Every named region is a tectonic plate.
Every glowing point is where two of them meet.
Earth's outer shell isn't one solid piece. It's cracked into large, rigid slabs of rock called tectonic plates, drifting slowly over the softer, hotter rock beneath them.
Almost every earthquake, volcano, and mountain range traces back to what's happening at a plate boundary — exactly what each glowing point on the globe above shows in motion.