Barbara E. Luedtke
Department of Anthropology
University of Massachusetts/ Boston
Paper delivered April 11, 1996, as part of forum on "Chaos
or Congruence? Regional Lithic Data Bases in North America",
at annual meeting of the Society for American Archaeology in New
Orleans, LA. (Amended slightly 12/11/96)
Lithic sources have been a topic of archaeological interest
in New England for over 100 years, but at this point we have not
drawn together information about quarries, material characteristics,
and geochemistry into a coherent data base. Furthermore, regional
archaeologists have just begun to discuss a host of issues such
as the structure of a regional data base, the level of detail
that should be included, "quality control" for data
to be entered, and how to provide access to the data base. This
presentation will introduce the forum, summarize progress thus
far for New England, and outline other issues that need to be
addressed by those of us committed to the development of comprehensive
and congruent lithic data bases.
I first became involved with lithic data bases while working on
my dissertation, which involved compiling data on chert sources
in the Upper Great Lakes region (Luedtke 1976). In 1987 I gave
a paper at the SAA meetings in Toronto in which I called for development
of a much larger lithic data base, and made some suggestions about
how such a data base might be structured (Luedtke 1987). Much
of this paper was incorporated into an appendix of my recent book
on chert (Luedtke 1992). So I thought I knew something about this
topic until I attended a conference in Maine a year ago and discovered
that: a) there were already many more people than I knew about
working more or less independently on lithic data bases in the
Northeast alone, and b) there were many issues relevant to such
data bases that I had never even considered, or at least hadn't
thought through enough to realize they might be problems. At that
point, I decided it would be a good idea to get an even broader
perspective by starting a conversation among people from across
the whole continent who were interested in this issue. Knowing
there were many more people interested in such data bases than
could possibly talk in any symposium, I decided to try the forum
format, which is designed to include a great deal of audience
participation. I invited a number of people to speak about what
is being done with regard to lithic data bases in their regions,
and also about their concerns with the process, just as a start
for the larger conversation.
If, as I suspect, we are currently in a state of chaos with regard
to the development of lithic data bases, it will certainly take
us longer than one morning to achieve congruence. My goals for
this forum are much more modest. First, I simply hoped to get
a lot of us together in one room so we can meet each other and
begin talking. Second, I hoped to get a feel for what is already
being done, and what models we might have for further work. Third,
I wanted to get as many of the issues out on the table as possible:
what do people think are absolute necessities to discuss? What
are the problems they foresee? I have some ideas of my own, which
I'll mention shortly, but my experience at the Maine conference
suggests to me that there will be many more. Finally, I hoped
this forum might help us begin a process that will lead toward
building consensus on some of the issues.
I'll start off with a brief summary of the history of lithic data
bases in New England. This is a challenging region for such endeavors
because stone tool makers here used an unusually wide variety
of lithic materials (Calogero and Philpotts 1995). Obsidian is
nonexistent and chert is scarce, so volcanic and metamorphic rocks
such as quartz, rhyolite, hornfels, quartzite, argilllite, silicified
shale, and basalt played a more important role here than they
usually do in lithically better-endowed regions. These volcanic
and metamorphic rocks outcrop widely, but at many outcrops the
materials are too coarse or too fissile even for New England knappers.
Artifact-quality varieties often occur only in small outcrops,
sometimes dikes, sills, or contact zones only a few meters in
diameter. To further complicate the issue, all of New England
was glaciated during the Pleistocene, so while many bedrock quarries
are small and spatially restricted, the same materials are often
available in secondary deposits which are sometimes located considerable
distances from their bedrock sources.
Nevertheless, New England archaeologists, like archaeologists
everywhere, quickly recognized the importance of knowing the sources
of lithic raw materials. The first example of a proto- data base
that I am aware of is Henry Haynes' 1886 description of five New
England lithic sources (Haynes 1886). William Fowler also published
a summary of data on several sources (Fowler 1971) and Ron Thomas
included a few local sources in his pioneering effort to develop
a lithic data base (Thomas nd). Other publications that include
data relevant to such a data base have different goals, such as
documentation of individual quarries (e.g. Bonnichsen 1982; Bowman
1981; Bowman and Zeoli 1978; Gramly 1980; Pollock 1987; Ritchie
and Gould 1985) studies of how particular materials are distributed
on sites in the region (e.g. Bourque et al 1984; Strauss 1988,
1989) and studies of prehistoric exchange or interaction patterns
(e.g. Calogero 1991; Curran and Grimes 1989; Lavin 1983; Spiess
and Wilson 1989). There is no single publication that draws together
all the information available about lithic sources in this region,
and in fact much information about quarries and sources remains
in people's heads, and not down on paper (Luedtke 1993). We are
also accumulating increasing quantities of petrographic and geochemical
data, (e.g. Calogero 1991; Lavin 1983) some published, but much
still unpublished.
A somewhat different approach to lithic data bases involves the
assembling of lithic type collections, which can be found at many
regional museums, colleges, and universities, and which have also
been formed by many individuals and avocational societies. The
type collection developed by Jack Holland at the Buffalo Museum
of Science is probably the most comprehensive. Each of these type
collections is completely autonomous; there are no widely accepted
standards for how samples should be collected, how large a sample
is adequate, what should be done to ensure that the samples are
representative, how samples should be labeled, etc.
In 1994, Dave Sanger of the University of Maine organized a conference
on Geoarchaeological Approaches to Lithic Sourcing in the Northeast;
this was the regional conference referred to above that was such
an eye-opener for me. Fifteen of us, representing 11 states and
provinces, came together to discuss common problems such as the
rationale for lithic sourcing, the role of hand specimens, student
training, interdisciplinary integration, nomenclature, and new
techniques. We agreed to work toward a regional data base, and
I was supposed to help develop a prototype, but this effort has
not progressed very far, partly because I believe there are still
many unresolved issues that need to be discussed. For example:
Structure of the data base
I haven't encountered anyone who disagrees with the concept of
creating a data base that includes a wide variety of information
about lithic sources including quarries, visible attributes, petrographic
descriptions, and chemical composition. Modern computer programs
with windows and hypertext, etc. make it easier than ever to compile
such multi-faceted data. However, we will need to decide on the
level of detail to be included. For example, in the case of trace
element data, do we want to include every single raw value, or
summary statistics only? What about "bad" values? How
much data on standards and laboratory procedures must be included?
We will also need to develop procedures for searching the data
base. Models exist from geology (e.g. Scott 1994) but I'd still
argue that it makes most sense to begin geographically, working
outward from the site where the artifact in question was found.
There was surprisingly little agreement at the Maine conference
as to whether the data base should be distributed in print or
electronic format. The latter has the advantage of being infinitely
expandable and easily added to or changed, but is in some ways
harder to use and could present security problems. Which leads
directly to the second area of concern:
Access and Control
It may be that those of us who went to college in the 60's have
never quite recovered, but my initial inclination was to create
"The People's Data Base" on the Internet, open to everyone,
and to which everyone could add data as they acquired it. Participants
in the Maine conference quickly pointed out the flaws in this
scenario, and further reflection has added more. For example if
the data base is to be universally accessible, then we need to
think very carefully about how we provide data on quarry locations,
so that the data base does not become a looter's guide to quarry
sites. If only very general locational coordinates are given,
the sites will be protected but the data base will be less useful
for legitimate users. On the other hand, if precise coordinates
are given some people may be reluctant to provide locations of
quarries they know about, and this also weakens the usefulness
of the data base. Perhaps we need a separate but linked data base
for quarry data.
Another access issue results from the fact that a number of CRM
companies now offer lithic sourcing as one of the analytical services
they can provide to archaeologists. Some of them may well consider
the source and material characterization data in their files to
be "proprietary information" that should not be revealed
to potential competitors. Is this data permanently "off limits"
to the rest of us? Are there ways we can protect the rights of
people who are trying to use their expertise and the data they
have generated to make a living as archaeologists?
Another problem with the concept of the "People's Data Base"
is quality control; who decides what is or is not to be included?
My initial inclination was to include everything and let the data
speak for themselves, but this now seems like a bad idea. Experienced
users may be aware that data generated by a particular technique
or a particular laboratory are suspect, but new users will tend
to assume that all the data are of equal validity unless they
are given reason to believe otherwise. Bad data will lead to incorrect
source identifications, and surely the archaeological literature
is already clogged with enough of those (Calogero 1992). I reluctantly
admit that there needs to be a panel of some type that decides
what data to put into the data base. But how is such a panel to
be chosen, and what safeguards can we develop to prevent tyranny
by the Rock Czars?
Units of analysis
A third area of concern is our units of analysis. Are "sources"
the same as quarries? Formations? Members? Groups? All of the
above, depending on circumstances? How do we deal with intra-source
variability? Many type collections include only the most characteristic
"typical" varieties of a material, but any visit to
a quarry shows that the range of variation in all characteristics
is considerable. Furthermore, examination of assemblages shows
that stone tool-making people did indeed use "atypical"
varieties of lithic materials, so we cannot continue to ignore
these. Finally, how do we incorporate data on secondary sources,
knappable materials in stream bed, glacial, and beach deposits
that may lie some distance from bedrock outcrops? If our knowledge
of bedrock sources is incomplete, our knowledge of secondary sources
is virtually nil. Yet these sources were indeed used, and their
distribution should be included in the data base.
Terminology
A fourth area of concern is terminology. As I've pointed out elsewhere,
there is no consensus within archaeology or geology as to the
exact meaning of basic terms such as flint, jasper, or chalcedony
(Luedtke 1992). We also need to develop standard terminology for
describing visible attributes such as color, texture, luster,
and diaphaneity. I know that others of you have begun to discuss
terminology, and Tim Church's Sourcebook is a helpful first step
(Church 1994). Furthermore, assuming we can reach consensus as
to our units of analysis, as discussed above, we will then have
to decide how to name them. A strong argument can be made for
simply following geological nomenclature, but there is also merit
in continuing to use terms that are already firmly ensconced in
the literature and in archaeologist's minds. After all, if I mention
Knife River Flint most of you know what I'm talking about, but
that's not necessarily true if I start talking about "silicified
lignite probably from the Golden Valley Formation".
In Greek mythology, Chaos was a void that existed before the creation
of the universe, a place of utter disorder and confusion that
nevertheless contained the potential for all creation. I'd like
to hope that our current chaos also contains the seeds of eventual
order, but I look forward to hearing what the rest of you think.
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Archaeological Museum and Research Center, Milford, DE.