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The **vivid colors** of the **aurora borealis** are one of the most mesmerizing aspects of the display. But what causes the different hues we see? The answer lies in the composition of our atmosphere. The most common color is green, which is produced by oxygen molecules at lower altitudes. Red, also produced by oxygen, appears at higher altitudes. Blue and purple are produced by nitrogen. Sometimes you'll even see a combination of colors, creating a truly spectacular sight. It's all about the type of gases and the altitude at which they are being excited by the charged particles. It is like the best **light show** on Earth, completely free and put on by the sun. It's like a cosmic paintbrush swirling across the night sky, creating a masterpiece that changes by the second. And it's not just the colors, but the shapes and patterns. Sometimes it looks like curtains of light, other times like swirling ribbons or flickering flames. It's a dynamic and ever-changing display, which makes it even more captivating. The colors are truly magical, turning the night sky into a canvas of wonder. If you were lucky enough to see the **green aurora** last night, you witnessed the most common and often brightest color. This is due to the abundance of oxygen in the lower atmosphere. The **red aurora**, on the other hand, is a bit rarer and appears at higher altitudes. And if you spotted the **blue aurora** or **purple aurora**, consider yourself extremely lucky. These colors are produced by nitrogen and are often more subtle. The **aurora**'s palette is a result of **space weather** at its finest.
