how will you relate the distribution of mountain ranges with the distribution of earthquake

The distribution of mountain ranges is closely related to the distribution of earthquakes because both primarily occur at tectonic plate boundaries. Mountain ranges typically form at convergent plate boundaries where two plates collide, causing the Earth's crust to buckle and uplift. This tectonic interaction also generates significant stress and friction, leading to earthquakes in these regions. Therefore, earthquake epicenters often cluster along the same boundaries where mountain ranges are formed. Additionally, mountain ranges and earthquakes are linked through the dynamic processes of plate tectonics. For example, the Himalayas are a prominent mountain range formed by the collision of the Indian and Eurasian plates, and this region experiences frequent earthquakes due to ongoing plate movements. The intense geological activity involved in mountain building often results in both earthquakes and volcanic activity, especially at convergent and divergent boundaries. In summary, the distribution of mountain ranges and earthquakes is a direct consequence of tectonic plate interactions—where plates converge, mountains rise, and earthquakes occur along the zones of collision and stress release.