California "faults" tend to be (locally) very small across - One visible section of the San Andres north of San Francisco is visible in a road cut on the north of Golden Gate as a band of crushed rock less than 4 feet across. But across the whole valley, multiple "strings" of faults and segments are often found. The fault zone movement (of high displacement sideways) is much more than just the distance across the fault line itself - and that fault line may have dozens - if not hundreds - of individual "faults" that make up the whole "line"
Liquefaction is a very, very localized effect in landfill areas, and even more so on slopes where the hill slumps in 100 - 150 circles. Is stable for 1/4 mile, then slumps again. A few rains later, another hill (otherwise looking identical) slumps nearby - but then stays still for ten years.
In the 1989 earthquake when several buildings sunk their first and second floors into the land fill on the Bay side of the city, one building sunk 15 feet. the one next door did not move.