Imagine you are hiking in or traveling through California landscapes viewing tilted layers of sedimentary rocks that are exhibit
ed on surrounding slopes. What were possible sources for the sediments in the rocks?
How did these dipping layers get lifted up there and then become exposed?
The burgess and Hoyt models both try to understand urban land use. Both models have the same assumptions (e.g all land is flat, the importance of centrality, and etc).
