Fagne-Famenne-regionen er egentlig ikke mere end den mest sydlige depression (på bestemte steder op til 20 km bred) af Condroz. Hvad der skiller sig ud i relieffet er, at dette område ligger betydeligt lavere end de øvrige depressioner i Condroz. Det skyldes, at undergrunden i Fagne-Famenne består af skifer fra karbon (hårdt blevet ler, der kan optage meget vand). Skifer viser lidt modstand mod frost. Under istiderne (glacialer) frøs det hos os i de lange vintermåneder. Vandet, der var i skiferne, blev til is. Vand, der fryser, udvider sig og har en enorm kraft. Derfor bliver klippematerialet nedbrudt til mindre stykker (erosion forårsaget af frostvirkning). I de kortere somre transporterede de enorme floder (der transporterer store mængder smeltevand) skiferne væk fra området.
Source: cartogis.ugent.be
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Source: cartogis.ugent.be
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Source: cartogis.ugent.be
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