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A pyroclastic flow, more broadly known as a pyroclastic density current, is a fast-moving current of hot gas and volcanic matter (collectively known as tephra) that flows along the ground away from a volcano. Pyroclastic currents travel at extremely high speeds and have extremely high temperatures.
Movements, Formation and movement of pyroclastic currents & Examples
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pyroclastic flow currents current flows water denser fluid eruption within density gravity volcanic ground volcano along material lighter known matter
| Subject | Predicate | Object | Confidence | Src |
|---|---|---|---|---|
| ridges | instance of | Their lower density sometimes allows surges to flow over higher topographic features or water | 0.80 | text |
| hills | instance of | Their lower density sometimes allows surges to flow over higher topographic features or water | 0.80 | text |
| rivers | instance of | Their lower density sometimes allows surges to flow over higher topographic features or water | 0.80 | text |
| and seas | instance of | Their lower density sometimes allows surges to flow over higher topographic features or water | 0.80 | text |
| Pyroclastic flow | has effect | Flow | 0.60 | section |
| Pyroclastic flow | has effect | Larger | 0.60 | section |
| Pyroclastic flow | has effect | Most | 0.60 | section |
| Pyroclastic flow | has effect | Flows | 0.60 | section |
| Pyroclastic flow | has effect | Pyroclastic | 0.60 | section |
| Pyroclastic flow | has effect | Temperatures | 0.60 | section |
| Pyroclastic flow | has effect | The | 0.60 | section |
| Pyroclastic flow | has effect | The Ancient Roman | 0.60 | section |
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