A hot spot is where a bum touches the earth
Viscosity is a fluid's resistance to flow. Fluids becomes less viscous as the liquid's temperature increases, becoming more viscous as the fluid gets cooler. A viscous fluid is sticky, thick and syrupy to a greater or lesser extent. Examples Treacle is quite viscous, but water is not. Hot engine oil is less viscous ('thinner') and runs more quickly and smoothly than cold engine oil.
Some types do. Really runny lava, or hot lava, like Hawaiian-type lava, does glow because it's so hot (like when you heat a piece of metal). Really viscous (sticky) lava, however, has a solidifying skin on top because the lava has cooled down. It's sort of like custard (except custard never glows)
Volcanoes that form islands over hot spots sometimes become dormant because they move away from the hot spot. If they move away from the hot spot, magma is no longer created.
there are different types of volcanoes for different reasons. how they form has alot to do with the type of lava said volcano produces. fluid basaltic lava tends to create shield volcanoes. spatter cones tend to form when hot erupting lava contains just enough explosive gas to prevent the formation of a lava flow, but not enough to shatter it into small fragments. hot expanding gas tears the lava into hot fluid clots.
Yes.
The asthenosphere.
A hot spot is where a bum touches the earth
Well,magma is hot moltten rock beneth earth's crust.If you touch it,well you know what happens-R.I.P.
lava ozzing out of a vent which is a hot spot
No. Block lava is low-moving viscous lava, usually of andesitic or similar composition. A pyroclastic flow is a very fast-moving mixture of hot ash, rock and gas.
Viscosity is a fluid's resistance to flow. Fluids becomes less viscous as the liquid's temperature increases, becoming more viscous as the fluid gets cooler. A viscous fluid is sticky, thick and syrupy to a greater or lesser extent. Examples Treacle is quite viscous, but water is not. Hot engine oil is less viscous ('thinner') and runs more quickly and smoothly than cold engine oil.
Some types do. Really runny lava, or hot lava, like Hawaiian-type lava, does glow because it's so hot (like when you heat a piece of metal). Really viscous (sticky) lava, however, has a solidifying skin on top because the lava has cooled down. It's sort of like custard (except custard never glows)
Volcanoes that form islands over hot spots sometimes become dormant because they move away from the hot spot. If they move away from the hot spot, magma is no longer created.
there are different types of volcanoes for different reasons. how they form has alot to do with the type of lava said volcano produces. fluid basaltic lava tends to create shield volcanoes. spatter cones tend to form when hot erupting lava contains just enough explosive gas to prevent the formation of a lava flow, but not enough to shatter it into small fragments. hot expanding gas tears the lava into hot fluid clots.
Basaltic flows much faster than rhyolite. Rhyolite is higher viscosity. Find a video of a basaltic lava flow like Hawaii, it flows like water when it's hot. Rhyolite eruptions usually act more like toothpaste if they're slow, or an explosion if fast.
No. There are 3 reasons.Lava is extremely hot, and falling in lava would result in certain death.Lava is dense, about the same density as rock, so you would not sink in far enough to swim.Lava is viscous, so ignoring the first two reasons, it would be like trying to swim in molasses with the most fluid lavas.