The Mid-Atlantic-Ridge is where two of Earth's plates split apart. The Mid-Atlantic-Ridge was formed along a divergent boundary where seafloor spreading is taking place.
Earthquakes usually occur around faultlines or plate boundaries because that's where plates split apart a long time ago. When two plates collide they form earthquakes.
At the boundry of two tectonic plates, you get volcanoes, earthquake epicentres and ( if its under the ocean) tsunamis.
A volcano will form at the boundary of two plates moving apart. This is because the two plates moving apart create a crack allowing molten lava to flow up from the mantle.
Continental Plates
Iceland is the mid-Atlantic country being split apart by the movement of the North American and Eurasian tectonic plates. The country's unique geological setting along the Mid-Atlantic Ridge results in active volcanic and geothermal activity, as well as gradual separation of the two tectonic plates.
The Earths surface changes shape when plates collide when the earths surface overlaps or when there are Earthquakes.
When two plates are pulling apart, it is known as divergent boundary or divergent plate boundary. This type of boundary results in the formation of new crust as magma rises to the surface and solidifies.
when two plates split and go away from eachother
earthquake!!!!!!
Divergent plate boundaries form once two plates begin to pull apart from each other.
Divergent Boundaries happen when two plates (oceanic or contental) begin to diverge, or move apart. Convergent Boundaries occur when two plates (again, oceanic or contential) begin to converge or move apart
Iceland is split by two tectonic plates, the North American Plate and the Eurasian Plate. This geological feature is visible at Thingvellir National Park, where a rift valley showcases the boundary between the plates.