Friday, July 30
The name says it all: Myvatn, lake of the midges. Thank god that, unlike the no-see-ums that can plague us in Maine, these little critters don’t bite. They just fly into your mouth, eyes, ears, you name it. We of course both brought midge nets to wear over a hat, but do we think to put them in the car? Of course not.
We woke to sunny, cloudless skies in Sey∂isfjör∂ur…and I mean woke. That’s the main building of the Hotel Aldan behind me, with the reception and two restaurants. By the way, for you gear geeks, I’m modeling a, if I do say so myself, very cool “tech” Icelandic sweater by the iconic Icelandic gear manufacturer 66 Degrees North. What makes it tech? A layer of Gore-Tex Windstopper beneath two layers of Icelandic wool. Not for summer in New Jersey!

The rooms in our building—the “Old Bank”—had been modernized but retained a lot of their old charm. But this was also the first place we had stayed without blackout curtains. So when I awoke, I thought it must be noon…but it was 4 AM. Luckily we were both able to go back to sleep once we’d been startled by the morning light.
The drive over the mountain pass was even more beautiful in this light, and we were soon in search of a bit of breakfast in Edilsta∂ir…which we found in a charming, funky bakery filled with books.
The road toward Myvatn passed at first through rolling green farmland, but soon entered yet another vast lava plane, with utter desolation. Looking south, an unusual mountain comes into view. Sue described it as a tent, I as a cloche.

This is Her∂ubrei∂, called Queen of Iceland’s mountains and beloved of the locals. It, too, is an extinct volcano; the climb to the summit is technical.
Turning north, we headed for a deep gorge that bisects the plain. There is a mile-long path from a car park toward Dettifoss, a huge waterfall in the middle of nowhere. Looking at the surrounding area, it is hard to believe that there is water nearby.

But water there is…and lots of it. As we turned a corner and came down a small slope, we were greeted with a rainbow.

And then we saw the falls.

Depending on who you talk to, Dettifoss is either the biggest or the second biggest falls in Europe (the Rhine Falls at Schaffhausen in Switzerland may have a higher volume / minute ratio, but they are not nearly as impressive). The power of the falls is so massive that it throws up spray hundreds of yards away; believe me, we felt it.
Another half mile up the gorge is a smaller but more beautiful waterfall, Selfoss.

We were on the “wrong” bank of the gorge to really see Selfoss. Here is what it looks like from the east bank.

Back on the ring road, we were now very close to Myvatn, but there were adventures in between. Just before crossing a low mountain pass, a road leads north into a valley dominated by the volcano Kafla. The Kafla system is underlain by a large magma chamber, producing a variety of geothermal effects above ground. We first passed one of Iceland’s largest geothermal power plants, but then the road rose up and on our left was a low rhyolite hill that we learned was called Clay Hill. The rhyolite from a previous eruption had been heated by geothermal heat and turned to clay over large stretches. A path leads through the lava field created during a nine-year period of eruptions beginning in 1975.


As we walked up through the rhyolite, we found active geothermal features: fumaroles, steam vents, and thermal pools.


The lava field was unusually interesting; the molten lava had flowed in relatively narrow bands, twisting their way down the hill.

At places you could see where the basalt lava had flowed over the previous rhyolite.

From the top of the hill there are splendid views of the main volcano, Kafla.

At the far left of this photo you’ll see what seems to be a large depression. That is one of the main craters, Viti, which has a small lake at its deep center. Vivi and Iggles might be tempted to hop in, but we think they’d find it a bit too hot!

Across the ring road is one final piece of this vast system, a geothermal area called Hverir. This is a readily accessible collection of boiling pots, vents, and fumaroles set against a brilliant rhyolite slope.


The video below suggests why you’re urged to keep your distance: the pools are not just hot…they contain sulphuric acid.
We reached our hotel for the next two days soon afterwards. The Fosshotel Mytvan is brand new and rather lovely. Our room is very comfortable and has a terrific view of the entire lake. Our room even has a balcony, but the midges got there first and seem to be enjoying themselves.
The restaurant has a huge wall of glass with a panoramic view of the region. From our table we saw not just the flattop mountains—volcanos with their lids blown off—that characterize the countryside around the lake, but, in the distance, one last glacier…an outlet glacier from Vatna that is so huge that it stands out from 80 kilometers away. If you expand the photo below, you can just see the glacier to the right of the dark hill in the middle.

Although they’re sitting just out of view, there were several very young children in the dining room, and of course we always imagine Nathaniel sitting near us!
So this was a truly Icelandic day: waterfalls, volcanos, and a glacier thrown in for good behavior.








































