摘要 : Between the years 1970 and 1975 the Eggestedt gravel pit in the vicinity of the hanseatic city of Bremen in Northern Germany has been very popular for collecting geschiebes (erratic boulders) from the gravels and sands of the Elst... 展开 Between the years 1970 and 1975 the Eggestedt gravel pit in the vicinity of the hanseatic city of Bremen in Northern Germany has been very popular for collecting geschiebes (erratic boulders) from the gravels and sands of the Elster glaciation. Sedimentary boulders as well as fossils, including baltic amber, and various magmatic and metamorphic geschiebes did occur. It is followed HOFLE (1976) in interpreting the Eggestedt gravel ridge as a kames deposit of the Elsterian stage. 收起