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Three types of volcanoes are Cinder Cone Volcanoes, Shield Volcanoes and Composite Volcanoes.
The color of cinder cone volcanoes is a blackish-gray.
Pyroclastic flows don't come from shield volcanoes. They come from cinder cone and sometimes composite volcanoes. Shield volcanoes only erupt runny lava.
Cinder-Cone Volcanoes and Composite Volcanoes
There are three. From smallest to largest, they are: Cinder Cones, Composite Volcanoes (also called Strata Volcanoes), and then Shield Volcanoes.
Three types of volcanoes are Cinder Cone Volcanoes, Shield Volcanoes and Composite Volcanoes.
The color of cinder cone volcanoes is a blackish-gray.
Three landforms that can be created from ash are cinder cone volcanoes, composite volcanoes, and shield volcanoes. Lava plateaus can also be formed.
Pyroclastic flows don't come from shield volcanoes. They come from cinder cone and sometimes composite volcanoes. Shield volcanoes only erupt runny lava.
Cinder-Cone Volcanoes and Composite Volcanoes
There are three. From smallest to largest, they are: Cinder Cones, Composite Volcanoes (also called Strata Volcanoes), and then Shield Volcanoes.
The Hawaiian islands are made of two types of volcanoes, shield volcanoes and cinder cone volcanoes. Shield volcanoes have broad bases with gentle slopes. Cinder cone volcanoes have steeper sides, are made from fragments of lava, and are usually located at the base of shield volcanoes.
There are four main types of volcanoes. These include shield volcanoes, cinder cones, composite volcanoes, and lava domes.
There are three kinds of cone volcanoes shield cones, composite cones, and cinder cones. Shield cones have very fluid lava. They erupt with a quiet lava flow. An example of a shield cone volcano is Mauna Loa. A shield cone is pretty much a little dome that has been flattened. Composite cones have sticky lava and rock bits. They have the most explosive eruptions An example of a composite cone volcano is Vesuvius. Composite cones are steep at the top but gentle at the bottom. Cinder cones have cinders. They have explosive eruptions An example is Paricutin. A cinder cone is very steep.
Volcanoes are grouped into four types: cinder cones, composite volcanoes, shield volcanoes and lava volcanoes. They are: Cinder Cones: They are circular or oval cones made up of small fragments of lava from a single vent. They have been blown into the air, cooled, and fallen around the vent. Composite: They are steel-sides and composed of many layers of volcanic rocks. Mt. Rainier and Mount St. Helens are examples of this type of volcano. Shield: Shaped like a bowl or shield in the middle, they have long gentle slopes made of basaltic lava flows. The volcanoes that formed the basalt of the Columbia Plateau were shield volcanoes. Lava Volcanoes: Deep sided mound formed by lava that is too thick to flow. The lava piles up near the vent.
Shield volcanoes are made from runny lava and steep sides. Cinder cone volcanoes are made from lava layers that alternate with layers of cinder. composite volcanoes shoot lav into the air.
cinder strato and shield shield is the least dangerous and the lava slowly flowsa down cinder erupts tephra not lava like a shield and is cone shaped strato is the most dangerous it erupts both tephra and lava