Fig. 431.—Contorted and faulted laminated rock. Cook Inlet. (Gilbert, U. S. Geol. Surv.)

Fig. 432.—Faulting shown in a cobblestone. The fault-planes have become veins by deposition from solution. The figure shows how the relative ages of crossing-faults may be determined. (Schrader, U. S. Geol. Surv.)

Fig. 433.—Figure showing minute faulting. The length of the specimen is 8 inches. The number of faults is nearly 100. (Photo. by Church.)

Fig. 434.

Fig. 435.