What type(s) of eruptions are common on stratovolcanoes?
Very explosive and life threatening types of eruptions.
Stratovolcanoes tend to form in locations where the crust is being subducted below a continent. Partial melting of the descending slab goes on at a certain depth and the lighter felsic magma starts to rise up to the surface. When it breaks the surface, a stratovolcano forms, usually in a catastrophic fashion. See pic.
This explosive nature is due to the very viscous nature of the magma - this means it is very sticky and has a tendency to cool quickly and plug up. When it does get plugged and a rising magma section pushes through, it tends to be explosive (e.g volcanoes on the west coast of North America).
This is in contrast to the more shield type volcanoes where the magma is more viscous, tends to flow easily and does not get plugged up (e.g. the Hawaiian volcanoes).
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Stratovolcanoes commonly experience explosive eruptions due to the high viscosity of their magma. These eruptions involve a combination of gas, ash, and lava fragments. Additionally, effusive eruptions, characterized by the flow of relatively fluid lava, can also occur.
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When evaluating a one-sided limit, you need to be careful when a quantity is approaching zero since its sign is different depending on which way it is approaching zero from. Let us look at some examples.
When evaluating a one-sided limit, you need to be careful when a quantity is approaching zero since its sign is different depending on which way it is approaching zero from. Let us look at some examples.
When evaluating a one-sided limit, you need to be careful when a quantity is approaching zero since its sign is different depending on which way it is approaching zero from. Let us look at some examples.
When evaluating a one-sided limit, you need to be careful when a quantity is approaching zero since its sign is different depending on which way it is approaching zero from. Let us look at some examples.
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