Galatia Channel:Discussion: Difference between revisions
Jump to navigation
Jump to search
Alan.Myers (talk | contribs) No edit summary |
Alan.Myers (talk | contribs) No edit summary |
||
Line 16: | Line 16: | ||
{{Galatia Channel Page}} | {{Galatia Channel Page}} | ||
[[Has parent page::Galatia_Channel:Evolution_of_a_Peat_-_Contemporaneous_Channel_-_The_Galatia_Channel,_Middle_Pennsylvanian,_of_the_Illinois_Basin| ]] | [[Has parent page::Galatia_Channel:Evolution_of_a_Peat_-_Contemporaneous_Channel_-_The_Galatia_Channel,_Middle_Pennsylvanian,_of_the_Illinois_Basin| ]] | ||
{{#set:Prev_Page=Galatia Channel:Murphysboro Coal and Oraville Channel}} | {{#set:Prev_Page=Galatia Channel:Murphysboro Coal and Oraville Channel}} | ||
{{#set:Next_Page=Galatia Channel:Model of Channel Development}} | {{#set:Next_Page=Galatia Channel:Model of Channel Development}} |
Revision as of 15:39, 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
References