Abstract
Abstract
Four medial moraines on three glaciers in Jotunheimen, Norway, are
described. The structure and debris characteristics of the moraines allow
three debris-transport routes to be identified: (1) discrete concentrated
longitudinal septa containing subglacially comminuted debris; (2) diffuse
longitudinal septa containing passively englacially transported debris; and
(3) supraglacially transported spreads containing rock-fall debris entrained
below the firn line. Two of the moraines, occurring down-glacier of
nunataks, are nourished by a combination of (1) and (3). The remaining two
moraines are nourished solely by englacially transported rock-fall debris
(2). Transport routes (1) and (2) represent two distinct types of
longitudinal englacial debris septum. The contribution of debris from more
than one glacial transport path to single medial moraines indicates the
value of a flexible, process-based approach towards moraine classification,
with emphasis on the dynamic links between basin morphology, glacial debris
entrainment, and moraine characteristics.
Publisher
International Glaciological Society
Cited by
19 articles.
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