The top of soil Zone IIb in the area surrounding the mound was, on an
average, about 0.7 feet below the surface of the floodplain. The bottom
of the mound structure, however, extended to an average depth of 1.4
feet below the floodplain surface where it terminated within Zone IIb
(Fig. 3). Thus the surface of Zone IIb immediately beneath the mound
formed a shallow, saucer-shaped depression which must have resulted from
digging away of the topsoil before the mound was erected. This shallow
pit (perhaps originally 1.0 to 1.5 feet deep) was approximately the same
size and shape as the base of the mound.
OCCUPATIONAL FEATURES
Besides the mound itself, two occupational features were found in the
Mound A area: (1) an area of burned soil within the mound fill (Feature
No. 1), and (2) a sub-mound burial (Burial No. 1). Each is described
separately below.
_Feature No. 1_
This was an elongated area of heavily burned, sandy clay lying within
the matrix of the mound fill (Fig. 3). Since the northern end of Feature
No. 1 was not completely excavated, the exact dimensions were not
determined; but the maximum length was evidently between 9 and 10 feet,
while the maximum width was 4.3 feet. The long axis ran approximately
north-south. Profiles revealed a lenticular cross section with a
pronounced thickened area near the mid-point of the east edge. Near the
center the burned zone was 0.5 feet thick; the thickened area near the
east edge reached a maximum thickness of 1.5 feet.
[Illustration: Fig. 3
HARROUN SITE—41UR10
PROFILE OF MOUND A
(ALONG N20 LINE)
dark gray, sandy mound fill
Feature No. 1
Zone IIb sand, sub-mound
Zone IIa sand
HARROUN SITE
41UR10
PROFILE OF MOUND B
(IDEALIZED SECTION THROUGH CENTER OF MOUND)
floor of House No. 3
central hearth
post molds
stump disturbance
humus
gray, sandy mound fill
whitish, sandy mound fill
undisturbed sub-mound soil]
The surface of Feature No. 1 was burned to a conspicuous degree of
hardness and was sharply demarcated from the soft, unfired mound fill
which overlay it. Beneath the central portion, heat had produced a thin
zone of reddish sand which merged gradually with the underlying grayish
sand of the mound fill.
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