NO
Guatemala City is located approximately 75 miles (120 kilometers) away from the closest plate boundary, which is the subduction zone along the Middle America Trench where the Cocos Plate is subducting beneath the Caribbean Plate.
Tsunamis usually originate at plate boundaries, particularly at subduction zones, but once they are triggered they can cross thousands of miles of ocean, striking areas far from any plate boundary.
Far-field stresses triggered by portions of the northern boundary stress the African plate. Intraplate stresses are the driving forces in the South American plate
Canada is on the North American plate, the eastern part of this plate extends to the mid-Atlantic ridge, however this is far from Canada. The western coast of Canada is a subduction zone for the most part with a small amount of the Queen Charolette fault towards the north. The subduction zone is called the Cascadia subduction zone.
The area of volcanic activity far from a tectonic plate boundary is called a "hotspot." Hotspots are characterized by plumes of hot mantle material that can create volcanic islands and chains, such as the Hawaiian Islands. These volcanic activities occur independently of tectonic plate movements, often resulting in long-lived eruptions in a localized area.
Its to do with the viscosity of the lava, the thicker (more viscous) the lava the slower and less far it will travel making a shield volcano. This happens on a constructive plate boundary. on a destructive plate boundary the lava is less viscous and runs further making a conical shaped volcano
None. Kilauea is over a hot spot, far from the nearest plate boundary.
2000 miles
Guatemala City is located approximately 75 miles (120 kilometers) away from the closest plate boundary, which is the subduction zone along the Middle America Trench where the Cocos Plate is subducting beneath the Caribbean Plate.
Tsunamis usually originate at plate boundaries, particularly at subduction zones, but once they are triggered they can cross thousands of miles of ocean, striking areas far from any plate boundary.
mantle plume
Yes, that is correct. Hot spots are areas of volcanic activity that occur far from tectonic plate boundaries. The magma from the hot spot rises to the surface, forming volcanoes such as the Hawaiian Islands.
Far-field stresses triggered by portions of the northern boundary stress the African plate. Intraplate stresses are the driving forces in the South American plate
Canada is on the North American plate, the eastern part of this plate extends to the mid-Atlantic ridge, however this is far from Canada. The western coast of Canada is a subduction zone for the most part with a small amount of the Queen Charolette fault towards the north. The subduction zone is called the Cascadia subduction zone.
Hot spots!
The area of volcanic activity far from a tectonic plate boundary is called a "hotspot." Hotspots are characterized by plumes of hot mantle material that can create volcanic islands and chains, such as the Hawaiian Islands. These volcanic activities occur independently of tectonic plate movements, often resulting in long-lived eruptions in a localized area.
The far west coast, along California, is the location of a famous plate boundary known as the San Andreas Fault. This fault is a transform fault boundary, meaning that the Pacific plate to the west and the North American plate to the east rub against each other in a parallel motion but don't create new lithosphere or destroy old lithosphere. This fault is the reason for all the large and small earthquakes in the California area, including the San Francisco earthquake of 1906.