This chapter treats that part of the West Spitsbergen Orogensouth of Isfjorden (Figs 10.1, 10.2, 10.3). It follows the samepattern as the last in treating the stratigraphy of the area,then the structure. Southwestern differs from central westernSpitsbergen in being of greater length, more stratigraphic varietybut less pronounced Cenozoic deformation. This appears to decreasein intensity southwards. There is, moreover, a conspicuous contrastsouth of Isfjorden from a fold belt with many thrusts to.
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