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Antarctic Peninsula and Polar Circle 2020 Feb 10 2020 -13

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Ice is Nice – Glacier Fun Facts<br />

Gaby Pilson, Hiking Master & Expedition Guide<br />

Glaciers have, quite literally, shaped our world. Without glaciers, the rolling hills <strong>and</strong> wide valleys we know<br />

today would look very different, but it turns out that these icy giants have a much longer <strong>and</strong> more storied<br />

history than many of us would initially suspect. Here are some of the best fun facts about glaciers:<br />

11<br />

1<br />

Not just anything can be a glacier. In fact, there’s<br />

a size requirement that a piece of ice has to<br />

meet to become a glacier. Anything considered a<br />

glacier must be at least 0.1 km 2 (nearly 25 acres)<br />

in area to be worthy of the name. Although<br />

there’s a minimum size requirement to be<br />

considered a glacier, there’s no upper limit to<br />

glacierhood. The longest glacier on earth is the<br />

Lambert Glacier of <strong>Antarctic</strong>a, which measures<br />

out to some 434 km (270 mi) long. The world’s<br />

largest non-polar glacier is the Fedchenko<br />

Glacier of Tajikistan, which measures a<br />

respectable 77km (48mi) long.<br />

© Renato Granieri<br />

© Renato Granieri<br />

2<br />

Glaciers are formed by snowflakes. Although it’s<br />

crazy to think that a tiny snowflake can create<br />

something as large as a glacier, without snow,<br />

glaciers would never exist in the first place. To<br />

form a glacier, massive amounts of snow must<br />

accumulate <strong>and</strong> persist in a single location all<br />

year long for hundreds, if not thous<strong>and</strong>s of<br />

years. During this time, the individual snowflakes<br />

found in the snowpack change in a process<br />

known as snowflake metamorphosis, where<br />

individual ice grains fuse together <strong>and</strong> get bigger<br />

<strong>and</strong> air bubbles get smaller. Once the icepack<br />

builds up enough mass to start flowing downhill,<br />

then, voila! We have a glacier.<br />

3<br />

Glaciers are found all over the world, not just in<br />

the polar regions. While the majority of glaciers<br />

<strong>and</strong> glacial ice is concentrated in high northern<br />

<strong>and</strong> southern latitudes, glaciers are found even<br />

near the equator, such as on Mount Kilimanjaro<br />

in Tanzania <strong>and</strong> in the mountains of Ecuador.<br />

That being said, about half of the world’s<br />

200,000 glaciers are found in one place: Alaska.<br />

There, glaciers cover a whopping 72,500 km 2<br />

(28,000 mi 2 ) of the US state’s total area. That’s a<br />

lot of ice.<br />

© Werner Kruse<br />

4<br />

Glaciers are basically really, really, really slow-moving rivers. To be considered a glacier, a large mass of ice<br />

must be physically moving downhill. This movement downhill is driven by gravity <strong>and</strong> is the main reason<br />

why glaciers also act as major agents of erosion. Since glaciers move downhill, they often remove <strong>and</strong><br />

transport large boulders <strong>and</strong> chunks of rock, depositing them much further downhill then where they<br />

started.<br />

<strong>10</strong>-22 FEB <strong>2020</strong><br />

Volume 2, Issue <strong>13</strong>

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