File:C605-Figure-37.jpg: Difference between revisions
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{{Galatia Channel Image | {{Galatia Channel Image | ||
|File name= | |File name=C605-Figure-37.jpg | ||
|image_no=Figure 37 | |image_no=Figure 37 | ||
|caption=Interpretive diagram showing sequential development of the Leslie Cemetery channel. (a) The Francisco channel is eroded and filled with sediment, largely sand. (b) Springfield peat accumulates in swale left by the abandoned channel. (c) Flowing water reoccupies the channel during the later stages of peat accumulation. Peat encroaches from the margins as the channel migrates laterally. (d) A marine incursion drowns the region and deposits black shale and limestone. Channel filling inverts the topography because of differential compaction. | |caption=Interpretive diagram showing sequential development of the Leslie Cemetery channel. (a) The Francisco channel is eroded and filled with sediment, largely sand. (b) Springfield peat accumulates in swale left by the abandoned channel. (c) Flowing water reoccupies the channel during the later stages of peat accumulation. Peat encroaches from the margins as the channel migrates laterally. (d) A marine incursion drowns the region and deposits black shale and limestone. Channel filling inverts the topography because of differential compaction. | ||
|page1=Other_Channels_Related_to_the_Galatia_Channel | |page1=Other_Channels_Related_to_the_Galatia_Channel | ||
}} | }} | ||
Revision as of 15:54, 11 July 2020
Figure 37 Interpretive diagram showing sequential development of the Leslie Cemetery channel. (a) The Francisco channel is eroded and filled with sediment, largely sand. (b) Springfield peat accumulates in swale left by the abandoned channel. (c) Flowing water reoccupies the channel during the later stages of peat accumulation. Peat encroaches from the margins as the channel migrates laterally. (d) A marine incursion drowns the region and deposits black shale and limestone. Channel filling inverts the topography because of differential compaction.
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| current | 19:29, 23 August 2023 |  | 1,535 × 1,872 (579 KB) | Alan.Myers (talk | contribs) |
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