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The 35 pages that link to Pyroclastic flow, each with the reason it gives.

• StratovolcanoBroader topic: Explosive stratovolcano eruptions can generate flows that race down the slopes.

• Volcanic eruptionBroader topic: This highly destructive hazard can race down a volcano during explosive eruptions.

• VolcanismBroader topic: It is among the most destructive hazards of explosive volcanism.

• Lava flowCompared with: Unlike a lava flow, it can race down slopes and overwhelm areas with little warning.

• Lava domeNarrower topic: Dome collapse is one source of these lethal currents.

• LavaCompared with: Unlike lava, it is a turbulent mixture of gas and particles rather than a coherent molten flow.

• VolcanologyBroader topic: These currents are among the most destructive hazards produced by eruptions.

• TephraCompared with: Unlike airborne tephra fall, a pyroclastic flow transports fragments in a dense current.

• TuffRelated: Deposits from these currents commonly compact into welded or unwelded tuff.

• Granular flowBroader topic: It is a hazardous natural flow of particles suspended in gas.

• Mount PinatuboRelated: These flows swept down Pinatubo's slopes during the 1991 eruption.

• Yixian FormationRelated: Some researchers have proposed volcanic burial events as a cause of mass mortality in fossil beds.

• Explosive eruptionBroader topic: These currents can devastate areas close to an explosive eruption.

• KrakatoaRelated: Krakatoa’s pyroclastic flows crossed the sea and devastated nearby coastal areas.

• Mount TamboraRelated: These flows devastated settlements and landscapes around Tambora during the eruption.

• 1991 eruption of Mount PinatuboRelated: These flows devastated areas near the volcano during the 1991 eruption.

• Tibesti MountainsRelated: Explosive eruptions helped form the range’s volcanic deposits and calderas.

• Mount AsoRelated: Aso’s major explosive eruptions have produced these dangerous currents.

• 1883 eruption of KrakatoaRelated: Hot currents from the eruption crossed the strait and devastated coastal settlements.

• Lava fieldCompared with: Unlike a lava field, its deposit is made chiefly of fragmented material, not solidified molten rock.

• Mount MerapiRelated: Collapsing Merapi lava domes generate these destructive currents down the volcano’s slopes.

• 1902 eruption of Mount PeléeNarrower topic: The flow that devastated Saint-Pierre was the eruption’s principal killing mechanism.

• Mount ShastaRelated: Future eruptions could send these dangerous currents down Shasta’s flanks.

• AvachinskyRelated: Explosive eruptions at Avachinsky can generate flows hazardous to nearby slopes.

• Emi KoussiRelated: Explosive phases of the volcano’s history produced pyroclastic deposits.

• Minoan eruptionRelated: Pyroclastic flows spread across Thera during the eruption’s final stages.

• Complex volcanoRelated: Repeated flows can reshape slopes and bury earlier volcanic features.

• GalerasRelated: Such flows pose a severe danger during explosive activity at Galeras.

• Katia and Maurice KrafftNarrower topic: This lethal hazard killed the Kraffts and shaped public understanding of eruption danger.

• MayonRelated: Mayon’s explosive activity can send these currents down its slopes.

• MistiRelated: This lethal hazard is among the dangers assessed for communities near Misti.

• Mount AsamaRelated: Explosive activity at Asama can generate flows that threaten areas near the summit.

• Mount Tambora eruptionRelated: Pyroclastic flows devastated settlements on Sumbawa during the eruption.

• Mount UnzenRelated: Dome collapses at Unzen generated the lethal flows of June 1991.

• Volcán de ColimaRelated: Explosive eruptions at Colima can generate flows that threaten areas near the cone.