At the completion of this stage, the site of Britain was at 30°S and Nova Scotia at about 45°S. This collision is represented by the Caledonian folding or in North America as an early phase in the Acadian orogeny.
Ao remate desta etapa, Gran Bretaña estaba a 30° S e Nova Escocia a uns 45° S. Este choque está representado polos dobramentos caledonianaos ou en Norteamérica como unha fase inicial da oroxenia acadiana.