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Welcome back structural geology fans! Today is a big day as we hit on one of the most important skills for a field geologist; the ability to take measurements on structures and put these measurements on a map that lets other geologists know exactly what you saw out there. To begin, layers of rock are basically planes of rock, and faults and joints are basically planar breaks in rock, and even with a fold we can imagine a plane of symmetry, and thus measuring planar features is key to our science. A place on a plane can be described in just two intersecting lines, but we go a bit farther to not only say where we are on the map, for which you can go back to the beginning of this series to review latitude and longitude or the USPLS system to get your location, but today we are going to learn how to represent the orientation of any plane in 3d space at your location on the map. To do this, we use the concepts of strike and dip. A strike is defined as the direction of the line made by an in