The natural phenomenon associated with the aurora borealis is solar activity, particularly solar wind. The aurora, commonly known as the Northern Lights, occurs when charged particles from the sun collide with Earth’s magnetic field and atmosphere. These collisions excite atmospheric gases, causing them to emit light and create the stunning displays of color that characterize the aurora. This phenomenon typically occurs in high-latitude regions, such as northern Canada, Scandinavia, and Alaska. The aurora borealis showcases the interplay between solar dynamics and Earth’s magnetic field, offering a breathtaking visual experience.