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Westminster Hall, Palace of Westminster was originally constructed in the 11th Century, mainly of Caen Stone, a fine grained Middle Jurassic limestone from Normandy. This limestone showed poor durability, and high susceptibility towards erosion and pollution damage.
Thus there has been a long history of regular restoration and repair using a wide variety of other limestones, many of which have themselves eroded. Continued modern repair has benefited from a scientific perspective re. identification of these stone types, their durability, and cause of decay.
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