Nature’s lil cinnamon rolls

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Nature’s lil cinnamon rolls

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What in the world is this? It’s a snow roller (aka snow bale), formed when a thin layer of snow atop ice is pushed by the wind, almost as if someone was making a snowman. But there are no humans involved, just nature. Freaky and fabulous, yes?
Do you want to build a snowman? If you do, you may be lucky and get a bit of a hand from nature. Shown here are what is known as snow rollers; a rare, but beautiful phenomenon. In order for a snow roller to form, some optimum conditions must be present. Firstly, the ground must be covered in a layer of ice to ensure the snow doesn’t stick, but sits, and has freedom to move. Next, the snow must not be tightly packed and the wind conditions must encourage movement but not break the weak, starting layers. For an added boost, a downward slope is preferable. If all these factors occur, a snow roller is born, with layers getting progressively thicker and taking on a cylindrical shape. As they grow, the less compact ice in the centre often blows out, creating a doughnut effect as shown in this image. -Jean Photo by:https://www.flickr.com/photos/jahdakinebrah/
Snow roller in Wiltshire (Brian Bayliss)

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Snow roller.
From Earth Science Picture of the Day; February 19, 2017:
Archive - Snow Roller
Each Sunday we present a notable item from our archives. This EPOD was originally published February 17, 2003.
Referred By and Summary Author: Michael Ellestad
Snow rollers occur when there is powdery snow on the ground and on top of that a layer of wet and very sticky snow. A gust of wind will lift up the wet snow from the dry and roll it into a cylindrical mass resembling a roll of insulation. Sometimes the rolls will be hollow, but these are solid. The largest one at the bottom of the picture measures 9 inches (23 cm) in diameter. These snow rollers were spotted in Adams County, Ohio last week.
Related Links:
Snow Roller
What Is A "Snow Roller"
Snow Rollers on the Camas Prairie
Ohio Rollers
Snow Donuts
During winter throughout the United States, one could have found snow rolls or “snow donuts” much like these in many regions of the Appalachian Mountains. Snow donuts accumulate when sticky but light weighted snow precipitate in windy conditions. In order to accumulate, the snow must exist on a layer of ice and be wet and light in weight. The snow must also be around 0 degrees C (32 degrees F). The formations come to be by accumulating, rolling in the shape/direction of the wind, then accumulating a bit more, freezing, and rolling, and so on. The conditions have to be absolutely perfect in order for these rare formations to occur so witnessing them in nature can be a difficult and an exciting feat.
--Pete D
Photo Credit: http://bit.ly/1fhmvYH
References: 1. http://www.wrh.noaa.gov/otx/photo_gallery/snow_rollers.php 2. http://www.huffingtonpost.com/2014/01/07/us-cold-weather-_n_4557877.html 3. http://www.washingtonpost.com/world/photos-of-the-day/2014/01/28/34f899ca-881a-11e3-916e-e01534b1e132_gallery.html#photo=4