Despite the fact that I am still in New York on vacation (except for things like on-line payroll and P-card reviewing and approving, which can’t wait), I’m taking a bit a of a break from reading mysteries and eating Christmas goodies to work on several things I have in progress. I’m not going to be able to finish any of them, since I don’t have any books here for checking references, and most of the images I want to use are in the Aperture vault on my computer back in Barrow. However, I can do outlines, and get a fair bit of the text drafted before I get home, at least for some of them.
In order they are: 1) PowerPoint & accompanying paper on Iñupiat and Cold War Science for a conference in Munich, 2) encyclopedia article on Western Thule 1300-1750AD in North & Northwest Alaska (in 7000 words maximum!), 3)PowerPoint on Alaskan archaeological sites and threats to them from climate change as it has been observed to be occurring for a conference in Tromsø, Norway, 4) article I’m working on with Claire Alix and Owen Mason on Ipiutak at Nuvuk, 5) encyclopedia article on Barrow sites (Nuvuk, Birnirk and Utqiagvik), 6) paper on ethnographic data on storage of whaling gear, and 7) a paper on whaling gear recovered from archaeological sites which are known to have had whaling taking place.
These all have places they are to go, and times they need to be there. Nothing concentrates the mind like deadlines, except perhaps the threat of execution…
I woke up and turned on the radio this morning in time to hear the morning fellow recommend paying attention to the weather. Since most folks here do that anyway, it was obvious that something a bit unusual was coming.
…COASTAL FLOOD WATCH REMAINS IN EFFECT FROM 2 AM AKDT SATURDAY THROUGH LATE SATURDAY NIGHT…
A COASTAL FLOOD WATCH REMAINS IN EFFECT FROM 2 AM AKDT SATURDAY THROUGH LATE SATURDAY NIGHT. LOW PRESSURE 400 MILES NORTH OF BARROW EARLY THIS AFTERNOON WILL STRENGTHEN TONIGHT AS THE LOW MOVES SOUTH. BY SATURDAY MORNING THE LOW IS EXPECTED TO BE ABOUT 250 MILES NORTH OF BARROW. STRONG NORTHWEST WINDS WILL DEVELOP ALONG THE BACKSIDE OF THE LOW. WIND SPEEDS OF AROUND 25 KNOTS ARE EXPECTED IN BARROW LATE TONIGHT THROUGH SATURDAY NIGHT WITH WINDS TO 35 KNOTS OFFSHORE.
THE SEA ICE IS NOW NEAR SEASONAL MINIMUMS AND THERE IS OPEN WATER SEVERAL HUNDRED MILES TO THE NORTHWEST OF BARROW. THIS WILL CAUSE SEAS NEAR SHORE TO BUILD TO 9 TO 13 FEET ON SATURDAY. THE SEAS ARE EXPECTED TO BREAK ALONG OR NEAR SHORE. IN ADDITION TO THE HIGH SEAS A STORM SURGE OF UP TO 2 FEET IS POSSIBLE AROUND THE TIMES OF HIGH TIDE SATURDAY AND SATURDAY NIGHT. SIGNIFICANT BEACH EROSION IS EXPECTED WITH MINOR COASTAL FLOODING POSSIBLE AROUND THE TIMES OF HIGH TIDE. THE AREA AROUND STEVENSON STREET NEAR THE BOAT LAUNCH BY THE CITY PLAYGROUND IS PARTICULARLY VULNERABLE TO FLOODING. OTHER LOW SPOTS ON DOWN THE BEACH WILL ALSO HAVE THE POTENTIAL FOR MINOR FLOODING.
ADDITIONALLY…SIGNIFICANT EROSION TO THE BLUFFS ARE LIKELY AS WELL.
PRECAUTIONARY/PREPAREDNESS ACTIONS
… A COASTAL FLOOD WATCH MEANS THAT CONDITIONS FAVORABLE FOR FLOODING ARE EXPECTED TO DEVELOP. COASTAL RESIDENTS SHOULD BE ALERT FOR LATER STATEMENTS OR WARNINGS…AND TAKE ACTION TO PROTECT PROPERTY. NOW IS THE TIME TO MAKE PREPARATIONS AND MOVE ALL PROPERTY WELL AWAY FROM THE BEACH.
Not what I needed to hear… Turns out it’s the first big fall storm. With the ice so far out, that means lots of room for the wind to put energy into the water, which means big waves and a storm surge. That means beach erosion for sure, and maybe coastal flooding. Our weather forecasts here are a bit less accurate than those most other places, because there are no observing stations where the weather is coming from. It’s sort of like trying to predict weather in Pennsylvania using data from nothing but a weather station in Chicago.
I don’t like fall storms and coastal erosion. Aside from the dangers associated with flooding (the house I live in floated in 1963, and if it does it again we might wind up in a sewage lagoon), erosion is the most immediate threat to coastal archaeological sites. I spend my summers trying to organize things so that we got well ahead of erosion at Nuvuk and now are trying to stay that way.
2004 fall storm erodes NuvukNuvuk bluff slumps from effects of surf
The thing is, Nuvuk, where “the houses are all gone under the sea” to borrow T.S. Elliot’s phrase, is just one of many important sites. Utqiagvik, Nunagiak, Ipiutak, Tikigak (Point Hope), and so on down the coast. Most of the sites on the Beaufort coast from Point Barrow east to the Mackenzie River Delta in Canada have already washed away and out of the archaeological record.
I had lunch today with Monica Shah. She is one of two conservators (people with specialized training in the preservation of delicate and fragile items, like artifacts) in Alaska. She’s also a fellow Bryn Mawr alumna. Monica has been assisting and advising on the conservation of the wooden artifacts from the Ipiutak feature at Nuvuk, including the only two full-sized Ipiutak sled runners ever recovered. When we started, she was a free-lancer. She went to work for the Anchorage Museum, and they’ve been kind enough to let her continue working on the sled runners.
We went to a new restaurant on 4th Ave., called South. It has good sandwiches and generally HUGE portions. I can recommend the salmon salad, and Monica said the egg salad was tasty if rather sloppy. They have outside tables, but are a bit hampered by a tour company which picks up busloads of tourists right in front of them. Most of the tables were taken up by waiting tourists, most of whom weren’t buying anything. I hope they don’t get run out of business.
The Nuvuk artifacts are getting to the point in treatment where they need to come out of the PEG baths they’ve been in and get looked at by a professional. We figured out that Monica should be able to squeeze in a visit to Barrow in February. With any luck, we may be able to get good pictures of the sled runners in a few more months!
One of the great things about doing archaeology in the Arctic is that the preservation can be spectacular. Artifacts often froze the winter after they were abandoned, and only thawed when they were excavated. This means we get to find a lot of the bone, wood ivory and leather items that were undoubtedly part of most precontact people’s tool kits. We don’t have to guess at what people were using or extrapolate from a few stone tools that did manage to be preserved; we can see it firsthand.
This is not always an unmixed blessing. Arctic archaeology sometimes suffers from an embarrassment of riches.
Boxes with wood from the Driftwood Feature (DWF).
In the past, archaeologists generally only saved the artifacts from a site. Animal bones and soil were pretty much ignored, or at best documented in the field (there are a lot of excavated houses in the Arctic where the animal bones are still piled at the edge of the excavation where they were left decades ago). As archaeological science advanced (radiocarbon dating began about 60 years ago) and people began to do more things with faunal (animal) remains and soil samples, people began to collect a lot more, and to bring it back to museums to save, on the assumption that one day someone would be able to do something informative with it. The idea is still a good one in theory, but it is bumping up against various realities. For one thing, in most areas these sorts of things require storage in climate controlled conditions or they will deteriorate and become useless. They are often quite bulky compared to just the artifacts. Most museums simply don’t have any place to put all this stuff! Some of the better-funded places, like the Smithsonian Institution, have built large off-site storage facilities in areas where real estate is a bit less expensive, just to keep all this stuff. But such places require operational funds and new staff, and that costs money too. Most places can’t really afford that. Some institutions have started charging for putting collections there, but there are problems with that as well.
So part of the new reality for archaeology is that we can’t keep everything. The question is how to decide what to keep and what not to keep. In general, the artifacts are kept. No problem there. The issue is how to deal with the other things.
It’s even more complicated for the Nuvuk project. We have had several areas where massive amounts of organic material, with some artifacts and faunal remains mixed in, were encountered. While one might normally choose to excavate this all in the field, in a couple of cases the areas were right at the erosion face, and could literally have vanished overnight. Combine that with a very cold field situation, where mild hypothermia can dull excavators’ thought processes, it didn’t seem like that was the best plan, since it risked data in a variety of ways. I decided to take tightly-provenienced (with very accurate information on where they were from) bulk samples, which can then be processed in the lab, where it is warm and we have good lighting, magnifying lenses and water to wash the dirt and gravel off so we can get a good look at everything. If excavators recognize an artifact in the field, it gets recorded there, but the idea is that we’ll find the less obvious ones in the lab.
Contents of one bucket shot laid out on a tray.A closer look
One of the areas with a massive amount of organic material was what we called the Driftwood Feature. This level is about 1 meter (39 inches) below the Thule graves. It was actually permanently frozen, and therefore everything organic was in great shape. It looks like there was an Ipuitak dwelling (maybe there were more that had already eroded–we don’t know) on a ridge near the ocean. Sometime between 300-400 AD there was a huge storm, which washed all sorts of things (driftwood, bark, marine invertebrates, shellfish, peat, etc.) up onto the beach, all the way up to where the people were living. It left what is called a strand-line. It looks like they either left in a hurry and didn’t come back, or didn’t survive, since a number of artifacts were still there. The strand-line continued along what had been the beach ridge, and we wanted to see if there was any evidence of more human activity besides the one dwelling. Because there was so much wood, and a number of the artifacts at the dwelling had been wood, we had a needle in a haystack problem, with the haystack about to fall into the ocean (which it did the next winter). So we bulk sampled.
Close-up of the Ipiutak layer at DWF. We excavated many square meters of this!
Now we are going through some of the bulk samples. I’ve been very lucky to have Dr. Claire Alix, a French scholar who specializes in Arctic driftwood and its use by humans, involved with the project since the very early days. She was based in Fairbanks, Alaska, for many years, but has recently gotten a teaching and research position at the Sorbonne in Paris. This is wonderful, since Claire is a great person & really deserves it, but it certainly complicates the logistics of her research on this wood!
Dr. Claire Alix in the Nuvuk Lab
Claire arrived on this morning’s plane, and is already hard at work going through samples from 2009 which were excavated after she left the field. She is looking for all worked (altered by people) items, picking out things that we can’t yet identify for further examination, and recording amounts & types of wood, bark, and other identifiable organics. The non-worked identified material is then being lab discarded. I’ve got the computer map up and color-coded so Claire can look at it when she needs to, Laura is unwrapping the samples, and I’ll probably end up doing the data entry in the catalog. She leaves again on Wednesday night, and won’t be back in the US until sometime after January, so we’ve got a lot to do, and not much time to do it.
Claire and Laura hard at work.Lab discards--on closer examination they turned out not to be cultural.
Later this fall we are going to start going through soil samples and so forth. We hope to be able to reduce the volume they take up. Some of that will be done by separating the actual sample material of interest from the gravel matrix. Where that isn’t possible (for example with large logs or whalebone) we will have to sub-sample, retaining only a portion of the total sample volume. Otherwise, we’re going to run out of room.