Update 2023-July-18: It turns out that the name "Manganese Pool", used in most published sources, appears to be the correct name for this feature, despite what the sign says.
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Notes and Observations on Geysers in Yellowstone and Elsewhere
Update 2023-July-18: It turns out that the name "Manganese Pool", used in most published sources, appears to be the correct name for this feature, despite what the sign says.
Kayak tours are offered by Paddleboard Rotorua.
Visted the Rotorua lakeshore and the Government Gardens. Once again, most of the features were murky, acid-sulphate springs and formation. Whangapipiro Pool (aka Rachel Spring) was the one clear, alkaline boiling feature behind a rock wall across the street from the lawn bowling and croquet lawns.
On some maps I've seen a trail along the north side of Puarenga Stream north of Whakawerawera. Investigated it and found that other than one large boiling pool, it doesn't provide any better access or views to the features along the stream inside the village.
The afternoon was spent at the geyser overlook along the Pohaturoa Trail in the Whakawerawera Forest Preserve. From there, over a period of about three hours, saw multiple eruptions of all the features on Geyser Flat.
Pohutu seems to have had a short duration eruption, about 15 minutes long, followed by a short interval, about 36 minutes. That eruption was more normal for the last few days, lasting about 45 minutes with an interval of just under 1-1/2 hours. It's interesting that during the last few days, Pohutu was in eruption about half the time, no matter what the duration was.
Saw several series from Mahanga, and again they seemed to be different than previous days, in both length of series and in interval between series. One series was long, about 16 minutes, followed by 34 minutes of quiet. The next series was only a few weak splashes, and then inactivity for 15 minutes. That series duration was almost 20 minutes long, and Mahanga hadn't restarted by the time we left a half hour later.
Finally, we got to see two eruptions of Kereru. The first was a complete surprise, as usual. The second came about 100 minutes later, just as Pohutu was starting. So I should have gotten it on video, but unfortunately I was so zoomed in that the view was bouncing around and I was watching the geysers, not the little screen. So I didn't get much more than some nice still shots.
In any case, we have seen Kereru on four different days, and pairs of eruptions with intervals ranging from around 70 minutes to about two hours. I'd say that Kereru is quite active, or we got extremely lucky.
On the way back, we visited one last thermal feature. Deep in the forest of non-native California Redwoods is a small mudpot. It's probably one of the most unusual settings for a thermal feature that I've encountered.
Today was much nicer than yesterday, so it was a day to get out and about. There's more than just geothermal areas in and around Rotorua, and we spent some time on them. But we also visited Tikitere (Hell's Gate) for a couple of hours.
It's sub-divided into several distinct thermal areas, two of which have trails in them. Walked all the trails for a couple of hours. It's another acid sulphate area with many large pools filled with gray water with areas of convection, and lots of sulferous ground. There were a couple of pools with water being thrown a couple of meters high.
At the entrance to the area, next to the bathing pools is a steam vent, which is probably an uncapped steam well. A nice, artificial fumarole.
We didn't visit it on our prior trip, and I doubt we will be visiting it again. Like seeing an eruption of Lady Knox, at least now we know what we are missing.
A rainy day, heavy at times, but it got a bit sunny in the early afternoon, so we went to spend a couple of hours in Kuirau Park.
First stop was to take a look at Spring #721. This is the feature which erupted over 100 meters high for 15 minutes on a January Friday back in 2001. Now its just an opaque pool with some slight convection.
Visited the area along Tarewa Street, where several houses had to be abandoned when the springs they were built over reactivated. One of the springs is fairly large and clear and hot, which seems different in an area where most are opaque and acidic. Nearby is another hot feature, which is believe is #712, Parekohoru, that was boiling up about 30cm or so.
Kuirau Lake was steamy thanks to the high humidity from the rains. The boardwalk on the northeast side was fenced off. It looked like the lake might have risen just enough to start flooding and undermining the walkway.
The small spouters next to the Jaycee Thermal Monument seemed pretty much unchanged from the visit four years ago. The same could be said of most of the rest of the features.
After two hours, the rains started up again as we were leaving.
Today we returned to the Whakarewarewa thermal area, but on the Maori village side. We got a late start because we misunderstood the types of tours offered. You can't see Korotiotio and Parekohoru on the Geothermal Walks self-guided tour, but need to take the Village Legacy Tour. But that also includes access to the Pohutu viewpoint, where we spent much of our time.
The view of the Geyser Flat, while not close, is still pretty good. You can see enough of Kereru to get an idea of what it is doing, and Mahanga is visible at the same time. We arrived there while Pohutu was active. It was probably early in the eruption of Pohutu, because it continued to erupt for half an hour. We saw the start of a Mahanga series which lasted about 12 minutes.
After 45 minutes or so, Te Tohu started, and almost immediately, we also got an eruption of Kereru. As in the other times we've see it erupt, it seemed to have been quiet before the eruption. Afterwards, it was having strong minors for the next hour or so.
Two hours later, an eruption of Pohutu had come and gone. There were three series of Mahanga eruptions, lasting from 9 to 14 minutes. Pohutu had been erupting for about 12 minutes, and it was three minutes short of two hours when we got to see a second Kereru eruption.
At that point, we took our Geothermal Walk. The area covered is large, with numerous hot pools with occasional mudpots and areas of what appear to be perpetual spouters. The underbrush is thick is many places, hiding features so much that you can hear them, but not see them.
Since we still had an hour before closing, we went back to the overlook, but were blocked out by some tours. By the time we got to the platform, it looked like Kereru was finishing an eruption. Over the next hour, it had many strong minors. Some of these would put up jets of water well above the higher Geyser Flat platform. If that was an eruption, then the interval was about 1-1/2 hour, which fits our previous experiences.
During that time watching the minors, we saw Mahanga end a series, then have another that was still going 19 minutes later, when we finally had to leave the area. At that time Pohutu was still about ten minutes away from another eruption.