To determine the youngest geological feature based on the principles of original horizontality, superposition, and cross-cutting relationships, you should consider the following:
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Original Horizontality: Sedimentary layers are originally deposited in horizontal layers. If the layers are tilted or folded, that has happened after the deposition.
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Superposition: In an undisturbed sequence of rock layers, the oldest layers are at the bottom, and the youngest layers are at the top.
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Cross-Cutting Relationships: If a geological feature (like a fault or intrusion) cuts through another feature, the one that is cut is older than the one that is doing the cutting.
Without viewing the diagram and the specific features labeled with their corresponding letters, it would not be possible to determine the youngest feature. If you can provide further details about each feature's relationship with one another, I can help you analyze that information.