Analyzing these layers of ash help scientists learn more about the rock columns in the three locations is c) Scientists can determine the age of the ash layer in one location and use that information to estimate the age ranges of matching sequences of rocks in other locations.
Scientists can determine the location of the volcano that erupted by comparing the thickness of the ash layer in each of the columns. While the thickness of the ash can provide some clues about the proximity to the volcano, it's not a definitive indicator and other factors like wind and terrain can also influence thickness.
Therefore, by dating the ash layer in one location using carbon-14, scientists can then use that age as a reference point to estimate the age ranges of rock layers containing similar ash deposits in the other locations. This allows them to establish relative timelines and potentially correlate rock sequences across different regions.**