EAA 2015 and Glasgow

We went to Glasgow where the 2014 European Archaeology Association was held, by way of Anchorage and Reykjavik. Because flights from Barrow are disrupted fairly frequently, we went down a bit early, and had a chance to visit with our daughter. There was a pretty amazing double rainbow and a nice lenticular cloud.

We flew Icelandair to Reykjavik and then from there to Glasgow. Glasgow was great. The people who live there seem really proud of their city. The cab driver on the way in from the airport was recommending museums, and in particular Christ of Saint John on the Cross by Dali at the Kelvingrove Art Gallery & Musuem. Glasgow was once the second most prosperous city in the UK, and the residents seem to have been very civic-minded. The Kelvingrove was built to house the collections that were donated by prominent Glaswegians, using funds from an international exposition and public subscriptions. It houses a fair bit of Charles Rennie Mackintosh material. We got in a good visit our last day there. Unfortunately, some of the other Mackintosh venues were under renovation.

Charles Rennie Mackintosh table & chairs. — Charles Rennie Mackintosh table & chairs from one of the famous tea room interiors.

The meetings were held in various venues at the University, including some very old lecture halls and more modern buildings.

University of Glasgow Main Building tower

Nuvuk Archaeology Project alum Dr. Tony Krus chairing a session in a centuries-old lecture hall

We spent most of our time around the University. There were a number of good restaurants & pubs, particularly along Ashton Lane. We tried a bunch of them. We never made it to this one,which was apparently an isolated inn before Glasgow got so big, near a pond where local curlers used to throw rocks. This is apparently where they went afterwards back then, as curlers are wont to do :-).

Our session (Archaeology and Climate Change) was heavily advertised. Tom Dawson, the organizer, had managed to get leaflets put up all around campus before the session, so it was very well attended. As you can see, there were participants from all over. I talked about the threats to frozen coastal sites from climate change, with an emphasis on the Barrow area. I was able to incorporate images from the storm that had happened the week before. There were some other pretty bad situations, but none that were worse. On the other hand, some people are making strides in dealing with these issues with public help, which is good given the turn-around time for even successful funding applications.

Poster for our session on Archaeology and Climate Change.

The conference featured a very nice party, spread across two venues, both within a block of our hotel! One was Òran Mór, a converted church which now houses performance space and a bar. The upstairs had been rented for the party. It had obviously been redone from its days as a church. The other was the glass house at the Glasgow Botanic Gardens, just across the way.

Òran Mór from the outside, with a blue halo on the tower.

Interior space at Òran Mór, with a crowd of EAA delegates

Approaching the Glass House at the Glasgow Botanic Garden

The conference banquet was held in the main hall at the Kelvingrove. It was sponsored by Glenmorangie (the distillery near Glasgow) so there were samples of a couple of their special products. After the speeches and dinner, there was a fine band and dancing.

Dancing at Kelvingrove. BT Wygal and Katie Krazinski by pillar at center.

A busy autumn

When I last posted I had just left for a trip to two conferences in Europe. Since then, I’ve been in 4 countries, given two papers (at EAA 2015 in Glasgow and CHAGS 11 in Vienna), submitted an organized SAA session for next spring, come home, gone to Fairbanks for shotgun qualification, come back home, had two of the WALRUS project participants up here to cut samples from the bones that the interns have been finding in the collections, written part of two reports, drafted two abstracts for a meeting in November, and started on a proposal for an edited volume dealing with climate change & archaeology. I haven’t managed to post at all.

Last week was a tough week for Barrow in many ways, with the deaths of several community members, including long-time mayor Nate Olemaun Jr.. On a brighter note, Barrow took three whales on Friday, and another three today.

Videos, and reports of more erosion

I managed to get a couple of videos of the evaluation of things exposed by erosion at Ukkuqsi on Thursday uploaded to YouTube. You can see them here, and here.

Unfortunately, the erosion continued, and additional items were exposed after I left for a trip to two conferences in Europe, possibly including human remains (this is the site where the little frozen girl was found in 1994). The North Slope Borough is taking care of the situation at the moment.

Things have eroded out elsewhere in the Barrow area as well. At one point I was on the phone with someone from the North Slope Borough about one site, when someone else called about something found at another location entirely. And I now have a voicemail about yet another location!

Yet More Erosion

There is a very large storm, with winds up to 50 mph and big waves from the west battering the Chukchi coastline from Barrow south. It has created a major storm surge, with big waves and coastal erosion. An emergency has been declared in Barrow due to flooding and road damage.

I flew back from Wainwright yesterday evening, and even through the storm was just building, the waves were already hitting Walakpa. I couldn’t get pictures but it did not look good.

Today was much worse. Late this afternoon, I got a series of calls about something washing out at Ukkuqsi, where the little frozen girl Aġnaiyaaq was found. Aqamak Okpik from IHLC got things organized, with Morrie Lemen coming out to NARL in a bigger truck than mine to take me in to take a look. The North Slope Borough Fire Department came over, and two firefighters suited up and tied a rope onto me so I could go down and take a look.

The big concern was that a burial was eroding out, since there have been several in that area. In the end, it looked like part of a house (maybe two superimposed) with a whalebone and a baleen toboggan. We retrieved a few bones and a piece of structural wood that were going to fall in any minute, and hope to be able to get a radiocarbon date or two. I only got hit by one big wave.

Closeup of eroding structure from the beach.

Hope to get some video or at least frame grabs available soon.

Walakpa, July 30, 2015

We got up with the goal of getting packed up. It wasn’t clear if the UICS logistics staff would be able to come and get us today, but we decided to finish all the field work, and pack up as much as possible. We got right on the screening, and recording of the edges of the midden and the units on the Pipe Monument mound. Owen went to work on a detailed profile of CS 2.

CS 2 after excavation and preparation for detailed profiling.

Once that was well in hand, it still wasn’t clear if we would be able to get home. I needed to go in to Barrow to make sure everything was progressing with the other project, so we decided I could take trailer load of field gear, samples and some of my gear back to town. That way, we would need less help getting back, and if the pickup wasn’t going to happen until tomorrow, I could bring back my sleeping bag and sleep in the mess tent.

Once I got to town, I unloaded and did some more work on the other project. It turned out that some logistics folks were available, so I went back down with them, and we managed to get everything back to town, and into the UICS yellow building. Everybody got to sleep in a real bed.

Walakpa, July 29, 2015

Last night was not particularly restful. The collapse had complicated matters quite a bit. However, after breakfast, we went back to work.

The old location was not viable, so I picked a new spot about a meter south, which became Column Sample 2 (CS 2). There was a bit of an overhang, and a very deep crack behind the bluff face. We needed to get all that material out of there. It took a bit of thought to figure out how to do it (not a usual archaeological operation, fortunately). Finally, we put a blue tarp down on the bottom of the main cleft so we could drag fill without anyone having to be under any overhangs or unstable areas, everybody got out of the way, and I cut the overhang back while standing as far back from it as possible. We then took the material out with a bucket brigade. Once that was done, I levered all the cracked material off, and we took it out the same way.

Once that was done, I decided that we would excavate in levels labeled with letters, so we could proceed quickly, rather than wait for Owen to try to match levels in the detailed CS1 profile, which could have been a slow process. It seemed like the fairly warm, dry weather was letting the face dry out while detailed profiling was happening, and the longer it was exposed the more chance of another collapse. Owen would do another detailed profile after we got the column sample.

I also decided to make the sample a bit smaller in volume. CS 1 we had been trying for 75 cm x 75 cm (mostly because that size fit between some prior disturbances), but 50 cm x 50 cm seemed more manageable in the time we had left. One gallon from each sub level was retained as a bulk sample, and the remainder of sediment from the sub level was screened through 1/8″ and 1/4″ mesh.

We were just getting started when someone arrived to do a coastal DGPS survey that is part of the coastal mapping aspect of the Barrow Area Information Database project. He passed on a message that said my boss needed me to come back into town. (There is no effective connectivity at Walakpa, which is why this is being posted after the fact). I reviewed recording stratigraphy (or artifacts if any showed up) with Laura Crawford, made sure everyone knew how to use the InReach is needed, and headed back to Barrow by ATV around 1PM.

Something had come up with one of the compliance projects we are working on, and I needed to talk to people and draft some documents. I made it back to Walakpa around 10PM.

On the way, I met some folks out for an evening ride, and they stopped over to visit. One of them had spent a lot of time at Walakpa when she was younger, and had some great stories. I hope we can get them recorded for future generations.

The rest of the folks had managed to complete the column sample, so we talked about closing up shop tomorrow. We just need to finish screening, record the Test Units on the Pipe Monument midden, and backfill the TUs.

Walakpa, July 28, 2015

Owen and Laura got up early and screened what we had dug last night. Owen worked to finish the profile. There is an apparent marine level at Level 13.

CS 1 profile

We had problems with both transit and radio batteries. Despite that, I showed Laura how to run the transit, so I don’t have to be awake all the time. We shot in the remaining levels of CS 1, as well as the new test units on the mound.

Laura and Owen continued taking CS 1 down. Unfortunately, after the dinner break, they returned to find that the bottom of the profile had collapsed.

It was a pretty depressing situation. It left an overhang, so there was no way to just continue safely. It mean that we would have to start over again in the morning.

Walakpa–July 27, 2015

We went to work in earnest today. Owen went to work on recording the stratigraphy of the profile we had chosen for the column sample (CS 1). I had him marking the bottom of each level so we could continue excavation even after he went to sleep. Anne Garland and Laura kept working on the tests on the mound with the monument. The SW quad of the 1×1 came down on a cryoturbated sterile layer. There was metal throughout the cultural levels. We expanded northward to examine some wood in that wall.

Owen Mason examining the profile of CS 1.

Meanwhile, I set up the transit and began shooting in the CS 1 profile, as well as the bluff edge. The NW quad of TU 1 had similar results, so we put some 50x50s closer to the bluff edge to see if we could find datable material and the edge of the feature.

Mary Beth Timm and I took naps, so we could stay up late and work on the CS 1 profile. After dinner, we shot in the upper levels of the CS 1 profile, as well as a polar bear jaw that was exposed in Level 12, so that it would not get stepped on. Mary Beth & I started excavating CS 1. We are excavating in natural stratigraphic levels, with any level that is more than 5 cm in depth broken into 5 cm sub-levels. One gallon from each 5 cm is being kept as a bulk sample, and we are screening the remainder.

Midnight double selfie. Anne & Mary Beth at work on CS 1.

We kept going until it go so dark that we really couldn’t see the soil colors, which was around 2 AM. We had accomplished a fair bit, so we headed off to bed.

The weather is often best at night. It was really beautiful. A pair of loons was swimming on the lagoon.

Today, back in Barrow

Jeff Rasic from the National Park Service, along with Rebekah DeAngelo from Yale and her grad student Brooke Luokkala are in town to do some work, along with Laura Crawford, at the Birnirk National Historic Landmark site, which is on UIC lands (and yes, the actual name of the place is Piġniq, but the site has been written about as Birnirk, so I’m using that name for the site). Becky and Brooke got in Sunday, after travel from the east coast, and Jeff got in yesterday. However, the weather was pretty bad, so we postponed real fieldwork until today.

I did see them in the field briefly yesterday. I had to take a quick trip to the point to check on something for UIC Lands. On the way back, I met them near the Birnirk site, unfortunately a bit stuck in gravel. They were successfully extracted and continued their tour of Barrow.

Today we went out to Birnirk. We looked at all the mounds, Jeff got GPS points on mounds and other reference points, and Laura did quite a bit of coring. I flagged the perimeter of a “box” that we hope to have some of Craig Tweedie’s crew do detailed DGPS measurements on. That data can be used to make a contour map of the site, which can then be compared to the map James Ford made in the early 1950s, when he was there with Carter. It should be interesting to see how much sea level has changed. It clearly has risen since the earliest houses were occupied, and even since the early aerial photos, but the question is, how much?

Part of the crew visiting one of the mounds at Birnirk.

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