Which cross section best represents the general bedrock structure of New York State alleghenynplateau?

The general bedrock structure of the Allegheny Plateau in New York State is characterized by a series of gently folded and tilted sedimentary rock layers, primarily consisting of sandstone, shale, and limestone. These layers are typically arranged in a westward-dipping manner, reflecting the geological history of sediment deposition and subsequent tectonic activity. A cross section would show the alignment of these strata, along with features such as valleys and ridges formed by erosion. Overall, the structure highlights the region's complex geological processes and its rich Natural Resources.