Final answer:
Contact metamorphism occurs due to high temperature and low pressure when magma intrudes pre-existing rock, leading to different metamorphic facies based on pressure conditions.
Explanation:
Contact metamorphism occurs in rock exposed to high temperature and low pressure when hot magma intrudes or lava flows over pre-existing rock. This process produces various metamorphic facies such as hornfels, greenschist, amphibolite, or granulite facies based on pressure conditions. Contact metamorphism is associated with the heat from magma chambers and occurs at shallower depths, resulting in fine-grained rocks lacking foliation.
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