Cindercone
A combination volcano develops from repeated lava eruptions and the accompanying tephra deposits Tephra is the debris from the eruption..
Composite
Capulin volcano is a cinder cone volcano. It is a steep-sided volcanic cone built by the accumulation of volcanic debris around a vent, which is formed during eruptions characterized by explosive eruptions of tephra and pyroclastic flows.
Yes, shield volcanoes can sometimes produce tephra during explosive eruptions. However, these eruptions are less common compared to the effusive lava flows that are typically associated with shield volcanoes. Tephra produced by shield volcanoes tends to be finer-grained compared to the tephra from stratovolcanoes.
A tephra cone volcano, also known as a cinder cone volcano, is made entirely of tephra. Tephra is a term for fragmented material produced by a volcanic eruption, such as ash, cinders, and bombs. Tephra cone volcanoes are typically small in size and have steep slopes due to the build-up of tephra fragments from explosive eruptions.
Cinder cone volcano
A cinder cone volcano forms from tephra eruptions. Tephra consists of volcanic matter like ash, cinders, and volcanic rocks exploded into the air during an eruption, which then settle around the vent to form a steep-sided cone-shaped structure.
because of volcano eruptions
Cinder cone volcano
Mount Pelee is a stratovolcano, which is a composite volcano that consists of both lava flows and layers of volcanic ash and tephra. It is not a cinder cone volcano, which is typically smaller in size and formed by eruptions of mostly cinder and ash.
The cone of a volcano is the mountain of erupted material that makes up much of the visible part of the volcano.The cone of a mountain is a the pile of material around a volcanic event formed from precious eruptions. The cone may consist of tephra, cooled lava flows, or a combination of both.
a volcano