Without seeing what the features are it is difficult to know the correct answer. Someone would need to know what the features are to know which is may interrupt a volcano.
composite
The arenal volcano is a cindercone volcano not a composite.
Galeras is a Strato/Composite volcano because of it's gently sloping sides.
Mt. Etna is kind of a cross between a shield volcano and a composite volcano
No. The term compostie volcano describes a kind of volcano, not a kind of volcanic eruption. The Soufrière Hills on Montserrat is indeed a composite volcano, however, whether it is erupting or not.
composite
The arenal volcano is a cindercone volcano not a composite.
Galeras is a Strato/Composite volcano because of it's gently sloping sides.
Mt. Etna is kind of a cross between a shield volcano and a composite volcano
A stratovolcano is a type of volcano with steep sides composed of alternating layers of solidified lava flows, volcanic ash, and rocks. A composite volcano is another name for a stratovolcano, both refer to the same type of volcano.
No. The term compostie volcano describes a kind of volcano, not a kind of volcanic eruption. The Soufrière Hills on Montserrat is indeed a composite volcano, however, whether it is erupting or not.
Mount Mayon, the Phillipines, is a stratovolcano, or a composite volcano. The lava erupted has a high silica content and high viscosity, and is mainly andesitic. Mount Mayon is categorised as active, and is viewed as a 'perfect volcano' due to the symmetry of sides.
A composite volcano, also known as a stratovolcano, is typically large and symmetrical in shape. They are characterized by steep sides and a conical or dome-shaped appearance. These volcanoes are made up of alternating layers of lava, ash, and rock debris.
Stratovolcanoes, also known as composite volcanoes, are typically the steepest type of volcano. They are characterized by steep sides due to their alternating layers of lava flows, ash, and volcanic rocks. Examples of stratovolcanoes include Mount St. Helens in the United States and Mount Fuji in Japan.
The three main types of volcanoes are shield volcanoes, stratovolcanoes (composite volcanoes), and cinder cone volcanoes. Shield volcanoes have gently sloping sides and are formed by layers of lava flows. Stratovolcanoes are characterized by steep sides and explosive eruptions. Cinder cone volcanoes are small, steep-sided volcanoes built from explosive eruptions that eject fragmented rock.
It is a shield volcano, as it occurs on a divergent pllate boundary (constructive boundary)
The three main types of volcanoes are shield volcanoes, cinder cone volcanoes, and composite (or stratovolcanoes) volcanoes. Shield volcanoes have gently sloping sides and are formed by layers of lava, while cinder cone volcanoes are steep-sided with a conical shape and are made of pyroclastic material. Composite volcanoes are a mix of both lava and pyroclastic material, with a classic symmetrical cone shape.