Rhine Glacier
48°05′12″N 9°12′59″E / 48.08667°N 9.21639°E / 48.08667; 9.21639Status melted 
The Rhine Glacier was a glacier during the last glacial period and was responsible for the formation of the Lake Constance.[1]
References
- ^ Shirley, Martha Lou (1966). Deltas in Their Geologic Framework. Houston, Texas: Houston Geological Society. p. 109. ASIN B000BWESNW. OCLC 491277.
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