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For many rocks, the only real A part of the P-T path recorded from the mineral assemblage and texture of your rock would be the 'peak' of metamorphism -- the ailments of your thermal highest (i.e., the maximum temperature and the pressure at the utmost temperature). Should the rock had a sedimentary or volcanic protolith, you are able to infer the rock started off in the surface, reached peak conditions at some temperature and depth inside the Earth, and returned on the floor (where by the rock was collected).
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Consequently, The form of the path, combined with time facts, offers information regarding the driving forces
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