The Leptepu fjord is part of a 68 km (42 mi) longitudinal structural fault that runs from north to south, profoundly remodelled through the passing of the continental glaciers during the glaciations of the Quaternary period. The ice field that slid through the fiord, trapped between high mountains, carved the valleys deeply - they have subsequently been partially refilled with sediment, resulting in a remaining depth of up to 500 m below current sea level. In numerous places there is evidence of the glacio-isostatic structures that survived the postglacial eustatic advances during the last 15,000 years. More information...
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