Distinctive Striping Pattern in Siberia Puzzles Researchers

Central Siberian Plateau September 2016

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September 15, 2016

Researchers are confusing over an unique striping pattern in the Central Siberian Plateau.

Earth science satellites are typically utilized to observe particular functions of the world—landforms, climatic chemistry, ocean patterns. But at the very same time, they regularly reveal us things that couple of individuals have actually seen and even searched for.

In February 2020, our group saw a twitter message with a strange and stunning image from Russia near 66 degrees north latitude. It became a clinical investigator story and an unsettled case.

Central Siberian Plateau October 2020

October 29, 2020

In the images above and listed below, obtained by the Operational Land Imager (OLI) on Landsat 8, stripe patterns weave around the hills of the northern Central Siberian Plateau. On steeper hills, the stripes form tight loops that spiral from the top of the hill to the bottom. As they come down towards the riverbanks, they begin to fade. Eventually, the stripes vanish at lower elevations and at latitudes.

There are numerous possible causes for the distinct striping pattern, and the responses differ by the season and by the competence of the scientist.

Central Siberian Plateau Summer Fall Winter

September 15, 2016 – October 29, 2020

This part of the Central Siberian Plateau lies within the Arctic Circle, where air temperature levels stay listed below freezing for the majority of the year. Much of the landscape is covered in permafrost that can extend 10s to numerous meters listed below the surface area. There are various levels of strength, however this location typically has permafrost protection for 90 percent of the year.

The land does periodically thaw, and cycles of freezing and thawing are understood to produce polygon, circle, and stripe patterns on the surface area (described as “patterned ground”). In the case of the images above, the stripes might be lengthened circles extended on the slopes by such thawing cycles. Yet research studies have actually revealed that this kind of striping generally takes place at a much smaller sized scale and tends to be oriented downslope.

To geomorphologists, the nature of the soil provides another description for the stripes. In areas this cold, soils can become Gelisols—soils with permafrost in their leading 2 meters and typically with darker and lighter layers identified by more raw material or more mineral and sediment material. As the ground freezes and defrosts, the layers separate and blend vertically in a procedure called cryoturbation. The consistent freezing and defrosting action through the seasons can trigger layers to line up in a striping pattern. Different tundra plants—lichens, low shrubs, and moss—may grow preferentially on these Gelisol layers, highlighting the stripes we see from above. But this hypothesis has actually not been shown at big scales.

From a geologist’s point of view, the various stripes appear comparable to sedimentary rock layers. Thomas Crafford of the U.S. Geological Survey called the pattern “layer cake geology,” where sedimentary rock layers have actually been exposed and dissected by disintegration. As snowmelt or rain takes a trip downhill, pieces of sedimentary rock are cracked away and sent out down to the gorges listed below. Such disintegration might trigger a step-like pattern that looks like stripes from area comparable to a piece of layer cake. This pattern is likewise described as “cliff and bench topography.”

Cliff and Bench Topography


In the winter season Landsat image at the top of the page, snow triggers the striping pattern to stand apart more than in other seasons. The benches would be the lighter stripes (covered in snow) and the cliffs would be darker stripes. The Arctic digital elevation map above, based upon information from the ArcticDEM Project, offers a clearer point of view on the possible cliff and bench functions.

Cliff Bench Topography


“It looks like small canyons, maybe like the Badlands of South Dakota. The horizontal striping appears to be different layers of sedimentary rock,” stated Walt Meier, an ice expert at the U.S. National Snow and Ice Data Center. “The shape of the erosion pattern looks a bit different than standard sedimentary erosion, but my guess is that is due to the permafrost. The rivers are eroding through frozen ground. There could also be some effect from frost heaves affecting the topography.”

Several rivers crossed the plateau, consisting of the Markha, and as the stripe pattern moves closer to the river, it begins to fade. This might be an outcome of sediment accumulation along the riverbanks from countless years of disintegration.

Louise Farquharson, an Arctic geologist at the University of Alaska-Fairbanks, indicated an area in northern Alaska with a really comparable stripe pattern that might be formed by a comparable procedure.

NASA Earth Observatory images by Joshua Stevens, utilizing Landsat information from the U.S. Geological Survey and topographic details from the ArcticDEM Project at the Polar Geospatial Center, University of Minnesota. Story by Andi Brinn Thomas, with Mike Carlowicz.

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