In a reverse or thrust fault or a nape.
Reverse fault
Reverse Fault
a reverse fault
Reverse fault
This a reverse or dip-slip fault.
Submersion zone, as described in the theory of plate techtonics.
The rocks that are forced up and over the rocks below the fault surface are referred to as "hanging wall" rocks. This occurs in a specific type of fault known as a thrust fault, where compressional forces cause the hanging wall to move upward relative to the footwall, which is the block of rock below the fault surface. This movement can result in significant geological features, such as mountain ranges.
This geological phenomenon is called overthrusting, where older rocks are pushed up and over younger rocks due to tectonic forces. It results in the older rocks being positioned above the younger ones.
In the rock cycle, rocks change into differant types of rocks over time. For example, igneous rocks might break into sediments that form sedimentary rocks.
Non-clastic rocks are formed through chemical and organic processes. Chemical rocks like limestone are formed when minerals in water precipitate out and accumulate. Organic rocks like coal are formed from the remains of plants and animals that are buried and compacted over time. These processes occur without the transportation and deposition of sediments like in clastic rocks.
The process that wears down rocks and makes them smoother over time is called erosion. This can occur through various mechanisms such as wind, water, ice, or the movement of other rocks. The continuous abrasion and breaking down of rock surfaces contribute to their smoothing over time.
Sedimentary rock forms after erosion and deposition occur. Erosion breaks down existing rocks into sediments that are then transported, deposited, and compacted over time to form sedimentary rocks.