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.
Both subduction zones and spreading centers.
SPREADING ZONES Spreading zone occurs in the border of two tectonic plates. This happens when the plates generally move away from each other creating an opening for the magma to force through the surface.
Explosive volcanoes are most common at subduction zones.
No. Tropical climate zones are found in lower latitudes.
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.
composite volcanoes
Tropical zones.
The most violent earthquakes are generally associated with subduction zones where tectonic plates collide and one is forced beneath the other. These subduction zones can produce very large and destructive earthquakes, such as the 2004 Indian Ocean earthquake and tsunami. Spreading centers, on the other hand, usually produce smaller earthquakes due to the gradual separation of tectonic plates.
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they dont affect it
Both subduction zones and spreading centers.
The plates are actively spreading submarine ridges in the middle of the oceans, subduction zones in ocean trenches or mountain ranges on the continents, or margins where the plates slide past one another. Most of the world's earthquakes occur at plate boundaries.
On the other side of the plate there is most likely growth, through something like sea floor spreading.
Hydrothermal vents are found along seafloor spreading centers on the bottom of the oceans.
SPREADING ZONES Spreading zone occurs in the border of two tectonic plates. This happens when the plates generally move away from each other creating an opening for the magma to force through the surface.
Explosive volcanoes are most common at subduction zones.