yes
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.
Both shield volcanoes and cinder cones erupt low-viscosity basaltic lava and have eruptions that are only mildly explosive if at all.Cinder cones are small, steep-sloped volcanoes composed primarily of a chunky variety of basalt called scoria.Shield volcanoes are large, gently sloping volcanoes composed primarily of layers of lava flows.
The three major types of volcanoes are shield volcanoes, stratovolcanoes (composite volcanoes), and cinder cone volcanoes. Shield volcanoes have gentle slopes and are formed by low-viscosity lava flows, stratovolcanoes are steep-sided and composed of layers of lava and ash, and cinder cone volcanoes are small, steep-sided cones made of pyroclastic material.
Here is a good article outlining the major types of volcanic eruptions, including diagrams:http://en.wikipedia.org/wiki/Types_of_volcanic_eruptions
No. The Hawaiian islands are shield volcanoes.
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 cones generally have a very steep slope. This slope is also considered gentle compared to the cones' short height.
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!!
Cinder cone volcanoes erupt explosivly.
No. Cinder cones are formed by basaltic magma.
The main types of volcanoes are shield volcanoes, stratovolcanoes (composite volcanoes), cinder cone volcanoes, and lava domes. Shield volcanoes have gentle slopes and are formed by fluid lava flows. Stratovolcanoes are tall, steep-sided cones composed of layers of lava and ash. Cinder cone volcanoes are small, steep-sided cones made of pyroclastic material. Lava domes are mounds of thick, slow-flowing lava piling up near a volcano's vent.
There are three. From smallest to largest, they are: Cinder Cones, Composite Volcanoes (also called Strata Volcanoes), and then Shield Volcanoes.