Abstract
A section of Precambrian rocks, recently exposed at road-work, gives for a distance of less than 100 m an illustration of the geological evolution during that time. On a surface of Pregothian granite are deposited arkose, porphyrite, rhyolitic porphyry, ignimbrite, and conglomerate belonging to a belt of Gothian supercrustals which crosses eastern Småland in WNW—ESE-direction. The whole series is steeply raised. According to hitherto made age determinations the age of the Gothian rocks of southern Sweden seems to be about 1700–1800 m.y. (Welin 1966).

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