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botswana/namibia - Cour international de Justice

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unsubstantiated thesis that Botswana now adduces scientific evi<strong>de</strong>nce and refers to the<br />

consi<strong>de</strong>rable published writings on the geomorphology and hydrology of the Chobe and<br />

Upper Zambezi Rivers.<br />

325. The <strong>Cour</strong>t is respectfully referred to the scientific evi<strong>de</strong>nce based on geomorphology and<br />

hydrology and substantiated by fieldwork contained in the First Opinion of Professor F.T.K.<br />

Sefe, University of Botswana, in the Appendix to Chapter VII of the Memorial of Botswana<br />

for a general <strong>de</strong>scription of the geomorphology of the region, to his Second Opinion relating<br />

more specifically to the hydrology of the Chobe River and the Island, and to the<br />

Sedimentological Study of Professor Sefe, ma<strong>de</strong> with the assistance of Mr. I.M. Muzila, B.Sc.<br />

(C. Engineering), Principal Hydrological Engineer, Department of Water Affairs, Ministry of<br />

Mineral Resources and Water Affairs, Government of Botswana. Mr. Muzila by training and<br />

by reason of his professional duties, has unrivalled knowledge and experience of the<br />

hydrology of the Chobe River. This Second Opinion and Sedimentological Study and the<br />

Analysis of Professor Alexan<strong>de</strong>r's Expert Report, also carried out by Professor Sefe, are all<br />

contained in Volume 2 of this Counter-Memorial, and form an integral part of Botswana's<br />

case.<br />

326. The population and habits of the wildlife provi<strong>de</strong> evi<strong>de</strong>nce that the southern channel<br />

constitutes no barrier for transit to the island, and its shallow tranquil waters are used by<br />

hippopotamus as a resting place, undisturbed by river flow or navigation of craft.<br />

(C) Botswana's case relating to the River Chobe based on scientific evi<strong>de</strong>nce<br />

327. Botswana's case is supported by the following propositions relating to the Chobe River;<br />

each of these are <strong>de</strong>alt with in greater <strong>de</strong>tail below at the passages as indicated.<br />

(i) The Chobe is the geographical feature in Article III of the 1890 Agreement<br />

328. Article III of the Anglo-German Agreement of 1890 i<strong>de</strong>ntifies the Chobe River as the<br />

geographical feature along which the boundary "<strong>de</strong>scends" to its junction with Zambezi,<br />

(paras.355 to 362 below).<br />

(ii) The Chobe is a river in<strong>de</strong>pen<strong>de</strong>nt of the Zambezi River<br />

329. The Chobe River is a river in<strong>de</strong>pen<strong>de</strong>nt of the Zambezi River. It flows downstream from<br />

its source in the Angolan Highlands to its junction with the Zambezi at Kazungula (paras.363<br />

to 364 below).<br />

(iii) The Chobe has a stable profile as a perennial mature river<br />

330. Scientific evi<strong>de</strong>nce based on geomorphology and hydrology and substantiated by field<br />

work and analysis <strong>de</strong>monstrates the in<strong>de</strong>pen<strong>de</strong>nt function of the Chobe River as a perennial<br />

mature river, the existence over many thousand years of the present alignment of the northern<br />

channel, and the stability of the present configuration of the island with visible and nonerodible<br />

banks in the northern channel (paragraphs 363 to 364).<br />

(iv) The Chobe is a perennial river with visible and stable banks

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