Nearby springs and brooks do not always supply the water needed for life. This example from Wimmis presents the way groundwater.
Nearby springs and brooks do not always supply the water needed for life. In the Jura mountains this problem was solved by collecting roof drainage and storing it in an underground reservoir such as the cistern (112). In the Valais, water from glacial brooks was led via kilometre-long canals (Suonen, bisses) to villages and pastures, sometimes over precarious structures on the walls of cliffs. The Midlands faced similar problems but found other solutions.
Each region solved its problems within the bounds of nature. This example from Wimmis presents a further way – groundwater! In this case in the 19th century a well shaft was sunk. A round hole was dug and walled with stone. Today the water level is at a depth of five meters, but ground water wells were often ten or more meters deep.
This wellhouse is a constructively simple building: a timber frame stands on dressed stone. Boards are nailed on and a shingled roof protects the well from wind, weather and contamination. Instead of having to pull up a heavy water bucket, a wooden pump lightens the work.
The wellhouse stood to the east of Wimmis on the Pintelmatte meadow and supplied water for the livestock in the neighbouring stall. The Pintel is a hill with a limestone underbase and therefore has limited reserves of water. Nevertheless, water was able to rise from the depths toward the surface. The water level in the wellshaft was originally seven metres down. The wellhouse was in service until 1980.
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