6. Excessively explosive type of eruption of gas and pyroclastic, just like our Pinatubo Volcano in Zambales. 7. These eruptions take place along fissures, or long cracks, rather than a central vent....


6. Excessively explosive type of eruption of gas and pyroclastic, just like our Pinatubo<br>Volcano in Zambales.<br>7. These eruptions take place along fissures, or long cracks, rather than a central vent.<br>8. Characterized by tall eruption columns that reach up to 20 km high with pyroclastic flow<br>and ash fall tephra like that of Paricutin Volcano in Mexico.<br>Down<br>1.A periodic weak to violent eruption characterized by fountain lava, just like the Irazu<br>Volcano in Costa Rica.<br>4. Considered non-explosive eruptions. Very little pyroclastic material is produced.<br>15<br>16<br>

Extracted text: 6. Excessively explosive type of eruption of gas and pyroclastic, just like our Pinatubo Volcano in Zambales. 7. These eruptions take place along fissures, or long cracks, rather than a central vent. 8. Characterized by tall eruption columns that reach up to 20 km high with pyroclastic flow and ash fall tephra like that of Paricutin Volcano in Mexico. Down 1.A periodic weak to violent eruption characterized by fountain lava, just like the Irazu Volcano in Costa Rica. 4. Considered non-explosive eruptions. Very little pyroclastic material is produced. 15 16

Jun 11, 2022
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