Archive for the ‘Very Far’ Category


Welcome Sign at Alaska/Yukon Border

I’ve lived in Alaska for almost seven years now. It’s a really interesting place in a lot of ways, and right now is a fascinating time to be here. People often think of it as being extremely different from the Southwest, but there are actually a lot of similarities, and there are a number of parallels especially between New Mexico and Alaska that make the two feel pretty similar to me.

One major difference, however, is the status of archaeology and understanding of prehistory in Alaska versus the Southwest. Southwestern archaeology has been going on in earnest for over a hundred years and has led to quite detailed understanding of many aspects of the region’s prehistory. The findings of archaeologists, especially at iconic sites like those at Chaco Canyon, have also been well incorporated into the region’s self-understanding and sense of identity. While the mythology of the Southwestern “mystique” has a lot of problems and doesn’t always accurately reflect what is now known about the historical and prehistoric record, there is no denying the importance of archaeology there.

Alaska is a very different story. While the region’s obvious importance to theories about the peopling of the Americas from Asia has led to a long history of archaeological interest, the research that has been conducted over the years has been frustratingly difficult and its results highly fragmented and confusing. Part of this is because of the remote location and poor preservation of archaeological remains in many parts of the state, but those factors don’t come close to explaining all of it. It seems like the prehistory of Alaska is just very complicated and doesn’t easily fit any of the straightforward theories people have come up with for its role in continental or hemispheric events.

That said, part of the issue is the relatively small amount of research done in Alaska to date, and that does indeed reflect in part the region’s remoteness and the difficult conditions for both preservation and research. As a result, the archaeological literature on Alaska is frustratingly thin and largely technical and specialized, with a relative lack of the sorts of introductory, popularized accounts that are a dime a dozen in the Southwest. One good introduction, however, that I have recently come across is Ellen Bielawski’s In Search of Ancient Alaska.


Welcome Sign, Utqiagviq (Barrow), Alaska

This book is definitely a very general introduction, and it doesn’t go into very much detail at all about the various archaeological cultures that have been identified or the theories about how they relate to each other. It is however a good starting point, especially for the absolute beginner. It is primarily organized by culture area, according to the general schema used by modern Alaska Native institutions like the Alaska Native Heritage Center, which is a reasonable approach to organize the archaeological data.

There is also a chapter on the archaeology of the very early inhabitants of the state, which is probably of the most interest to general readers outside Alaska due to its relationship to the peopling of the Americas. What this chapter shows, however, is both how little we actually know about these early inhabitants and how hard it is to relate their remains to either comparably early people elsewhere or to later people anywhere. This is an accurate reflection of the state of knowledge on this, despite how frustrating it seems.

I don’t have much more to say about this book, but I do recommend it as a general introduction to a topic that I find very interesting even though it is so poorly understood. I would really like to be able to write more about Alaskan prehistory the way I write about Southwestern prehistory, and I’ve tried to some extent, but the data currently just isn’t there for the same level of discussion and interpretation.


Russian Orthodox Church, Ninilchik, Alaska


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Kotzebue, Alaska

From time to time I like to point out interesting resources I come across, even if they’re not directly related to Southwestern archaeology. One that I just saw via an article in my local paper today is a new website with pictures and information on artifacts discovered in 2013 during construction of a fiber optic line in Kotzebue, Alaska by the Alaska-based telecom company GCI. The artifacts, mostly bone tools, date to the thirteenth century AD based on two radiocarbon dates, and are associated with the Thule culture, which is directly ancestral to the Inupiaq people who now live in Kotzebue and the surrounding region.


Wind Farm, Kotzebue, Alaska

I’ve been to Kotzebue several times, and it’s an interesting place. It is located slightly north of the Arctic Circle and serves as a “hub” community for the Northwest Arctic region of Alaska, which means it’s a larger community (with a population of about 3,000) that provides services to the smaller villages in the region. Relevant to my own work, Kotzebue has also been a pioneering community for renewable energy development in Arctic environments. Like most rural Alaska communities, Kotzebue is not interconnected to a larger electric grid, so it runs its own system, which has historically been primarily based on diesel generation. However, the local electric utility has been integrating wind turbines into its diesel-based power system for about 20 years now, and wind currently provides a substantial portion of its total power production (18.5% in State Fiscal Year 2015). It doesn’t get as much attention as Kodiak, another pioneering Alaska community that has used a combination of hydro and wind power to make its electrical system virtually 100% renewable, but it’s nevertheless an impressive achievement in a very challenging environment.


Aerial View of Wind Farm, Kotzebue, Alaska

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Visitor Center and Fajada Butte from Una Vida

Visitor Center and Fajada Butte from Una Vida

I often read articles on the archaeology of other parts of the world to gain a better understanding of the context for Chaco. The areas I focus on for this are primarily those that had interesting things going on contemporaneous with the Chacoan era, but I also look to some extent on archaeological phenomena in other places that are comparable to the Chaco Phenomenon itself to see if there are any lessons for understanding Chaco to be drawn from them.

Recently I’ve been reading a bit about the archaeology of Tiwanaku, Bolivia, which falls into both categories. The period of Tiwanaku’s florescence overlaps with Chaco’s to some extent, although it falls most earlier, but more importantly the history of research there has some intriguing parallels to the history of Chacoan studies and may hold some useful lessons. My account of Tiwanaku here is drawn mainly from John Janusek’s 2004 review article, as well as some other papers by Janusek and others who seem to share his general perspective.

Tiwanaku itself is a major site located on the Bolivian altiplano near Lake Titicaca. It is in a very stark and desolate-seeming location, which makes its monumental architecture seem incongruous (sound familiar?). Early explorers noted that the site pre-dated the Inka empire, and some considered it the oldest site in the whole Andean region. Archaeological investigations in the early twentieth century showed that the latter characterization was definitely not accurate, but they also found little evidence of domestic occupation, and the idea arose that Tiwanaku was a vacant ceremonial center and pilgrimage destination, which some interpreted as the center for a religious movement that was spread by the expansionary state centered at the site of Wari further north in Peru.

Starting in the 1950s, however, a new archaeological program sponsored by the nationalist government of Bolivia and led by Carlos Ponce Sanginés conducted extensive excavations at the site and concluded instead that Tiwanaku was the urban capital of an expansionist state, which rivaled Wari and eventually even conquered it. By the 1980s researchers from the US were invited to work in the area as well, and their research has generally supported this reconstruction of Tiwanaku rather than the “vacant ceremonial center” hypothesis, although the idea that Tiwanaku actually conquered Wari didn’t hold up. Janusek is part of this research tradition, which is why the fact that my information on the site comes mainly from him is important. There are apparently still other archaeologists who still hold to the older interpretation, but there don’t seem to be many.

Anyone who is familiar with the history of research at Chaco should see the similarities here. One important difference, of course, is that the early research at Chaco assumed that it was a residential rather than a ceremonial center. It was not until the work of the Chaco Project in the 1970s that it began to seem like the great houses in the canyon were something other than “pueblos” in the traditional sense. While the idea of Chaco as a vacant ceremonial center was never universal, and it arose rather recently in the history of Chacoan research, it has been quite influential in recent years. Recent research, such as that of Chip Wills, Steve Plog, and Steve Lekson, has been moving away from this idea, however, and back to the idea of a substantial population in the canyon. In parallel with Tiwanaku, however, many of these recent interpretations have seen Chaco as more of a complex, hierarchical society than a set of autonomous, egalitarian villages. This makes the monumental architecture that is a hallmark of the Chaco Phenomenon seem like more of an expression of hierarchical than spiritual ideals.

One important lesson of Tiwanaku, however, is that these are not necessarily mutually exclusive. The monumental architecture and art at the main site and other sites considered to be regional centers of the same polity (“outliers” in Chacoan terminology?) is generally interpreted as reflecting a religious ideology that supported the hierarchical structure of the Tiwanaku state. This is hardly unusual in early states, of course, but the fact that Tiwanaku was not originally considered to be such a state makes it more relevant to the case of Chaco, which is in the same situation.

Another important similarity between the two systems is in the presence of astronomical alignments in the monumental buildings, and the resultant implication that astronomical observation and the maintenance of a calendar were important elements in the societal system. Tiwanaku was apparently the first society in the region to show this astronomical focus, and Janusek, in a paper on Tiwanaku religion, links this explicitly to its success as a state. In that paper he argues that the changes in monumental construction at Tiwanaku proper were linked to changes in the religious ideology of the site, which over time came to incorporate diverse regional traditions as well as cosmic cycles into a complex, syncretic religion that supported and justified the spiritual and material power of the Tiwanaku elites. As Janusek concludes:

Tiwanaku’s long rise to power in the Andean altiplano was predicated on the integration of diverse local ritual cults and various symbolic dimensions of the natural environment into a reasonably coherent, supremely elegant and powerfully predictive religion. The shifting physicality of Tiwanaku’s religious monuments attests the construction and ongoing transformation of an urban landscape that not only visually expressed the altiplano’s ‘natural’ forces and cycles, but, via recurring construction and ritual, simultaneously shaped new social practices and Tiwanaku’s ever-increasing political influence and productive coordination, intensification and expansion. Tiwanaku was an imperfect and potentially volatile integration of religious cults, productive enterprises and societies. The material objectification of a seductive religious ideology that infused the monumental centre with numinous natural forces and simultaneously projected those forces across distant Andean realms helped drive Tiwanaku’s very worldly imperial mission.

I haven’t seen this same argument applied explicitly to Chaco, but I think it may apply there as well. The part about incorporating diverse cultural traditions seems to match pretty closely with the well-known diversity of material culture at Chaco, with different sites within the canyon, and even different parts of some of the larger sites, showing ties to different parts of the region. I don’t know of any pre-Chacoan sites in the Southwest that show obvious astronomical alignments the way Chaco does, so it seems probable that the Chacoans were the first to figure out these alignments, and they may have also been the first to develop the rigorous calendrical knowledge that such mastery of astronomy implies. I hadn’t really thought about that as a source of Chacoan power before reading about Tiwanaku, but it certainly makes sense. This is a good example of the way reading about these far-flung places has practical advantages for understanding Chaco.
Janusek, John W. (2004). Tiwanaku and Its Precursors: Recent Research and Emerging Perspectives Journal of Archaeological Research, 12 (2), 121-183 DOI: 10.1023/B:JARE.0000023711.96664.1b

Janusek, John W. (2006). The Changing ‘nature’ of Tiwanaku Religion and the Rise of an Andean State World Archaeology, 38 (3), 469-492 DOI: 10.1080/00438240600813541

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Anvil City Square, Nome, Alaska

Anvil City Square, Nome, Alaska

I realize it’s been pretty quiet around here the past few weeks. I’ve been very busy with work lately, especially attending conferences and traveling to far-flung corners of the state, and my life has been kind of crazy in other ways too, so I haven’t had much time to devote to blogging. I have been working on a post on the Numic Spread to continue some of the themes from my recent posts on the Fremont, but I need to wait until I have more time to finish it. There are also a lot of other topics I’d like to post about when I get a chance. Hopefully things will calm down a little in the next few weeks and I’ll have some more time. In the meantime, have some pictures of Nome, where I attended a meeting yesterday.

City Hall, Nome, Alaska

City Hall, Nome, Alaska

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Sign with Summer Solstice Sunrise and Sunset Times, Anchorage, Alaska

Today is the summer solstice, and here in the “land of the midnight sun” the longest day of the year is very long indeed. In Anchorage, we don’t quite get to 24 hours of daylight, but it is nevertheless well after 11:00 pm as I write this and the sun is still up. North of the Arctic Circle they do have periods where the sun doesn’t set at all, for varying lengths of time depending on latitude. The northernmost community is Barrow, which gets several weeks of non-stop daylight in the summer (with a corresponding period of darkness in the winter, of course).

Given that the solstice falls right in the middle of this period of extreme daylight, it might be expected that Arctic peoples would mark it in some way, as many other societies around the world do (including the indigenous cultures of the US Southwest, as extensively documented in prior posts here). And this does indeed appear to be the case, though with a typically Alaskan twist.

Whalebone Arch with Umiak Frames, Barrow, Alaska

The Inupiaq Eskimos of the North Slope of Alaska, which lies entirely above the Arctic Circle, have traditionally had a whaling-based subsistence system, and to a considerable degree still do. They hunt whales in the spring (and in some villages also in the fall) using a type of traditional skin boat known as an umiak. These are large, open boats made of a wooden frame covered with the hides of walruses or seals, made according to a rigorous traditional protocol. They are used in other areas further south along the Bering Sea coast as well, but their close association with whaling is most pronounced on the North Slope. A recent article by Susan Fair discussed them in the context of their architectural uses as temporary shelters in various settings and their cultural importance in both whaling and the demarcation of ceremonial and other culturally important spaces at certain times.

One of those times is the Whale Feast, often known as Nalukataq (although that name technically refers only to the blanket toss that is one of the most famous elements of it). This ceremony is held only in years when at least one whale has been taken, and while its exact date varies it is scheduled for sometime around the summer solstice. As the name “Whale Feast” implies, the main focus of this event is on sharing the meat from harvested whales with the community, and it is an opportunity for the whaling captains (known as umialiit) who own the umiaks to demonstrate their generosity and show off their prowess.

Umiak on Sea Ice, Barrow, Alaska

Fair focuses in her article on the role the umiaks play in both the ceremony and the social system behind it, in which the small number of umialiit in a village form an elite within it and the umiak serves as a symbol of their power and prestige, but I was more interested in the timing of the feast. The spring whaling season at least in Barrow generally ends in late May or early June (it had recently ended when I was up there at the end of May and there were umiaks with flags raised indicating whaling success all over the place), so having the feast in late June makes a certain amount of just practical sense given the preparations necessary, but I do wonder if there is a deeper significance to the association with the solstice, perhaps as a vestige of a large role for indigenous astronomy in the pre-Contact era. I have not been able to find much information on archaeoastronomy or ethnoastronomy in Alaska, but given the high latitude and spectacular celestial phenomena that abound here I’m sure Native people have long been attuned to the sky. Recent changes, especially aggressive Christian missionization that sought to stamp out Native religion, has obscured a lot of the earlier cultural practices, but I wonder if things like the timing of the Whale Feast preserve bits and pieces of aspects of traditional knowledge that are otherwise forgotten. Certainly a topic that could use more attention, I think.

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USGS Sign, Anchorage, Alaska

One hundred years ago today, one of the biggest volcanic eruptions in recorded history took place in southwestern Alaska. The volcano, known as Novarupta, is located in what is now Katmai National Park, which was established in 1918 as a direct result of the eruption and its effects on the landscape. As a result, this anniversary is a big deal for the National Park Service in Alaska, which has a special issue of its journal Alaska Park Science devoted to the eruption as well as a special webpage of information on volcanoes in the region. The main institution involved in Alaska volcanology, however, is the Alaska Volcano Observatory, a joint program of the US Geological Survey, the University of Alaska Fairbanks Geophysical Institute, and the State of Alaska Division of Geological and Geophysical Surveys. They are spearheading much of the commemoration of Novarupta and have their own website listing events and other information on it.

The eruption of Novarupta began on June 6, 1912 and continued for three days. There are various contemporary reports of the eruption from people who were in the area at the time, including one by I. M. Dailey of the US Coast and Geodetic Survey, who was stationed 150 miles away in Seldovia at the time, which was soon published in the Bulletin of the American Geographical Society and is now available free through JSTOR. Other reports come from the larger town of Kodiak, even closer to the eruption, where a foot of ash fell in the course of sixty hours of darkness. A fuller picture of what had happened at the site of the eruption itself didn’t emerge until a series of expeditions over the next few years sponsored by the National Geographic Society traveled to the vent site and undertook a variety of studies that had an enormous impact on the emerging field of volcanology. In an article in the aforementioned special issue of Alaska Park Science Judy Fierstein, a USGS volcanologist who has done extensive research at Novarupta and other volcanoes at Katmai, summarizes both the early reports and studies and more recent work that has clarified the reconstruction of exactly what happened over those three days in 1912.

Many of the early National Geographic expeditions were led by the botanist Robert Griggs, who would be quite influential in shaping interpretations of Novarupta. He discovered and named Novarupta itself, although Fierstein notes that he actually concluded erroneously that the main vent for the eruption was not there but at Mt. Katmai six miles away, which collapsed dramatically into a huge caldera during the event. Subsequent research has revealed, however, that while most of the magma that erupted was indeed stored in a chamber under Mt. Katmai, it actually erupted through Novarupta. Understanding exactly how this complicated internal “plumbing” system of the two volcanoes worked is one of the continuing challenges in ongoing research on the eruption.

Griggs also discovered and named the famous “Valley of Ten Thousand Smokes” where flows of ash from the eruption filled a large valley downslope from Novarupta. At the time Griggs visited just a few years after the eruption, this valley was filled with steaming fumaroles where the still-hot ash met various water sources, and the astonishing sight prompted the poetic name. Within a few more years, however, most of the fumaroles had stopped steaming, and they’re pretty much all dead now. Still, the name remains, as does the strikingly barren landscape with little vegetation having recovered even a hundred years later. The area is so otherworldly that it was actually used as a training ground in the 1960s for astronauts preparing to go to the moon.

Remarkably, despite the scale of Novarupta, which ejected more than three cubic miles of magma in the form of a cloud of ash thousand miles wide and 100,000 feet high that wind currents eventually carried as far as Algeria, there were no deaths from the eruption. The inhabitants of the three Native villages near the volcano had fled after a series of earthquakes in the days leading up to the eruption indicated that a major catastrophe was likely, and the few other communities in this sparsely populated area were far enough away that the levels of ash fall they received were substantial but not deadly. Even Kodiak, which was the hardest hit community due to both proximity and wind direction, managed to get through the initial period of fear and panic during which the whole population took refuge on a Coast Guard cutter docked in the harbor, and it soon recovered its earlier prosperity. The residents of the three closest villages were unable to return to their homes, of course, and were resettled in other communities elsewhere on the Alaska Peninsula, where their descendants reside to this day. All this is in striking contrast to the death toll of over 36,000 people from the eruption of Krakatoa in 1883, which was of a similar magnitude but occurred in a much more densely populated area.

Indeed, the lack of major cultural or long-term environmental effects from Novarupta (outside of the immediate area, of course) initially led one prominent archaeologist, Don Dumond of the University of Oregon, to initially discount the role of volcanic eruptions in general as a force shaping the culture history of the Alaska Peninsula. Dumond conducted long-term excavations primarily in the Brooks River area of Katmai National Park from the 1950s to the 1980s, and his interpretations based on that work have been enormously influential in shaping interpretations of the region’s prehistory. Initially he saw no particular correlation between the numerous volcanic ash layers in his Brooks River sites, which he assumed came from eruptions of the numerous local volcanoes, and the cultural changes visible in the archaeological record. More detailed geophysical work on the ash itself, however, led one volcanologist to suggest that some of the larger ash layers at Brooks had come from various known eruptions at Aniakchak, a very large volcano about 150 miles further south on the Peninsula. If eruptions had deposited ash that far away, they must have been much larger than Novarupta, which would therefore not necessarily be a good guide to their ecological or cultural effects. Dumond therefore decided to look over the record of ash deposits and culture history in other parts of the peninsula to determine if these ash layers really were as widespread as they should be if they came from Aniakchak or another very large volcano.

He published his findings in a 2004 paper, and the results were intriguing but inconclusive. Many other sites on the Peninsula did have ash layers that could potentially be from the same eruptions as the major Brooks River ones, but difficulties in precisely dating these layers and relating them to the dating of the known eruptions at Aniakchak left the issue largely open. While this particular study was largely inconclusive, I find the general idea of trying to determine the relationships between volcanoes and human history very interesting (as longtime readers will recall), so hopefully more research along these lines in this exceptionally volcanically active area will shed more light on the question, which is potentially of great importance in explaining certain cultural and linguistic phenomena.

Regardless of whether volcanic eruptions were major factors in the prehistory of Alaska, it’s clear that they are a major risk factor for us today because of a new development since 1912: the rise of air travel. We need only recall the havoc wreaked by the eruption of Eyjafjallajökull in 2010 (a vastly smaller eruption than Novarupta) to realize how big an effect a major eruption can have on aircraft, and southwestern Alaska is one of the most heavily traveled air routes in the world for both passengers and freight. Indeed, one of the main reasons the Alaska Volcano Observatory was established was to monitor Alaska’s volcanoes for their risk to air traffic. One study using simulations based on the scale of the Novarupta event found that a similar event today could potentially shut down essentially all air traffic throughout the northern hemisphere (and, in the unlikely event that ash moved into the southern hemisphere as well, even the whole world). And note that this is by no means an extremely unlikely occurrence; eruptions of this scale happen regularly, and while there hasn’t been one since Novarupta, there’s every reason to think another one will happen at some point. The only thing to do is to keep watching the volcanoes and studying their past eruptions to try to glean insights for the future. This hundredth anniversary of one of the most important such eruptions is an excellent opportunity to remember that.
Dailey, I. (1912). Report of the Eruption of Katmai Volcano Bulletin of the American Geographical Society, 44 (9) DOI: 10.2307/200811

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Welcome Sign, Barrow, Alaska

I recently had the opportunity to spend a few days in Barrow, Alaska, which is a really fascinating place in a whole bunch of ways. It’s certainly unlike any other place I’ve ever seen, either in Alaska or outside it. The coexistence of a vigorous tradition of subsistence whaling with a huge influx of money from the North Slope oil fields, combined with the presence of numerous scientists and other researchers stationed at the former Naval Arctic Research Laboratory (NARL) gives the place a mixture of cultures and perspectives that I’m pretty sure doesn’t exist anywhere else in the world. The unpaved streets and rough wooden facades of the buildings in Barrow belie the extremely sophisticated infrastructure supporting them.

The modern community of Barrow descends from the ancient Inupiat village known as Utqiagvik (also known as Ukpiagvik), and a portion of the old village is still visible as ruins within the modern city. There’s not much to see except a series of low mounds representing old houses, but some of the mounds still have bits of  the whale bone supports of the houses protruding, which is interesting. Much of Utqiagvik has been excavated, and an interesting article by Georgeanne Lewis Reynolds published in 1995 explains some of the lessons learned for archaeology more generally from the excavations at this site. Reynold’s approach falls within the “behavioral archaeology” school established by Michael Schiffer at the University of Arizona, which emphasizes the “formation processes” that lead to the archaeological record as it uncovered in excavations. The basic idea behind this is that what we see in a site when it is excavated is usually not a “snapshot” of daily life at a given moment in the past, a la Pompeii; instead, it is usually a sort of palimpsest of a variety of activities in a given location over time, further complicated by natural processes that occurred after the final human use of the site that serve to further obscure human activities. This general area of study is known within archaeology by the term “taphonomy” (itself taken from paleontology), although Reynolds does not use this term in her article.

Welcome Sign at Utqiagvik Site, Barrow, Alaska

As Reynolds points out, these natural processes are particularly important in the Arctic, where freeze-thaw cycles lead to major movements of soil layers and associated artifacts, coastal erosion destroys significant parts of sites like Utqiagvik located on coastal bluffs, and the sudden movement of large blocks of ice onto the bluff top, known in Inupiaq as ivu, can catastrophically destroy anything in the ice’s path. One famous ivu at Utqiagvik appears to have killed the well-known “frozen family” at Mound 44, preserving in place a Pompeii-like scene of domestic life that has provided details of ancient domestic life not generally available, but at the cost of also destroying much other evidence about the house on account of its destructive nature.

As for cultural formation processes, Reynolds identifies abandonment and reuse of structures as the main processes that can be detected at Utqiagvik. Many house mounds were abandoned, with most of the usable artifacts and bulding materials in them either taken away by the inhabitants who left or scavenged later by others, with the result that few conclusions about specific uses of space within the structures can be made. Some of these were later reused, which adds additional complications to interpretation.

Whale Bone House Support Protruding from Mound at Utqiagvik

Ultimately, Reynolds concludes that formation processes are more easily determined at sites like this at the level of architectural units (i.e., houses), rather than at the level of individual artifacts. All the formation processes she describes have a tendency to move artifacts away from their original locations where they were used, meaning that few conclusions about artifact use or social practices can be made from the locations where artifacts were excavated. The overall assemblage of artifacts from a given structure is a more reliable guide to the use of that structure in general, although even here processes such as abandonment and reuse complicates the picture for any given time period.

This may all seem fairly obvious, but it actually constitutes a fairly strong critique of the influential approach to archaeological inference promoted most famously by Lewis Binford, whose “processual” approach (part of the “New Archaeology” he and others spearheaded in the 1960s) depends crucially on the ability of archaeologists to draw wide-ranging conclusions about prehistoric societies based in part on the distribution of artifacts in excavated sites. Schiffer’s focus on the ways the archaeological record was actually formed is an important reality check on this approach, emphasizing that these sorts of conclusions can really only be made when certain specific conditions obtain. Reynolds’s paper serves largely to apply this general approach to the exceptionally complicated situation in the Arctic, where things are not necessarily as they seem.

Mounds at Utqiagvik, Looking toward Downtown Barrow, Alaska

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