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Radolfzeller Aach
The Radolfzeller Aach (also known as Hegauer Aach) is a right or north tributary of the Rhine in the south of Baden-Württemberg (Germany).
It is approximately 32 km long.
== Course ==
The source of the river is the ''Aachtopf'' in Aach, the largest spring in Germany, at a height of 475 m above sea level. The water emerges from a karst cave. About two thirds of the water originates in the headwaters of the Danube. Between Immendingen and Möhringen an der Donau and in Fridingen, water from the Danube disappears underground (this is known as the ''Danube Sinkhole''); this water reappears in the Aachtopf.
The river first flows through a number of nature reserves in the Hegau area. This segment of the river is known as ''Hegauer Aach''. It then flows South to Singen, where it is known as ''Radolfzeller Aach''. The last six kilometers of the lower course flow through a nature reserve called ''Radolfzeller Aach Ried''. It flows into the northwestern part of Lake Untersee (the ''Zellersee'') between Radolfzell and Moos. At the mouth, the average discharge is 10 m3/s, making it the fourth largest contributor to Lake Constance.
抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』
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