when lava flows down it the lava that stayed on it gets hard
The three main types of volcanoes are shield volcanoes, stratovolcanoes (composite volcanoes), and cinder cone volcanoes. Shield volcanoes have gently sloping sides and are formed by layers of lava flows. Stratovolcanoes are characterized by steep sides and explosive eruptions. Cinder cone volcanoes are small, steep-sided volcanoes built from explosive eruptions that eject fragmented rock.
No, cinder cone volcanoes typically have steep sides due to the accumulation of loose volcanic material, such as cinder and ash, that build up around the vent. As a result, they tend to have a steeper profile compared to other types of volcanoes.
Some examples of cinder cone volcanoes in the Philippines include Mount Malindig on the island of Marinduque and Mount San Carlos in Negros Occidental. These volcanoes are characterized by their steep sides and typically smaller size compared to other types of volcanoes.
A volcanic mountain with a narrow base and steep sides is typically called a volcanic cone or a cinder cone. These cones are formed from explosive eruptions that eject mostly tephra and volcanic ash, resulting in their characteristic steep shape.
Cinder cone
Shield volcanoes are made from runny lava and steep sides. Cinder cone volcanoes are made from lava layers that alternate with layers of cinder. composite volcanoes shoot lav into the air.
The three types of volcanoes are shield volcanoes, cinder cone volcanoes, and stratovolcanoes. Shield volcanoes have broad, gently sloping sides, cinder cone volcanoes are steep-sided with a circular or oval shape, and stratovolcanoes are tall, conical volcanoes built up by many layers of hardened lava, tephra, pumice, and volcanic ash.
A steep-sided volcano of lava and tephra is called a stratovolcano. Stratovolcanoes are characterized by their tall, conical shape and explosive eruptions caused by the buildup of pressure from gases and molten rock beneath the surface.
The three main types of volcanoes are shield volcanoes, cinder cone volcanoes, and composite (or stratovolcanoes) volcanoes. Shield volcanoes have gently sloping sides and are formed by layers of lava, while cinder cone volcanoes are steep-sided with a conical shape and are made of pyroclastic material. Composite volcanoes are a mix of both lava and pyroclastic material, with a classic symmetrical cone shape.
Three 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, while stratovolcanoes are characterized by alternating layers of lava and ash. Cinder cone volcanoes are small, steep-sided volcanoes formed by pyroclastic material ejected during eruptions.
shield volcanoes have cinders that come out then land on it. that's what makes them bigger than cinder cone volcanoes.
Cinder-cone volcanoes are built by thick lava that is thrown high into the air and falls as chunks or cinders. These mountains form as a cone shape with narrow base and steep sides.