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Tracing the Source of the Elephant And Hippopotamus Ivory from ...

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These flood basalts have 87 Sr/ 86 Sr values <strong>of</strong> 0.70304-0.70429 in <strong>the</strong> northwestern<br />

Ethiopian highlands (data represented in Figure 47 by solid red circles; see Figure 61 for<br />

geological map <strong>of</strong> <strong>the</strong> region and locations <strong>of</strong> samples tested).<br />

Basalts <strong>from</strong> Southwestern Ethiopia were analyzed for strontium isotopes by<br />

Ayalew et al. (1999), again demonstrating a small range <strong>of</strong> 0.7031-0.7039 (Figure 47,<br />

represented by solid green triangles). Figure 62 illustrates <strong>the</strong> location <strong>of</strong> <strong>the</strong>se samples.<br />

Moreover, Barbieri et al. (1976) have similar values at an average <strong>of</strong> 0.7035 ± 0.0004 (n<br />

= 6) for Late Tertiary-Quaternary basalts <strong>from</strong> <strong>the</strong> Harar Plateau, 50 km nor<strong>the</strong>ast <strong>of</strong> Gara<br />

Badda (Kennan et al. 1990: 41).<br />

Figure 62: Map <strong>of</strong> southwestern Ethiopia showing <strong>the</strong> main volcanic geology and sample<br />

locations (white circles) (Ayalew et al. 1999: 383, figure 1).<br />

150

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