We must know what portion of previous fieldwork is known from direct observation vs. interpretation. With maps, this distinction isn't clear most of the time. A perfect example of this is the concept of the “state-line fault,” resulting when two different geologists mapping two adjacent areas disagree on how the maps join. | We must know what portion of previous fieldwork is known from direct observation vs. interpretation. With maps, this distinction isn't clear most of the time. A perfect example of this is the concept of the “state-line fault,” resulting when two different geologists mapping two adjacent areas disagree on how the maps join. |