Cindercone volcanoes are small, steep sided, narrow based, loosely packed cones made entirely of pyroclastic material from moderately explosive eruptions.
It's the classical and most common conically-shaped ("Triangular") form of volcano.
The arenal volcano is a cindercone volcano not a composite.
Mount Amukta is a stratovolcano, also known as a composite volcano. This type of volcano is characterized by steep slopes and explosive eruptions due to its high viscosity magma. Stratovolcanoes are typically found near subduction zones.
A cinder cone volcano has a conical shape with steep sides. It is typically smaller in size compared to other types of volcanoes and is formed from the accumulation of tephra, such as volcanic ash and cinders, around a vent.
The three types of volcanoes are shield volcanoes, stratovolcanoes (composite volcanoes), and cinder cone volcanoes. Shield volcanoes have gentle slopes and are formed by lava flows, stratovolcanoes are tall, steep-sided volcanoes built up by layers of hardened lava, rock, and ash, and cinder cone volcanoes are relatively small, steep-sided volcanoes made of pyroclastic material.
1.Stratovolcano (most common) 2. Shield (least common) 3. Cindercone
Cindercone
The arenal volcano is a cindercone volcano not a composite.
Mount Paricutin is a cinder cone volcano
No, it is not. It is a stratovolcano (synonym = composite volcano). There is a small cinder cone though on its south flank.
Mount Amukta is a stratovolcano, also known as a composite volcano. This type of volcano is characterized by steep slopes and explosive eruptions due to its high viscosity magma. Stratovolcanoes are typically found near subduction zones.
steep sides
Mexico it is a cindercone
shield,cindercone,composite,extinict
Cinder cone
Hey, I was just wondering what kind of volcano Mt. Bromo is? Is it a compostive, shield, or cindercone? I have no idea and im doing this for a report so ya please help me! haha thanks! -Meggan <3
A cinder cone volcano has a conical shape with steep sides. It is typically smaller in size compared to other types of volcanoes and is formed from the accumulation of tephra, such as volcanic ash and cinders, around a vent.
The three types of volcanoes are shield volcanoes, stratovolcanoes (composite volcanoes), and cinder cone volcanoes. Shield volcanoes have gentle slopes and are formed by lava flows, stratovolcanoes are tall, steep-sided volcanoes built up by layers of hardened lava, rock, and ash, and cinder cone volcanoes are relatively small, steep-sided volcanoes made of pyroclastic material.