A series of marbles, schists, and quartzites similar to those in the Kongsfjorden, probably of Hecla Hoek age, occurs in the Snoefjella and Dovrefjella area, north of Ekmanfjorden. The structure and metamorphism agree with the general Caledonian trend, but various anomalies are present which are as yet unexplained. Only tentative correlations can be attempted. Igneous rock in the form of a porphyritic olivine basalt occurs on Eidsvoll hill, where the remnants of two flows can be discerned. Four chemical analyses are given.

GeoRef, Copyright 2004, American Geological Institute. Reference includes data from Bibliography and Index of Geology Exclusive of North America, Geological Society of America, Boulder, CO, United States