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Generally increase with depth, occasionally making abrupt jumps termed seismic-velocity discontinuities.
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The foci of an eclipse is 2.
subbduction zones
type of faulting depth frequency of shakin proximity of epicentre distance of earthquake focus magnitude
Generally increase with depth, occasionally making abrupt jumps termed seismic-velocity discontinuities.
Earthquake foci can be used to mark the earths plate boundaries . The movement along the plate boundary causes the earthquake. Knowing where the foci is can help predict future earthquakes in that scientists can monitor the area for shifts in the plates.
1 peanut butter and jelly sandwich plus a ham and cheese bagel. Equals a delicious lunch. This has ntohing to do with the foci. It's impossbibe.
tectonic plates.
The foci basically outline or emanate from the subducting slab (plate). Multiple foci locations can be used to tell the degree of dip/position of the subducting slab. The distribution patterns also give depth at which melting of slab occurs because earthquakes don't emanate from a partially melted slab, so the deepest earthquake may indicate last solid state of slab.
what is the maximum depth of a deep-focus earthquake
There is no way to answer this. The magnitude of an earthquake does not correlate with its depth.
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0 depth is the surface of the earth,and increasing depth is downwards
The distribution of earthquake with regard to the location and depth of focus can be best explained with tectonics.
Trifocal
230km