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  1. The "funnel" is the path through which magma, gases and ash are channeled during an eruption. While a standard crater is usually less than 1 km in diameter, its shape is defined by the balance between the upward force of the eruption and the downward pull of gravity on the loose volcanic debris (tepRead more

    The “funnel” is the path through which magma, gases and ash are channeled during an eruption. While a standard crater is usually less than 1 km in diameter, its shape is defined by the balance between the upward force of the eruption and the downward pull of gravity on the loose volcanic debris (tephra). If the eruption is extremely large and the summit collapses entirely, the funnel-shaped crater is replaced by a much larger, basin-like caldera. The funnel shape is the most common feature of “Cinder Cones” and “Stratovolcanoes” worldwide.

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  2. Magma is a "reducing" environment, meaning it lacks free oxygen. The gases released are those that were trapped in the Earth's interior since its formation or recycled through subduction. While nitrogen, hydrogen and carbon-based gases are common, oxygen only exists in the volcano as part of chemicaRead more

    Magma is a “reducing” environment, meaning it lacks free oxygen. The gases released are those that were trapped in the Earth’s interior since its formation or recycled through subduction. While nitrogen, hydrogen and carbon-based gases are common, oxygen only exists in the volcano as part of chemical compounds like CO2 or SO2. This is an important distinction in planetary science, as it shows that the early Earth’s atmosphere (formed by volcanic outgassing) was “anoxic” (lacked oxygen) until the evolution of cyanobacteria.

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  3. This high percentage of water vapor is what drives the explosiveness of many volcanoes. As magma rises toward the surface, the dissolved water turns into steam. This steam expands rapidly, shattering the magma into ash and powering the eruption column. This process is similar to opening a shaken botRead more

    This high percentage of water vapor is what drives the explosiveness of many volcanoes. As magma rises toward the surface, the dissolved water turns into steam. This steam expands rapidly, shattering the magma into ash and powering the eruption column. This process is similar to opening a shaken bottle of soda. Besides water vapor, the remaining 10-20% of gases include carbon dioxide and sulfur dioxide. The release of this water vapor over billions of years is one of the primary theories for how the Earth’s oceans were originally formed.

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  4. The Philippines sits on a complex "mobile belt" between the Philippine Sea Plate and the Eurasian Plate. This leads to the formation of multiple volcanic arcs, such as the Luzon arc. Famous active volcanoes like Mayon (known for its perfect cone), Taal and Pinatubo are all located here. The archipelRead more

    The Philippines sits on a complex “mobile belt” between the Philippine Sea Plate and the Eurasian Plate. This leads to the formation of multiple volcanic arcs, such as the Luzon arc. Famous active volcanoes like Mayon (known for its perfect cone), Taal and Pinatubo are all located here. The archipelago’s small landmass combined with its intense tectonic setting means that volcanic hazards are a constant part of life. While Indonesia has the highest total number of volcanoes, the density and frequency of activity in the Philippines make it a global “hotspot” for volcanology.

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  5. The Lipari Islands are a volcanic arc. Stromboli is the most famous because of its constant activity, but the island of Vulcano (from which we get the word "volcano") is also part of this group. These islands have been inhabited since ancient times and their volcanic activity has deeply influenced MRead more

    The Lipari Islands are a volcanic arc. Stromboli is the most famous because of its constant activity, but the island of Vulcano (from which we get the word “volcano”) is also part of this group. These islands have been inhabited since ancient times and their volcanic activity has deeply influenced Mediterranean mythology and science. Because they are easily accessible by sea, they have been studied for centuries, helping to establish the foundations of modern volcanology. The islands are now a UNESCO World Heritage site due to their unique geological phenomena.

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