Certain characteristics

Interesting as this illustration is of how

strati graphical formations can be created, this early mention of Egypt must

serve as an occasion to introduce certain reservations regarding that country,

in relation to the subject under discussion. For it should be said at once that

Egypt has certain characteristics which make it less suitable than others do

for the study of mounds.

This is perhaps partly to be attributed to

the abundant supply and general use of building stone, which greatly prolonged

the survival of Egyptian buildings. But it is also partly due to the fact that,

in the narrow valley of Upper Egypt, land is too valuable to allow large ruin

fields of brick buildings to remain derelict; and the fellahin have long since

discovered that the occupational debris with which such ruins are Hide, when

spread over their fields, makes the finest fertilizer available.

Burin any case, those who have approached

the subject of Egyptology will know that archaeology in Egypt, when it took the

form of actual excavation, has always been concerned almost exclusively with

stone temples, tombs and cemeteries. Mounds in Egypt are confined for the most

part to the Delta of the Nile; and, with so much else to attend to, their

excavation has till now been very considerably neglected.

So let us glance once again at the pattern

of countries in which mounds are everywhere found and have been more generally

excavated. From Egypt they spread northward through the Levant and westward

through Anatolia to the Balkans. Eastward they follow the curve of Breasted’s

“crescent” through the rich farmlands in the foothills of the Armenian

mountains to Iraq and Persia and so, southward of the Elburz range, to

Afghanistan and the Indus valley.

Mesopotamia

But the focal point of the whole area,

where mounds are so plentiful that they become the most characteristic feature

of the landscape, is the twin river valley of Mesopotamia which is in fact not

a valley at all but a vast province of partially irrigated alluvial desert. It

is a habit of thought to apply the name Mesopotamia to this basin of alluvium,

which represents half of modem Iraq. But it has come to be known to our own

generation that the first human settlers in this province, the ancestors of the

later Sumerians, were themselves comparative latecomers, and that the

undulating hill country of northern Iraq had a much earlier record of Neolithic

farming communities.

This may help to explain the impression,

which has grown upon one, after long periods of travel in those parts, that the

Assyrian uplands around Mosul and their westward extension through the valleys

of the Khabur and Balik rivers into North Syria must have been the most thickly

populated area of the completely ancient world. Certainly today, they are more

thickly studded with ancient mounds than any other part of the Near East.