During Quaternary glacial periods, the Šumava / Bayerischer Wald mountains were subject to mountain glaciations. Recent studies have focussed mainly on the several well-developed cirques. However, the glacial geomorphology of the mountain range as a whole has not yet been mapped from digital data. Here we use high-resolution digital elevation models to identify over 300 erosional and 40 depositional landforms of glacial origin. Our study provides a map of glacial geomorphology for the whole mountain range across the Czech Republic, Germany, and Austria, with an up-to-date overview of previously investigated sites and newly identified glacial features in areas that have not previously been surveyed. The results of our mapping study can further be validated by field surveys and will serve as a basis for future reconstructions of palaeoglaciation in the Šumava / Bayerischer Wald mountains.

在第四纪冰河时期，Šumava/ Bayerischer Wald山脉遭受了山间冰川的影响。最近的研究主要集中在几个发达的马戏团。但是，整个山脉的冰川地貌尚未从数字数据中绘制出来。在这里，我们使用高分辨率的数字高程模型来识别300多个冰川起源的侵蚀地貌和40个沉积地貌。我们的研究提供了整个捷克共和国，德国和奥地利的整个山脉的冰川地貌图，并提供了以前调查过的地点的最新概况以及以前未调查过的地区的新发现的冰川特征。