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http://www.answers.com/ > http://www.answers.com/main/what_content.jsp > http://www.answers.com/main/words.jsp > http://www.answers.com/library/Dictionary-cid-29095 (Click to enlarge) fault
normal fault
reverse fault
strike-slip fault
(Precision Graphics) n.
[Middle English faulte, from Old French, from Vulgar Latin *fallita, from variant of Latin falsa, feminine past participle of fallere, to deceive, fail.]
Faulting occurs in all three of these
Up and down faulting can also be called normal faulting or graben faulting, depending on the specific geological context. These terms refer to the movement of rock blocks along faults, where one block moves downward relative to the other.
Faulting is caused by the stretching or compression of rock by tectonic plate movements
The three different types of rock movement in earthquakes are normal (extensional) faulting, reverse (compressional) faulting, and strike-slip (lateral) faulting. Normal faulting occurs when rocks are pulled apart, reverse faulting involves rocks being pushed together, and strike-slip faulting involves horizontal movement along a fault line.
The two main types of faulting are normal faulting, where the hanging wall moves down relative to the footwall, and reverse faulting, where the hanging wall moves up relative to the footwall.
The hanging wall is the block of rock that lies above an inclined fault plane or dip in the Earth's crust. It moves down relative to the footwall during faulting or mining activities.
when a trent is created
yes, they can
faulting
there is faulting
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Faulting is important to humans because it can lead to the formation of valuable resources like mineral deposits or groundwater reservoirs. Additionally, faulting plays a key role in the movement of tectonic plates, which can cause earthquakes and tsunamis, impacting human populations and infrastructure. Understanding faulting is crucial for assessing and mitigating geological hazards in areas prone to tectonic activity.