National Institute of Informatics - Digital Silk Road Project
Digital Archive of Toyo Bunko Rare Books

On plate 5 I have represented the three sites one above the other according
to their order of succession, and have assigned values, in feet of strata, to the
intervals that were due to periods of abandonment and wastage.

Into the method adopted in estimating the culture-gaps, there enter both
geological and archeological factors. In chapter II it was shown that the observa-
tions made in our shafts proved that the delta lies on the piedmont belt of tilting,
or rather of the reciprocal movement due to removal of load to the plainward
side by the deposition there of alluvial silts. It was shown also that in the part
of the delta upstream from the alluvial shore-line, the channel of the stream was,
at repeated intervals, alternately cut down to a considerable depth, and again
filled up with silts. We were able to determine definitely two such cuttings-down
and three fillings-in or aggradings, all during the lives of the three sites. Now,
these geological events ran parallel with the human history of the delta-oasis, and
since they have an important bearing on this history in several directions, I have
platted them on plate 5 parallel with the cultures.

The North Kurgan was founded on a previously dissected valley at a time
when this valley was aggrading, and the valley continued to fill till towards the
end of the oldest culture. The first settlement extended down the side of the
valley to a level 28 feet below the present surface of the delta-plain, which latter
we will use for a datum in this discussion. At this level we find in shaft I standing
house construction, and at the same level in shaft II there occurred in alluvial
sediments fragments of the pottery characteristic of this oldest culture. No pot-
tery was found below this. From —28 feet upward the alluvium contains this
oldest pottery as far as —20 feet, where there occurs the evidence of the filling
having ceased; for the presence of pottery characteristic of the upper culture of
the kurgan intimately associated with charcoal and animal bones indicates an
occupation of a dry plain and not of a flood-plain.

The relative time during the life of the oldest occupation at which this aggrad-
ing ended is determined proximately as follows. It was shown in chapter II
that we were able to determine that the rate of growth of the alluvial silts in the
valley was to that of the culture-strata as 1 to 2.5. Now the 8 feet of silts between
—28 and —20 feet are the equivalent of 20 feet of culture-strata at the ratio of
1 to 2.5. But the oldest occupation of the kurgan has 45 feet of strata, leaving
a range of 25 feet before the end of the first culture within which to place the end
of the aggrading. I have taken the mean, and placed the time of ending of the
aggrading at a point 12.5 feet of culture-strata before the end of the life of the first
settlement, that is, opposite 32.5 feet above the base of the kurgan. The next
aggrading had already begun before the first settlement of the South Kurgan,
which, like its northern neighbor, was started on the edge of a valley; and it
continued until there had accumulated 52 feet of culture-strata, as stated in chapter
II, and is so represented on the diagram. That the valley was then cut down
to at least —28 feet, and had aggraded at least 12 feet before the beginning of the
upper or iron culture, is shown by the presence at 16 feet in shaft B of pottery