The thickness of lava is generally dependent on the eruption rate of the volcano. The flow rate of lava is measured by the lava's viscosity. Highly viscous lava does not flow well or travel great distances. Low viscosity lava can flow for great distances.
There is no lava on the sun. The sun is made mostly of hydrogen and helium and is much hotter than lava. The density of the sun's outer layer's is quite low, about 0.37% that of Earth's atmosphere, while the inner core is compressed to a density about 6 times greater than that of the densest substances on Earth.
A cinder cone volcano has basaltic lava.
The Arenal Volcano is a cinder cone volcano
Paricutin is a volcano in Michoacán, Mexico. The volcano is a cinder cone volcano. This means that the volcano is made up of layers of ash and stones that erupt out of the earth when the volcano erupts.
Basaltic. There is more gas content than in most basaltic magma so that when a cinder cone erupts, The pressure builds up and makes the eruption somewhat explosive. Tephra, or dried lava/magma, is shot up, and joined to the volcano making it larger.
A cinder cone volcano....found in my 8th grade science book page 136(:
A cinder cone volcano has basaltic lava.
lava
The Arenal Volcano is a cinder cone volcano
makes it bigger
Paricutin is a volcano in Michoacán, Mexico. The volcano is a cinder cone volcano. This means that the volcano is made up of layers of ash and stones that erupt out of the earth when the volcano erupts.
A cinder cone volcano....found in my 8th grade science book page 136(:
Basaltic. There is more gas content than in most basaltic magma so that when a cinder cone erupts, The pressure builds up and makes the eruption somewhat explosive. Tephra, or dried lava/magma, is shot up, and joined to the volcano making it larger.
A composite volcano.
A composite volcano is a combination of a cinder cone and a shield cone. The top of a composite volcano is steep like a cinder cone. The bottom of a composite volcano is flatter, like a shield volcano.
Lava, watervapour, ash, cinder, carbondioxide.
The way a volcano is being formed, depends on the type of lava. Cinder cone volcanoes is made from andesitic lava. This type of lava is especially thick, and therefore is won't be able to ''run'' very far from the volcano. In this way, each time a cinder cone volcano erupts, it will create a new layer of lava, making the volcano higher and higher each time, but it will not increase its base area very much. It's different with shield volcanoes. They are made from another kind of lava which will advance very far from it's vent. Therefore the shield volcano won't often be very tall, but it can have a very large base area
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.