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The Neoproterozoic Chuar Group consists of 1,600 m (5,200 ft) of exceptionally well-preserved, unmetamorphosed sedimentary strata that is composed of about 85% mudrock. The Group is the approximate upper half of the Grand Canyon Supergroup, overlain by the thin, in comparison, Sixtymile Formation, the top member of the multi-membered Grand Canyon…
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group canyon chuar dolomite grand formation strata member kwagunt beds sandstone mudrocks walcott galeros arizona ma supergroup carbon members consists
| Subject | Predicate | Object | Confidence | Src |
|---|---|---|---|---|
| Chuar Group | Country | United States | 1.00 | infobox |
| Chuar Group | Named by | Walcott (1894) and Noble (1910, 1914) | 1.00 | infobox |
| Chuar Group | Named for | Chuar Canyon | 1.00 | infobox |
| Chuar Group | Other | dolomite and sandstone | 1.00 | infobox |
| Chuar Group | Overlies | Nankoweap Formation | 1.00 | infobox |
| Chuar Group | Primary | mudstone | 1.00 | infobox |
| Chuar Group | Region | Arizona, Utah | 1.00 | infobox |
| Chuar Group | Sub-units | Kwagunt Formation Galeros Formation | 1.00 | infobox |
| Chuar Group | Thickness | 1,600 m (5,200 ft) at maximum | 1.00 | infobox |
| Chuar Group | Type | Geological formation | 1.00 | infobox |
| Chuar Group | Underlies | Sixtymile Formation and, as part of the Great Unconformity, the Tapeats Sandstone | 1.00 | infobox |
| Chuar Group | Unit of | Grand Canyon Supergroup | 1.00 | infobox |
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