Exact(60)
These ranges are part of the Togo-Atakora Mountains, which extend northward into Togo and Benin.
These ranges are formed of sand washed ashore and blown inland by the trade winds.
These ranges also vary quite a bit by individual VC.
These ranges agreed well with our data.
These ranges formed the unique domains of localized plastic deformation.
These ranges are: Packet loss : 0 19 (1% step).
These ranges are in agreement with Koudjonou et al. (2008).
These ranges were described in Aller et al. (1987).
These ranges were determined by inspecting various inversion-based models and the regional seismotectonic setting.
These ranges and "reductions" highlight the uncertainty and normal variations in the measurements.
These ranges were considerably distorted by the studies among members of lay headache organisations.
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