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welcome to glen tilt this valley in the grampian highlands contains some of the most important outcrops in world geology because it was here that james hutton established that granite is not deposited out of precipitating sea water but actually is an intrusive igneous rock nudge the lower glen the river cuts through well-layered sedimentary rocks well actually theyamp;#39;re made of sedimentary rocks theyamp;#39;ve been changed by the actual heat and pressure and recrystallized but you could still see the original layering and banding so thereamp;#39;s no dispute those were once deposited well underwater by the action of sedimentary processes but in the high ground at the head of the valley well we go up into the kingdoms where thereamp;#39;s a lot of granite and in the later part of the 18th century there was a debate as to the geological significance of granite in the earliest days of the science of geology some people thought that granite was the product of sedimentary processes