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botswana/namibia - Cour international de Justice

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421. This photograph is part of a series flown by the South African Defence Authorities in<br />

June 1977, in accordance with a survey plan, copy of which has been obtained from the<br />

Directorate of General Surveys, South Africa, and appears in the Botswana Supplementary<br />

Atlas to this Counter-Memorial. to be used in the production of the 1978 Joint Air<br />

Reconnaissance Intelligence Centre map (The JARIC map) (See the Botswana Atlas, Map<br />

22).<br />

422. As the photography was required for reconnaissance mapping, the scale of the original<br />

series was very small; (1:150,000 or 1 cm = 1.5 kms.).<br />

423. Even at this scale it is quite evi<strong>de</strong>nt that the eastern and southern channel is very much<br />

smaller than the western and northern channel, almost disappearing near the Headquarters of<br />

the Chobe National Park and around the Sediment Spit marked 'A'. It is probably for this<br />

reason that the military cartographers showed the southern channel as an inlet on the JARIC<br />

map and not as a through channel.<br />

424. This 1977 JARIC aerial photograph is shown in Figure 13 of the Second Opinion of<br />

Professor Sefe, Appendix 2 to the Counter-Memorial, p.53. It was scanned at high resolution<br />

and false colour applied to the resulting image. The contrast between the northern and<br />

southern channel is revealing, showing the southern channel to be shallower than the northern<br />

channel. The southern channel between the 'lagoon' sector and its confluence with the<br />

northern channel and in the bend of the mean<strong>de</strong>r loop has the same colour tone as the Kasai<br />

channel, indicating that both are of shallower <strong>de</strong>pth than the northern channel.<br />

The June 1997 Photographs (Scale 1;20,000 and 1:17,000) taken on 5 June 1997 (Photo K).<br />

Reproduced with labels at page 187.<br />

425. This photography was un<strong>de</strong>rtaken as the high-flood waters were receding to illustrate the<br />

present-day situation around Kasikili/Sedudu Island and is the first official air-photograph<br />

taken in this area since 1985. The surface of the island is still partially covered by shallow<br />

water as is the central sections of the sediment spit marked 'B' in the southern channel.<br />

G92 - July 1997 aerial photograph<br />

G35 - June 1997 aerial photograph with labels<br />

426. The Namibian Memorial refers to "the existence of ..sandbars and the changes in their<br />

position and shape over the years" as indicative of active river flow (Namibian Memorial,<br />

p.56,para.155) and Professor Alexan<strong>de</strong>r purports to i<strong>de</strong>ntify such sandbars on Diagram 5 of<br />

sheet 18 (Namibian Memorial, Vol.VI,Part 2, and see also Part 1, p.23, para.8.13) and cites<br />

this as evi<strong>de</strong>nce that the southern channel is active and is therefore the main channel.<br />

427. Reference to this photograph at the points marked 'B' and 'C', clearly reveals these same<br />

sediment bars in essentially the same size, shape and location, as on the 1925 photograph<br />

(photo 'A') and in<strong>de</strong>ed on all the intervening photographs in the series.<br />

428. This is visual proof that these features are permanent surface features over a period of 72<br />

years and are in no way 'active'. This fact therefore completely contradicts the Professor<br />

Alexan<strong>de</strong>r's theory that they are proof of an active channel.

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