Les Drazey is a lieu-dit north of the village of Chambolle-Musigny. The reddish-brown soil, 50 to 60 cm thick, contains a variety of blunt-to-rounded limestone fragments. The substratum at Les Drazey is formed of a variety of limestone fragments, cemented together by salmon-colored clayey limestone. This conglomerate rock is the result of major erosion that occurred as the topography of the Côte de Nuits took shape. Les Argillières is a lieu-dit southeast of the village of Chambolle-Musigny. The light-colored soil is not very stony and is about 40 to 50 cm thick. The underlying substratum of Les Argillières can be seen in a neighboring hollow (possibly an old clay mine).