6.3 Richter scale quake - undersea - slightly South of Lyttleton Harbour off Banks Peninsular, which is a few kilometresSouth-East of the centre of Christchurch on the South Island of New Zealand.
The point is the epicentre of the earthquake.
The Christchurch earthquake was a magnitude of 6.3
Its epicentre
The epicentre of an earthquake is the point on the earth's surface away from which the seismic waves produced by an earthquake radiate. This is similar to the way waves or ripples in a pond move outwards in concentric circles from the point where you throw a stone into the water. As such the epicentre is the point on the earth's surface directly above the earthquake's focus or hypocentre (the point within the earth where the fault rupture or movement actually occurs).
It's very possible that Christchurch could have another earthquake. However, the possibility is low, as Christchurch had no major earthquake before the earthquake in 2010.
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The recent Christchurch Earthquake hit on 22nd February at 1:24pm
just near Market Rasen in Lincolnshire
RECENT AND HUGE On the 4th of September 2010 there was an earthquake magnitude 7.1 in Christchurch and then on 22nd of Febuary there was a 6.3 earthquake inb Christchurch
The epicentre was near charing cross just south-east of Darfield. to find out the time size and locayon +depth ot all tremers go to geonet .co.nz
169 people confirmed dead
The point is the epicentre of the earthquake.
New Zealand sits on a fault line, so earthquakes are relatively frequent. The devastating earthquake in February 2011 affected Christchurch and the surrounding Canterbury region at the southern end of the South Island. The epicentre occurred at Lyttelton, a small town on the harbour not far from Christchurch.
The Christchurch earthquake was a magnitude of 6.3
Its epicentre
The underground centre of an earthquake is the Hypocentre or focus.
The epicentre of an earthquake is the point on the earth's surface away from which the seismic waves produced by an earthquake radiate. This is similar to the way waves or ripples in a pond move outwards in concentric circles from the point where you throw a stone into the water. As such the epicentre is the point on the earth's surface directly above the earthquake's focus or hypocentre (the point within the earth where the fault rupture or movement actually occurs).