Which is the most likely fault line in New Zealand?
The Wellington Fault, which extends up through the Hutt Valley, is widely considered the most likely one of these to fracture in the next hundred or so years. But it could be another fault either adjacent to Wellington (such as the Ohariu Fault) that fractures first, and it could either be in the near future or not for several hundreds of years.
Why does God still find fault in US?
For who [including myself] has [ever] resisted His will and purpose?” You will say to me, therefore, “Why then does he still find fault? For who resists his will? ” You will say to me, therefore, “Why then does He still find fault? For who can resist His will?” Thou wilt say then unto me, Why doth he still find fault? For who withstandeth his will?
When was the last time the Alpine Fault fractured?
Over many millions of years the uplift has totalled about 20,000 metres, but erosion has limited the mountain tops to less than 4000 metres. During the last 1000 years, the Alpine Fault has fractured four times, at intervals of about 150-350 years. The last fracture is widely believed to have been in 1717. So the maths is not comforting.
Is the Alpine Fault related to the Christchurch earthquake?
In a direct sense, it does not, in that neither the September 2010 or the February 2011 earthquake involved fracture of the Alpine Fault. But these earthquakes were related to the pressure exerted between the two great plates, of which the Alpine Fault is the most explicit sign.
Which is the best description of a normal fault?
normal fault – a dip-slip fault in which the block above the fault has moved downward relative to the block below. This type of faulting occurs in response to extension and is often observed in the Western United States Basin and Range Province and along oceanic ridge systems.
Where can I find a tour of the Hayward Fault?
The U.S. Geological Survey has a new website that offers a virtual tour of the Hayward fault.
Which is an example of a right lateral fault?
strike-slip fault – a fault on which the two blocks slide past one another. The San Andreas Fault is an example of a right lateral fault.
How is a thrust fault different from a reverse fault?
thrust fault – a dip-slip fault in which the upper block, above the fault plane, moves up and over the lower block. This type of faulting is common in areas of compression, such as regions where one plate is being subducted under another as in Japan. When the dip angle is shallow, a reverse fault is often described as a thrust fault.