180 likes | 283 Views
Earthquake Lab:. S. The lag time for St. Louis is 21 seconds. P. Features associated with the San Andreas Fault. Fault Scarps Steep mountain fronts Offset streams (Dogleg streams) Sag ponds and lakes Valleys in fault zones Changes in rock type. Offset fence Point Reyes.
E N D
S The lag time for St. Louis is 21 seconds P
Features associated with the San Andreas Fault • Fault Scarps • Steep mountain fronts • Offset streams (Dogleg streams) • Sag ponds and lakes • Valleys in fault zones • Changes in rock type
Offset fence Point Reyes
Fault Scrap Central California scarp Linear valley Linear ridge Offset stream
Spot the clues that would tell a geologist if she was walking in this area that a fault-line is here. Color in rock types Tc,and Tnv What do they tell you? When did these fault-lines roughly last move? Using Tnv, calculate the speed of movement since the middle of the eocene.
Qos Tnv Tnv Tnv
A. Seismicity (1969-89) before Loma Prieta San Jose could be next! B. Loma Prieta earthquake and aftershocks