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botswana/namibia - Cour international de Justice

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561. At paragraphs 294 to 296 the Botswana Memorial drew attention to the inaccuracy and<br />

distortion resulting from the superimposition on geographical features of the drawing of a line<br />

to indicate a boundary. The Sketch Maps of Bechuanaland Protectorate which were used to<br />

illustrate the Bechuanaland Reports beginning in 1912 illustrate the unreliability of <strong>de</strong>piction<br />

of <strong>international</strong> boundaries on maps. The Botswana Atlas sets out copies of the maps for the<br />

years 1911-1915 (Maps 8 to 11). Mr. Rushworth very fairly states the position:<br />

"The 1912 version has the boundary on the south si<strong>de</strong> of the Chobe, changing to the north si<strong>de</strong><br />

in 1915 and back to the south si<strong>de</strong> in 1946 (sic). This <strong>de</strong>monstrates that when, for clarity, a<br />

boundary has to be shown alongsi<strong>de</strong> a feature, the si<strong>de</strong> it appears is chosen by the<br />

draughtsman as a matter of convenience." (Namibian Memorial, Vol.V, Annex 102,p.41).<br />

562. The Sketch Map of Bechuanaland Protectorate 1:2000,000 War Office Printed at OSO<br />

1913 provi<strong>de</strong>s a further illustration of the problems which boundaries along rivers present to<br />

mapmakers. Rushworth a<strong>de</strong>quately sums up:<br />

"Boundary alongsi<strong>de</strong> features at alternating si<strong>de</strong>s. No island in Chobe. Note in key against<br />

boundary symbols 'Where these follow a road or the main channel of a river they have been<br />

shown to one si<strong>de</strong> to prevent confusion". (Namibian Memorial, Vol. V. Annex 102,p.42).<br />

563. The continuing perplexity of mapmakers as how to indicate boundaries on rivers is well<br />

illustrated by the maps in Group d. in Mr. Rushworth's list of maps. Two methods adopted<br />

were either to place the boundary line on one or other bank of the river or to indicate it along<br />

the river but omitting any line at a bifurcation. In<strong>de</strong>ed, by the time of the 1933 British War<br />

Office Map of Bechuanaland Protectorate, standard practice as regards intercolonial<br />

boundaries along rivers was to place them alongsi<strong>de</strong> the river bank, alternating from one si<strong>de</strong><br />

of the river to the other at regular intervals, of 10, 50 or 100 miles, according to the scale of<br />

the map.<br />

(G) A Chronological Survey of the Available Maps<br />

564. A general chronological survey of the available maps will now be given. For quick<br />

reference, at the end of this Chapter, a complete list is given of the maps in chronological<br />

or<strong>de</strong>r for which Botswana has provi<strong>de</strong>d copies in its Atlas accompanying its Memorial and in<br />

its Supplementary Atlas accompanying this Counter-Memorial. For a <strong>de</strong>tailed examination of<br />

the additional maps referred to by Botswana in this Chapter and of the 41 serial maps listed by<br />

Mr. Rushworth, the <strong>Cour</strong>t is respectfully referred to the list of maps appen<strong>de</strong>d to this Chapter<br />

and to Appendix 1 to this Counter-Memorial.<br />

(i) The period prior to the 1890 Agreement<br />

565. The maps, as well as the reports of the early explorers of Southern Central Africa, such<br />

as Livingstone, Selous, An<strong>de</strong>rson, Schulz and Hammar, and Reid, all substantiate the<br />

existence of the Chobe River as an in<strong>de</strong>pen<strong>de</strong>nt perennial river (See Chapter 6, paras 355-65).<br />

The Sketch Map of the Chobe River by Dr. Benjamin Bradshaw (Botswana Atlas, Map 1)<br />

provi<strong>de</strong>s a valuable early and reasonably accurate <strong>de</strong>piction of the configuration of the island<br />

and the two channels. As Mr. Rushworth comments, the scale and shape of the river is<br />

remarkably good and the southern channel is accurately portrayed. In addition to the marked<br />

sinuosity of the southern channel, of particular note is the sharp right hand turn which marks<br />

the western entry point of the southern channel which is to be contrasted with the continuity

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