Uniformly dipping rock strata () draw structure contours on the geological contacts. (ii) determine the dip of the beds. (iii) complete the cross section along the line yz. (iv) where you can see the top and bottom of the beds on the map (b, c, d and e) calculate the thicknesses of these beds. indicate an inlier and an outlier on the map. (v) 0 scale e.

Why might a single rock layer exhibit different types of sedimentary rocks within it? view available hint(s) why might a single rock layer exhibit different types of sedimentary rocks within it? such a rock layer, termed a facies, when traced laterally represents a variety of depositional environments that formed in a sequence over time. such a rock layer, termed a facies, when traced laterally represents a single depositional environment that formed over time. such a rock layer, termed a facies, when traced vertically represents a variety of depositional environments that formed at the same time across a broad area. such a rock layer, termed a facies, when traced laterally represents a variety of depositional environments that formed at the same time across a broad area. such a rock layer, termed a facies, when traced vertically represents a variety of depositional environments that formed in a sequence over time.