Fault lines
The edges where tectonic plates meet are called "plate boundaries." There are three main types of plate boundaries: divergent, where plates move apart; convergent, where plates collide; and transform, where plates slide past each other. Each type of boundary is associated with different geological activities, such as earthquakes, volcanic activity, and the formation of mountain ranges.
They could meet and cause an earthquake.
Breaks in the Earth's crust where plates meet are called plate boundaries. These boundaries are classified into three types: divergent, convergent, and transform boundaries, depending on the motion of the plates.
The Plate Boundaries. It could be called the plate boundary, plate edge, or continental divide. With tectonic plates, they meet at the fault line.
The edges of continental plates are called fault lines because they are boundaries where tectonic plates meet and interact. These interactions can create faults, which are fractures within the Earth's crust where rocks have moved relative to each other. Fault lines are prone to seismic activity such as earthquakes due to the stress and movement along these boundaries.
plate boundary
They could meet and cause an earthquake.
because the crust is thinner and the techtonic plates meet.
The edges of Earth's tectonic plates are called plate boundaries. At plate boundaries, the plates interact with each other through processes such as subduction, seafloor spreading, and transform faulting.
a solid with flat sides meet at sharp edges and corners is called crystal structure
It is called a vertex
Fault lines
vertex
Places, where plates meet, are called plate boundaries. There are seven significant plates along with countless minor plates. You can see that a plate can be made of both oceanic crust and continental crust. Interactions between the plates change our planet.
A corner where three edges meet is also called a vertex. A vertex can be also used in Algebra 2, in Quadratic Equations.
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Edges meet at a vertex.