Lava is thrown into the air, which breaks into small fragments that solidify and fall around the vent to form a circular or oval cone.
Most cinder cones have a steep slope, wide crater and are the most abundant of the three major volcano types.
Composite Volcanoes
Stratovolcanoes
Composite Volcano
large, typically steep sided, symmetrical cones of large dimension formed from alternating layers of lava flows, volcanic ash, cinders, blocks, and pyroclastic materials.
Conduit System
One of the most important feature of a composite volcano
Composite Volcanoes
They are formed from viscous, or sticky, lava that does not flow easily.
Shield Volcano
built almost entirely of fluid lava flow thus these volcanoes are not steep.
Shield Volcanoes
The lava is not accompanied by pyroclastic materials, which makes shield volcanoes relatively safe
Shield Volcanoes
Eruptions at shield volcanoes are only explosive if water somehow gets into the vent.
Active Volcanoes
have had at least one eruption during the past 10,000 years.
Active Volcanoes
They are those that erupted recently and still showing regular activity like emission of gases, lava and ash flows.
Inactive Volcanoes
have not erupted for the last 10,000 years and is not expected to erupt again in a comparable time scale of the future.
Inactive Volcanoes
There are no signs of volcanic activity for a long period of time because magma supply is cut off.
Inactive Volcanoes
the physical form of the volcano has signs of intensive weathering and erosion.