Reykjavik |
Coming in to Keflavik |
Reykjavik
So, we booked the Hotel Klettur in Reykjavik and a shuttle to get us there from the airport.
Photo: Booking.com |
We figured it would be easy just to return to the same place. After the Greenland trip cancelled, I saw no need to change.
I have no strong preferences for hotels in Reykjavik. Had we not had a car to pick up in town, I might have skipped Reykjavik altogether. I had been there several times before and, with COVID, we were avoiding people.
Interesting rocks in the Hotel Klettur's lower level; Photo: Booking.com |
The Hotel Klettur room was small and the hotel was a bit away from the tourist areas (hence not as many restaurants nearby), but it was clean and serviceable and the staff was quite nice.
The room was a typical European hotel room; Photo: Booking.com |
Our rental car was set to be picked up in the early afternoon and, although I had planned on cabbing it, Scott wanted to walk! I never saw that coming. It was about two miles, most of it on a walking path by a major highway.
The day was quite a bit warmer than one would have expected for Iceland (I was rethinking all my packing and dying for some iced tea). The route didn’t have many food options, so we ended up eating smash burgers at a fast-food place that didn’t have ice for the drinks.
Just tell us the right place! |
Oddly, this has happened to us before, despite that the address we walked to was listed on all the confirmations and the Europcar website (heck, they even had directions!).
All they had was a hand-printed paper note taped to the door. The new location was another mile-ish.
Quite a hike! |
The map held up for the full trip |
I expected it to be a situation where they activate the in-car navigation system. Instead it was an ancient Garmin – the same model we had when GPS first became available.
We did use it a few times, but generally found our phones to be better.
And, I had an excellent map that I used most of the time. As it turns out, we never incurred additional data charges, so I think using our own is better. I don’t think I’ll rent a GPS in the future.
The only way to pay is via a cell phone |
There were places – mainly in Vestfirðir – where there was no service, but a phone is still necessary.
Fagradalsfjall
Anyway, once we got the car, Scott decided he wanted to go see the volcano.
This is what we wanted to see, but didn't; Photo: VisitIceland.com |
We vaguely knew there were some parking areas in Grindavík that accessed trail where you could see the volcano. We also knew the routes had moved as the volcano advanced and changed.
So, without much (any?) planning, we headed out to the Reykjanes Peninsula looking for the trail.
We knew you could hike, but we didn't know how far; Photo: Hit Iceland |
Then, on March 19, a vent opened in the Fagradalsfjall system, which last erupted 6,000 years ago, and started to spew lava.
The Fagradalsfjall system is three miles wide and nine miles long and sits between two other systems: Svartsengi and Krýsuvík.
Kleifarvatn geothermal lake in Krýsuvík |
Deep-Earth lava; Photo: Scott Stevens |
Although there are many ancient shield volcanoes on Earth, none has never been studied in real time.
The eruption has ebbed and flowed, but has not stopped.
Sometimes lava shoots into the air and the glow can be seen as far away as Reykjavik.
We weren't there when this was happening; Photo: VolcanoDiscovery.com |
In May, two defensive barriers were built as an experiment to stop lava flowing into the Nátthagi valley where telecommunication cables are buried, and further on to the southern coastal road, the Suðurlandsvegur. However, within a week, the lava soon flowed over the top of eastern barrier. Lava flowed over the western barrier on within a month. (Satellite photo credit: Pierre Markuse from Hamm, Germany)
Lava flow blocked the main trails to viewing areas in June. A new 650-foot-long wall has been built and more barriers are planned, although it is expected that the lava will eventually flow over the area into the sea. A proposal to build a bridge over the road to allow the lava flow underneath was rejected. Lava now covers an area approaching two square miles and is 330 feet deep around the volcano.
So, we found the parking area, which was fairly full, and, after using our cell phone to pay the parking fee, we headed off (without jackets, rain gear, walking sticks or water) to see what we could see.
After a mile or so, we rounded a corner and saw the lava flow. It was still smoking in some areas but had no active red lava.
We made it to the lava flow |
Pretty steep; Photo: Reykjavik Grapevine |
We could not see the eruption (and had no idea if it was active) and it was clear that it would be at least another hour of slogging uphill to see anything.
We reluctantly (but wisely) turned back, deciding we would plan better for when we returned to Grindavík at the end of the trip.
Photo: VisitIceland.com |
Unfortunately, all the air tours are out of the old airport in Reykjavik rather than closer Keflavik. It looks like we now had a good reason to drive back to the city in addition to returning our first rental car.
Back in Town
So, we drove back to town, pretty tired, but hungry.
Photo: Reykjavik Kitchen |
No, we didn’t explore much of Reykjavik (except the car dealerships and big box stores along the road to the rental car office), but we’ve been to Reykjavik multiple times before. We were anxious to get on the road and see the country.
I apologize that this blog has very few original photos. For some reason, almost everything I took at the volcano was not in focus (wrong settings). I promise more photos of mine in all the upcoming blogs.
No comments:
Post a Comment