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The Great Unconformity is the unconformity observed by John Wesley Powell in the Grand Canyon in 1869. It is an exceptional example of relatively young sedimentary rock strata overlying much older sedimentary or crystalline strata. The intervening period of geologic time is sufficiently long to raise the earlier rock into mountains which are then eroded…
Applications, Powell's Unconformity, Grand Canyon & Possible causes of the Great Unconformity
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unconformity great grand canyon september time rocks years last accessed 22 2013 powell's tonto group period rock vishnu basement strata
| Subject | Predicate | Object | Confidence | Src |
|---|---|---|---|---|
| Great Unconformity | is a | unconformity observed by John Wesley Powell in the Grand Canyon in 1869 | 0.90 | text |
| Great Unconformity | part of | a continent-wide unconformity that extends across Laurentia | 0.85 | text |
| Great Unconformity | has cause | There | 0.60 | section |
| Great Unconformity | has cause | One | 0.60 | section |
| Great Unconformity | has cause | Neoproterozoic | 0.60 | section |
| Great Unconformity | has cause | This | 0.60 | section |
| Great Unconformity | has cause | Snowball Earth | 0.60 | section |
| Great Unconformity | has cause | The | 0.60 | section |
| Great Unconformity | has cause | When | 0.60 | section |
| Great Unconformity | has cause | Cambrian | 0.60 | section |
| Great Unconformity | has cause | Neoproterozoic Snowball Earth | 0.60 | section |
| Great Unconformity | has cause | Alternatively | 0.60 | section |
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