alot.
Both cinder cone and shield volcanoes are primarily composed of basaltic lava flows. However, cinder cone volcanoes are characterized by steep slopes, smaller size, and built up from pyroclastic material like ash and cinders, while shield volcanoes are much larger with gentle slopes built from numerous lava flows.
ash and cinder volcanos erupt small solid of rocks and fragments and ash.composite cone volcanos erupt with runny lava fowllowed by explosive thick lava.thats the difference between them....by:kosraegurl aj;)
It is thick, slow moving lava called Pyroclastic Flow.also known as high viscosity
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.
A cinder cone volcano typically has basaltic lava, which is low in silica content and flows easily. This results in the formation of steep-sided cones made of mostly cinders and volcanic ash.
Both cinder cone and shield volcanoes are primarily composed of basaltic lava flows. However, cinder cone volcanoes are characterized by steep slopes, smaller size, and built up from pyroclastic material like ash and cinders, while shield volcanoes are much larger with gentle slopes built from numerous lava flows.
they erupe if theres alot of lava inside and the volcano has no more spaca and it erups
ash and cinder volcanos erupt small solid of rocks and fragments and ash.composite cone volcanos erupt with runny lava fowllowed by explosive thick lava.thats the difference between them....by:kosraegurl aj;)
A cinder cone has basaltic lava, which has a fairly low viscosity.
It is thick, slow moving lava called Pyroclastic Flow.also known as high viscosity
lava
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.
Not acid lava, basic magma.
Lava is spewed out of a vent like a cannonball, forming a cone-shaped volcano.
A cinder cone volcano typically has basaltic lava, which is low in silica content and flows easily. This results in the formation of steep-sided cones made of mostly cinders and volcanic ash.
A Stratovolcano is a steep volcano made mostly of layers of ash, lava and cinders. Stratovolcanoes have a tendency to be very explosive and produce significant quantities of ash.
The lava of cinder cone volcanoes is typically black, dark red, or dark brown in color. This is due to the high iron and magnesium content in the lava, which gives it a darker appearance compared to other types of lava.