Earth Systems Science
Contact metamorphism is the process of mineralogical and textural changes in rocks due to the heat from nearby molten rock or magma intrusions. This localized transformation occurs when existing rocks, called protoliths, are subjected to intense heat but not significant pressure, leading to changes primarily in the mineral composition and structure of the surrounding rock. The result is typically the formation of new minerals, often characterized by a distinctive texture known as 'hornfels.'
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