かさいりゅう
火砕流
1. pyroclastic flow
2. Pyroclastic flowA pyroclastic flow (also known scientifically as a pyroclastic density current) is a fast-moving current of superheated gas (which can reach temperatures of about 1,000 °C) and rock (collectively known as tephra), which reaches speeds moving away from a volcano of up to 700 km/h (450 mph). The flows normally hug the ground and travel downhill, or spread laterally under gravity. Their speed depends upon the density of the current, the volcanic output rate, and the gradient of the slope.
Read “Pyroclastic flow” on English Wikipedia
Read “火砕流” on Japanese Wikipedia
Read “Pyroclastic flow” on DBpedia
Read “Pyroclastic flow” on English Wikipedia
Read “火砕流” on Japanese Wikipedia
Read “Pyroclastic flow” on DBpedia
火災流 【かさいりゅう】
火災流: Irregular kanji usage.
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