The Rhine Glacier was a glacier during the last glacial period and was responsible for the formation of the Lake Constance.[1]
| Rhine Glacier | |
|---|---|
 Reconstruction of the front of the Rhine glacier near Sigmaringen showing blockage the Danube course during the Riss glaciation. | |
  Rhine Glacier | |
| Location | Bavaria top |
| Coordinates | 48°05′12″N 9°12′59″E / 48.08667°N 9.21639°E |
| Status | melted |
 | |
References
edit- ^ Shirley, Martha Lou (1966). Deltas in Their Geologic Framework. Houston, Texas: Houston Geological Society. p. 109. ASIN B000BWESNW. OCLC 491277.
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