The Windhoek area in Namibia is characterized primarily by normal faults, which are associated with tectonic extension. These faults are part of the larger geological framework of the region, influenced by the East African Rift system. The presence of these faults can lead to significant geological features, such as rift valleys and associated sedimentary basins. Additionally, some areas may exhibit minor strike-slip faults due to lateral tectonic movements.
A fault that occurs on folded rock layers is likely to be a thrust fault, where one block of rock is pushed up and over the other. This type of fault is common in areas where horizontal compression forces have folded the rock layers.
It is a strike-slip fault.
Strike-slip faults are the most common fault type around the San Andreas Fault.
Normal Fault
The fault type is a normal fault, called the Spirit Lake Fault, and it runs approximately 9 miles to the north of Mount St. Helens.
If a fault occurs in an area where rock layers have been folded, the type of fault it is likely to be is thrust faulting. This type of fault will have the ground on one side of the fault, move up and over adjacent ground.
A: raid 0raid 0 is no fault tolerance...coz it writes the data parallely and it doesnot contain any mirror in that.
The Hayward Fault is a Strike-slip Fault.
A fault that occurs on folded rock layers is likely to be a thrust fault, where one block of rock is pushed up and over the other. This type of fault is common in areas where horizontal compression forces have folded the rock layers.
hgvuygyug
It is a strike-slip fault.
a strike slip fault
Probably reverse fault because folding is the result of compressional stres and reverse faults are caused by compression
The Hayward Fault is a Strike-slip Fault.
The Owens Valley fault is a normal fault
Strike-slip faults are the most common fault type around the San Andreas Fault.
reverce fault.....