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.
What is the relative age of a fault that cuts across three horizontal sedimentary rock layers?A. The fault is older than the middle layer. B.The fault is younger than all the layers it cuts across.C. The fault is the same age as the top layer. D. The fault is older than all the layers it cuts across == ==
the pppx
the pppx
fault-block mountain.
Fault lines are important in the formation of folded mountains because they serve as zones of weakness in the Earth's crust where rock layers can move and fold due to tectonic forces. When pressure builds along these fault lines, it can cause the rocks to bend and fold, eventually leading to the creation of folded mountain ranges. The movement along fault lines can uplift and deform the Earth's crust, resulting in the formation of complex folded mountain structures.
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.
What is the relative age of a fault that cuts across three horizontal sedimentary rock layers?A. The fault is older than the middle layer. B.The fault is younger than all the layers it cuts across.C. The fault is the same age as the top layer. D. The fault is older than all the layers it cuts across == ==
the pppx
the pppx
fault-block mountain.
A fault called a normal fault occurs when tectonic plates pull apart and tensional stress causes the rock layers to break and move along the fault line. In a normal fault, the hanging wall moves down relative to the footwall due to the extensional forces acting on the rocks.
Fault lines are important in the formation of folded mountains because they serve as zones of weakness in the Earth's crust where rock layers can move and fold due to tectonic forces. When pressure builds along these fault lines, it can cause the rocks to bend and fold, eventually leading to the creation of folded mountain ranges. The movement along fault lines can uplift and deform the Earth's crust, resulting in the formation of complex folded mountain structures.
Reverse Fault
A folded mountain. This type of mountain is formed by the folding of rock layers due to compressional forces in the Earth's crust, creating a series of folds and uplifted areas. Examples include the Appalachians in North America and the Zagros Mountains in the Middle East.
Probably reverse fault because folding is the result of compressional stres and reverse faults are caused by compression
Fault-block mountains. These are created when rocks along a fault are uplifted and tilted, forming steep mountain ranges with prominent peaks and valleys. An example of such mountains is the Sierra Nevada in California.
Fault