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Litli Geyser, Gamli Laugin, Fluðir, Iceland
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Deildartunguhver, Borgarförður, Iceland
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Álfaauga, Haukadalur, Iceland
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Strokkur, Haukadalur, Iceland (Pt.4)
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Strokkur, Haukadalur, Iceland (Pt.3)
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Strokkur, Haukadalur, Iceland (Pt.2)
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Strokkur, Haukadalur, Iceland (Pt.1)
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Ystihver, Reykjahverfi, Iceland
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Tour of Hveravellir, Iceland
Names and designations based on map at the back of in Jarðhitarannsóknir á Hveravöllum 1996 by Helgi Torfason, photos at Volcanic Springs, and my best guesses. This video was taken shortly after our arrival as it was getting dark.
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Gjósandi Geyser, Hveravellir, Iceland
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Hveragerði Geyser, Iceland
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Observations for 2023 September 27
Another side trip to watch an hour or so of Strokkur eruptions. Today it was raining but the wind wasn't as strong. Also early enough that we missed the tours. (although tour season seems to be pretty much over.)
In a series of fourteen eruptions, we saw a couple of two strong burst eruptions, along with along with at least three weak eruptions. The second bursts both came about 20 seconds after the first, when it looked like the pool was just trying to quietly refill. The weak eruptions were followed by short intervals, in one case well less than two minutes, while it was ten minutes following the two bursts. Most of the other intervals were around five to seven minutes.
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Observations for 2023 September 26
First we revisited Littli Geyser at Gamla Laugin/Secret Lagoon in Fluðir. While it was dry, it was also overcast and extremely windy (as in having to pay attention to the gusts or be blown over.)
The activity has changed a bit since the last visit three weeks ago. This time we saw six major eruptions from 9 to 12 minutes apart. The four eruptions for which I got a duration all lasted 38 seconds. In all cases the vent drained after the eruption as after the major eruptions in our previous visit.
Then it was on to Haukadalur. It's my opinion that the wind was having an adverse effect on Strokkur. We saw a number of weak eruptions, some only a couple of meters high. The intervals seemed longer also. That the runoff channel from the pool was exactly downwind could easily explain the changes.
While we did see some two burst eruptions, only once was the second burst powerful. The one three burst we saw had a boil up for the second, then a weak third burst.
I did finally get to see a full eruption of Alfaauga. I waited about half an hour, with overflows of increasing intensity occurring every eight minutes or so. Before the eruption there was strong conventing over the vent and some boiling up, but no splashes. Then an overflow continued and there was an eruption lasting just over two minutes. When it appeared that the pool had dropped down to the previous level between the overflows, I assumed I had seen the major eruption and left. (By then had been out in the wind for over 2-1/2 hours, and time to head in.) Just under two hour earlier I had caught the end of another eruption, but I have no idea if those were consecutive.
Behind and to the left/west of Alfaauga was a pool with water level just below the rim. During my wait, at one point the pool was full and pulsating. Then the next time I looked, it was back down. Not sure of the name or activity of this feature.
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Observations for 2023 September 25
Revisited Hveragerði today, in order to visit some new areas and the revisit the activity there. The weather cooperated, as it wasn't too windy, there was no rain, and the sun even came out for a while, allowing for a backlit eruption video.
Found the locations of Grýla and Leppaluði, a couple of boreholes which erupted years ago. Grýla has its own little turnout along the road with a warning sign, even though it was overgrown and not at all steaming, and obviously not active in a long time. A 5cm wide hole in a rock, years ago it could be induced to erupt up to 10m high. Leppaluði is a circular concrete platform about 5m across that has been filled in, and also does not steam. But between it and the river was a small area of what appeared to be sinter gravel.
Farther north along the road is the Gufudalur golf course. Up on the hillside are several areas of thermal activity. In a ravine just outside are a couple of mudpot like features. In the course itself, between a couple of the hole is a thermal pond in which there was a spouter active. There's a sign, "Fallreitur" in front of it, which may be the name, or a warning for golfers. This feature really can only be see on the uphill side, and consists of an opening in a pennisula in the pond. Nearby were a couple of other muddy vents. (It seems this course and Arikikapakapa in Rotorua are the only courses with geothermal hazards.)
Farther up the hillside were another fairly dry mudpot and an old wellhead steaming away. I could not find the features Dirk Niermann calls "Lava Pool" and "Rey-8" and "Rey-9". Also did not try to locate Littli Geyser or Gosi I and II, as I couldn't find good descriptions of their locations. Seems Littli was up near the Agricultural Station we passed by on the way to hillside features the last visit.
We also revisited the Hveragerði Geothermal Park, mostly to see the eruptions of Eilifur Goshver/Eternal Geyser. This feature was nice an regular while we were there, with intervals within a few seconds of 20m15s. A quick burst of steam to 10 meters, but quite entertaining. The pool near the entrance also became active with eruptions when I was able to observe it.
There are reports of this feature only becoming active around 2016, and on the Apple Maps satellite view, there's a suspicious rectangular object located at that location. These satellite maps are several years old, based on the various new roads missing on them. The Google Maps satellite view shows a steaming area.
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Observations for 2023 September 17
South of Húsavík is another Hveravellir. This one used to have several geysers, but all but one has been replaced by greenhouses.
The remaining geyser is Ystihver, a large raised bowl at the base of a hillside. It's about ten meters across, superheated and has been altered in several ways over the last century. There is a drain pipe which keeps the water level just below the rim. There are multple channels for the runoff.
The activity itself consists of periods of calm followed by a heavy boil or bursting. Some of the bursting can reach four meters high, and start with an explosive bubble. These eruptions put water out over the entire rim, and there are catch basins which we never saw water reach them, so it must be capable of even stronger activity on occasion.
On the south side is a concrete structure which has enclosed a small boiling feature, Strokkur. A couple of other geysers were similarly enclosed and are part of the greenhouse complex to the southwest. To the north are a couple of pyramids which contain well heads which are used to supply hot water to the town of Húsavík.