It would be on the sea bed, directly above the focus that would be under the sea bed, in the crust :)
It depends on the size of the earthquake. If it was just a very very minor shudder, then it would not make much of a tsunami, nor would it go very far. However, if there is an earthquake like the one that just hit Japan, then that could cross the pacific ocean.
that cant happen
onew
When the ocean bottom slipped, the tsunami went out from the epicenter in all directions. If there had been an island 30 meters high (100 feet) near the epicenter, the tsunami would have covered it. As it was the tsunami spread out as it went. Land close to the epicenter such as Ceylon, Thailand, and Western Indonesia, got hit the worst. When it got to Africa, the tsunami was about a meter high (3 feet). It was in between in the areas in between. Still, It went all the way from Indonesia to Africa because the earth moved so much.
We typically use the word "epicenter" when discussing earthquakes, so the lat/long of the epicenter would depend on the earthquake under discussion. You can see each of the recent earthquakes on the US Geological Survey's web page at the link below.
The three stations' rings that showed the distance from the epicenter and in that area would be where the epicenter is.
depends on the focus and epicenter depends on the focus and epicenter
Hello
That would be the epicenter.
It depends on the size of the earthquake. If it was just a very very minor shudder, then it would not make much of a tsunami, nor would it go very far. However, if there is an earthquake like the one that just hit Japan, then that could cross the pacific ocean.
No. The answer is, first the earth trembles (there is earthquake), and if that earthquake is in sea or ocean, the water would be quaked too. As a result tidal waves will be created.. and that is Tsunami
A tsunami is an ocean wave that is caused by an earthquake. It would occur after an earthquake.
The intensity would be higher near the epicenter.
Because that is where the energy of the earthquake is released. As the energy travels farther away from the epicenter, it is dissipated as mechanical force.
All other factors being equal, the seismic waves will be felt most strongly at or near to the epicentre of the earthquake.
The term that describes the point on the Earth's surface above the area where an earthquake originates is it's epicenter.
The simplified answer is that it works much in the same way you would determine the source of a sound (which is also in waves). Multiple measurements of the intensity are taken from different locations are used to triangulate an earthquake.