Almost a century after the 1906 earthquake, Stanford geophysicists have revisited San Francisco's ''Big One'' and now paint a new picture of a fault that was ready to go and that ruptured farther and faster than previously supposed.
Almost a century after the 1906 earthquake, Stanford geophysicists have revisited San Francisco's ''Big One'' and now paint a new picture of a fault that was ready to go and that ruptured farther and faster than previously supposed.