But here in the Arctic, we have geology.
From our portholes on the Lyubov Orlova, we glimpse the steep cliffs and bleak hills of Devon Island (largest uninhabited island on earth, used for Mars-simulation exercises), Bylot Island, and Baffin Island.
It is an abstract landscape, forbidding and secretive. Or so it seems from the ship.
On land, geology becomes the storyteller. We go ashore in the zodiacs (all landings are “wet landings”) and realize that we are standing upon a vast field of polygonal humps in the tundra, frost boils created by millennia of freezing and thawing: the frost-heaving tosses up rocks and then they settle in a pattern as elaborate and defined as a honeycomb.
Frost boils are the commonest form of patterned ground in the Arctic, but you should not think less of them for that.
Pingos are larger and have the character of archeological remnants. They are conical hills with solid clear ice at their center, and I long to use the word in Scrabble. Occasionally someone will mistake a palsa for a young pingo, but that would be a mistake because at its core the palsa has frozen peat. We did not see any palsas so I could not embarrass myself by misidentifying it as a pingo. We did cross landscapes of lumpy peat mounds, spongy hummocks that defied one’s knees, not unlike moguls.
1 comment:
I love these posts, with all their new words like pingos.
Did you know that Emily Dickinson read about Franklin's disappearance and the endless searches for his remains in "The Atlantic Monthly" in the 1850s? Apparently, she was completely fascinated by the story.
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