No. The Hawaiian islands are shield volcanoes.
The Hawaiian islands were formed by shield volcanoes. However, cinder cones are also present on top of some of them.
The Hawaiian volcanoes can form cinder cones, however the type of volcano they are classified as is shield volcano due to their broad sloping sides and the ability for their lava to flow.No. The Hawaiian islands are shield volcanoes.
yes
Yes, although technically, strato-volcanoes *are* cinder cones (composite cones), built up of layers of ash. But the term "cinder cones" (ash cones) is usually applied to smaller cones that form within the vicinity of large volcanic calderas, such as Crater Lake in Oregon. They may be associated with either strato-volcanoes or shield volcanoes.
Cinder cone volcanoes erupt explosivly.
No. Cinder cones are formed by basaltic magma.
There are three. From smallest to largest, they are: Cinder Cones, Composite Volcanoes (also called Strata Volcanoes), and then Shield Volcanoes.
Cinder cones are the mountainous structure built up by some volcanoes. Most of the material that makes up the cone is ash and cinders expelled from the top of the cone.
No. Shield volcanoes are quite large. Cinder cones are the smallest volcanoes.
Cinder cone volcanoes are usually found on dry land and in corn fields
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.
Shield volcanoes and cinder cones