Rhine Glacier
48°05′12″N 9°12′59″E / 48.08667°N 9.21639°E / 48.08667; 9.21639Status melted ![Map](https://maps.wikimedia.org/img/osm-intl,10,a,a,270x200.png?lang=en&domain=en.wikipedia.org&title=Rhine_Glacier&revid=1162118497&groups=_c75988bbdd344065b084e98e670e0d3a22326bc9)
![Map](https://maps.wikimedia.org/img/osm-intl,10,a,a,270x200.png?lang=en&domain=en.wikipedia.org&title=Rhine_Glacier&revid=1162118497&groups=_c75988bbdd344065b084e98e670e0d3a22326bc9)
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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