Based on fourteen radiocarbon datings, mainly of marine molluscs, a shoreline displacement curve has been constructed for Verdalsøra, Central Norway. The sample localities are described briefly. The curve is compared to curves based on datings of gyttja, especially the curve from Frosta 30 km further SW.
Radiocarbon datings and morphological features at Verdal point to a slow regression during the time interval 7,000-8,000 B.P. A preliminary equidistant shoreline diagram is presented.