Aberdeen
Aberdeen's architecture is known for its principal use during the Victorian era of granite, which has led to its local nickname of the Granite City or more romantically the less commonly used name the Silver City, since the Mica in the stone sparkles in the sun. The hard grey stone is one of the most durable materials available and helps to explain why the city's buildings look brand-new when they have been newly cleaned and the cement has been pointed. Unlike other Scottish cities where sandstone has been used, the buildings are not weathering and need very little structural maintenance on their masonry. The buildings can however become noticeably darker as a result of pollution and grime accumulated over the years. There has however been great success in cleaning the buildings which can result in their façade being restored back to much how they looked originally.
Being sited between two river mouths, the city has little natural exposure of bedrock. This leaves local geologists in a slight quandary: despite the high concentration of geoscientists in the area (courtesy of the oil industry), there is only a vague understanding of what underlies the city. To the south side of the city, coastal cliffs expose high-grade metamorphic rocks of the Grampian Group; to the south-west and west are extensive granites intruded into similar high-grade schists; to the north the metamorphics are intruded by gabbroic complexes instead. The small amount of geophysics done, and occasional building-related exposures, combined with small exposures in the banks of the River Don, suggest that it is actually sited on an inlier of Devonian "Old Red" sandstones and silts. The outskirts of the city spread beyond the (inferred) limits of the outlier onto the surrounding metamorphic/ igneous complexes formed during the Dalradian period (approximately 480–600 million years ago) with sporadic areas of igneous Diorite granites to be found, such as that at the Rubislaw quarry which was used to build much of the Victorian parts of the city.
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