MediaWiki API result

{
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            "*": "Subscribe to the mediawiki-api-announce mailing list at <https://lists.wikimedia.org/postorius/lists/mediawiki-api-announce.lists.wikimedia.org/> for notice of API deprecations and breaking changes."
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    "query": {
        "pages": {
            "419": {
                "pageid": 419,
                "ns": 0,
                "title": "Reel Limestone Member",
                "revisions": [
                    {
                        "contentformat": "text/x-wiki",
                        "contentmodel": "wikitext",
                        "*": "{{Editwithform}}\n{{Tree\n|category1=Paleozoic Erathem\n|category2=Pennsylvanian Subsystem\n|category3=Absaroka Sequence\n|category4=McLeansboro Group\n|category5=Missourian Series\n|category6=Bond Formation\n|category7=Limestone\n|tree1=McLeansboro Group\n|tree2=Bond Formation\n|tree3=Reel Limestone Member\n|tree21=Paleozoic Erathem\n|tree22=Pennsylvanian Subsystem\n|tree23=Missourian Series\n|tree31=Absaroka Sequence\n}}\n==Primary source==\nWillman, H. B., Elwood Atherton, T. C. Buschbach, Charles Collinson, John C. Frye, M. E. Hopkins, Jerry A. Lineback, and Jack A. Simon, 1975, Handbook of Illinois Stratigraphy: Illinois State Geological Survey Bulletin 95, 261 p.\n\n==Contributing author&#40;s&#41;==\nM. E. Hopkins and J. A. Simon\n\n==Name==\n\n===Original description===\nThe Reel Limestone Member of the Bond Formation (Worthen, 1875, p. 55).\n\n===Derivation===\nNamed for Reel's Corner, Wabash County, (NE? 8, 1S-12W).\n\n===Other names===\n\n===History&#47;background===\n\n==Type section==\n\n===Type location===\n\n===Type author&#40;s&#41;===\n\n===Type status===\n\n==Reference section==\n\n===Reference location===\n\n===Reference author&#40;s&#41;===\n\n===Reference status===\n\n==Stratigraphic relationships==\nThe Reel Limestone is the first limestone above the Shoal Creek Limestone and lies 85-100 feet above it. It is generally underlain by a thin, black fissile shale that directly overlies the Flannigan Coal.\n\n==Extent and thickness==\nThe Reel Limestone occurs in eastern and southeastern Illinois, and is 1-3 feet thick.\n\n==Lithology==\nThe Reel Limestone is dark gray.\n\n==Core&#40;s&#41;==\n\n==Photograph&#40;s&#41;==\n\n==Contacts==\n\n==Well log characteristics==\n\n==Fossils==\nThe Reel Limestone contains many small gastropods, pelecypods, brachiopods, and incrusting Foraminifera.\n\n==Age and correlation==\n\n==Environments of deposition==\n\n==Economic importance==\n\n==Remarks==\n\n==References==\nWORTHEN, A. H., 1875, Geology and paleontology: Geological Survey of Illinois, v. 6, 532 p.\n\n{{Codes\n|membercode=1950\n|geo_unit=--\n}}"
                    }
                ]
            },
            "649": {
                "pageid": 649,
                "ns": 0,
                "title": "Reelsville Limestone Member",
                "revisions": [
                    {
                        "contentformat": "text/x-wiki",
                        "contentmodel": "wikitext",
                        "*": "{{Editwithform}}\n{{Tree\n|category1=Paleozoic Erathem\n|category2=Mississippian Subsystem\n|category3=Gasperian Stage\n|category4=Kaskaskia Sequence\n|category5=Pope Megagroup\n|category6=West Baden Group\n|category7=Paint Creek Group\n|category8=Chesterian Series\n|category9=Ridenhower Formation\n|category10=Limestone\n|tree1=Pope Megagroup\n|tree2=West Baden Group\n|tree3=Paint Creek Group\n|tree4=Ridenhower Formation\n|tree5=Reelsville Limestone Member\n|tree21=Paleozoic Erathem\n|tree22=Mississippian Subsystem\n|tree23=Chesterian Series\n|tree24=Gasperian Stage\n|tree31=Kaskaskia Sequence\n}}\n==Primary source==\nWillman, H. B., Elwood Atherton, T. C. Buschbach, Charles Collinson, John C. Frye, M. E. Hopkins, Jerry A. Lineback, and Jack A. Simon, 1975, Handbook of Illinois Stratigraphy: Illinois State Geological Survey Bulletin 95, 261 p.\n\n==Contributing author&#40;s&#41;==\nElwood Atherton, Charles Collinson, and Jerry A. Lineback\n\n==Name==\n\n===Original description===\nThe Reelsville Limestone Member of the Ridenhower Formation (Malott, 1919, p. 10-11).\n\n===Derivation===\nNamed for Reelsville, Putnam County, Indiana.\n\n===Other names===\n\n===History&#47;background===\n\n==Type section==\n\n===Type location===\nThe type section of the Reelsville Limestone Member is on the Eel River, just south of Reelsville, where the member is 2.5 feet thick.\n\n===Type author&#40;s&#41;===\n\n===Type status===\n\n==Reference section==\n\n===Reference location===\n\n===Reference author&#40;s&#41;===\n\n===Reference status===\n\n==Stratigraphic relationships==\nThe Reelsville Limestone Member is the uppermost member of the Ridenhower Formation.\n\n==Extent and thickness==\n\n==Lithology==\nThe Reelsville is classified as a formation in Indiana. It is dominantly limestone but contains beds of shale. It is not differentiated in the type section of the Ridenhower Formation, and it has limited distribution in southeastern Illinois, mostly in subsurface. The ''Agassizocrinus cf. leavis'' Peak Zone is equivalent to the Reelsville Member.\n\n==Core&#40;s&#41;==\n\n==Photograph&#40;s&#41;==\n\n==Contacts==\n\n==Well log characteristics==\n\n==Fossils==\n\n==Age and correlation==\n\n==Environments of deposition==\n\n==Economic importance==\n\n==Remarks==\n\n==References==\nMALOTT, C. A., 1919, \"American Bottoms\" region of eastern Greene County, Indiana- a type unit in southern Indiana physiography: Indiana University Studies, v. 6, 61 p.\n\n{{Codes\n|membercode=4400\n|geo_unit=--\n}}"
                    }
                ]
            }
        }
    }
}