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  • Conglomerate: The Sedimentary Rock of High-Energy Streams
    The sedimentary rock most likely to have been deposited in a very high-energy stream is conglomerate. Here's why:

    * High Energy: Conglomerate is formed from large, rounded clasts (rock fragments) that are cemented together. These large clasts require significant energy to be transported and deposited.

    * Stream Energy: Fast-flowing rivers with strong currents have the energy to carry large rocks, pebbles, and gravel.

    * Rounding: The rounded shape of the clasts in conglomerate is a result of the abrasion and collision that occurs as they are transported by the water.

    Other possibilities:

    While conglomerate is the most likely, other rocks could form in a high-energy stream:

    * Breccia: If the clasts are angular rather than rounded, it suggests rapid deposition and less time for rounding.

    * Sandstone: Fine-grained sandstone can form in high-energy streams, but the clasts will be smaller and more evenly sized than in conglomerate.

    In summary: Conglomerate is the best indicator of a very high-energy stream environment.

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