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With regards to fluids, consistency is an estimation of how thick or syrupy it is, and the magma thickness characterizes the size and state of a well of lava. Despite the fact that the magma is multiple times more thick than water, it can at present stream huge spans. At the point when magma has low consistency, it can stream effectively over long separations.
The lavas is a molten rock that is made from the magma upwelled in the mantel layer. Generally, it's very thick and does not flow very well.
- The viscosity of lava is about the resistance of the fluid to the change in shape and as per lava is concerned it refers to the thickness and strength of lava. The viscosity of lava is 100,000 more than water.
- The Rhyolitic magmas are highly viscous. The viscosity is divided into basaltic that is low, andesitic that is intermediate or medium, and rhyolite that is high. An example of this is the felsic lava.
Learn more about the talk about the viscosity of the lava.
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