Snowflake is a beautiful and interesting phenomenon in nature.

There are many interesting facts about snowflakes that you may not know.

1. Snow Isn't Simply White

It might surprise you to learn that snow and ice aren't white. While commonly perceived as such, this notion isn't entirely accurate. Those who have delved into the world of snowflakes understand that the "white" appearance is actually translucent.

The reflection of sunlight on the snowflakes makes them appear white. These polygonal ice crystals catch light from various angles, scattering the entire spectrum of colors.

Snowflakes exhibit a remarkable range of hues beyond white. dust, pollutants, or even freshwater algae with a penchant for chilly climes can transform snowflakes into shades of black, orange, or blue.

2. Formation around Core Particles

Snowflakes form around a central particle, be it dust or pollen.

The formation of snowflakes is therefore completely different from that of freezing rain (consisting of frozen raindrops) or hail (frozen raindrops that then combine with water as they fall). Advanced microscopy can be used to examine the original material that forms snowflakes.

3. Effects on Sound

Newly descended snowflakes are adept sound absorbers, ushering in a sense of serenity after the bustling commotion. Conversely, when snow melts and refreezes, the resultant ice can reflect sound waves, amplifying audibility and propagation.

4. Snow Terminology

It's often claimed that Inuit languages boast 50 words for snowflakes. This assertion, once considered speculative, has gained credence over time. Still, the Inuit's lexicon of snowflakes pales in comparison to that of the Scots.

Scholars attest to a staggering 421 snowflake-related expressions in the Scots' linguistic repertoire. Among these are terms like 'skelf' (denoting a substantial snowflake), 'spitters' (conveying minuscule snow whipped by the wind), and 'unbrak' (capturing the inception of snowmelt).

5. Snow on Mars

Scientific models crafted by NASA propose the possibility of sudden and substantial snowfall during the Martian summer in its northern regions. Given Mars' cloud cover and subterranean ice deposits, this envisaged snowfall isn't far-fetched.

6. Snow's Adaptability

Ordinarily, snow necessitates air temperatures hovering around freezing point for its formation. Yet, if prolonged rainfall engenders a drop in ambient temperature, a snow-conducive environment can manifest even if ground temperatures reach as high as 6 degrees Celsius.

7. Snowflakes in Swift Descent

Snowflakes descend leisurely or at speeds nearing 14 kilometers per hour, contingent upon atmospheric conditions. As these flakes plummet, they amass moisture, and gusts can accelerate their journey earthward. The span of an hour typically elapses from a snowflake's departure from clouds to its gentle landing below.