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This video explores using strike lines to determine the strike and dip of beds on a geologic map. The map shows units A-F with topographic contours at 800, 900, and 1000 feet. The elevation starts to go uphill at 1000 feet, then reaches 1100 feet before going downhill at 900 feet. By following the rule of Vs, it is clear that the direction is uphill. The narrator visualizes hiking up through different elevations, noting that even though the downhill is tucked in, the overall trend is uphill.
