Rephrased - How do the movements of plate tectonics form different volcanoes?
Plate tectonics form several faults. You can have a subduction fault, where one plate slides under another. These faults more often than not produce stratovolcanoes that erupt explosively and with little to no warning. Stratovolcanoes are formed as a result of crustal melting from crust that was previously the ocean floor, and has melted again in a recycling process. This process heats magma under the fault zone and causes volcanoes to pop up. The west coast of the United states and the Cascade Range is one of these zones.
You can also have spreading plates, like the North American and European plates, which ware moving apart from each other. Iceland is a good example of this spreading which can be observed at Thingvallir. Crustal spreading allows magma to quickly rise to the surface creating eruptions such as fissure vents, lava fields, and cinder cones.
compare volcano formation at different plate boundaries
Instead of doing that, just compare your penis with someone else's penis.
the volcanoes on venus are yellow
Land Volcanoes eat lamas and underwater volcanoes eat camals
FALSE
not necessarily but there are other valves for the magma to escape.
All volcanoes emit water vapor and other gases.
It is the largest in Africa.
the volcanoes on venus are yellow
Land Volcanoes eat lamas and underwater volcanoes eat camals
Shield Volcanoes - Wide base found at constructive plate margins Composite Volcanoes - Steeper Sides found at Destructive (subduction) margins
scientists are almost able to predict volcano eruptions because of all the signs we get that we can compare to what has happened before other volcanoes erupted...
Volcanoes can form from other other volcanoes in the ring of fire
FALSE
There are volcanoes all over the planet.
not necessarily but there are other valves for the magma to escape.
Cone volcanoes are typically the tallest and largest. The two other types of volcanoes are shield volcanoes and composite volcanoes.
From their bottoms on the ocean floor to their peaks, the Hawaiian volcanoes are the tallest in the world - even taller than Mount Everest. That is the main difference.
Shield Volcanoes - Wide base found at constructive plate margins Composite Volcanoes - Steeper Sides found at Destructive (subduction) margins