The three types of volcanoes are shield volcanoes, stratovolcanoes (composite volcanoes), and cinder cone volcanoes. Shield volcanoes have gentle slopes and are formed by lava flows, stratovolcanoes are tall, steep-sided volcanoes built up by layers of hardened lava, rock, and ash, and cinder cone volcanoes are relatively small, steep-sided volcanoes made of pyroclastic material.
The Arenal Volcano is a cinder cone volcano
Volcano Pacaya in Guatemala is a complex stratovolcano, which means it is composed of layers of lava, ash, and other volcanic debris. It has a conical shape like a stratovolcano but has different types of eruptions like shield volcanoes.
A composite volcano, also known as a stratovolcano, is a tall, steep-sided volcano with alternating layers of solidified lava flows, volcanic ash, and other volcanic debris. They are characterized by explosive eruptions due to their high viscosity magma. Examples include Mount St. Helens and Mount Fuji.
Stratovolcanoes or composite volcanoes are tall conical mountains composed of lava flows and other ejecta in alternate layers, the strata that gives rise to the name. Stratovolcanoes are also known as composite volcanoes because they are created from multiple structures during different kinds of eruptions.
Cone volcanoes are typically the tallest and largest. The two other types of volcanoes are shield volcanoes and composite volcanoes.
The three types of volcanoes are shield volcanoes, stratovolcanoes (composite volcanoes), and cinder cone volcanoes. Shield volcanoes have gentle slopes and are formed by lava flows, stratovolcanoes are tall, steep-sided volcanoes built up by layers of hardened lava, rock, and ash, and cinder cone volcanoes are relatively small, steep-sided volcanoes made of pyroclastic material.
The Arenal Volcano is a cinder cone volcano
Volcano Pacaya in Guatemala is a complex stratovolcano, which means it is composed of layers of lava, ash, and other volcanic debris. It has a conical shape like a stratovolcano but has different types of eruptions like shield volcanoes.
No, Paricutin in Mexico is not a composite volcano; it is classified as a cinder cone volcano. Paricutin formed in a cornfield in 1943 and is characterized by its steep slopes and conical shape, typical of cinder cone volcanoes. Composite volcanoes, on the other hand, are usually larger, have more complex structures, and are formed from alternating layers of lava flows, ash, and volcanic rocks.
A composite volcano, also known as a stratovolcano, is a tall, steep-sided volcano with alternating layers of solidified lava flows, volcanic ash, and other volcanic debris. They are characterized by explosive eruptions due to their high viscosity magma. Examples include Mount St. Helens and Mount Fuji.
Stratovolcanoes or composite volcanoes are tall conical mountains composed of lava flows and other ejecta in alternate layers, the strata that gives rise to the name. Stratovolcanoes are also known as composite volcanoes because they are created from multiple structures during different kinds of eruptions.
Cinder volcanoes have more of funnel shape with a crater like top while a composite volcano simply has an opening at the tip where the lava comes out.
AnswerVolcanoes can be active or inactive. When a volcano is active there is magma or lava moving around getting ready to make an explosion. When a volcano is inactive there is either rocks and bits of other stuff melting in the main vent making magma getting ready to become active or they are not doing anything, just sitting there like a mountain.The four main types of volcanoes are shield volcanoes, composite volcanoes, also called stratovolcanoes, cinder cones, and lava domes. Composite volcanoes are the most abundant, and an example is Mount Fuji in Japan. These volcanoes are formed from layers of ash. In contrast, shield volcanoes are gently sloping volcanic mountains built almost fully of lava flows. They were named on account of their shape , which is reminiscent of an ancient warrior's shield. These volcanoes are typically much larger then composite volcanoes. Lava domes and Cinder cones are much smaller than shield or composite volcanoes.AnswerThey are, cinder cone, composite cone, shield cone, and extinct volcano.
Stratovolcanoes are typically the tallest type of volcano. They are characterized by their steep sides and symmetrical cones formed by alternating layers of lava flows, volcanic ash, and cinders. Notable examples include Mount Fuji in Japan and Mount Rainier in the United States.
After the Alaska volcano formed, other volcanoes have formed.
They are: - Shield volcanoes - Composite volcanoes - Cinder cone volcanoes Maybe you can use this for your homework if you have any problems come to answers.com you can sign up too!!