It is a common misconception that there IS always ash. In some volcanoes, such as Hawaii, barely any ash is generated due to eruption.
It all depends on the type of magma. Mafic magma tends to be non-viscous (quite runny, as magma goes), and so will flow freely. Because of this, gases can escape easily and so little pressure builds up.
This is important as ash is essentially pulverised rock that is thrown up due to large-scale explosive eruptions.
In intermediate-felsic magmas (or lavas), the viscosity (I may have just made that word up), is greater, and felsic lavas in particular are very viscous, due to their relatively low temperature compared more mafic magmas. Therefore, gases find it harder to escape the magma, especially as it cools and hardens in the volcano itself, and rarely flows down the mountainside.
Therefore, pressure begins to build due to all the trapped gases. This pressure, when great enough, causes the magma above it, as well as rocks that make up the volcano itself, to blast outwards in an explosive eruption. This generates large volumes of pulverized rock (ash) and small rock fragments.
Because this ash is light enough to remain airbourne, it can stay in the atmosphere for months and even years after the initial eruption. Some eruptions from these strato-volcanoes in the past have caused widespread global cooling, leading to crop failure, and this is even one of the theories for the extinction of the dinosaurs (except dinosaurs didn't have crops, but you know what I mean).
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Volcanoes are cone-shaped mountains that can eject lava, ash, and gases from a vent in the Earth's crust. They are formed by the accumulation of erupted material over time.
Andesitic composite volcanoes typically eject pyroclastic material, which includes ash, pumice, and volcanic bombs. These materials are a result of explosive eruptions caused by the high viscosity of andesitic magma, leading to the build-up of pressure within the volcano.
Cinder cones are generally formed when volcanoes eject a combination of ash, cinders, and lava fragments during explosive eruptions. These materials pile up around the vent, creating a steep-sided cone-shaped hill. The eruptions are typically short-lived and can occur suddenly.
A steep-sided volcano formed entirely of ash and cinders is called a cinder cone volcano. These volcanoes are typically smaller in size compared to other types of volcanoes and are formed from explosive eruptions that eject mostly fragmented volcanic material.
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Volcanoes are cone-shaped mountains that can eject lava, ash, and gases from a vent in the Earth's crust. They are formed by the accumulation of erupted material over time.
Andesitic composite volcanoes typically eject pyroclastic material, which includes ash, pumice, and volcanic bombs. These materials are a result of explosive eruptions caused by the high viscosity of andesitic magma, leading to the build-up of pressure within the volcano.
Cinder cones are generally formed when volcanoes eject a combination of ash, cinders, and lava fragments during explosive eruptions. These materials pile up around the vent, creating a steep-sided cone-shaped hill. The eruptions are typically short-lived and can occur suddenly.
A steep-sided volcano formed entirely of ash and cinders is called a cinder cone volcano. These volcanoes are typically smaller in size compared to other types of volcanoes and are formed from explosive eruptions that eject mostly fragmented volcanic material.
ash
Ash clouds are emitted from volcanoes.
Three landforms that can be created from ash are cinder cone volcanoes, composite volcanoes, and shield volcanoes. Lava plateaus can also be formed.
Volcanoes with high levels of water in their lava produce ash, those with dry lava produce no ash.
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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.
Composite VolcanoesComposite Volcanoes. Composite volcanoes are tall, cone shaped mountains in which alternate layers of lava alternate with layers of ash. This happens when smooth lava flows alternate with explosive eruptions of lava fragments.