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Wicander. The Changing Earth: Exploring Geology and Evolution, 2nd ed. Belmont: West Publishing Company, 1997.
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conditions across the sea floor. By mid-Mississippian time however, shallow-water carbonate deposition resumed, until the final
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The basal—that is, the lowest and oldest—units of the
Kaskaskia consist of clean
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the
Kaskaskia is well known for its widespread carbonate and
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strata, which in fact compose most of the rocks; the
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226:is a superb example of such evaporite deposits.
173:, and ended by mid-Mississippian time. A major
206:. These sandstones are followed by extensive
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229:Beginning in the middle to late Devonian,
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181:, called the "Wallbridge Unconformity".
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638:Carboniferous System of North America
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658:Canadian geologic formation stubs
643:Devonian System of North America
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560:This article about a specific
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177:separates it from the lower
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507:in the United States is a
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618:Devonian United States
198:belt to the east, the
169:, peaked early in the
165:that began in the mid-
648:Mississippian Series
628:Carboniferous Canada
249:late in the period.
235:Marcellus Formation
179:Tippecanoe sequence
135:Tippecanoe sequence
25:Stratigraphic range
19:Kaskaskia Sequence
159:Kaskaskia sequence
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266:(pp. 539–44)
163:cratonic sequence
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125:Absaroka sequence
39:389.0–323.2
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573:expanding it
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349:Terreneuvian
247:epeiric seas
233:such as the
231:black shales
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175:unconformity
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33:Serpukhovian
464:Guadalupian
359:Miaolingian
193:Appalachian
612:Categories
459:Cisuralian
396:Llandovery
319:Ordovician
253:References
243:regression
208:carbonates
200:Ozark Dome
189:sandstones
565:formation
505:formation
469:Lopingian
364:Furongian
216:evaporite
121:Underlies
354:Series 2
329:Devonian
324:Silurian
314:Cambrian
196:orogenic
167:Devonian
141:Location
131:Overlies
115:Sequence
411:Pridoli
401:Wenlock
339:Permian
245:of the
146:Country
427:Middle
406:Ludlow
380:Middle
262:
239:anoxic
224:Canada
186:quartz
161:was a
151:Canada
29:Emsian
422:Early
375:Early
569:stub
509:stub
432:Late
385:Late
260:ISBN
157:The
111:Type
47:PreꞒ
222:in
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97:Pg
41:Ma
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102:N
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72:C
67:D
62:S
57:O
52:Ꞓ
36:~
31:-
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