Divergent plate boundaries are regions where two tectonic plates move away from each other. This movement creates a gap that allows magma to rise from the mantle and form new volcanic activity. The most notable volcanoes found along these boundaries are located at mid-ocean ridges, such as the Mid-Atlantic Ridge.
One prominent example of a volcano located on a divergent plate boundary is the Eyjafjallajökull in Iceland. Iceland sits on the Mid-Atlantic Ridge, making it a hotspot for volcanic activity due to the continuous separation of the North American and Eurasian Plates. Other examples include the Snæfellsjökull and Krýsuvík volcanic systems in Iceland.
Additionally, divergent boundaries are not limited to oceanic settings. The East African Rift is another example where continental divergence is happening, leading to the formation of rift volcanoes such as Mount Kilimanjaro and Mount Meru.
Overall, volcanoes along divergent plate boundaries typically produce basaltic lava, which is relatively low in viscosity. This results in less explosive eruptions compared to those found at convergent plate boundaries, where tectonic plates collide.