This is something very interesting when just like rainwater dissolves the bedrock on the Earth’s crust and produce sinkholes. And its meltwater on a glacier’s surface can melt ice and form sinkholes too. Sinkholes on glaciers are often called Moulin’s, French for mill. Moulin’s form when summer melts water streams on the surface of the glacier uncovers a crevasse or other weak spot in the ice and begins to pour down through the ice.

As the water moves downward, it’s turbulence and heat generates a narrow, tubular and vertical shaft, up to ten meters wide. That can go all the way down to the bottom of the glacier, hundreds of meters deep. Water entering a Moulin and eventually exits the glacier at a base level. Where it acts like a lubricating fluid that plays a huge role in how fast the glacier flows.

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The melting water accelerates the glacier’s flow to the sea. Where large chunks break off to form icebergs. Then leading to farther ice loss by speeding disintegration of the ice sheet. Given sufficient water flow, a Moulin’s can straightforwardly form over the course of just a month. This was once formed; the shaft will stay open as long as there’s meltwater to feed the Moulin.

If the meltwater freezes, the Moulin’s will start to fill up with snow and close up. Moreover, few Moulin’s have been observed to be present in a similar spot for numerous years. However, the spot will continually move forward with the flow of the ice. 

Also Read: Soda and Salt Lake Natron in Tanzania

A hiker descends inside a moulin, Greenland
A hiker descends inside a moulin, Greenland
A hiker stands next to a massive moulin on Snowbird Glacier.
A hiker stands next to a massive moulin on Snowbird Glacier.

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An explorer scaling a moulin on Mer de Glace glacier in Chamonix, France.
An explorer scaling a moulin on Mer de Glace glacier in Chamonix, France.
An explorer scaling a moulin on Mer de Glace glacier in Chamonix, France1.
An explorer scaling a moulin on Mer de Glace glacier in Chamonix, France1.
Meltwater pouring into a moulin on Greenland.
Meltwater pouring into a moulin on Greenland.
Schematic drawing of glacial features illustrating how moulins transport surface water to the base of the glacier.
Schematic drawing of glacial features illustrating how moulins transport surface water to the base of the glacier.
Surface water entering a moulin on Athabasca Glacier.
Surface water entering a moulin on Athabasca Glacier.
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Originally posted 2017-12-21 17:19:38.

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