English (United Kingdom)

https://curated-unify.zendy.io/wp-json/zendy-region/v1/featured_content/oa?rat=en

https://curated-unify.zendy.io/wp-json/zendy-region/v1/highlighted_journal/

Global: Zendy Plus annual

Presents the access of premium content as premium feature

Premium Content

Presents the keyphrase highlighting as premium feature

Keyphrase Highlighting

Presents the summarisation as premium feature

Summarisation

Insights

Presents the pdf analysis as premium feature

PDF Analysis

Presents the zaia usage as premium feature

ZAIA

Global: Zendy Tools annual

Global: Zendy Free Plan

Global: Zendy Tools monthly

Global: Zendy Plus monthly

The Upper Pleistocene Wurm Glaciation Recessional Stadesof the Alpine foreland glaciers of the Rhine area, and the firstAlpine boundary complex of the Late Pleistocene. In the Rhine area of the Wurm glaciation, the recessionalStades can be morphologically subdivided by means of glacial boundary complexes. The Würm-Stem-on-the-Rhinecomplex is evidence for an upper Wurm readvance of theforeland glaciers after an intensive melting period (± 16 000y BP?). The first Late Pleistocene readvance of the localnorthern Alpine glaciers appears as the Würm-Weissbadcomplex (± 14 000 y BP?), while in the main network of theglaciation no reaction is recognizable. In the Upper Pleistocene of the Wurm, the equilibrium line of the Rhine glacierwas at an elevation of 1000 m. The first readvance of localglaciers in the Late Pleistocene took place at an elevation ofabout 1500 m

Die hochwürmzeitlichen Rückzugsphasen des Rhein-Vorlandgletschers und der erste alpine Eisrandkomplex im Spätglazial