If site Bran were buried more deeply and compacted over time, how would its porosity and rock stability likely change?
If a strong flood event deposited an additional coarse layer on the Lorn site, how might this change the site's overall stability?
If the environment that formed S3 experienced a gradual decrease in transport energy over time, what long-term change would likely occur in the rock's structure?
Why does S2 show a fractured structure compared with the other formations?
What trend can be inferred between transport energy and the observed structural condition of the formations?
If the alpine streambed environment continued to experience rapid deposition, how would that likely affect the rate of lithification?
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