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• '''Figure 49''' Stage 1: Deposition of the Delafield Member as a series of coalescing deltas during the onset of a glacial stage as the sea level began to fall. The product is a thick succession of clastic rocks that coarsen upward.  +
• '''Figure 50''' Stage 2: Channel incision of delta sediments.  +
• '''Figure 51''' Stage 3: The Galatia channel developed a meander belt.  +
• '''Figure 52''' Stage 4: The change to a humid climate caused the Springfield peat to begin to form.  +
• '''Figure 53''' Stage 5: Springfield peat accumulates across a large area of the basin.  +
• '''Figure 54''' Stage 6: A warming climate brought rapid melting of the glaciers and a sea-level rise. The Galatia channel became an estuary, subject to strong tidal currents.  +
• '''Figure 55''' Stage 7: Peat swamps drowned as the estuary became an embayment. Dykersburg sediments rapidly buried the peat.  +
• '''Figure 56''' Stage 8: As the transgression continued apace, the entire basin area was submerged in deep water, which became stratified and anoxic, and black mud (Turner Mine Shale) was deposited.  +
• '''Figure 57''' Stage 9: Normal marine circulation resumed near the apex of an interglacial stage (marine highstand), bringing a brief interlude of carbonate sedimentation (St. David Limestone).  +
• '''Figure 58''' Stage 10: Marine regression begins the next cycle.  +