Cinder cone lava typically has a temperature range of about 1,100 to 1,200 degrees Celsius (2,012 to 2,192 degrees Fahrenheit) when it erupts. This type of lava is generally basaltic, which means it has a lower viscosity and can flow relatively easily. The high temperatures contribute to the formation of the cinder cone structure as the lava cools and solidifies into small fragments that accumulate around the vent.
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.
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.
Tambora was a composite cone.
Mount Kenya is neither a composite cone, cinder cone, nor a shield cone. It is a complex stratovolcano made up of layers of lava and 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.
A cinder cone has basaltic lava, which has a fairly low viscosity.
lava
Not acid lava, basic magma.
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.
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.
No. Cinder cone volcanoes erupt fountains of lava, which is how the cinder cone is built up. Cinder cones that are nearing the end of activity may also produce lava flows.
makes it bigger
Tambora was a composite cone.
Both erupt basaltic lava, which has a low silica content and a high temperature.
Mount Kenya is neither a composite cone, cinder cone, nor a shield cone. It is a complex stratovolcano made up of layers of lava and ash.
when lava flows down it the lava that stayed on it gets hard
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.