At the constructive plate margin, as I think you mean, largely basalt from extruded upper-Mantle material.
Examples are Iceland, the Giant's Causeway and the Isle of Staffa (host to Fingal's Cave). The latter two are flood-basalts from the early rifting that led to the Atlantic Ocean. Iceland is on the junction of two oceanic-ridge constructive margins: the Mid-Atlantic and the Reykjanes, Ridges.
Please someone correct me if the latter name is wrong - I did that from memory!
At a divergent boundary tectonic plates move apart.
i believe its the rift valley
The region where tectonic plates move toward, apart or horizontally past one another.
When two plates move apart it forms a hole but new crust is formed.
Magma seeps up through the two plates from the mantle and form volcanos.
Long crack that forms as two tectonic plates move apart
At a divergent boundary tectonic plates move apart.
Tectonic plates interact at plate boundariesThey move apart at divergent boundaries
Oceanic trenches are the gaps which form when the tectonic plates move apart. They are the very deepest parts of the ocean.
is formed at a divergent plate boundary
A rift valley.
The plates move apart, which is called a divergent boundary.
Divergent Boundary
Earthquakes and Tsunami.
The tectonic plates move at about the same speed your finger nails grow. The gap the plates create when they move apart is constantly being closed up by magma moving up from the mantle.
i believe its the rift valley
The awnser is rift vally