Barvaux se encuentra en la conocida zona de caliza del Devón. La zona de caliza es una estrecha franja al sur de Fagne-Famenne y consiste casi exclusivamente en caliza del Devón Superior. Es como un escalón hacia las Ardenas. Está a bastante más altura que la depresión de Fagne-Famenne. Los ríos que provienen de las Ardenas y que atraviesan esta región dan origen a espectaculares fenómenos de disolución. En geología, estos fenómenos de disolución se llaman karst.
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Source: cartogis.ugent.be
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Source: cartogis.ugent.be
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