Two tectonic plates moving toward one another are at a
convergent boundary.
divergent boundary.
subduction boundary.
transform boundary.

convergent boundary.

Explanation:

    Unsurprisingly among scientists, continents and ocean floors are in continuous motion. This movement occurs through magmatic currents in the innermost layers of the Earth (convection currents), which eventually alter the position of the immense blocks of rock floating above the magma, called tectonic plates.

   Thus, this movement of the plates eventually leads to constant shocks in their meeting regions, which causes seismic and volcanic activities around the globe. The boundaries between such tectonic plates, however, may follow different orientations, thus determining the classification that will be exposed below.

Divergent Boundary

    In this type of limit, there is the separation between plates. In the space created between the two large blocks, the formation of a new crust occurs through the solidification of the magma. It can occur on continents or oceans.