botswana/namibia - Cour international de Justice
botswana/namibia - Cour international de Justice
botswana/namibia - Cour international de Justice
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(ii) The misrepresentation that the 'Alexandrine' channel is the sole channel to carry<br />
substantial flow, and that such flow comes from the floodwaters of the Zambezi<br />
288. The 'Alexandrine channel' is an invention of Professor Alexan<strong>de</strong>r and set out in his<br />
Report:-<br />
"Photographs 3, 4 and 5 show that the left bank of the southern channel along this reach of the<br />
southern channel is only a few centimetres above the stagnant water level in the channel. The<br />
shape and characteristics of the bank show that flow takes place across the island (italics<br />
ad<strong>de</strong>d) and into the southern channel along this reach of the channel." (Namibian Memorial,<br />
Vol.VI, Part 1, Expert Report, p.24,para.9.4).<br />
289. When the Zambezi is in flood, flow is:-<br />
"along a broad band on the Island (Zone d in Diagram 4,Sheet 17) that has a lighter and<br />
smoother surface on the aerial photographs. The southern channel is located within this band<br />
that i<strong>de</strong>ntifies the southern channel as being the path along which the bulk of the water in the<br />
Chobe River is conveyed". (Namibian Memorial, Vol.VI, Part 1, Expert Report, p.35, para.<br />
12.7).<br />
290. This is a gross misrepresentation of the topography and hydrology. It totally contradicts<br />
the observable facts on the ground. Photograph 2, Sheet 20 and Photo 4, Sheet 21 of the<br />
Expert Report, (Namibian Memorial, Vol.VI Part 2) show the extent of the island covered by<br />
this broad band. No left bank is visible but a line drawn in a north-easterly direction across the<br />
Island is labelled in Photo 2, in what seems a total disregard of the discernible facts, as the<br />
"centre of the main channel". In fact the line across the island to which Professor Alexan<strong>de</strong>r<br />
refers, far from being a bank of a river, is an extension of the inlet at the eastern end of the<br />
southern channel, and is a low lying sub-channel, dividing the western higher part of the<br />
island from the lower eastern sector. Reference to the August 1947 aerial photograph reveals a<br />
string of pools/damp areas in the mid-section of this sub-channel. The presence of pools of<br />
water in the low-lying parts of the island is confirmed by the Landsat (Satellite) imagery of<br />
June 1975, particularly the false colour composite in Figure 14 (Professor Sefe's Second<br />
Opinion, page 56, para. 75).<br />
291. Contrary, therefore to his general requirement of visible banks, the left bank of this<br />
'southern channel' has no visible bank. In his Report Professor Alexan<strong>de</strong>r attempts somewhat<br />
mystifyingly to explain this absence:-<br />
"..the course of the Chobe River can be readily and unambiguously <strong>de</strong>termined along the<br />
whole length of the river from Point (8) on Map 2 on Sheet 29 right through to the confluence<br />
of the Chobe River and the Zambezi River at Point (12) on the map. Along those reaches of<br />
the Chobe River where the left bank of the river is not visible, the left edge of the main<br />
channel has to be <strong>de</strong>termined by other means bearing in mind that it is the edge of the zone<br />
along which the largest proportion of the annual flow in the river is conveyed." (Namibian<br />
Memorial, Vol.VI, Part 1, Expert Report, p.19. para.7.14.)<br />
This is an example of his introduction of <strong>de</strong>liberate confusion as to the significance of banks.<br />
292. A further point to note is that, on Alexan<strong>de</strong>r's thesis, even assuming the major source of<br />
flow is floodwater, the closer location of the northern channel to the Zambezi and its flood