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An aulacogen is a failed arm of a triple junction. Aulacogens are a part of plate tectonics where oceanic and continental crust is continuously being created, destroyed, and rearranged on the Earth’s surface. Rift zones are places where new crust is formed. An aulacogen is a rift zone that is no longer active.
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| Subject | Predicate | Object | Confidence | Src |
|---|---|---|---|---|
| Aulacogen | is a | failed arm of a triple junction | 0.90 | text |
| Aulacogen | is a | rift zone that is no longer active | 0.90 | text |
| Aulacogen | is a | East African Rift or the Ottawa-Bonnechere Graben in Ontario and Quebec | 0.90 | text |
| Aulacogen | is a | Eocambrian rift system formed as a product of intracontinental rifting during the breakup of Pannotia | 0.90 | text |
| Aulacogen | is a | failed rift zone that was active during the Early Cambrian during the breakup of the supercontinent Rodinia and the opening of the Iapetus Ocean | 0.90 | text |
| Aulacogen | located in | southwestern Oklahoma and extends into northeastern Texas | 0.90 | text |
| the Mississippi River | instance of | These can later become the pathway for large river systems | 0.80 | text |
| Aulacogen | related to Characteristics | Aulacogens | 0.60 | section |
| Aulacogen | related to Characteristics | These | 0.60 | section |
| Aulacogen | related to Characteristics | Mississippi River | 0.60 | section |
| Aulacogen | related to Characteristics | The | 0.60 | section |
| Aulacogen | related to Characteristics | Because | 0.60 | section |
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