Final answer:
Given the information you provided, the weathering apparent in the 360° photo of the Stone Foundation in Wisconsin is likely due to Exfoliation. This type of weathering, common in Wisconsin's freeze-thaw cycles, is supported by similar conditions observed in Gale Crater imagery.
Step-by-step explanation:
The type of weathering seen at the Stone Foundation in Wisconsin, given the context of your 360° photo, likely suggests Exfoliation. This is a geologic process where rocks crack, often forming series of shells that look like the layers of an onion.
It can happen when the pressure exerted by overlying material has been removed due to erosion or excavation. In Wisconsin, this process is common due to the state's freeze-thaw cycles, adding weight to the identification of exfoliation. Furthermore, Gale crater images by Curiosity rover show sedimentary rocks, which are often subject to exfoliation weathering as they are made up of layer upon layer of deposited sediment.
Learn more about Exfoliation