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• File:C605-Figure-50.jpg  + ('''Figure 50''' Stage 2: Channel incision of delta sediments.)
• File:C605-Figure-51.jpg  + ('''Figure 51''' Stage 3: The Galatia channel developed a meander belt.)
• Galatia Channel:Model of Channel Development  + ('''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.)
• Galatia Channel:Figures  + ('''Figure 3''' Satellite image of the mouth of the Mississippi River showing natural levees and crevasse splays. Fron Earthstar Geographic SIO, © 2020.)

• File:C605-Figure-52.jpg  + ('''Figure 52''' Stage 4: The change to a humid climate caused the Springfield peat to begin to form.)
• Galatia Channel:Model of Channel Development  + ('''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.)
• Galatia Channel:Figures  + ('''Figure 3''' Satellite image of the mouth of the Mississippi River showing natural levees and crevasse splays. Fron Earthstar Geographic SIO, © 2020.)
• File:C605-Figure-53.jpg  + ('''Figure 53''' Stage 5: Springfield peat accumulates across a large area of the basin.)
• File:C605-Figure-54.jpg  + ('''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.)
• File:C605-Figure-55.jpg  + ('''Figure 55''' Stage 7: Peat swamps drowned as the estuary became an embayment. Dykersburg sediments rapidly buried the peat.)
• File:C605-Figure-56.jpg  + ('''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.)
• File:C605-Figure-57.jpg  + ('''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).)
• File:C605-Figure-58.jpg  + ('''Figure 58''' Stage 10: Marine regression begins the next cycle.)
• Galatia Channel:Channels and Cyclothems: A Summary Model  + ('''Figure 58''' Stage 10: Marine regression begins the next cycle.)