Blue Lagoon & Reykjavík

14 June

Reykjavík City Hall

Writing 2010.06.15.0135 Hotel Centrum, Reykjavík, Iceland

I woke up about an hour ago, and despite several games of sudoku, I still can’t get to sleep. The moderate twilight that passes for nighttime at these latitudes isn’t helping either, although I think the biggest culprit is that the room is too warm. Judging by the steady snores, Jonathan is deep in the sleep of exhaustion, as he got no sleep the two previous nights running. I’ve cracked open the window to let in some air to freshen the stuffy warmth. So in the meantime, I browsed the previous day’s pictures, and would like to catch up on the journal before our planned departure at 0800.

The flight into Keflavik was uneventful and not too long, about four and a half hours. The airport sits on a peninsula southwest of the capital on a wind-swept flatland. (I suspect that I’m going to be using that word - windswept - frequently.) We briefly met John H. on the plane - he sat directly behind us, while Diane H. was across the aisle.

Kristín collected us outside of customs where in addition to John, Diane, and Paul, we were joined by Margie V. and Shirley C. The main goal of the morning was the Blue Lagoon, but as our flight had arrived at ~0645, and the Lagoon doesn’t open until 0900, we had some time for the scenic route.

After loading our bags into the trailer, we boarded our medium sized bus, and headed southward along the coast. We passed the remnants of the old US army base now taken over by a local university that uses the housing for dormitories. Jonathan commented that the landscape between Keflavik and Reykjavik was a moonscape, and the region we drove through met that description. Kristín pointed out that the land we were passing was very young geologically and the elements had not yet worn the surface down to create topsoil. Most of the vegetation in the area was moss, lichens, and small grasses. Also present were many patches of lupine - an import from Alaska. Being a legume, the lupine fixes nitrogen and builds the soil, although Kristín reported that there was concern in some environmental quarters that it might dislodge some native species. So amid the moonscape, there were occasional sweeps of purple where the lupine was established.

Along the westward facing shore, we stopped at the rift, where it comes ashore. The “rift” is a remarkably brief word at odds with the magnitude of the phenomenon it describes. This is the location where the North American and Eurasian tectonic plates separate from each other moving in the opposite directions (about one inch per year at this location). Most of the rift lies under the Atlantic Ocean as the mid-Atlantic ridge, but it makes landfall in Iceland resulting in a landscape that is decorated with volcanic and geothermal sites.

The place we stopped looked like it was in the middle of nowhere - a road to a parking lot and a paved trail into the barren topography. However there was a small pedestrian bridge over a modest sized ravine. That ravine turned out to be a rift valley and the bridge technically spans two continents.

From the sign at the bridge:
According to the theory of continental drift, the earth’s crust is composed of 7-8 massive plates and several smaller ones. Constantly shifting, their edges move together, drift apart, and collide with each other, producing earthquakes, mountains, volcanic eruptions, and fault lines.
Where these plates meet under the world’s oceans, mountainranges up to 2,000 – 4,000 meters high and up to 70,000 km long rise up from the seabed, breaking to the surface in a few places. Where you are now standing is the meeting place of two such plates, the Reykjanes Ridge. Part of the larger North Atlantic Ridge, it is the meeting place of two continents; North America to the west, and Eurasia to the east.
Directly ahead of you, the plates are drifting apart at an average rate of about 2 cm each year. Even as your read this, the one on which you stand is moving at a rate of about 1 cm per year to the northwest, while the other is edging southeast at the same speed. Between these plates run rivers of molten rock, which solidify as lava when they reach the surface. At the same time, faults and crevasses are formed in gaps between the plates due to the massive horizontal and vertical forces being constantly exerted on them.
Earthquakes and volcanic eruptions produced by this continuous movement occur in clusters which may last from anything from a few years to several decades, followed by centuries of relative calm. Looking up towards the lighthouse and hot springs, many of the lava fields you see were formed during the last eruptions phase of the Reykjanes Fault, which occurred in the early years of the 13th century.
Several more submarine eruptions have taken place on the Reykjanes Ridge in our own century, although no new islands have been formed. In 1783, one did rise to the surface just of Eldey, and was given the name Nyey (New Island). Composed of only volcanic ash, it was swept back beneath the waves, however, by the storms of the following winter.
The Reykjanes Ridge is still a highly active volcanic zone, and fire from deep in the earth will undoubtedly once again burst to the surface in the area which you now see. Just exactly where – or when – is a question no one can answer.

From the rift we headed on to one of those geothermal sites, the Blue Lagoon. The Blue Lagoon is actually a man-made attraction that arose from the geothermal electric plant. The spent hot water was pumped into these lagoons as waste, however the workers at the plant enjoyed bathing and swimming in the warm water. They also found that the high mineral content was beneficial in treating psoriasis and other skin conditions. So the site has a very nice spa and restaurant. We still arrived before the the lagoon itself opened for swimming and bathing, but the coffee shop was open so Jonathan and I were able to grab some breakfast as non had been provided on the flight.

The water in the lagoon is milky white with a blue tint - visibility into the water is only an inch or so. Although the lagoon was created in a lava field the bottom is sandy and frequently feels like a smooth glass surface. The reason for that occasional smoothness is visible around the water’s edge where the white silicates have precipitated on the black stone of the lava. The depth of water varied but was never over my head - and it was usually about half that.

We lounged in the warm water for an hour or so - I chose to forego smearing my face with the silica paste that has such restorative powers. We boarded the bus to head to Reykjavik along with four additional walkers who had joined us for our dip into the Blue Lagoon - Ronnie D, Kevin B, Gisele C, and Jerye M. As we drove into Reykjavík, the landscape transitioned abruptly from moonscape to green.

After checking into the hotel, and getting our assortment of battery chargers set up, we walked through Reykjavík with our guides Kristín and Erling pointing out sites of interest. This tour was interrupted by lunch featuring a sampler of Icelandic cuisine - fish casserole, smoked lamb, and fresh fish.

Click on the images for a larger view

The walkway that appeared to lead to nowhere.

The rift.

No explanation needed.

The pathway from the parking lot through the lava fields to the spa.

Outside the spa, the milky blue-tinted water amid the piles of lava.

Another view.

After taking our dip, wereconvened in the coffee shop. The structure in the middle distance is a swim-up bar.

Our hotel in Reykjavík - it was downtown and convenient to many attractions and restaurants.

I forget who this stern faced fellow is, but the sculptor gave him a scowl worthy of biting into a lemon.

A local feline - taken with a sense of melancholy, as we had lost one of ours, Argo, the week before (*sniff*).

Erling, Paul, Jerye, and Kristín - the durable corrugated iron siding is typical.

Jonathan takes a snap, obscuring John, in front of another iron-clad house in a bright color.

The first Icelandic poppies are spotted.

A colorful arrangement of flowers (and cat statuary) in front of a local home.

Evidence! Lunch included the fish casserole in the mason jar.

Writing 2010.06.15.1810 Hotel Rangá, between Hella and Hvolsvöllur, Iceland

After lunch we walked to the top of the hill where the new Hallgrímskirkja church is located. It’s an impressive modern work in concrete that seems appropriately designed in this northern environment. The interior is well lit by windows with little stained glass. From there we walked back down the hill to city hall, which is situated on (and perhaps half in) the pond. There is a parliament of waterfowl on the pond with seagulls, ducks of various types, geese, and swans. Inside, there is a large topographical map of the island that Erling used to describe the upcoming tour. After leading us back to the hotel, we were on our own for dinner.

Click on the images for a larger view

The parliament building.

Hallgrímskrkja - the external motifs were taken from the Icelandic landscape. The statue in front is Leif Erikson.

Inside was light and airy.

The pipes of the organ.

The baptismal font was a stylish creation in glass.

I thought the two-way pews were a neat innovation.

The stained glass in the doors was about all that was present.

The vestibule is used as a gallery to display the work of local artists.

A view to show the structure behind the main façade.

'The Pearl' stores the geothermally heated water for circulation to local homes and businesses.

City hall sits on the pond (Tjörn) that's a favorite of the local waterfowl.

A sampler - arctic tern, eider duck (the black and white one on the water) mallards, a goose, and a swan (at top).

More waterfowl with the swans in the picture.

Erling uses the topographical map in City Hall to describe the upcoming tour.

One of the restaurants Kristín recommended was the Fish Company (Fiskfélagið), which was located in the basement of a building less than a five minute walk from the hotel. The curtains were “sweaters” of knitted wool in the dimensions of the window, and the tie-backs were in the shape of two arms of a sweater. I had an appetizer of pork belly with gnocchi, spicy chorizo, and potatoes with a black olive puree, followed by a slow cooked salmon with an Asian inspired sauce reminiscent of teriyaki accompanied by corn in three forms - meal, kernel, and popped. The portions were generous and I wish we had shared or skipped the appetizer as I couldn’t finish the salmon which was very good. I commented to Jonathan that the chef was obviously being creative, but I found the output a bit “fussy”. Also, I don’t get “foam” on the dinner plate – it has got to be the silliest culinary trend going today.

I took the image above off a display in the visitor center at Skaftafell National Park (on the 17th) showing the volcanic systems of Iceland. I "unskewed" the image, filled in some blank areas around the edge resulting, and violá - an image I can use to show where were were (approximately). I added the yellow dots and yellow location text, everything else came from the original display.
So today, we stopped at the Blue Lagoon and Reykjavík.