Smith Volcano and Binintiang Malaki
Smith Volcano and Binintiang Malaki are different from other volcanoes because they are a part of a larger volcanic edifice, and they are actually cones made from pyroclastic materials. We call them pyroclastic cones or cinder cones.
What are cinder cones?
Cinder cones are a type of volcanic cones. They are also known as pyroclastic cones and scoria cones. It forms after a violent volcanic eruption, usually after the lava solidifies in the air and accumulates near the vent. Usually, the height of cinder cones varies from a few meters to hundreds of meters high.
Location of Smith Volcano
Smith Volcano is a cinder cone located near Babuyan Claro volcano, in the island of Babuyan in extreme northern Luzon. This volcano last erupted in 1924, and it is one of the most active volcanoes in the Babuyan Group of Islands.
Location of Binintiang Malaki
Binintiang Malaki is a cinder cone that formed in the northwestern edge of Taal Volcano Island. It is only 263 meters high, but it is known for violent eruptions. The last time an eruption took place in Binintiang Malaki was in 1715. Today, most of Taal Volcano’s activities are centered around the Main Crater.
For more information about volcanoes, please check the link below:
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