where two continental plates collide
Igneous rock, and specifically basalt.
Xenoliths are blocks of older rock enclosed in a body of younger igneous rock.
Granite is most commonly found in continental crust areas, especially in mountain ranges and regions with a history of tectonic activity. It is also commonly found in areas with ancient rock formations that have undergone significant metamorphism.
Felsite is commonly found in areas with igneous rock formations, such as volcanic regions or mountainous areas. It can also be found in some metamorphic rock formations.
Rock salt crystallizes from halite, which is a mineral form of sodium chloride commonly found in sedimentary rocks.
the faul-block mountains are made of huge tilted blocks of rock that are separated from surrounding rock by fault
Tilted blocks are formed through the process of tectonic activity, such as mountain building or faulting. When layers of rock are subjected to stress and pressure, they can be uplifted or tilted at an angle. This can create distinct blocks or sections of land that are tilted relative to each other.
Tilted blocks of rock along mid-ocean ridges are caused by the process of seafloor spreading. As new oceanic crust forms at the ridge axis, it pushes older crust away, creating faults and fractures that result in the tilting of blocks of rock. This tilting is a result of the spreading and rifting of the crust as it moves away from the ridge axis.
A texture know as foliation is common in metamorphic rock and garnets are more commonly found in metamorphic rock than other rock types of the crust.
phosphorus is commonly found in the earths crust because it is a rock
sandstone
In granite rock
this questions answer is true they are tilted or folded.
Galena is a mineral. not a rock, but is commonly found emplaced in sedimentary rock from hydrothermal deposition in faults and fissures.
Galena is a mineral, not a rock, but is commonly found emplaced in sedimentary rock from hydrothermal deposition in faults and fissures.
These mountains form when faults or cracks in the earth's crust force some materials or blocks of rock up and others down. Instead of the earth folding over, the earth's crust fractures (pulls apart). It breaks up into blocks or chunks. Sometimes these blocks of rock move up and down, as they move apart and blocks of rock end up being stacked on one another.
Igneous rock, and specifically basalt.