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The functional dimensions of earth oven cooking: An analysis of an accidently burned maize roast at the C. W. Cooper site in West-central Illinois
Gregory D. Wilson, Amber M. VanDerwarker
University of California, Santa Barbara
Despite the prevalence of earth ovens, a subclass of pit features used for cooking, there is little consensus regarding how these cooking features were used or about the foodstuffs that were prepared in them. To provide a more detailed understanding of earth oven cooking in the archaeological record, we analyze the archaeobotanical contents, stratigraphy, and morphology of a cooking pit recently excavated at C. W. Cooper, an early Mississippian (A.D. 1150–1200) site in west-central Illinois in order to contribute to research on late Prehistoric foodways. Filled with nearly 100 ears of maize, this earth oven presents the opportunity to document the process of undertaking a maize roast. The volume of maize and its presence within a dense concentration of cooking, processing, and storage facilities allows us to consider the communal nature of outdoor earth oven cooking in the 12th century Central Illinois Valley and the socioeconomic dimensions of commensal politics more broadly during the Precolumbian era.
Keywords: Mississippian, earth oven, maize, pit features, cooking techniques, Midwestern archaeology
Introduction Pits are common archaeological features that were
once used to store and process foodstuffs in the
ancient American Midwest and Midsouth. Archaeo-
logical analyses of pit features have contributed
substantially to understandings of late prehistoric
foodways in the North American Midcontinent
(Binford et al. 1970; Fortier 1983; Harris 1996; Holt
1996; Kelly et al. 1987; Koldehoff and Galloy 2006;
Stahl 1985). For example DeBoer’s (1988) famous
study of the Mississippian pit features revealed that
subterranean storage features could have been used
to conceal agricultural surpluses from central admin-
istrators seeking to extract tribute payments.
Moreover, Bardolph’s (2014) recent analysis of early
Mississippian (A.D. 1100–1150) pit features in the
southern Central Illinois River Valley demonstrated
that local groups maintained traditional Woodland
era conventions of food storage and preparation
while adopting an array of other Mississippian
practices and forms of material culture. This paper
contributes to archaeological research on pit features
and foodways through an investigation of the
functional dimensions of earth ovens, a subclass of
pit features used for cooking. Earth ovens are
generally identified based on the presence of oxidized
soils, burned fill zones, and concentrations of fire
cracked rocks. Despite their prevalence in the
archaeological record in the eastern United States,
there is little scholarly consensus regarding how these
cooking features were used or the kinds of foodstuffs
that were prepared in them. To highlight both the
antiquity and ubiquity of this form of cooking we
draw on abundant ethnographic, ethnohistoric, and
archaeological evidence of earth oven cooking in
other areas of the New World.
We add to this body of literature on earth ovens
through an analysis and discussion of the contents
and structure of a cooking pit recently excavated at
the early Mississippian C. W. Cooper site (A.D. 1150–
1200), a small bluff top village in west-central Illinois
(FIG. 1). Specifically, we consider the archaeobotani-
cal assemblage recovered from inside this pit, in
addition to evaluating the pit’s stratigraphy and
morphology. Filled to the brim with nearly 100 ears
of maize, this earth oven feature allows us to
document the process of undertaking a maize roast.
The volume of maize and the location of this feature
within a dense concentration of cooking, processing,
and storage facilities also enables a consideration of
Correspondence to: Amber M. VanDerwarker, Department of Anthropology, University of California, HSSB 2001, Santa Barbara, CA 93103-3210. Email: [email protected]
166 � Trustees of Boston University 2015 DOI 10.1179/0093469015Z.000000000118 Journal of Field Archaeology 2015 VOL. 40 NO. 2
the communal nature of outdoor earth oven cooking
in the Central Illinois Valley during the 12th century.
The Antiquity and Use of Earth Oven Features in the New World The earliest evidence of earth ovens in the New
World dates between 8500–8000 B.C. and can be
found in Alaska, the Pacific Northwest, and the
Great Plains (Thoms 2008, 2009). In addition to these
early cases, Thoms (2008, 2009) has documented
abundant cases of earth oven/hot rock cooking
throughout the western United States, combining
ethnographic and archaeological evidence to achieve
a fair amount of resolution, thus allowing for the
identification of these features on archaeological sites
(Fish et al. 1985). Earth ovens have also been
documented in the archaeological and ethnographic
records of Mesoamerica (Dering 1999; Leach and
Sobolik 2010; Salazar et al. 2012) and South America
(Van Den Bel 2010). Unfortunately, while there is
abundant archaeological evidence of earth oven use
in the eastern United States, ethnographic evidence of
this type of cooking technology is generally lacking
from the eastern United States.
Most ethnographic evidence of earth oven cooking
in the New World highlights the cooking of meat and
plant products high in fiber and carbohydrates. The
majority of documented plant species include root
and tuber plants, or those high in toxicity, such as
Camassia, Allium, and Agave (Fish et al. 1985; Leach
and Sobolik 2010; Wandsnider 1997). By cooking
these plants in the earth oven, they ‘‘render foods
more nutritious and digestible’’ (Thoms 2009: 573).
Moreover, the general size of the cooking feature is
Figure 1 Select sites from the Central Illinois River Valley.
Wilson and VanDerwarker An analysis of a maize roast at the C.W Cooper site, IL
Journal of Field Archaeology 2015 VOL. 40 NO. 2 167
often correlated with the amount of food being
prepared, thus their size can be used to infer the scale
of the event for which the food is meant (Salazar et al.
2012; Thoms 2008, 2009).
Recent ethnobotanical and ethnographic research
in the Maya lowlands by Salazar et al. (2012)
documents the roasting of whole maize ears in
traditional Maya earth ovens. The context of this
particular maize roast was a first fruits feast
celebrating the initial maize harvest of the season
(Salazar et al. 2012: 291). The earth oven was dug to a
depth of about 60 cm, the deepest of all the ovens
documented in the study, which is not surprising
given the communal nature of the event. A fire was
built inside the pit, and once the fire died out, the
cooks covered the coals with leaves, on top of which
were placed the maize ears. The maize ears were
slightly wet to retain moisture during the cooking
process. More leaves were then laid atop the row(s) of
maize, following by an earthen cap, after which the
oven was left unattended overnight, or for several
days, depending on the level of heat (Salazar et al.
2012: 291).
Ethnographic and ethnoarchaeological accounts
closer to the study area provide more specific insight
into how ancient people of the Midsouth would have
used earth ovens (Black and Creel 1997; Hough 1926;
Peacock 2008; Teit 1900; Thoms 2008). Our survey
of this literature highlights two main methods of
heating: indirect, placing heated rocks on the ground
surface or in a shallow pit for slow cooking, and
direct, building a fire inside a pit. The indirect method
was practiced by the Chopunnish (Nez Perce) in the
Pacific Northwest:
[T]he Indians prepared a large fire of dried wood, on which was thrown a number of smooth stones from the river. As soon as the fire went down and the stones were heated they were laid next to each other in a level position and covered with a quantity of branches of pine, on which were placed bear flesh, the boughs and the flesh alternated for several courses, leaving a thick layer of pine on the top. On this heap was then placed a small quantity of water, and the whole covered with earth to the depth of 4 inches. After remaining in this state about three hours the meat was taken off (Elliot Coues 1893 [in Hough 1926: 36]).
There are also ethnographically documented exam-
ples of indirect cooking techniques in which a fire is
built over the floor of a rock-lined pit. Foodstuffs
were then laid overtop the stones once the fire burned
down to coals (Hough 1926: 37).
An example of the direct method comes from an
observation of a group of California Indians. In 1877
Stephen Powers (in Hough 1926: 37) wrote that
‘‘…under stress of hunger [the Tlelding] ate soaproot
(Chlorogalum pomeridianum), the poisonous properties
of which they extracted by baking it in large quantities
in the ground, covering it over with green leaves and
building a fire over it, which was allowed to burn many
hours, when the root is said to be sweet and palatable.’’
Wandsnider’s (1997) ethnographic cross-cultural study
of pit cooking technology found that the use of these
two methods largely depended on the types of food
being cooked. Fires were often built inside pits for the
purpose of high temperature cooking. Alternatively,
heated rocks covered with layers of vegetation were
often used to prepare foods requiring a moist cooking
environment. However, sometimes the two methods
were used in conjunction for a long duration and high
temperature cooking.
Several scholars have attempted to archaeologi-
cally differentiate between these direct and indirect
cooking techniques (Binford et al. 1970; Fortier 1983:
120–124; Koldehoff 2002; Stahl 1985). Research by
Binford et al. (1970) at the Hatchery West site in
Clinton County, Illinois has provided one of the
earliest and most detailed investigations of Late
Woodland (A.D. 500–1000) and Mississippian (A.D.
1000–1400) earth ovens. Two subclasses of earth
ovens, deep and shallow, were identified at the site.
Deep earth ovens averaged 65 cm in depth and were
flat-bottomed pits with oxidized floors and side walls.
Shallow earth ovens averaged 43 cm in depth and
were generally basin-shaped in profile; these pits
differed from deep earth ovens in that they lacked in
situ evidence of soil oxidation but instead possessed
traces of redeposited, oxidized soils and other heat-
altered materials mixed into different fill layers.
Binford and colleagues (1970) interpreted the deep
earth ovens to be indirect cooking facilities and the
shallow earth ovens to be direct cooking facilities.
Recent experimental research, however, indicates
that these functional assignments may be incorrect;
Koldehoff (2002) observed experimentally that cook-
ing fires placed directly on pit floors resulted in a
pattern of oxidized subsoil that penetrated several
centimeters along their basal walls. Moreover, this
pattern of oxidation only occurred after a pit was
exposed to a high temperature fire for several hours
(Koldehoff 2002: 190). Thus, the presence of oxidized
soils in the deep earth ovens at Hatchery West
indicates they were probably direct cooking facilities.
It is also likely that the shallow earth ovens lacking
oxidized soils were used for either indirect cooking or
short-term direct cooking activities.
The excavation of a number of deep earth oven pits
with straight walls and flat bases at the Late
Woodland Mund site (A.D. 500–650) in the Ame-
rican Bottom region of western Illinois has provided
additional detailed information on the identification
of earth ovens (Fortier 1983: 120–124). These features
were morphologically similar to the deep earth ovens
Wilson and VanDerwarker An analysis of a maize roast at the C.W Cooper site, IL
168 Journal of Field Archaeology 2015 VOL. 40 NO. 2
at Hatchery West but lacked similar evidence for soil
oxidation along their bases. A number of earth ovens
from the Mund site also each contained a discrete
stratum of burned limestone near the base. In several
cases, this burned limestone layer was found to lie
directly beneath a black greasy layer, which has been
interpreted as decomposed thatch or matting (Fortier
1983). Considering the presence of burned limestone
and the absence of oxidation, Fortier argued that
these represented indirect cooking facilities (Fortier
1983: 124).
It is interesting that the vast majority of the earth
ovens excavated at Late Woodland sites, such
as Range and Woodland Hill (A.D. 500–800) and
terminal Late Woodland (A.D. 800–1050) sites in the
American Bottom region, lacked oxidized soils
altogether. It appears that the act of placing heated
rocks and foodstuffs into a relatively deep pit may
have been the predominant cooking technique during
the Woodland occupation of this region. As we
discuss below, this trend does not appear to have
been the case for the Central Illinois River Valley,
located approximately 170 km north of the American
Bottom.
The C. W. Cooper Site Earth Oven It is clear from the above discussion that there is
significant variation among features identified as
earth ovens at archaeological sites located in Illinois
and in North America. At present it is difficult to
interpret this variability in functional terms, espe-
cially considering that most of the known earth ovens
in archaeological contexts represent disposal (not
cooking) in their final context. The recent excavation
of a pit feature containing the remains of an
accidently-burned maize roast at the C. W. Cooper
site in Fulton County, Illinois provides the opportu-
nity to better understand the functional dimensions
of these ancient cooking facilities.
The C. W. Cooper site is located on the western
bluffcrest of the Illinois River Valley (FIG. 1). Pre-
vious excavations at the site in 1982 and 1983 by the
Upper Mississippi Valley Archaeological Research
Fund uncovered portions of a small Mississippian
village dating to the latter half of 12th century A.D., as
well as a later Oneota village dating to the early 14th
century. Surface artifact distributions cover an
estimated 3 ha although the densest concentration
of subsurface features at the site is restricted to a
3000–4000 sq m area that begins at the edge of the
bluff and extends northwards. Further excavations
funded by the National Science Foundation were
conducted at the site between 2011 and 2013. These
excavations encompassed 204 sq m of the site,
uncovering portions of seven early Mississippian
period (A.D. 1150–1200) buildings and 47 pit features.
A complex of five superimposed pit features,
including the earth oven in question (Feature 13),
was found along the southern edge of these excava-
tions (FIG. 2). Feature 13 was located roughly in the
middle of this pit complex and dates to the
Mississippian period of the site. It was superimposed
by one pit (Feature 12) that was superimposed by
another (Feature 1). This earth oven had a circular
opening that was 120 cm in diameter. It extended
52 cm in depth with out-curving walls toward the top
and a flat base. This feature was excavated by natural
stratigraphic layers which allowed for a detailed
reconstruction of its use and abandonment.
The base of the Feature 13 pit consisted of a layer
of orangeish-red oxidized clay that extended several
centimeters into the surrounding subsoil (FIGS. 3, 4).
This zone of oxidation also extended up the lower
sides of the pit. Above this oxidized stratum was a
thin layer of charred fibrous plant material, resem-
bling wild grass, which appears to have lined the base
Figure 2 Map of the University of California, Santa Barbara
excavations at the C. W. Cooper site.
Wilson and VanDerwarker An analysis of a maize roast at the C.W Cooper site, IL
Journal of Field Archaeology 2015 VOL. 40 NO. 2 169
of the pit to facilitate cooking (FIG. 5). Atop this
fibrous plant material was a dense layer of charred
maize. This layer was removed in its entirety and
processed as several flotation samples totaling 107 L.
Multiple, intact charred cobs with kernels still
attached were present in this layer, as were thousands
of maize kernels, cupules, and smaller cob fragments
(FIG. 6). Unfortunately, these whole ears of maize
(complete with cobs and attached kernels) did not
remain intact during removal. Typically, these maize
ears would have been removed from the pit once fully
cooked; thus, the sheer abundance of burned maize in
this oxidized pit feature indicates that the pit was
abandoned during or after the cooking process and
was never cleaned out.
Our reconstruction of the cooking methods, based
on the pit’s stratigraphy and contents, indicates that
the maize was covered with a layer of clay upon
which a fire was built—as evidenced by wood
charcoal overlaying the clay. In its final form, this
layer of clay was burned until it had hardened,
suggesting that it had been intentionally laid in
uniform thickness over the maize as a protective
buffer from the fire. The near incineration of the
maize appears to have been the result of the intensity
or duration of the fire built above this clay layer. This
fire was evidently too hot or left unattended for too
long, resulting in the burning of the maize until it
became an inedible mass. More than 300 carbonized
wild grass and weedy seeds were identified above the
clay layer, and their abundance above the maize layer
strongly suggests that they were intentionally laid on
top of the clay layer, perhaps as kindling for the fire.
After it was discovered that the maize had burned
beyond edibility, the feature was capped with refuse
and abandoned.
The plant data A total of 11 flotation samples (107 L of soil) were
taken from Feature 13 representing the entirety of the
feature fill (with the exception of the fibrous plant
Limits of excavation
Burned maize
Burned clay
Refuse deposit
Refuse deposit Feature 13Feature 12
SS
Rocks
Ground surface Feature
9 Feature 10 Feature 1 SS
0 20 cm
Figure 3 Profile map of the Feature 13 earth oven at the C. W. Cooper site.
Figure 4 The oxidized clay layer overlying the burned maize
in Feature 13, C. W. Cooper site.
Figure 5 Fibrous plant material at the base of the Feature 13
earth oven, C. W. Cooper site.
Figure 6 Burned maize at the bottom of the Feature 13 earth
oven, C. W. Cooper site.
Wilson and VanDerwarker An analysis of a maize roast at the C.W Cooper site, IL
170 Journal of Field Archaeology 2015 VOL. 40 NO. 2
layer below the maize ears) (TABLE 1). Samples were
floated using a Model A Flote-Tech machine during
the summer of 2011; light and heavy fractions were
bagged separately and shipped to the University
of California, Santa Barbara (UCSB) Integrative
Subsistence Laboratory (ISL) for identification and
analysis. Although the materials from the light and
heavy fractions were processed and sorted separately,
data from the two fractions were combined for
analysis. According to standard practice, the light
fractions were weighed and then sifted through
2.0 mm, 1.4 mm, and 0.7 mm standard geological
sieves. Carbonized plant remains from both fractions
were sorted in entirety down to the 2.0 mm sieve size
with the aid of a stereoscopic microscope 10–4x.
Residue less than 2.0 mm in size was scanned for
seeds, which were removed and counted; in addition,
taxa encountered in the 1.4 mm sieve that were not
identified from the 2.0 mm sieve were also removed,
counted, and weighed. Maize cupules and acorn
nutshells were also collected from the 1.4 mm sieve as
these materials tend to fragment into smaller pieces
and can be underrepresented in the 2.0 mm sieve.
Botanical materials were identified with reference
to the macrobotanical comparative collection at
the UCSB ISL, various seed identification manuals
(Martin and Barkley 1961; Delorit 1970), and the
USDA pictorial website (2011). All plant specimens
were identified to the lowest possible taxonomic level
(TABLE 2), although taxonomic identification was not
always possible as some plant specimens lacked
diagnostic features altogether or were too highly
fragmented. As a result, these specimens were
classified as ‘‘unidentified’’ or ‘‘unidentified seed.’’
In other cases, probable identifications were made;
for example, if a specimen closely resembled a maize
cupule, but a clear taxonomic distinction was not
possible (e.g., the specimen was highly fragmented),
then the specimen was identified as a probable maize
cupule and recorded as ‘‘cf. maize cupule.’’ Once
the plant specimens were sorted and identified, we
recorded counts, weights (g), portion of plant (e.g.,
maize kernels versus cupules), and provenience
information. Generally, most of the seeds identified
in the samples were too small to weigh, and thus only
counts were recorded. Hickory nutshell and maize
remains were both counted and weighed. Seven of the
11 flotation samples produced exceptionally large
quantities of plant remains, yielding sample weights
in excess of 1000 g (with two exceeding 3000 g). In
order to deal with these large samples in a timely
manner, we recorded the total weight for each of the
11 samples and then subsampled them using a riffle
splitter. After the samples were split, the subsamples
chosen for analysis were also weighed. We used this
weight information to extrapolate figures for plant
weight, wood weight, and taxa counts/weights from
the subsample to the total sample. By dividing the
total sample weight by the subsample weight, we
arrived at a figure that defined the proportional
relationship between the sample and its respective
subsample. This figure was used as a multiplier for
the actual counts/weights recorded from the sub-
sample to determine the proportionally equivalent
counts/weights for the total sample.
In total, 52,966 maize fragments weighing 760
grams were identified in this feature (this does not
include the possible ‘‘cf.’’ identifications); more than
44,000 of these fragments were kernels, with the
remainder consisting of cupules and cob fragments
(TABLE 2). Measurements were taken on complete
maize kernels and cupules as part of a related project
(Gracer et al. 2013) and reveal that maize kernels
from Feature 13 are wide and crescent shaped (FIG. 7).
Cob fragments from the 1983–1984 excavations at
C. W. Cooper reveal the presence of 8-, 10- and
12-row maize varieties. These cobs, graciously pro-
vided by Dr. Lawrence Conrad, derive from screened
and hand-excavated contexts and were analyzed by
VanDerwarker in the UCSB ISL. Angle measure-
ments from the Feature 13 maize cupules confirm the
presence of 8-, 10-, and 12-row cobs, in addition to
cupules from the occasional 14-row cob; the majority
of cupules measured, however, come from 10- and 12-
row cobs, suggesting that the maize in this feature
may represent the Midwestern Twelve Row variety
Table 1 Inventory of flotation samples taken from Feature 13 at C. W. Cooper.
Catalog # Sample volume Total sample weight* (g) Plant weight (g) Wood weight (g)
6 26 3161.76* 345.66 9.50 10 10 208.62 1.80 0.85 18 13 485.55 5.36 2.83 19 6 180.79 3.50 0.69 23 10 1711.43* 2.01 0.63 24 6 1038.82* 2.15 0.55 25 11 3052.51* 17.27 1.46 28 4 2545.00* 46.93 3.76 29 1 324.60 2.95 0.27 30 13 1481.15* 167.76 6.68 31 7 1130.20* 201.19 2.33
*denotes that a subsample was taken.
Wilson and VanDerwarker An analysis of a maize roast at the C.W Cooper site, IL
Journal of Field Archaeology 2015 VOL. 40 NO. 2 171
common to the broader Illinois region (Fritz 1992).
Based on average kernel counts from 10- and 12-row
cobs of North American heirloom varieties (from the
UCSB ISL comparative collection), we estimate that
these kernels come from approximately 95 ears of
maize. If we assume a consumption rate of three ears
of maize per person, then this maize roast could have
fed about 31–32 people. Some of the cupules, however,
may derive from 8-row cobs, which would translate
into more ears of maize represented by the kernels.
Regardless of row number, it is clear that this maize
roast was meant to feed a large group of people, on the
order of several households.
While the maize represents 97% by count (99% by
weight) of the plant materials recovered from the
Feature 13, the remaining taxa identified nevertheless
bear mentioning (TABLE 2). A fair amount of nut-
shell fragments was also encountered, dominated by
hickory (Carya spp.), which was found scattered
Table 2 Inventory of plants identified in Feature 13 at C. W. Cooper (cf.5probable but uncertain identification).
Common name Taxonomic name Counts Weights (g)
MAIZE Maize cob fragment Zea mays 68 24.79 Maize cob fragment cf. Zea mays cf. 30 0.14 Maize cupule Zea mays 8826 32.52 Maize cupule cf. Zea mays cf. 6 0.01 Maize kernel Zea mays 44,074 702.42 Maize kernel cf. Zea mays cf. 9 0.09 Total maize (cf. not included) 52,968 759.73 NUTS Acorn Quercus spp. 28 0.13 Acorn meat Quercus spp. 2 0.08 Acorn cf. Quercus spp. cf. 14 0.1 Hazelnut cf. Corylus sp. 1 Hickory Carya spp. 318 3.49 Hickory cf. Carya spp. 4 0.08 Black walnut Juglans nigra 1 0.05 Total nuts 368 3.93 WEEDY SPECIES Amaranth Amaranthus spp. 6 Bedstraw cf. Galium spp. 4 Bulrush Scirpus spp. 19 Bulrush cf. Scirpus spp. cf. 11 Carpetweed Mollugo spp. 1 Cheno/am Chenopodium/Amaranthus 1 Chenopod Chenopodium spp. 310 Goosegrass Eleusine indica 2 Grass family Poaceae 173 Knotweed/smartweed Polygonum spp. 9 Knotweed/smartweed cf. Polygonum spp. cf. 4 Maygrass Phalaris caroliniana 1 Purslane Portulaca spp. 51 Sedge family cf. Cyperaceae 4 Spurge family cf. Euphorbiaceae 1 Tick clover Desmodium spp. 7 Total weedy species 604 FRUITS Maypop cf. Passiflora incarnata cf. 4 Nightshade Solanum spp. 2 Total fruits 6 MISCELLANEOUS Bean cf. Phaseolus sp. cf. 4 Bearsfoot Polymnia uvedalia 1 Squash/gourd rind Cucurbita/Lagenaria 4 Sunflower Helianthus annuus 4 Sunflower cf. Helianthus annuus cf. 1 Total miscellaneous 14 UNIDENTIFIABLE 588 2.19 UNIDENTIFIABLE SEED 25 Total plants 54,618 766.09
Figure 7 Maize kernel image from the Feature 13 earth oven,
C. W. Cooper site.
Wilson and VanDerwarker An analysis of a maize roast at the C.W Cooper site, IL
172 Journal of Field Archaeology 2015 VOL. 40 NO. 2
throughout all the zones of the pit feature. Given that
nutshell was generally used secondarily as a fuel
source, it is not surprising that it was identified in the
upper layers of the pit. The same reasoning can be
applied to the presence of grass seeds and weedy seeds
(which include bedstraw [Galium spp.], chenopod
[Chenopodium spp.], bulrush [Scirpus spp.], purslane
[Portulaca spp.], smartweed/knotweed [Polygonum
spp.], tick clover [Desmodium spp.], and unidentified
members of the grass family [Poaceae]), as these
species were likely used as kindling for the fire set
atop this earth oven. The presence of these species in
the lower levels of the feature is best explained as
intrusive; the intrusion of small seeds and nutshell
fragments into the maize layers of the earth oven
likely originated in a small area of the pit where the
burnt clay layer did not entirely cover the feature.
Discussion and Conclusions A close consideration of the morphology, stratigra-
phy, and archaeobotanical contents of Feature 13 at
the C. W. Cooper site has provided important insight
into one method in which earth ovens were used to
cook food in the late prehistoric Midwest. In this case
a clay layer placed directly over a large number of
maize ears which served to shield the maize from direct
contact with a fire built above it. This particular
cooking event represents a direct method insofar as a
fire was built inside (but at the top of) the pit, but could
also be considered indirect in that a thick clay layer
buffered the maize from direct contact with the fire. It
is clear that the method of cooking used in this feature
differs from techniques used in the majority of the
ethnographic examples, in which the cooks built the
fire (or placed hot rocks) at the base of the earth oven
(Hough 1926: 37; Salazar et al. 2012; Thoms 2008,
2009; Wandsnider 1997). Indeed, the Maya account of
their maize roast, which is the case most analogous to
the C. W. Cooper earth oven, documents the use of hot
coals at the bottom of the pit (Salazar et al. 2012);
despite this singular difference, the layering of vegeta-
tion, maize, and earth was identical in both cases.
Given that no coals or hot rocks were placed below the
maize layer in the C. W. Cooper earth oven, the
oxidized base of this pit is testament to the high
intensity and long duration of the fire built atop it. Pits
with oxidized soils have also been identified at other
late prehistoric era sites in the Central Illinois River
Valley. Esarey (2000) reported the presence of a
number of Late Woodland pits exhibiting oxidized
bases at the Liverpool Lake site in Mason County
Illinois. Moreover, Bardolph (2014) recently docu-
mented a number of heavily oxidized pits at the early
Mississippian Lamb site (A.D. 1100–1150) in Schuyler
County, Illinois. Because most of these earth ovens
were cleaned out and later refilled with refuse, it is
unknown if they were used in exactly the same way as
the C. W. Cooper site feature. The presence of heavily
oxidized soils in these features, however, indicates
their likely use in direct cooking activities.
One of the most important insights gleaned from
the analysis of the C. W. Cooper earth oven is the
large amount of food (ca. 95 maize ears) it was used
to cook. The scale of this maize roast reinforces
previous assertions that such features were used in
the preparation of communal meals, possibly feasts.
Indeed, expansive excavations conducted at the Late
Woodland Range site in the American Bottom region
revealed that earth ovens were often located in areas
shared by multiple households, an arrangement that
led Kelly (1990) to interpret them as communal
cooking facilities. Based on the data presented here,
the nature and scale of the cooking that took place in
Feature 13 indicate that earth ovens at the C. W.
Cooper site were also used for the communal
preparation of foodstuffs. Whether or not the maize
roast that occurred in Feature 13 was conducted as
part of a first fruits celebration, as documented in the
Maya case, is unclear. Ethnohistorical studies from
the southeastern United States provide ample evi-
dence of annual events marking the first maize
harvest, known regionally as the Busk or Green
Corn Ceremony (Hudson 1976). While it is tempting
to interpret the C. W. Cooper earth oven as part of an
annual harvest feast, it is simply not possible to
achieve this level of specificity. We can say that the
C. W. Cooper maize roast was meant to involve a large
gathering of people, perhaps the entire community
that was residing that the site. This is an important
point as the late 12th century was an era when the
regional population was beginning to establish larger
and more nucleated settlements. Feasting events such
as the one represented in the Feature 13 earth oven
deposit may have been instrumental in integrating
these expanded communities.
This investigation of earth oven functionality is
part of a broader, ongoing effort to understand
diachronic changes in foodways in the late Prehistoric
Central Illinois River Valley. Our recent analysis
of changing plant subsistence during the Late
Woodland–Mississippian transition revealed a sig-
nificant increase in maize production and consump-
tion during the early Mississippian period, the latter
period represented by the C. W. Cooper plant
assemblage (excluding the Feature 13 maize remains)
(VanDerwarker et al. 2013). It is interesting that the
earth oven feature at C. W. Cooper represents the
persistence of a Late Woodland cooking technique
traditionally embedded within a context of commun-
alism but that simultaneously incorporates a rela-
tively new dietary element—in this case, maize. While
maize was certainly present in Late Woodland diets
Wilson and VanDerwarker An analysis of a maize roast at the C.W Cooper site, IL
Journal of Field Archaeology 2015 VOL. 40 NO. 2 173
of the Illinois Valley, it did not become a significant
staple food in the region until the early Mississippian
period (VanDerwarker et al. 2013). While we may
never know the reason this large outdoor roasting
event failed, the fact that it did fail provided us the
opportunity to see how earth ovens were constructed,
used, and the types of foods prepared within in the
Central Illinois Valley and perhaps the broader
Midwestern United States.
Acknowledgments This material is based upon work supported by the
National Science Foundation under grant 1062290.
We acknowledge Amy Gusick and Kristin Hoppa for
their careful excavation of this feature, as well as their
participation in preparing a preliminary conference
version of this manuscript that was presented at
the 2011 Southeastern Archaeological Conference in
Jacksonville, Florida. We also acknowledge the work
of Jennifer Alvarado in sorting and counting the
abundant maize remains from Feature 13. Finally,
we thank Dana Bardolph and Danielle Kurin for
providing comments on earlier drafts. Thanks also to
Larry Conrad for providing access to maize cobs
from earlier WIU excavations of the site.
Gregory D. Wilson (Ph.D. 2005, University of North
Carolina, Chapel Hill) is Associate Professor at the
University of California, Santa Barbara. His research
is concerned with issues of social inequality, identity
politics, and violence in Precolumbian North and South
America, through a lens of household and community-
centered archaeology.
Amber M. VanDerwarker (Ph.D. 2003, University of
North Carolina, Chapel Hill) is Associate Professor at
the University of California, Santa Barbara. She has
been involved in field and laboratory work in Mexico,
eastern North America, and Peru. Her research
encompasses a variety of methods, regions, and themes
that focus on the relationship between humans and food
in the New World, especially during the period of
transition to agriculture.
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/ENU (Settings for the Rampage workflow.) >> >> setdistillerparams << /HWResolution [2400 2400] /PageSize [612.000 792.000] >> setpagedevice