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Ignimbrite is a type of volcanic rock, consisting of a typically welded tuff. Ignimbrites form from the deposits of pyroclastic flows, which are a hot suspension of particles and gases flowing rapidly from a volcano, driven by being denser than the surrounding atmosphere. New Zealand geologist Patrick Marshall (1869–1950) coined the term ignimbrite from…
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ignimbrites tuff may flow volcanic welding rock pumice structures form density welded deposition en masse pyroclastic composition rheomorphic lower commonly
| Subject | Predicate | Object | Confidence | Src |
|---|---|---|---|---|
| Ignimbrite | is a | type of volcanic rock | 0.90 | text |
| Ignimbrite | is a | deposit | 0.90 | text |
| foliation | instance of | but more work needs to be carried out to discover if the majority of ignimbrites have these vertical variations in order to say which process is the most common.A model based on… | 0.80 | text |
| pyroclasts were formed during laminar viscous flow as the density current comes to a halt | instance of | but more work needs to be carried out to discover if the majority of ignimbrites have these vertical variations in order to say which process is the most common.A model based on… | 0.80 | text |
| pervasive foliation are a result of load compaction | instance of | Structures | 0.80 | text |
| and other structures are the result of remobilization by load | instance of | Structures | 0.80 | text |
| deposition on inclined topography | instance of | Structures | 0.80 | text |
| imbricate fiamme | instance of | and structures | 0.80 | text |
| observed in the Green Tuff | instance of | and structures | 0.80 | text |
| were the result of late stage primary viscous flow | instance of | and structures | 0.80 | text |
| imbricate fiamme | instance of | although the shear could be responsible for some of the structures | 0.80 | text |
| xenocrysts | instance of | but some may be exotic crystals | 0.80 | text |
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