A reverse fault, my friend.
A reverse fault may form when rocks are compressed.
A normal fault may form when rocks are pulled apart. In a normal fault, the hanging wall drops down relative to the footwall due to tensional forces pulling the rocks apart.
a divergent boundry
Rocks being pulled apart are under tension. This is found at divergent plate boundaries. It is a tension fault.
Trust faults typically have low dip angles. A high-angle thrust fault is called a reverse fault. A reverse fault occurs primarily across lithological units where as a thrust usually occurs within or at a low angle to lithological units.
Geologists study fault lines by mapping the rocks on either side of the fault, looking at the geometry of the fault (such as its orientation and displacement), and analyzing the types of rocks and their characteristics. They may also use techniques like seismic reflection surveys, ground-penetrating radar, and drilling to understand the structures within the Earth's crust along a fault line.
Yes it can form an igneous rocks as because of pressure it may melt and form into igneous rocks.
Veins or dykes of minerals like quartz, calcite, or pyrite can form along cracks or faults in rocks. These mineral veins are known as 'veins' and are the result of precipitation of minerals from hot fluids circulating within the Earth's crust.
When plates move apart or diverge, it is called a normal fault (happens along a divergent boundary). When plates collide or converge, a reverse fault occurs (when the hanging wall pushes up, and the foot wall pushes down). When plates slide past each other, it is called a strike-slip fault, which typically occurs at a transform plate boundary.Also, if you are still having doubts, do more research on strike-slip faults, normal faults, and reverse faults by just typing it in.
Extrusive rocks form above the surface, cooling quickly and bearing a glassy or fine texture and may be vesicular. Intrusive rocks form below the surface and form slowly, giving it a coarse texture.
Some extrusive rocks such as lava and ejecta form in minutes. Stalactites may form in a few tens of years, but commonly longer. Other rocks may take millions of years, and may have to be recycled through metamorphism to attain their final form.
The burial process involving sedimentary rocks is usually characterized by the gradual accumulation of sediments over time. These sediments are compressed and cemented together to form rock layers, which can further undergo burial and lithification to become sedimentary rocks. This process may also involve tectonic forces that cause these rocks to be buried deeper within the Earth's crust.