I am so desperately far behind on blogging on travel, which was the original point of this blog a decade ago. So, I suspect there's going to be a mad rush of blog posts about a number of trips, without nearly enough commentary, with the hope being that in a less chaotic time I'll come back and add more detailed and mature reflection.
Here's a picture I snapped in Iceland. The American and Eurasian tectonic plates run through Iceland, which helps explain the island's seismic activity (including a mild series of earthquakes when my son and I were visiting). There is a bridge, fairly close to the airport in the far southwest of the island, where you can stand on a bridge connecting the two plates. Apparently you can also arrange to dive between the two plates, although I've forgotten whether it is in the north or the south of the island. The gap between the tectonic plates enters Iceland around 8:00 o'clock and exits around 12:00 o'clock, if you view the island as a clock face.
Here's a picture I snapped in Iceland. The American and Eurasian tectonic plates run through Iceland, which helps explain the island's seismic activity (including a mild series of earthquakes when my son and I were visiting). There is a bridge, fairly close to the airport in the far southwest of the island, where you can stand on a bridge connecting the two plates. Apparently you can also arrange to dive between the two plates, although I've forgotten whether it is in the north or the south of the island. The gap between the tectonic plates enters Iceland around 8:00 o'clock and exits around 12:00 o'clock, if you view the island as a clock face.
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