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Observations for 2019 Jan 22


Wasn't sure what to expect today. The amount of information about New Zealand thermal activity is minuscule compared to Yellowstone, and usually out of date or of historic interest only.

Our accommodations in the Holiday Park are within walking distance of Te Puia at Whakarewarewa, so we headed over about 30 minutes before opening. It was easy crossing, since the new traffic circle features some pedestrian underpasses.

But first we investigated the steam coming from the other side of the fence, within the golf course. There we found a pair of large, wet, but noisy mudpots. That was a nice start.

Over at Te Puia we could see areas of steam as we walked up to the entrance station. We waited a bit, but were the first on the grounds as the gates opened at 07:58. We quickly made our way past the "cultural exhibits" to our real target-- the thermal activity.

When the Geyser Flat became visible, we could see Te Tohu (Prince of Wales Feathers) erupting, and what looked like Pohutu slopping. Down the ramp and moments later we came across Pohutu in full eruption.

Here's where our ignorance came into play. We didn't really know what to expect next. The signs said that there were one to two eruptions per hour, but this one kept on going. After reaching full height, it seemed to die down after about 15 minutes, only to pick back up and rise back up to a full 17-20 meters. After twenty minutes of video recording, I gave up.

This eruption lasted about 53 minutes. About five minutes before the end, it became obvious that things were dying down as the activity of both geysers slowed. They finally stopped together, or within seconds of each other.

Since we didn't know what the intervals might be, we explored the area in the vicinity where we could come back quickly if things started happening there. The immediate vicinity reminds me of Geyser Creek. Lots of hot ground with steaming cracks and openings. A number of what look like decrepit features that might once have been springs and geysers, but are now just another fumarole. There are lots of areas of sulphur being deposited, bright yellow covering the formations of what used to be geysers.

One feature we knew about was Kereru. Unlike the other nearby features, which are depositing standard gray sinter, it is surrounded by black sinter. The vent is in an alcove below the platform of Pohutu and company. We finally figured out where it was located, and that it wasn't doing anything but steaming gently. Our information from last week said that it seemed to start overflowing giving a few minutes warning.

When we returned to Pohutu, Te Tohu was again in eruption, so we waited for Pohutu. About seven minutes later, Pohutu started splashing, and the eruption began about six minutes after that. This eruption also seemed to have periods of alternating between full height and something about half. It lasted about ten minutes less than the previous one. During this eruption Kereru did nothing, as before.

So again we took advantage of the gap to investigate the area further away. There we found lots of steam vents and mudpots surrounded and obscured by lush green plant-life. We walked up to Te Waikite, which used to be the largest geyser in the area, located at the top of a huge mound of old sinter. We returned at about noon to wait for Te Tehu's start.

During that wait, Kereru still did nothing that we could see, and once Te Tohu started, we decided to find a different place to see the start. From this vantage point, Kereru was not visible.

About ten minutes after we left, Suzanne saw the sudden appearance of a huge steam cloud from down there. We both ran down in time to see the tail end of the eruption. These eruptions last only about 30 seconds, but can easily reach 20 meters. Needless to say, we were a bit disappointed, as from what we knew, that was our one and only chance to see a geyser that reports said erupted a few times a week to maybe a few times a day.

The reports we had said that after an eruption, there was a series of minors, some which could be fairly strong, and as high as the platform above it where Pohutu is located. We saw some minor splashes, but they were at best only a few meters high, and were anywhere from 5 to 10 minutes apart during the next half hour.

Pohutu started during this time, so we watched it while keeping an eye out on Kereru. Then we noticed that the splashes seemed to be getting bigger and more frequent. Not only that, but it seemed like the water was pooling in the vent. In anticipation of the next minor, I started the video recording. Almost immediately I was rewarded with a minor that kept building while water started to flood out the vent. The interval between two major eruptions, and this was no minor, was 49 minutes.

The water floods out over the sinter shield between the vent and the river in one big, sustained wave while the height was comparable to that of the still erupting Pohutu, even though the vent is about five or six meters lower.

Following this eruption, we started getting minor play every two or three minutes. These were much stronger than the splashes we'd seen earlier. Pohutu ended about ten minutes later, with a duration almost identical to the previous eruption. There was no way we were going to be leaving this area this time.

This splashing continued for about the next 90 minutes. Pohutu started another eruption about an hour into this wait. Then Kereru was mostly quiet for about twenty minutes. Unlike previously, the splashes were strong from the beginning, and coming so frequently that I stopped recording individual spurts.

Twenty minutes later, the splashes had turned into full minors less than a minute apart, and Pohutu was still erupting, about 70 minutes after it had started. That's when Kereru started looking so good that I had to start recording. Within a minute, it erupted for the third time that day, with this interval about 2h12m. The length and height were no different from the second eruption.

And, as after the previous eruption, minor play every two to three minutes started again. Pohutu's eruption continued with it finally ending with a duration of 1h34m.

We took the opportunity to explore the last of the areas we hadn't visited, over by Papakera Geyser. We observed the wash zone around it, and that it was gently overflowing. By the time we returned, Te Tohu was again in eruption. Kereru was still having minors. We decided to get the start of Pohutu, and then leave. We figured that the area would close by the time Pohutu's next eruption ended, and Kereru wouldn't have had enought time for a fourth eruption, so no point in sticking around further. It had been a long, eventful and wonderful day.

But it turns out we got one last surprise. Looking back on the area, we discovered Pohutu off, a mere twenty minutes after the start. This short eruption followed a long duration and interval. It would have been interesting to know what that meant, but maybe for the best that we were about to be forced to leave.

A few other observations. The crowds would come and go. Unlike at Old Faithful, where the time of the next eruption governed the size, here it seemed to be based on how many bus tours there were. At times we had the area around Pohutu to ourselves. There were three other people besides us who witnessed the last eruption we saw of Kereru.

The Asian Invasion is not unique to Yellowstone. If anything, we are pretty lucky in that most gazers don't have to interact with these people except when they tromp down to Morning Glory or elbow their way to the railing during a New Crater/Steamboat eruption. On too many occasions these people would block my view to get their perfect picture, when I was already trying to stay to the side and out of the way. I had one woman, oblivious to her surroundings shove her umbrella in my face as she fumbled with her camera.

It was also disappointing how little information there was about the geysers. There are not guidebooks in the souvenier store. The closest I could find was a "thermal history" of the Maori. I heard several of the guides mention things that weren't true. They were still telling people Pohutu was erupting once or twice an hour, for example.There is nothing like geyser gazing, at least at Te Puia (we'll learn if that it also true at Orakeikorako in a few days.) A few gazers spending all day here over the period of a week would probably do more to pin down what sort of activity is going on than has been done in the last few years. (For example, is there really no connection between Kereru and Pohutu? I wonder, based on some things I saw about the minors.)

Tomorrow will be less intense, as it's mostly driving between several places that probably don't have natural geysers. But I should get to see my first induced eruption since 1986.


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Observations for 2019 Jan 21


After four days in New Zealand, finally got to see something erupt.

It is located at Te Aroha. Mokena Geyser is a bicarbonate drilled well which erupts periodically from a small hole, maybe 1cm across, at the top of a cylinder in a large concrete basin.

When we arrived, it was quiet. Off on the side was a locked metal cover. As I was standing there, I heard rumbiling start from beneath it. In a minute or so, steam was starting to quietly come out of the vent. The noise increased and small spits started from the vent. Over the next few minutes, the spitting increased in duration and size as the sound increased. At some point the activity would last for several seconds before having sort pauses, and the water was thrown about about a meter high.

This lasted for about ten minutes, and at times the water was thrown about four meters high. There never was much volume to the play. Eventually, the activity began to subside. It slowly reversed just the way it started. Every time I thought it was about to end, it would give a quick spit. Overall, the duration of activity was about 20 minutes.

After that, we headed for Rotorua. After checking in and buying some groceries, we went to Kuirau Park.

This is a bizarre place for someone used to Yellowstone. It's a city park. It's bounded by busy city streets, and where there's no thermal activity, there's a lawn, including several athletic fields.

There's no geyser activity there. Mostly it's scummy holes or watery mud pots. But there were a couple of clear, boils sputterers next to a large pile of cemented boulders that steamed near the top. These sputs were surrounded by a large flat area that appeared to have been wet at one time, but was drained. Most of the features there had the same look as if they had been higher not to long ago.

In addition, there was Kuirau Lake. This a a large boiling pool at the north end of the park. At one point, there's considerable overlow under the walkway and down a well-defined, wide shallow runoff channel. After about 40 meters or so, this flows into a hot pool which seems to act as a sink, as there was no other discharge anywhere in the area.

The lake as a nice overlook directly over the pool, and a boardwalk that cuts over one end of it. It reminded me a lot of Hot Lake in the Lower Geyser Basin.

Tomorrow the real fun begins, as we have reservations to visit some real, large geysers.


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Observations for 2018 October 16


After checkiing out, stopped in the store parking lot. Realized that Grand hadn't erupted, just as we saw the steamcloud rising from its location. Went out anyhow since it was a cold, dead calm morning. Got to Sawmill Group in time to see the end of the long second burst, and to see Vent and Turban quit.

Also saw that there were frozen puddles in some of Sawmill's runoff channel. Not sure what to make of it. Perhaps the water nearer the vent was too warm to pool and freeze, or maybe something else is going on there.


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Observations for 2018 October 15


Today started like yesterday. Temperature was in single digits when we arrived at Norris, and there were a couple of tour buses in the parking lot. Unlike yesterday, the tours were visiting the Back Basin instead of Porcelain Basin.

Set up on the upper platform again in anticipation of it eventually getting sunny, although that turned out to be several hours away. New Crater/Steamboat was more active than yesterday, but during those cloudy hours, it never had a good minor. (A good minor is one where it's time to use the camera.) Eventually clouds and fog broke and it started to warm up. Around noontime, moved down to the lower platform, as I can't tell what the South Vent is doing from the upper.

The activity did pick up a little, but it wasn't until 13:27 that it had a minor that showed that there was eruptive potential. That was followed four minutes later by another one, and then they started coming about ten to twelve minutes apart. All during this time the activity of the minors was concentrated in the North Vent, with the South not quite as strong as before other eruption.
But at 14:11, a minor started and built, and at 14:12, we got the eruption.

Both vents climbed slowly to full height, and were clean for the first minute or so. Then the fun began. North turned reddish-brown, and began spewing out rocks. Large rocks thrown to great heights. More rocks than I've seen in all of the five previous eruptions. After a few minutes, the water there seemed so thick that the North Vent was only erupting 10 or 20 feet high.

When I was down at the runoff, I saw (and recorded) a large chunk of reddish mud plopping onto walkway. Surprised me, because I didn't think rocks would be flying that far, so it was probably thrown there by the torrent of water coming down the channel.

There was very little wind, and what little there was had the steam column drifting away from us. Because of this, later in the eruption the condensing steam made for nice rainbows which seemed to appear on either side depending on where the wind was drifting.

Ended the day by going out at sunset for one last One Burst Grand. Got there in time to see a Turban delay, so it was a Two-Turban Delayed One Burst Grand eruption that we eventually saw. The temperature was about 26°F, which was about the same temperature at which we saw New Crater/Steamboat last week.


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Observations for 2018 October 14


Left the Old Faithful area where the temperature was 8°F and arrived at Norris at sunrise. Was probably even colder there. Turns out it is possible to sit and wait for a geyser at such temperatures, if you have a couple of blankets and are wearing lots of layers. The day never really got above freezing, although some places in sunlight did dry out a bit.

New Crater had some good surges early in our wait, then nothing much happened until a hour before we planned to leave. Even this activity wasn't encouraging, as I only got the phone out just in case, but never started recording. So it was mostly 9 hours of killing time.

Years ago I came across an interesting phenomena of hot ground, and encountered it again today. When warm, damp ground encounters frigid air, frost develops underneath pebbles and particles lying on that ground. That ice in turn causes the frost to grow, from the bottom, slowly pushing the top of the frost column up. I found large patches of this frost over by Echinus, on both sides of the boardwalk.


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Observations for 2018 October 13


Nothing much happening with New Crater. Spent an hour and a half there and did see some strong surges, but they were separated by minutes of nothing happening.

It was after we left that things got fun. It was snowing heavily, but I thought things were okay until we got to the cutoff that rises up on the hillside where Tanker Curve used to be. There was a line of cars stuck there, unable to get up the slope. It was a mess, and we ended up spending an hour waiting because we had no idea if this was a local problem, or the end of a long line.

Tried to get past once, and some foreign idiot in a rental cut in front of us and immediately lost traction. Once we got past, it was clear all the way to Madison. There we talked our way past the barricade crew by saying that we had a cabin at Old Faithful and all our stuff was there. I think they were there more to keep the idiots from getting in deeper, and by the way I was dressed, and the vehicle I was driving, I showed that I might know what I was doing.

So it took the better part of two hours to get back. By then it was time for Grand.

Unlike the rest of the week, it was windy. Which, despite the temperature being just at freezing, made it the most unpleasant time we've had this trip. And the wind kept shifting during the One Burst Grand eruption. Often we could see the tops of the jets above the mass off steam coming off the runoff and Vent, other times it was just a mass of steam.

Again it appears that there are changes in the Sawmill Group. For the first time in two years that I can remember, I saw Churn below overflow. Again there appeared to be gaps in the snowcover where Sawmill's runoff channels used to be.

Despite it being mid-afternoon on what was now a sunny day, we just weren't in the mood to be out in the weather any more. So tomorrow it's back to Norris, unless something happens overnight there.


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Observations for 2018 October 12


Knew that today was going to be fairly uneventful, a good day to catch up on other things besides Giant. It was cloudy at first, but cleared and when the sun was out, felt warm, especially when the wind died down.

Got up early again to catch the morning One Burst Grand eruption. From there, it was down to Fan & Mortar to see if it had erupted, and wait around a while since it hadn't.

From there it was on to Fountain, where it was obvious nothing was going to happen any time soon. So we looped around past Great Fountain, where we had to stop because it was in overflow. There were some nice sized bursts, so it wasn't totally a Flounder.

Back in the Upper Basin it was time for both Grand and Beehive. But first, saw Aurum from the parking lot. Then went over to Geyser Hill and ended up seeing Castle instead. Over at Grand we heard someone call Beehive during the One Burst Grand eruption. Sounds like either no one saw the Indicator, or there wasn't one.

The One Burst Grand was a bit of a weird eruption. It was obvious that we were having a delay, and it was so steamy it was hard to see the pool. Then I saw a nice boop boil over the vent, but nothing much happened after that for about half a minute. Then, in quick succession, there were several more boops, one maybe two meters high. Then the pool was quiet. It was another minute before Turban finally started, and it didn't sound all that vigorous. But it got stronger, and it looked like Grand's pool was getting steamier. Finally it became obvious that we were getting waves, and about to get a delayed eruption start.

Finally went back to Fan & Mortar where nothing much happened, again.

Over the last few days, it seems to me that there's been evidence of some sort of over-trickle from Sawmill. The way the snow was melted was one sign. Another was that today there were wet spots and pools in the runoff channel, long after the snow had melted. The photo is an attempt to show this. Unfortunately, this is about as high a water level as I've seen, but this past summer, I never saw any evidence of any water down those channels. (Maybe it's just wishful thinking...)


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Observations for 2018 October 11


The snow picked back up in the morning as we were loading up to head out. We were the first to head down basin. It was time for Grand, and the snow was deep enough that we decided to walk and not use the bikes. The boardwalks were really slick, especially on the older, polished plastic boards. But the view was wonderful, because it was dead calm and the clouds were actually starting to break, despite the snow.

The One Burst Grand didn't make us wait, and then it was time to head on toward Giant. That's when we noticed that not only was Bijou off, but there appeared to be a surge from Mastiff. Getting down there was slow going, thanks to the slippery walkways, but when we arrived it seemed obvious that there was some sort of medium to weak hot period activity. While there was a bit of water running down on the far left, that could have been from Feather and not Mastiff. In any case, it gave us a time to return for the next activity.

So there was time to check out Fan & Mortar, which did nothing while we were there, and see an eruption of Riverside. We trudged back to my truck at the Lower Ham's by the biketrail, not wanting to deal with the slippery walkways a second time.

Returned to the Giant platform by bike about 2-1/2 hours after the activity we saw, and then waited. It was pretty nice by then. Some sun, and absolutely no wind, which after this past summer, was quite a relief and made the cold easy to take. Grotto was in eruption, and there had't been sort of activity from the Southwest Vents recently.

It was the third pause after we arrived that things got interesting. It was only a minute from when we saw water in Mastiff until the start of Feather. Within a minute Mastiff was overflowing, and unlike the last few days, was surging and boiling up nicely. Saw at least one that was about 2 meters high, It took a while, but eventually Cave started to erupt, the first real activity we'd seen from it. There was no wind, so other than the steam coming from Mastiff's overflow, there wasn't any obscuring of the activity.

When Mastiff finally dropped, it took a minute for Bijou to finally restart. Feather never really calmed down, and with Bijou back on, Posthole started up too. Giant began surging, with long, sustained boil-ups from what seemed like a high water level. There were distinct pauses between the surges, but each on was little bigger then the previous, and they were putting out more and more water.

We finally got the eruption on a surge that was well above the cone, one that put out enough water to roll the log signs. There was still no wind, so the steamcloud rose straight up from the water column. The water discharge was not being pushed to the north, so Feather & co. weren't being inundated, but instead were actually erupting fairly strong steam.

Because of the conditions, there were very few people out and about the whole duration. At the start, a group of a half-dozen tourists were there to join us.

Grotto quit during Giant's eruption, but started again shortly before that last water from Giant was visible. The duration was long because everytime it looked like Giant had finished, it would put a spray of water out of the cone and on the platform.

After Giant, of course the thing to do is go and catch the next One Burst Grand eruption.

At Sawmill, I noticed what were either some changes, or the way the snow behaves in old runoff channels. In the morning, I could definitely see gaps along the runoff channels, as if the snow had been melted there. The water level in Sawmill was low, but it looked like there was a high water mark high enough for runoff. In the afternoon, all the snow had melted from the area, and there was water running down those same channels, with the water level in Sawmill high, almost at overflow. Will keep a watch on it for the few days we have left here.


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Observations for 2018 October 10


Today looked like it was going to be a repeat of yesterday, and it was and it wasn't.

It wasn't because the weather was different. The snow last night was over quickly, so there wasn't much accumulation. But it did mask a bit of ice, which made the boardwalks interesting in areas. The day started clear, became partly cloudy, and then warmed up as the sun came out. Warmed up enough for much of the ice and snow to melt, or turn to slush.

But Giant was a repeat of yesterday. We got out to find something probably happened shortly before we got there, then had to wait several hours for the next attempt at a hot period. In this case, it was Grotto, which was off for over four hours before it started at noon. For over an hour, Bijou looked like it was off all the time, with an occasion splash or two to let us know that it wasn't paused. It was like in years past when Grotto had just had a marathon eruption. Finally, there was some sort of real pause, with a lot of steam from Mastiff, and then Bijou started jetting heavily. Twenty minutes later was when Grotto started, followed at almost the same time by one of those long Feather eruptions where nothing much else happened. Pretty much a duplicate of yesterday's first hot period.

At least we got to see a couple of Grand eruptions with almost no wait. The first started as we were picking our way through the ice near Economic. (There were also coyote and goose tracks that preceeded us.) That eruption had a long second burst, which in the steamy cold was nicely backlit. It was impossible to see anything from most of the benches, though, especially near West Triplet. Then the second One Burst Grand eruption started before we even had a chance to get settled onto the benched. The snow was just starting up, so again it was a lot like a nighttime eruption, in that it was easier to tell what was going on by sound than by seeing anything.

Back at Giant, waited in the increasinly heavy snow showers. After about an hour, it was starting to stick to the boardwalk. Four hours almost exactly after the previous hot period, we got a repeat of yesterday's second hot period. The only real difference was Cave did erupt for a while. There was a feeble attempt at a restart, with Posthole and Feather blipping along for a few minutes, but Giant never had any surging during that time.

It's beginning to look like Giant has changed since the last eruption. I've yet to see any hot period that had any activity that looked encouraging, oras if Giant was trying to erupt but just not quite there. There's been little to no surging from Mastiff, even when it overflows heavily. Cave has been seen only once, and the restarts look like the first couple of minutes are missing, and are going directly to the after-effects where all the vents are splashing around.

Between hot periods Giant just looks quieter. The water level seems lower and there doesn't appear to be as much of the angled jetting as before.


The last couple of days there's been a crew putting together the edge logs along the new pavement. At first it looked like there were going to be buried in the dirt along the pavement edge, but as the photo shows, they are going be the low barriers like they have in places where parking is being discouraged.

I think this is a mistake. All these barriers are going to be used as seats, especially when they face a geyser like here at Grotto. People are going then be scuffing the ground in front of those logs. And then stand up and walk around, "off-trail". A better arrangement would have those barriers on the pavement, so that people seated on them would still have their feet on pavement. But, we'll see how things work out next year.


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Observations for 2018 October 09


So after yesterday's excitement, today wasn't much.

The day started at dawn with a trip down basin to see what had happened at Giant. Seeing Bijou active meant no eruption, and the depth charging without a wet, steaming platform implied that we had just missed a bathtub. Ended up waiting several hours in light, windless snow for a strangely weak hot period. Feather was on for a bit over 8 minutes, yet there was no overflow from Mastiff, and none of the other vents joined in. This activity also came well after Rocket and Grotto had finished.

Came back a couple of hours later. There was still intermittent snow, but the wind had picked up, making observations a bit more difficult and the wait much more uncomfortable. Again, probably arrived just after some sort of long pause from Bijou, as it didn't stop for the next hour. Grotto had close to a six hour interval, and it was an hour into that eruption when we finally got the hot period. (At the same time as Grand.) Mastiff flooded the area, and did have some meter high surging, But the restart was weak, with no activity from Posthole, and no surging from Giant. At that point, it was time to go in.

With the cold and with the Lodge closed, have reverted to driving to the Lower Ham's parking lot and biking from there. So it was right after we'd loaded up the bikes for a trip back to our Snowlodge cabin that Beehive's indicator started. We learned the hard way that a five minute indicator is not enough time to drive over to the Lodge cabins and go to Geyser Hill. Saw the start of Beehive just as we parked.

And that was it for the day. The expected snow, the kind that sticks and accumulates, started about then, and continued on until it got dark.


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Observations for 2018 October 08


Had to choose, so went to Norris. New Crater/Steamboat's interval was slightly long, but it sounded like it could erupt soon. Giant was way too long, and acting like it could still be a while.

We arrived a little after sunrise, to find not one, but two Asian Invasion tour buses in the parking lot. But it seemed that they had gotten their selfies overlooking Porcelain Basin and were heading out.

The walk out to the platform wasn't too bad, despite the heavy frost. At Old Faithful, when we left at dawn, the temperature was about 25°F. Only when we got to the platform itself did it become icy, and that was because of the mist coming from New Crater/Steamboat having frozen during the night. Settled in for a bit of a wait. The chair was on thin layer of ice, but the board cracks kept it from slipping around. It was about an hour later that the ice really started to form, as it warmed up enough so that instead of ice crystals, it was water droplets coming down.

For that first hour, nothing much happened. There was a surge around 09:36 that caused me to get my phone/camera out and recording, but that was it. It was pretty quiet, and I realized that this might be a good opportunity to do some video recording from places besides the platform. It should be easy to move around.

At around 10:05, an loud, obnoxious student tour group showed up. They seemed more interested in the icy platform that the geyser. About five minutes later, there was a large surge, one that stopped just as I was about to start the camera. I was actually a bit relieved that the eruption didn't start then.

Just before they arrived, I was cold enough that I decided to put on the rain pants as an extra layer of warmth. The wind had started up, and it was occasionally in my direction. Also got out the extra blanket and wrapped it around myself. But after they left, I decided that a quick walk around might help warm up. So I went up to the upper platform and then headed back. Just about as I reached the junction, another surge started. It was sudden, and it was big. I managed to get my camera started seconds before the water column started climbing.

First instinct was to head back to the lower platform to continue recording. I didn't get far, as the platform was being drenched. The wind and spray from the eruption was forceful enough that I did get to see my chair, sitting on the ice sheet, start sliding across the empty platform, all the way to the far railing.

I did stop recording and quickly moved our packs up out of the wet area. Then I rushed, as much as the slippery boardwalks would allow, back to take a height measurement. I got 60% at 130 meters, which comes to 78 meters or 256ft. This eruption did look a bit smaller than the previous one I measured. Still, that's still the second highest measurement I've ever made.

And as planned, I did do a grand tour. I continuously recorded the eruption from there to the upper platform, to the lower, down to the runoff channel (where it was raining heavily) then back to the lower platform, where a crowd had finally gathered. All that video will have to wait for our return before it gets posted.

I retrieved my umbrella and went back to record the runoff at the bottom. Turns out there were some really nice, bright rainbows in all that rain, especially once you got past Echinus, or on the far side.

Unlike previous eruptions, the water columns never turned brown. Because of the wind direction, the hillside above the North Vent was dry. It was also a short water phase. At some point in my recording, I realized that I was no longer seeing water, just hearing the powerful steam roaring out. This also confirms my previous observations that the brown columns are due to the surface runoff back into the vents (especially the North Vent.) The choking we saw previous was probably due to excess water stopping up the system at the surface, nothing deep.

When it came time to pack up the folding chairs, I discovered something else about the start. Both chairs had blankets (now thoroughly soaked) in them. Both blankets had various rocky debris on them, ranging in size for flecks and flakes, to a couple of chunks about the size of x. There were a number of the larger chunks scatter along the boardwalk edges and under the benches, too.

After about an hour of the steam phase, we decided it was time to head back and see what Giant had done. Still, the best part of the wind direction is that the parking lot never got hit. For all the eruptions we've seen this summer, we've never had to pack up in the rain. But we still had quite a bit of wet gear in the back, our chairs and blankets and umbrellas and outer coats.

And the lot had empty parking spots, despite it being the middle of the day. Quite a change from just a few weeks ago.

We returned to the Upper Basin at about 13:00. Last night we'd left our bikes in the Lower Store racks figuring we might want them today. Had just finished rearranging the packs to head down to Giant, with the expectation that we could dry a few things out down there, when got the call that there was a hot period starting. Is an nice, easy ride from that point, especially when you don't have to thread through the people wandering around Old Faithful. I got to the area while the Giant Indicator Pool was still full because Mastiff had not yet dropped.

This hot period seemed similar to the one we had seen the night before. Again, Feather didn't quit, and Giant had some surging, but never looked like it really wanted to erupt. Left the area with the expectation that there wouldn't be much happening out there until after dark.

So the rest of the day was pretty quiet. Finally got around to seeing a One Burst Grand. This one featured a wind direction that was constantly shifting, but getting wet some portion of the benches. Definitely something that doesn't happen there much.

Also paid a quick visit to Geyser Hill, just to see what it looks like. Disappointing the way the NPS has overreacted to the breakout under the boardwalk. Disappointed, but not expected. They always overreact. In this case, they could just close things from Pump to Doublet, and enforce it by pulling up the boardwalk over the outbreak.

Noticed that there are minor changes to the Sawmill Group. The runoff from Crystal and Old Tardy is diverting itself at the boardwalk to flood the grass on both sides of the walkway. I even starting to use the Penta runoff channel. Spasmodic was down well below overflow, while at the same time Sawmill seemed as high as I've seen it all summer. There's also steam visible in the little crack feather to the northeast of Spasmodic, something I cannot remember ever seeing before.

When we got to Norris, I wanted to visiting the indoor plumbing, but the door was locked. I had to visit again later, and it was unlocked. (And the parking lot almost empty. Definitely a high percentage of vehicles for people out to see one geyser in particular.) I noticed on the first visit that the cleaning crew truck was parked nearby, so I assume they locked them until the buses left, so they could stay clean for bit longer.