The stratigraphic observations Sample Clauses

The stratigraphic observations. After deforestation, an aligned outcrop of rocks presented itself at surface level, as above-mentioned, reflecting the bedrock or spine of the hillock (US 5000). The disintegration or alteration of these rocks represents a coating layer (US 4000) with spatial variations as to its texture: siltier to the east of the bedrock emergence and clayeyer to the west. Indeed, we observed a smaller inclination at the eastern flank compared to the much steeper western flank. Thus, when rain falls on the hilltop, the excessive water would probably descend towards the east, as evidenced here by means of an eroded area, interpreted as a run-off gully (F 202 and F 203). Four sections were documented within the perimeter of the excavation of which the first is located at the summit (Section A) and the other three concern the excavation’s northeastern wall profile (Sections B-D) (Fig. 9.3). The description of these four sections indicated a similar, relative succession of stratigraphic layers. This enabled us to reduce these sections to a single schematic one, consisting of five stratigraphic units (Fig. 9.4). The upper part of the profiles measures c.40 cm and consists of a humic, xxxxx silt layer containing artefacts. Its upper part, measuring between c.5 and 10 cm in thickness, represents the forest floor (US 1000). The lower part, situated at a depth of between 5 and 40 cm, corresponds to a dark coloured layer which is entirely restructured. In it ceramic material as well as fragments of charcoal were detected (US 2000). Below this first, superficial part, we observe a silt layer (slightly xxxxx and clayey) measuring between c.20 and 30 cm thick which is homogeneous and has a light brown to yellow ochre colour (US 3000). A clay layer corresponding to the alteration of the bedrock (US 4000) emerges as a N-S stretching row of boulders within the excavation’s perimeter. The non-altered red coloured bedrock (US 5000) was reached in a number of sections during the excavation (e.g. pit F 158).
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