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May 24, 2008

Observations for 24 May

Today showed a number of the ways that things can go wrong on a weekend trip, or at least how they can not be as good as they could be. Nothing catastrophic, like for last year when my old truck immediately needed repairs the day I arrived. Just a bunch of annoyances.

First, I left from home too soon, so I arrived in the park while it was still dark. I'd forgotten what nighttime driving here can be like. It's something I've never liked it, even if it's the one time of day that the roads are free of other vehicles. The odds of meeting up with a bison are just too great. To make things worse, there was thick fog almost the entire way from West Yellowstone. Doing 30mph was more than fast enough, but some stretches, like the Firehole south of the canyon until the Lower Basin, seemed to go forever.

And the bison still made their presence felt. There must have been a large herd using the road as a trail just a few hours earlier, because the lower part of my truck behind each wheel on the left side was thick with manure. I will definitely be visiting a carwash when I get home.

So I figure the best time to arrive would be just before sunrise.It will be light, but before the bison and most visitors are up and about and blocking the road. Last weekend I arrived after the ranger-in-a-box went on duty, and had to deal with both varieties of obstruction. I want to set up a nice routine that gets followed every trip, so I keep the thinking about it to a minimum. (The same goes for prepacking needed items not used at home, and making checklists for the stuff that I need to gather up.)

The weather wasn't nice either. The fog turned into gray overcast skies, which turned into precipitation. Unfortunately, it warmed up just enough so that it was rain and not snow. This continued off an on all afternoon, although it could actually be nice when the sun broke through and the wind died down With a limited amount of time, it seems a waste to be sitting and waiting to go out, but if there is nothing to wait for, there's also no point in getting soaked and chilled. This was typical weather for late spring, and one of the reasons I have usually avoided long visits this time of year. (Last year being an exception due to job commitments that worked out well.) I knew from the forecast it was going to be scattered rain. Just means in future years, springtime trips will be limited and subject to cancellation.

Then there were the petty annoyances: I broke the wire on the bike's odometer. It's horrible not knowing how far I've gone and how fast I'm going. On the other hand, I can get it fixed or replaced before the next trip, and will also figure out how to prevent it from happening again.

Perhaps for the best to get all these things out of the way. It does help set a baseline for what to expect, and I always prefer being pleasantly surprised when things go right. Having to use the rain and cold weather gear did show that I'd packed the right items And I've got another day and a half this trip, in which thngs can go either right or wrongl .

And what about the geysers themselves? I saw another Penta, which is always nice, even if I missed the start. On my way there I finally got to see activity in those features on the other side of Sawmill's runoff at the end of the bridge. I'd seen it before, sometime in the early '90s, but that had been from the walkway just below Crested. This eruption only lasted 39 seconds, so you've really got to be there to see it. The second vent between it and the river drained, then refilled to the rim only to drop down a foot. The water also turned a milky white in all the vents. During the Penta eruption, Churn filled as the rest of the group dropped, but no eruption.

There's also a new feature over on Geyser Hill at the north of that expanse of sputs between Depression and Arrowhead. At least I've never seen it before, and didn't see it last week. I really should try to get to Geyser Hill more often,and for more than just Beehive, especially since it's an easy walk from the Lodge Cabins. There's something about not being able to bike over there that keeps me away.

Grand at least waited until I could get out there this morning. I caught the end of Rift, which was probably the reason. The next Grand was during one of the aforementioned rainstorms. I tried to catch Daisy but a wind shift meant I saw a lot of steam, and not much Daisy. Giant is going to be a great timewaster for the next few weeks. It looks so impressive with all the activity until you realize its been essentially unchanged all month.

May 19, 2008

Old Tardy's Drain

Thanks to both Beehive and the bear closure, I was slow in getting downbasin for the morning Grand prediction, and so saw the start from north of Crested Pool. But as I walked toward the eruption through the Sawmill Group, I noticed something that hadn't been there when I left last July: a small hole near the point where the Old Tardy and the Crystal Spring runnoff channels combine.

Old Tardy Drain Old Tardy Drain
Old Tardy Drain Old Tardy Drain

Old Tardy's new drain, 2008 May 18
Once the Grand eruption ended, I got the chance to examine it more closely. From the lack of a splash zone, I quickly decided that it was not any sort of explosion feature. The erosion was clean, but was also fairly deep. I assume it was something that broke out a few weeks to several months ago. So I was a bit surprised when Scott Bryan told me that he hadn't noticed it just two days earlier. This implies that the opening was only a few hours old.

The opening is about 15 to 20 cm across, and a nice round shape. From the walkway, it appears to be undercut and layered in a manner similar to those openings that have over the years appeared across the walkway from Scalloped Spring. Early Sunday morning it could be seen steaming gently, but that could have been the result of all the hot water pouring into it. And a lot of hot water poured into it. During the Old Tardy eruptions that I saw, I would estimate well over half, but less than 90% of the water that would have gone into the runoff channel went down the hole instead.

Back in 1990 I sketched out maps of all the features in the Sawmill group, and on the one for the Old Tardy area I noted a couple of areas of steaming ground. One of these developed into the small slit in the runoff into Oval. (Which was spitting nicely during the Penta eruption Sunday morning.) Another one of these corresponds to the area of this new hold. So it's not really new, just that the lid has finally been removed. But unlike other holes in the area, this one has all that water flowing into it.

All that water is going somewhere, and, at least for a while, having a considerable effect on down below. That water has to go somewhere, and as it moves, ti will be causing erosion like that in the gravel on the surface. This could cause further holes to the surface to develop, or break into the plumping system of some of the other features of the area. But most likely I would expect we'll see nothing obvious. Still, it'll be interesting to see what happens next. We know that Slurp is a part of the Sawmill Group, and this drain lies between it and the rest of the group.

May 18, 2008

Observations for 18 May

After returning from last night's Grand eruption, I figured that today not only could I get a slow start, but would have several hours to head down basin to take a look at Daisy, Grotto, Giant and other points of interest. Except it didn't turn out that way.

As I was getting up and about in my cabin, I heard Scott's voice on the radio announcing that Penta was in eruption at 06:44. Knowing that most eruptions of Penta last well short of an hour, I was resigned to not seeing it erupting. So I was surprised when I biked up past Castle and there it was, still going strong at 07:30. I figured I had at least an hour before it was time for Daisy, so I could head over there and catch Penta draining away. Instead, it just kept going, with all the other members of the Sawmill Group full.

Penta/Sawmill 2008 May 18 Churn 2008 May 18
Penta/Sawmill 2008 May 18 Churn 2008 May 18

Penta, Sawmill & Churn Geysers, 2008 May 18
It was at the time that I noticed that the overflow of the vents by the Thumping Hole had ceased that I looked over and caught Churn in eruption. It had been going for a while, and like yesterday, wasn't able to get a picture. But now things were getting interesting, but at the same time, my plans for the morning were ruined. Unlike yesterday, Churn didn't have a series of eruptions. A hour later, however, Sawmill started. I wanted to get pictures of both Penta and Sawmill in eruption from several angle. I went down towards Belgian, and right after I turned around, I saw the first splashes from Churn. Gettting all three into a single frame with my ancient camera was a bit of a challenge, and you can see my best efforts aren't that good.

The Churn eruption seems have been the key to getting Penta to finally quit. As the window for the next Grand eruption was approaching, I took the opportunity to head back to the gas station to prepare for another wait. Sawmill was still going as I returned, but as it seems to do far too often, it quit about the time I passed Scallloped Spring.

Speaking of Grand. Both last night and today's series of Turban eruptions were quite similar. In both cases there was a "Two Turban Delay". Instead of heavy overflow and waves as in years past, in these cases there was visible bubbling in Vent along with what appeared to be a full pool. In both cases, the duration of Turban was short (less than 4 minutes) despite what appeared to be vigorous activity. The following Turban intervals were short, around 17 to 18 minutes, with the Turban eruption lasting around 6 minutes, which is typical activity in such a delay mode. The bubbling in Vent is hard to see unless you know where to look and what to look for, but I wouldn't mind if this became a preferred delay mode. (Sure beats the 7 Turban Delay which takes 10 or more...)

The photos of the new drain vent near Old Tardy will have to wait until tomorrow. I've discovered that, thanks to software upgrades in the last year, I only have one computer that can still read the old Kodak KDC format. And that requires and it can't connect directly to the computer I use to post these messages. So it's become a convoluted task, and probably the incentive I need to finally get a new camera.

I also confirmed that, with my iPhone, I can add geyser eruption times to my Geyser Log database while in the basin and during the actual eruption. The speed is modem-slow, but I can make things a little faster/better by changing around the webpage.

The drive home was exactly what was expected: 6 hours of dullness that ended in my garage.

Other Geyser Times

18 May 2008
  • Penta, 06:44ie, d>2h15m
  • Churn
    • 07:45ie, d>30s, during Penta
    • 08:54, d=1m16s, during Penta and Sawmill
  • Sawmill, 08:52, d=55m05s