Where Does Santa Get His Coal?


Santa has a source on an icy Arctic island!

Where Does Santa Get His Coal?
Credit: Dana Hunter

Were you naughty (or lucky) enough to get some coal in your stocking this Christmas? Congratulations! Coal is a fascinating rock and tells us a lot about the geology of ages past in the locations where it’s found.

You probably wouldn’t expect Santa to be able to locally source his coal – after all, it’s a rock that requires swampy or marshy areas with lots of lush plants. That’s not really what you find around the North Pole! But a mere 650 miles away, halfway to Norway, you’ll find an island that provides all the coal Santa would ever need. It’s the glacier-capped island of Svalbard, and Santa wouldn’t even have had to go digging when he first went looking for coal. It was right in plain sight:

On the west side of the main island Spitsbergen, the coal seams are exposed in the mountain sides on several locations, especially around the large fiord called Isfjorden in the center of the island. These coal outcrops were easy to discover for Europeans familiar with the visual appearance of coal. The Svalbard coal was first mentioned by the whale hunters of the 17th century, who used it on board their ships.

You wouldn’t be thinking of coal when you first land on the island. It’s a tiny bit warmer than other locations in its latitude, but it’s still very Arctic in its climate. The growing season can be measured in weeks rather than months some years. Plants don’t have a lot of time to grow. You won’t find densely populated marshes or swamps. So how did the coal get here?

A combination of climate change and plate tectonics provides the answer.

Svalbard is a well-traveled island. We don’t know all the places on Earth it’s been, but we do know that six hundred million years ago, it was chilling – literally – around the South Pole. Over the past half-billion years, it’s gradually made its way north, with a layover near the equator in the Devonian. Icy Antarctic deserts became blazing hot equatorial deserts for a time. In the early Carboniferous, Svalbard had crept back into the tropics, and newly-evolved plants took full advantage, flourishing in verdant swamps.

The swamps of Carboniferous Svalbard have no modern analogue anywhere in the world: not only were seedless plants and ferns extremely important in this community, but there were no birds singing or insects with humming wings. Birds did not emerge until Jurassic times 100 million years later, and all insects of the Carboniferous swamps had fixed wings.

As Svalbard continued its long travels north, the swamps were buried under sediment, and the plant matter compressed and gently cooked into coal.

But this isn’t the Arctic coal we’re looking for. It’s in the Arctic now, but it formed a long time ago and very far away. However, Svalbard is home to coal that formed either very close to or within the Arctic circle! Let’s zip forward to the Paleogene, around 60 million years ago, when Svalbard had reached a latitude of 65-68° N. You’d think, straddling the Arctic Circle, it would have been too cold for coal, but this was an epoch where temperatures on Earth were much higher than they are today. Svalbard was warm, humid, and with tectonic forces creating a deep basin, a perfect location for coal-creating plants to flourish. The coastal plain hosted thick peat mires that could stretch more than three miles across. They often became raised mires, which held back the encroaching sea and allowed even thicker peat to accumulate. Occasionally, the mires flooded and became swamps. All of that plant material then found itself buried under sediments, where it formed 100% Made-in-the-Arctic coal.

Later erosion and uplift would reveal coal seams that Santa could access with ease, even before the mines that powered the region opened. And Santa won’t have any trouble collecting locally-sourced coal even with most of the mines shutting down: if he can make it down a chimney safely, I’m certain he can visit old mineshafts without any problems.

So if you got coal in your stocking this year, celebrate it! It’s a rare example of the fact that coal can form in some very unlikely places, given the right conditions.

300-Million-Year-Old Tooth Wheel Found In Russian Coal.


s-UFO-TOOTH-WHEEL-largeThe Earth was so young 300 million years ago, the first land animals had yet to evolve into dinosaurs, most scientists believe.

If that’s the case, how do you explain the discovery in Russia of a piece of a gear shift — a common machine part — embedded into a hunk of 300-million-year-old coal. Has this artifact been correctly identified? And if so, who could have made this thing? And for what purpose?

According to Komsomolskaya Pravda, a resident of Vladivostok — near the borders of China and North Korea — named Dmitry, recently noticed something odd about a hunk of coal he had obtained to heat his home during the winter.

A metallic-looking rail or rod was pressed into the coal, prompting Dmitry to contact biologist Valery Brier, in the seaside Primorye region.

Initial examination of the strange object led researchers to assert it looked “very much like a toothed metal rail, created artificially. It was like parts [that] are often used in microscopes, various technical and electronic devices,” wrote Komsomolskaya Pravda.

The piece of coal in question originated from the Chernogorodskiy mines of the Khakasis region. The Voice of Russia, an international Russian broadcasting service, reported that since the coal deposits in this region of the country can be dated to 300 million years ago, experts are suggesting that the odd piece of metal found in the coal must be that old as well.

The Voice of Russia also said, “When geologists broke the piece of coal in which the metal object was pressed into and spot-treated it with special chemical agents, it turned out the the metal detail was unusually light and soft. … [It] was found to be composed of 98 percent aluminum and 2 percent magnesium,” which led to the implication that the metallic object was created artificially.

Source:huffingtonpost.com

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