Push together
Explosive volcanoes are most common at subduction zones.
Volcanoes are in concentrated zones.
They are concentrated in zones - specifically at or near convergent and divergent tectonic plate boundaries. There are a few exceptions that can occur within tectonic plates which are thought to be caused by mantle plumes which create hot spots. An example would be the Hawaiian Island chain which has formed roughly in the centre of the pacific plate.
Cone volcanoes which are likely to erupt explosively are found at subduction zones. Spreading zones (constructive plate boundaries) and hot spots produce quieter volcanoes because their lava is thinner. The ones at hot spots are shield volcanoes.
Its cool
Explosive volcanoes are most common at subduction zones.
Volcanoes are in concentrated zones.
Volcanoes are distributed in concentrated zones.
composite volcanoes
No, hotspot volcanoes do not occur along subduction zones. They occur when plates pass over mantle hot spots.
usually you find most of the zones of earthquakes and volcanoes at a plate boundary.
A buckling zone is a region in a structure where there is a risk of buckling or collapse under compressive forces. It is important to identify and reinforce these zones to prevent structural failure. Strengthening measures such as using bracing or adding reinforcements can help to mitigate potential buckling issues.
They are concentrated in zones - specifically at or near convergent and divergent tectonic plate boundaries. There are a few exceptions that can occur within tectonic plates which are thought to be caused by mantle plumes which create hot spots. An example would be the Hawaiian Island chain which has formed roughly in the centre of the pacific plate.
Cone volcanoes which are likely to erupt explosively are found at subduction zones. Spreading zones (constructive plate boundaries) and hot spots produce quieter volcanoes because their lava is thinner. The ones at hot spots are shield volcanoes.
Its cool
fault zones
No, volcanoes did not create humans.