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Pyroclastic flows occur during explosive eruptions of volcanoes.
There are similarities and differences. Cinder cones are generally much smaller than shield volcanoes or stratovolcanoes. Like shield volcanoes, they primarily erupt basaltic lava. However, like stratovolcanoes they have steep slopes and are composed of material that has erupted into the air and been welded together.
Large explosive eruptions are generally characteristic of stratovolcanoes.
The type of volcano is a composite volcano.
some of the stratovolcanoes and thier locations are the same that are composite because composite and starto is the same
Pyroclastic flows occur during explosive eruptions of volcanoes.
There are similarities and differences. Cinder cones are generally much smaller than shield volcanoes or stratovolcanoes. Like shield volcanoes, they primarily erupt basaltic lava. However, like stratovolcanoes they have steep slopes and are composed of material that has erupted into the air and been welded together.
Large explosive eruptions are generally characteristic of stratovolcanoes.
The type of volcano is a composite volcano.
They are ugly
some of the stratovolcanoes and thier locations are the same that are composite because composite and starto is the same
Stratovolcanoes, also called composite volcanoes are generally not made of basalt. While they may occasionally produce basalt, much of their material is andesite or dacite.
in the chloroplasts
Sprimarily stratovolcanoes.
Composite volcanoes are also called stratovolcanoes. They may rise as much as 8,000 feet above their bases and are generally much taller and wider than regular volcanoes.
Mount St. Helens is generally regarded as an explosive volcano, but like most stratovolcanoes, it can produce both explosive and non-explosive eruptions.
Not necessarily. The most powerful eruptions generally come from stratovolcanoes. These can be very tall, but do not have to be. The second most powerful eruption of the Twentieth Century was the 1991 eruption of Mount Pinatubo. This volcano is not nearly as tall as other stratovolcanoes. The most powerful eruptions come from supervolcanoes that often fail to build into any sort of mountain.