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.

Applications and Investigations in Earth Science (9th Edition)
9th Edition
ISBN:9780134746241
Author:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Chapter1: The Study Of Minerals
Section: Chapter Questions
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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
Transcribed Image 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
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