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There are three. From smallest to largest, they are: Cinder Cones, Composite Volcanoes (also called Strata Volcanoes), and then Shield Volcanoes.
Earth, Venus and Mars all have volcanoes.
Two examples of composite volcanoes are Mount St. Helens in the United States, which had a major eruption in 1980, and Mount Fuji in Japan, which is an iconic stratovolcano known for its symmetrical cone shape.
Those are known as stratovolcanoes or composite volcanoes. They are formed by alternating layers of lava and ash during periodic eruptions, resulting in a steep-sided cone shape. These types of volcanoes are commonly found at subduction zone boundaries.
The two main types of cone volcanoes are stratovolcanoes and cinder cone volcanoes. Stratovolcanoes are large, steep-sided volcanoes composed of layers of lava flows, ash, and volcanic rocks. Cinder cone volcanoes are smaller, symmetrical volcanoes formed from pyroclastic material ejected during eruptions.
There are three. From smallest to largest, they are: Cinder Cones, Composite Volcanoes (also called Strata Volcanoes), and then Shield Volcanoes.
Cone volcanoes are typically the tallest and largest. The two other types of volcanoes are shield volcanoes and composite volcanoes.
Earth, Venus and Mars all have volcanoes.
Mauna Loa, and Kilauea.
Two examples of composite volcanoes are Mount St. Helens in the United States, which had a major eruption in 1980, and Mount Fuji in Japan, which is an iconic stratovolcano known for its symmetrical cone shape.
mount Shasta and Lassen peak
Aetna, Vesuvius, Stromboli, etc..
Those are known as stratovolcanoes or composite volcanoes. They are formed by alternating layers of lava and ash during periodic eruptions, resulting in a steep-sided cone shape. These types of volcanoes are commonly found at subduction zone boundaries.
No. A prime number has exactly two different factors. A composite number has more than two different factors.NO. A number cannot be both prime and composite.
BartharbungaEyjafjallajokullGrimsvotnHeklaKatlaThese are all on Iceland.
The two main types of cone volcanoes are stratovolcanoes and cinder cone volcanoes. Stratovolcanoes are large, steep-sided volcanoes composed of layers of lava flows, ash, and volcanic rocks. Cinder cone volcanoes are smaller, symmetrical volcanoes formed from pyroclastic material ejected during eruptions.
An ash and cinder volcano, also known as a cinder cone, is typically smaller in size and composed of loose volcanic fragments like ash and cinders. In contrast, a composite volcano, or stratovolcano, is larger, more symmetrical, and made up of alternating layers of lava flows and volcanic ash. Additionally, composite volcanoes have more explosive eruptions compared to ash and cinder volcanoes.