Steep reverse fault in dolomitic marble at the Jazida do Urubu. Drag folds near the foot of the face are well defined along the fault plane but less distinct above. Small crenulations conforming to the regional fold pattern appear in a dark layer in the face about 0.3 meter above the man's head. Minas Gerais, Brazil. 1957. Figure 21 in U.S. Geological Survey. Professional paper 341-F. 1965. Professional Paper-0341

Digital File:wrm00020