Galatia Channel:Discussion: Difference between revisions

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{{Galatia Channel Page}}
{{Galatia Channel Page}}
==Notes==
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[[Has parent page::Galatia_Channel:Evolution_of_a_Peat_-_Contemporaneous_Channel_-_The_Galatia_Channel,_Middle_Pennsylvanian,_of_the_Illinois_Basin| ]]
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{{#set:Prev_Page=Galatia Channel:Murphysboro Coal and Oraville Channel}}
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{{#set:Next_Page=Galatia Channel:Model of Channel Development}}
{{#set:Next_Page=Galatia Channel:Model of Channel Development}}

Revision as of 15:40, 14 July 2020

Discussion

Observations from mines and boreholes through the Galatia channel and related features, as well as similar channels associated with older and younger coal beds, indicate that the old model of a Mississippi-style delta having natural levees and crevasse splays is due for revision. Combined with a better understanding and climate influences not available to earlier workers, these observations lead to a new model of channel development that has connotations for larger concepts of cyclic sedimentation.

Model of Channel Development
Linkage of Climate and Eustasy
Peat Developed at Lowstand
Rapid Transgression, Gradual Regression
Relationship of Effingham and Galatia Channels

Primary Source

Nelson, W.J., S.D. Elrick, W.A. DiMichele, and P.R. Ames, 2020, Evolution of a peat-contemporaneous channel: The Galatia channel, Middle Pennsylvanian, of the Illinois Basin: Illinois State Geological Survey, Circular 605, 85 p., 6 pls.

References