As the Sherburne formation was being deposited, the distance to the shore of the sea likely fluctuated due to changes in sea level, sediment supply, and tectonic activity. During periods of higher sea levels, the shoreline would have been farther inland, while lower sea levels would have pushed the shore further out. Additionally, sediment accumulation from nearby rivers and coastal processes would have shaped the landscape, impacting the proximity of the shoreline over time. Overall, these dynamic processes would have led to significant changes in the distance to the shore throughout the deposition of the Sherburne formation.
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