Some volcanoes explode like popcorn in the microwave, while others just bubble like a pot on the stove. Let’s find out why!
What's Inside the Volcano?
Think of a volcano like a soda bottle, it has pressure inside it. When you shake it up and open it quickly, boom! It explodes like a fizzy eruption.
But if you just let it sit on the stove, it slowly bubbles and hisses, that’s more like a gentle volcano.
The Pressure Game
Some volcanoes have magma (hot melted rock) that's full of gas. When the pressure gets too high, kapow! It explodes, like when you pop a balloon with your finger.
Other volcanoes are more laid-back. Their magma is slower and calmer, so they just bubble and ooze out, like a lava lamp slowly changing colors.
So it’s all about pressure and how fast things move inside the volcano. Some go boom, others just bloop!
Examples
- A volcano with thick, sticky lava might explode, while one with runny lava just bubbles.
- Imagine a cake batter versus honey, the thicker one is harder to pour out.
- Mount Vesuvius exploded because of its thick magma, but Kilauea only gently flows.
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See also
- What is Volcanic ash?
- What Makes Volcanoes Erupt?
- What Causes the ‘Ring of Fire’ Volcanic Activity?
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- Are 19.6 pounds of CO2 produced from burning a gallon of gasoline?
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