NORWEGIAN JOURNAL OF GEOLOGY The Late Neoproterozoic Smalfjord Formation of the Varanger Peninsula in northern Norway 133 The Late Neoproterozoic Smalfjord Formation of the Varanger Peninsula in northern Norway: a shallow fjord deposit B. Gudveig Baarli, Rebekah Levine & Markes E. Johnson Baarli, B.G., Levine, R. & Johnson, M.E.: The Late Neoproterozoic Smalfjord Formation of the Varanger Peninsula in northern Norway: a shallow fjord deposit. Norwegian Journal of Geology,Vol. 86, pp. 133-150. Trondheim 2006. ISSN 029-196X. The Smalfjord Formation in the Varangerfjorden area of northern Norway was deposited as valley fill during an interglacial period of the Varange- rian (Marinoan) glaciation. The paleovalley was initially cut by glacial erosion and braided rivers. Subsequent marine transgression due to glacial eustasy entered through the fjord valley mouth located to the present WNW and advanced across an irregular valley floor. As the initial transgres- sion slowed down, the shallow fjord acted as a normal storm-dominated estuary and was filled by a prograding bay-head delta and flood-tidal delta prograding from opposite ends of the paleovalley. The final stage of fjord fill was completed by tidal sandflats and braided-river deposits. The latter was due to isostatic rebound in the hinterland. Renewed transgression resulted in a return to marine conditions in the succeeding Nyborg Forma- tion, which spilled out of the paleovalley onto the surrounding areas. B. Gudveig Baarli, Rebekah Levine & Markes E. Johnson, Department of Geosciences, Williams College, 947 Main Street, Williamstown, MA 01267, USA, E-mail:
[email protected]. Introduction without glaciation. Laajoki (2001, 2002, 2004) provide additional support for the glacial theory, although he A common feature of the contemporary post-Pleisto- also recognizes local deposits of mass-flow origin.