The Northern Lights, or Aurora Borealis, are natural light displays that occur when charged particles from the Sun interact with Earth’s magnetic field and atmosphere. These glowing patterns of green, red, and purple light are typically seen in high-latitude regions near the Arctic. The aurora forms when solar particles collide with oxygen and nitrogen high in the atmosphere, releasing energy as light. Each display is shaped by the solar wind, Earth’s magnetic field, and atmospheric conditions—making every aurora unique. Capturing the Northern Lights requires clear, dark skies and a bit of patience, but the result is a glimpse into the dynamic connection between our planet and the Sun.
