To determine which feature is the youngest among the ones labeled N, G, R, and H using the principles of original horizontality, superposition, and cross-cutting relationships:
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Original Horizontality: Layers of sediment are deposited horizontally. Any tilted or folded layers were altered after they were deposited.
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Superposition: In an undeformed sequence of sedimentary rocks, the oldest layers are at the bottom and the youngest are at the top.
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Cross-Cutting Relationships: If one geological feature cuts across another, the feature that is cut is older than the feature doing the cutting.
To identify the youngest feature, look for:
- Features that are at the top of the sequence in stratigraphic order.
- Any features that cut through others, indicating they formed later.
Without seeing the diagram, we cannot definitively answer which letter corresponds to the youngest feature, but you can apply the above principles to analyze the labeled features. Evaluate which feature is either on top of the sequence or cutting through another feature to determine which one is the youngest.