Why It’s Called a Grassland

Look what happens! The grass grows, and dries in the sun, to catch the snow. No snow. A raven, though! But look…

… then it snows.

Now the grass is bent in an arc, down to the soil. The energy shift continues. Watch.

The even snowfall is soon uneven, built around structures created by grass, all with exposed faces collecting heat and lee faces collecting cold.

But there’s more! Soon, the hill, one even gradient of soil, becomes a series of waves.

Beautiful waves. Waves created by grass built to bend to the wind. Now it is bending the snow that is carried on the wind. That’s the same thing, isn’t it?

A day later, and the sun begins to work on the faces of heat and cold the grass has made out of the wind.

It creates miniature avalanches, slumps, and flow patterns in the snow, deepening wells and extending connective membranes. The snow will melt in these patterns. But that’s not all!

The grass also guides the deer. The grass turns them into wind.

They follow its patterns. So does the sun. Look at it, spilling between these clumps of snow buckwheat, which are holding the snow.

Just as the deer’s trails are made at the intersection of their angular anatomy, grass and gravity, so are the sun’s trails made at the intersection of their expansive planes, grass and the form of gravity known as exposure. The sun’s trails are flat. Look how grass makes dimension out of this flat world. The tiny avalanches in the image below show the grass at work.

The summer that will build new stalks of grass to harvest and sculpt the sun into the following spring’s water starts here, at first snow.

By the time spring comes along, most of the preparation has been done. Grassland people, this is your snow:

4 thoughts on “Why It’s Called a Grassland

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