The hypocentre (the point within the Earth where the rupture actually occurred) of the January 2010 earthquake was located at a depth of 13 km below the surface.
Assuming that you are referring to the earthquake that occured in January 2010, the focus or hypocentre (the point within the Earth where the rupture actually occurred) was located at a depth of 13 km below the surface. Please see the related question for further information.
The epicentre of an earthquake this the point in the earth where the earth moved (fractured) to cause the shaking of the ground. The 2010 Haiti earthquakes epicentre was located 15 miles WSW of Port-Au-Prince and was at a depth of 8.1 miles. it was a 7.0 magnitude earthquake.
Haiti is sandwiched north and south between two fault lines: the Septentrional Fault and the Enriquillo-Plantain Garden Fault. The epicenter of the Haitian earthquake of 12 January 2010 was 10 miles south of the capital Port Au Prince, directly on the Enriquillo-Plantain Garden Fault , at a depth of about 5.2 miles underground.
The focal depth of an earthquake is how far beneath the earth's surface the hypo-center of the earthquake.Because of its location in the Indian Ocean, however, its focal depth is measured as 30 kilometers below mean sea level, rather than being measured at the seabed.
The earthquake was so destructive for a number of reasons:The earthquake occurred at shallow depth - this means that the seismic waves have to travel a smaller distance through the earth to reach the surface so maintain more of their energy in particular this meant that the surface waves (which cause the vast majority of the damage during an earthquake ans which are the most rapidly attenuated and and have significant reductions in amplitude as the depth of the earthquakes focus increases) produced by the earthquake maintained a large amount of their energy maximising the damage they cause.The earthquake occurred in close proximity to a populated area. This again means that there is very little attenuation of the seismic waves (i.e they still have most of their energy and so are more destructive when they arrive).The buildings in Port-au-Prince and other areas of Haiti were in very poor condition in general and were not designed or constructed to be earthquake resistant.Please see the related question for further information.
The earthquake's epicentre (the point on the surface directly above the earthquake rupture zone) was 25 km WSW of the Haitian capital city, Port-Au-Prince. According to the US Geological Survey the exact co-ordinates were 18.457°N, 72.533°W. The hypocentre (the point within the Earth where the rupture actually occurred) was located at a depth of 13 km below the surface. Please see the related links and question.
The Christchurch earthquake that occurred in 2011 had a magnitude of 6.3. It caused widespread damage to buildings, infrastructure, and resulted in numerous casualties. The overall impact was significant due to the shallow depth of the quake and its proximity to urban areas.
The depth of focus of an earthquake with a magnitude of 7.2 can range from 10 to 700 kilometers below the surface of the Earth. At this depth, the earthquake originates within the crust or upper mantle, releasing energy that can cause significant shaking and damage near the surface.
Haiti's a very congested country, there are small buildings and houses as far as the eye can see. A 7.0 earthquake would crush any small structures in it's vicinity. Plus there were at least 52 aftershocks ranging from 4.5 up.The earthquake was so destructive for a number of reasons:The earthquake occurred at shallow depth - this means that the seismic waves have to travel a smaller distance through the earth to reach the surface so maintain more of their energy.The earthquake occurred in close proximity to a populated area. This again means that there is very little attenuation of the seismic waves (i.e they still have most of their energy and so are more destructive when they arrive).The buildings in Port-Au-Prince and other areas of Haiti were in very poor condition in general and were not designed or constructed to be earthquake resistant.
To completely describe where an earthquake started, you would need the coordinates of the earthquake's epicenter, the depth at which it originated within the Earth, and the fault line or tectonic plate boundary where the earthquake occurred. This information helps to pinpoint the exact location and provide insight into the geological context of the earthquake's origin.
approx 17km
700 km