between New York and Wilmington, Delaware, about twice a century, the USGS said, and smaller earthquakes are felt in the region roughly every two to three years.

  7. Medvedev–Sponheuer–Karnik scale - Wikipedia

    en.wikipedia.org/wiki/Medvedev–Sponheuer...

    No effect on objects. No damage to buildings. II. Hardly perceptible: Felt only by individuals at rest. No effect on objects. No damage to buildings. III. Weak: Felt indoors by a few. Hanging objects swing slightly. No damage to buildings. IV. Largely observed: Felt indoors by many and felt outdoors only by very few. A few people are awakened ...

  8. Seismic intensity scales - Wikipedia

    en.wikipedia.org/wiki/Seismic_intensity_scales

    Where an earthquake is not recorded on seismographs an isoseismal map showing the intensities felt at different areas can be used to estimate the location and magnitude of the quake. [1] Such maps are also useful for estimating the shaking intensity, and thereby the likely level of damage, to be expected from a future earthquake of similar ...

  9. Seismic risk - Wikipedia

    en.wikipedia.org/wiki/Seismic_risk

    The concepts of earthquake preparedness can help plan for emergencies arising from an earthquake. Building codes are intended to help to manage seismic risk and are updated as more is learned about the effects of seismic ground motion on buildings. This type of active improvement of mitigation of damage from earthquakes is known as seismic ...

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