Surviving a pyroclastic flow
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PYROCLASTIC FLOW A pyroclastic flow is a fast-moving current of extremely hot gas, volcanic ash, and rock fragments that rushes down the slopes of a volcano during explosive eruptions. These flows can reach speeds of over 320 km/h and temperatures exceeding 1,000 °C, making them one of the most dangerous volcanic hazards. Unlike lava flows, pyroclastic flows can travel great distances, destroy everything in their path, and cause widespread devastation due to their speed, heat, and suffocating as
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Semeru has erupted, sending a large pyroclastic flow racing downslope — a fast-moving mix of hot ash, gas, and volcanic debris that’s among the most dangerous eruption types. Stay safe, East Java. 🙏 📹 Netijen via Wa #Semeru #Geology #GeologyPage #Volcanology #Indonesia #PyroclasticFlow | Geology Page
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