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The Cemetery R12
El Salha 2004
Postcard from Sudan...

Kasura


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Working methods

The archaeological survey of the area has been conducted along 2 x 1 km transects both along the White Nile bank and towards the interior to the west. Such a strategy allowed us to test, at a good level of confidence, the archaeological potentiality of the region under scrutiny.
This intensive and systematic approach revealed a large number of prehistoric sites often heavily attacked by erosive agents and leaving on the surface isolated scatters of pottery fragments and/or lithic tools and debitage.
The spatial distribution of transects was planned to intercept different geo-morphologic features previously recognised on the base of aerial photos, satellite imageries and the available cartography and thus to study specific relationships between different environmental features and the archaeological evidence of different periods.

The archaeological record.

More than one hundred archaeological sites have been located so far, covering a time span from the Palaeolithic to the Post-Meroitic period. The oldest materials, dating to the Late Pleistocene (Middle and Late Palaeolithic) have been found in the Jebel Baroka area, while many sites dating to Early and Middle Holocene (Khartoum Mesolithic, Early and Late Neolithic) have been located at the feet of the Jebel and along the western bank of the White Nile. Later periods, Meroitic and Post-Meroitic evidence seem to be spread in the area, from the piedmont to the alluvial plain of more recent geological formation.
Among the sites we discovered two large cemeteries (10-U-3 and 10-U-21) with stone cairns have to be mentioned. Both of them were mapped with the aid of a Leica total station kindly provided by Leica Geosystem of Milan. Of the two cemeteries one (10-U-21) (Figs. 4-5) is quite surely of Post-Meroitic age. .
The second (10-U-3) (Figs. 6-7) occupies a large risen area on the edge of the alluvial plain and has two different types of stone cairns. One is built with black Nubian sandstone blocks, the other with white sandstone flakes. Some of the first type of graves have a central squared structure made by vertical flat slabs.
The other type seems to be less accurately built with sandstone flakes of different size irregularly placed to cover the burial. In both cases the diameter of the tumuli varies from 1 to 11 m with a 65% between 0.96 and 2.96 m. The black sandstone cairns are similar in shape to structures found in the eastern desert and dating to the 3rd millennium BC.
10-U-3, as mentioned above, is located on a rocky platform 2-3 m high, bordering the alluvial plain in the vicinity of the wadi Baroka were we have located several stone structures (Fig. 8) and concentrations of pottery and lithic of different age from the Neolithic to the Christian period. If a dating to the 3rd millennium BC of some of the graves in the cemetery will be confirmed by future excavation tests, all the area will results of major interest for the reconstruction of the prehistoric peopling of the area.
The other graveyard (10-U-21) consists of 21 cairns of a type well known in other Sudanese regions (Amri-Kirbekan and Jebel Kulgeili). Their shape is drop-like and the elevation is about 1m and can be dated to Post-Meroitic age.
To the same period are dated the earthen circular tumuli which were located along the Nile bank and on the alluvial plain (Fig. 9)
These tumuli are circular mounds built with earth mixed with
river pebbles above a burial chamber excavated in the ground.
They are usually organised in clusters of 5 to 10 and have a diameter which often exceeds 20 m. Only one tumulus of this kind has been excavated in the past (1953) next to the Al Oshara village. Stone cairns have not been found along the Nile bank. It is possible that this kind of structures were destroyed by the common practice to reuse the stones in building activities as suggested by the location of an almost completely depleted grave located next to the El Oshara village.
Meroitic materials were collected, along the Nile, at the surface of site 10-X-8, a large low mound which originates in the Mesolithic and Neolithic periods (Figs. 11-12). 1 km to the north of this site, an important Early Islamic settlement (10-X-5) was located. Here a section cut by a seasonal river course exposed a section with several anthropic layers, fireplaces and mud-brick structures (Fig. 10).