The best clear proof of tectonic forces we have is rock deformation. Folds and faults can be categorized, as other geological structures, and we learn from the classification that similar structures are formed by similar processes. We can learn to view the story left behind in the rock through the classification of the geological structures and understanding how they were formed. Actually, the secret to this understanding is geometry, which is the form and scale, and the orientation of folds, faults, and joints. It is not only the geological structures themselves, but also the erosion characteristics, the gaps in the geological record, that offer us information about the geological history of a given region.
For example, as erosion happened over a specific area, the material that was extracted from that region was placed somewhere else, so we could make correlations between the two regions by analyzing the sediments in one place and the missing record in another place.
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The best clear proof of tectonic forces we have is rock deformation. Folds and faults can be categorized, as other geological structures, and we learn from the classification that similar structures are formed by similar processes. We can learn to view the story left behind in the rock through the classification of the geological structures and understanding how they were formed. Actually, the secret to this understanding is geometry, which is the form and scale, and the orientation of folds, faults, and joints. It is not only the geological structures themselves, but also the erosion characteristics, the gaps in the geological record, that offer us information about the geological history of a given region.
For example, as erosion happened over a specific area, the material that was extracted from that region was placed somewhere else, so we could make correlations between the two regions by analyzing the sediments in one place and the missing record in another place.
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