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None in the middle of the US.

The major plate boundary that affects the US is the plate edge on the California coastline.

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17y ago

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Related Questions

Why is sudbuction not occurring at this plate boundary?

Since you did not tell us WHICH plate "this" one is, we cannot answer correctly


What type of plate boundary of kilauea volcano?

It is not on a plate boundary but in the middle of a plate. Kilauea has formed over a hot spot.


What type of plate boundary created Kilauea volcano?

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What plate boundary is the boundary at which plates collide or come together?

The plate boundary at which plates collide or come together is called a convergent boundary. At convergent boundaries, one plate is typically forced beneath the other in a process known as subduction. This collision can lead to the formation of mountain ranges, deep ocean trenches, and volcanic activity.


How far is Guatemala city from a plate boundary?

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.


At what type of boundary did the 1960 Chilean earthquake occur?

At a convergent boundary between oceanic and continental crust where subduction is occurring.


What are the all the boundary?

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Why is Hawaii located not at a plate boundary?

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What was the plate boundary at the new Madrid earthquake in 1811?

The New Madrid earthquakes of 1811-1812 occurred near the New Madrid Seismic Zone in the central United States. This region is not located near a traditional tectonic plate boundary, but rather is an intraplate seismic zone within the North American Plate. The earthquakes are believed to be the result of ancient faults within the continent that are reactivated due to regional stress.


Is haiti on a boundary between two plates or in the middle of one plate?

Haiti is located on the boundary between the Caribbean Plate and the North American Plate. This tectonic boundary is known as a strike-slip fault, with the plates sliding past each other horizontally, causing earthquakes.