Why La Palma is Like This vol. I: The Seamount that Soared

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Now that we’ve got the geologic context of the Canary Islands as a whole figured out, it’s time to zero in on La Palma. How did she get here? Why are all the recent eruptions happening only on one half of her? What might be in store for the future? Does the fact that the most recent eruption is the longest and most voluminous of her entire recorded history mean the island is doomed? And is her active volcanic ridge, Cumbre Vieja, going to fall into the ocean and wipe out the East Coast of North America?

(I won’t keep you in suspense on that last one: the answer is almost certainly a resounding no. So while we’ll talk a bit about former collapses that have shaped the island, we won’t be spending any time on the megatsunami theory. Sorry not sorry.)

A Brief History of La Palma

La Palma is the second-youngest Canary island, and is still growing. She is, in fact, the most vigorously volcanic of the Canary Islands, boasting the most eruptions on record since the Spanish settlers arrived. And that’s just the last 500-ish years of her history: she’s actually about four million years old, if you count from her birth as a bouncing baby seamount. Nearly all of those years involve very hot rocks. (more…)