12:05 1 .11 5G maps.unomaha.community – Private VAIDW vaduty TVU IIIULUID VIUVUTIUII VUIU W xpression (the equivalent of the red line for th U cut by these faults. In the footwall of the lowe the footwall of the higher fault it is at an eleva the higher fault it is at 210 m elevation. Draw ontal bed as it is cut by these two faults. You e given contour lines. Remember that the foot- t, and the hanging wall is that above. 100 m 500 m N. 400 m 400 m 300 m 200 m 400 m ** 100 m 500 m 500 m 400 m 300 m 300 m 200 m 200 m 100 m 100 m geologic contact Map for option 1. e below the red lines are structure contours on phic contours. xpression (the implied trace of the fault at the provided). Finidng points where topogrpahic a alue cross is the key. Is the fault dipping abov al upper fault, 100 m directly/vertically ab

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12:05 1 .11 5G maps.unomaha.community – Private VAIDW vaduty TVU IIIULUID VIUVUTIUII VUIU W xpression (the equivalent of the red line for th U cut by these faults. In the footwall of the lowe the footwall of the higher fault it is at an eleva the higher fault it is at 210 m elevation. Draw ontal bed as it is cut by these two faults. You e given contour lines. Remember that the foot- t, and the hanging wall is that above. 100 m 500 m N. 400 m 400 m 300 m 200 m 400 m ** 100 m 500 m 500 m 400 m 300 m 300 m 200 m 200 m 100 m 100 m geologic contact Map for option 1. e below the red lines are structure contours on phic contours. xpression (the implied trace of the fault at the provided). Finidng points where topogrpahic a alue cross is the key. Is the fault dipping abov al upper fault, 100 m directly/vertically ab

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