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This sample from the ruins of Rome, was obtained by the ancient Romans from the French Pyrenees. It was known to the Italian scalpellini as cipollino verde mandolato. The dark green/pale green/white colouring of this sample suggests that it is very probably from Pont de la Taule, an important source of cipollino mandolato in Roman times. Similar green nodular limestones, often just dark and light green, were obtained from other locations in the Pyrenees, most notably the Campan valley, which was to become the principle source in Medieval times and when the quarries reopened in the 17th century. Known variously as Campan vert, griotte vert, and vert moulin, this was used extensively in the Palace of Versailles, and was widely employed in the decoration of buildings worldwide in the late 19th and early 20th centuries. Quarrying at Espiadet in the Campan valley ceased late in the 20th century.
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