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  2. Epicentral distance - Wikipedia

    en.wikipedia.org/wiki/Epicentral_distance

    Epicentral distance refers to the ground distance from the epicenter to a specified point. [1] Generally, the smaller the epicentral distance of an earthquake of the same scale, the heavier the damage caused by the earthquake. On the contrary, with the increase of epicentral distance, the damage caused by the earthquake is gradually reduced. [2]

  3. Epicenter - Wikipedia

    en.wikipedia.org/wiki/Epicenter

    The Láska's empirical rule provides an approximation of epicentral distance in the range of 2,000−10,000 km. Once distances from the epicenter have been calculated from at least three seismographic measuring stations, the point can be located, using trilateration .

  4. Travel-time curve - Wikipedia

    en.wikipedia.org/wiki/Travel-time_curve

    Travel-time curve is a graph showing the relationship between the distance from the epicenter to the observation point and the travel time. [2] [3] Travel-time curve is drawn when the vertical axis of the graph is the travel time and the horizontal axis is the epicenter distance of each observation point. [4] [5] [6]

  5. Surface-wave magnitude - Wikipedia

    en.wikipedia.org/wiki/Surface-wave_magnitude

    The formula to calculate surface wave magnitude is: [3] = ⁡ + (), where A is the maximum particle displacement in surface waves (vector sum of the two horizontal displacements) in μm, T is the corresponding period in s (usually 20 ± 2 seconds), Δ is the epicentral distance in °, and

  6. Modified Mercalli intensity scale - Wikipedia

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

    It generally diminishes with distance from the earthquake's epicenter, but it can be amplified in sedimentary basins and in certain kinds of unconsolidated soils. Intensity scales categorize intensity empirically, based on the effects reported by untrained observers, and are adapted for the effects that might be observed in a particular region ...

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