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A fault in which the hanging wall has moved upward relative to the footwall
You can actually see where the rock layers moved on either side of the fault.
Most geologist consider a particular fault to be an active fault if it has moved during the past 10,000 years of the Holocene Epoch. An inactive fault is one that hasn't moved during the past 10,000 years of the Holocene Epoch.
The movement of the Hanging wall in the normal fault downward with the gravity whereas in the Reverse fault the hanging wall moved upward against the gravity
Fault rupture is 14km long along the southern edge of the city
A Fold (anticline or syncline) - but it is not a fault. A geological Fault is a break in the rock, with the rock on one side moved relative to that on the other..
Fault rupture is 14km long along the southern edge of the city
According to the book Natural Hazards, most geologist consider a particular fault to be an active fault if it has not moved during the past 10,000 years of the Holocene Epoch.
The terms you reference involve tectonic plates and fault lines or fault zones (transform fault).
According to the book Natural Hazards, most geologist consider a particular fault to be an active fault if it has not moved during the past 10,000 years of the Holocene Epoch.
The type of rock layers found on one side of the fault will either be repeated higher or lower on the other side of the fault. This proves that one side of a fault has moved (slipped).
The Christchurch fault line last moved on monday 13/03/13 at 7 pm. Eva is cool