Contact metamorphism generally occurs relatively close to the surface in a zone of contact between an intruding magma body and the country rock, which could be a sedimentary, igneous, or previously metamorphosed rock. Hornfels is a common resultant contact metamorphic rock.
The Geological process of metamorphosis takes geological time scales (except thermal contact metamorphosis - contact with lava) - It is not clear what you are asking but it is not metamorphosis.
In any given region, the youngest rocks are found closest to the surface. Stratigraphy, the study of layers, tracks each event during which rocks are laid down whether through sedimentation, volcanic activity or metamorphosis.
Contact metamorphism does not often produce the foliation caused by regional metamorphism
These will be metamorphic rocks:Regional metamorphosis occurs under heat and pressureThermal/contact metamorphosis occurs under heat only
metamorphosis
Metamorphosis caused by deep burial of a whole (regional) slab of rocks.
If sedimentary rock becomes intruded by a mass of magma in an igneous intrusion, it will turn into a metamorphic rock. The change takes place because of great pressure and intense heat.
igneous rocks change into metamorphosis rocks at extreme heat and pressure.
there were crystals
Mountains are made of many different rocks. Such as sedimentary, ingenious and metamorphosis rocks.
Crystals and minerals, but not fossils, as the intense pressure would have destroyed them (except in some rare contact metamorphic rocks).
Earth movements form metamorphic rocks by pressing, squeezing, and folding. Sometimes minerals are destroyed and new minerals are created