Having just crossed over the main fault again, you can see the prominent fault features - the sag pond at your feet and the road-like bench upon which the fault markers are standing. The sag pond is filling in with sediment, and if you’re visiting during the dry months, it probably looks like a shallow depression. The trail you just traveled is on a slight ridge, higher than the sag pond. Rarely will you find ridges like this one running parallel to the contours, which are lines that connect two points that are at the same elevation. Usually these ridges follow the drainage down the hill. This is called a pressure ridge and is another fault feature.