|| Snow is always changing. Snowflakes fall from the sky pointy and perfect, and once on Earth they take on a more practical shape. Temperature, wind, and weight all work to melt, move, form and deform the snowpack. Individual flakes turn into multi-faceted grains; a little round over here and a little square over there. Over time, these grains lock together to form the surface that bears our weight when we take a walk or ski down the mountain. Here’s a small piece of the larger puzzle, an individual grain from the Utah snowpack.
This grain was photographed against a 3mm snow classification grid on a BCA snow card. I used a 100mm 2.8 macro lens, a Canon 580ex in slave mode, and a Canon 7D. ||