Question

g Locate the epicenter of the 1906 quake. Does the amount of horizontal slip decrease faster along the northern end or the southern end of the rupture? (In other words, where does the amount of horizontal slip NOT increase along the rupture? The northern or southern end of the fault, in relation to the epicenter?)

Answer 1

In the 1906 earthquake along the San Andreas Fault, the epicenter was located near San Francisco. The amount of horizontal slip decreases faster along the northern end of the fault compared to the southern end. However, the rate of slip can vary along different sections of the fault.

Step-by-step explanation:

The San Andreas Fault in southern California is a transform boundary where the Pacific and North American plates slide past each other horizontally.

In the 1906 earthquake, the epicenter was located near San Francisco.

The amount of horizontal slip decreases faster along the northern end of the rupture.

This means that the amount of horizontal slip does not increase along the northern end of the fault, in relation to the epicenter.

However, it is important to note that the rate of slip can vary along different sections of the fault.