The gross morphology of the Precambrian basement of southern Sweden is analysed. The area has a domed form and emerges from under a cover of Palaeozoic rocks in the north and east and Mesozoic rocks in the south and west. It is studied with the aid of the distribution of small‑ and medium‑scale bedrock forms, remnants of ancient weathering crusts and cover rocks, and of topographic profiles. A map of erosion surfaces has been constructed for the southern part of the area. Exhumed sub‑Cambrian, sub-Jurassic and sub-Cretaceous inclined surfaces are cut by more horizontal surfaces at different levels, viz. at about 50 m, 90–125 m, the South Småland Peneplain with two slightly different levels at 125–165 m and 165–185 in, 200–230 in, and about...
The Parkajoki area in northeastern Sweden is situated near the central area of Fennoscandian glaciat...
International audienceTectonics and erosion are the driving forces in the evolution of mountain belt...
In low relief Precambrian gneiss terrain in eastern Sweden, abraded bedrock surfaces were ripped apa...
The relationships between different denudation surfaces/peneplains formed across crystalline basemen...
The degree of inheritance of the present topography from past geological events in the Småland-Bleki...
Abstract: The relation between Scandinavian landforms and Cenozoic uplift events is examined by anal...
The aim of this studv is to investigate interrelationships betweenbedrock relief and geological mate...
A laterally extensive and conspicuously smooth erosional surface is exposed near the Wenlock-Ludlow ...
Abstract: Basin modelling and compaction studies based on sonic data from the Mesozoic succession i ...
This paper deals with erosional forms, especially those caused by running water, in the central Sout...
Based on geological maps from the Geological Survey of Sweden, data (Berggrund 1:1 million). Backgro...
In Sweden, Jurassic strata are restricted to Skåne and adjacent offshore areas. Jurassic sedimentary...
Sedimentological analysis of the Early Jurassic Höör Sandstone in Central Scania, Sweden shows that ...
This is a study of the influence of the crystalline basement faults of the Polotsk-Kurzeme and the S...
none11siIn-situ weathered bedrock, saprolite, is locally found in Scandinavia, where it is commonly ...
The Parkajoki area in northeastern Sweden is situated near the central area of Fennoscandian glaciat...
International audienceTectonics and erosion are the driving forces in the evolution of mountain belt...
In low relief Precambrian gneiss terrain in eastern Sweden, abraded bedrock surfaces were ripped apa...
The relationships between different denudation surfaces/peneplains formed across crystalline basemen...
The degree of inheritance of the present topography from past geological events in the Småland-Bleki...
Abstract: The relation between Scandinavian landforms and Cenozoic uplift events is examined by anal...
The aim of this studv is to investigate interrelationships betweenbedrock relief and geological mate...
A laterally extensive and conspicuously smooth erosional surface is exposed near the Wenlock-Ludlow ...
Abstract: Basin modelling and compaction studies based on sonic data from the Mesozoic succession i ...
This paper deals with erosional forms, especially those caused by running water, in the central Sout...
Based on geological maps from the Geological Survey of Sweden, data (Berggrund 1:1 million). Backgro...
In Sweden, Jurassic strata are restricted to Skåne and adjacent offshore areas. Jurassic sedimentary...
Sedimentological analysis of the Early Jurassic Höör Sandstone in Central Scania, Sweden shows that ...
This is a study of the influence of the crystalline basement faults of the Polotsk-Kurzeme and the S...
none11siIn-situ weathered bedrock, saprolite, is locally found in Scandinavia, where it is commonly ...
The Parkajoki area in northeastern Sweden is situated near the central area of Fennoscandian glaciat...
International audienceTectonics and erosion are the driving forces in the evolution of mountain belt...
In low relief Precambrian gneiss terrain in eastern Sweden, abraded bedrock surfaces were ripped apa...