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Table: Naab - Regen

Deep groundwater layer Naab - Regen

Measurement site	County	Aquifer	Date	Groundwater level [m above sealevel]	Distance to surface [m]
WACKERSDORF 1KT	SAD	Burg- und Blasensandstein (Sandsteinkeuper)	02.04.2024 09:43	382.56	36.39
Tiefpegel Mooslohstraße		Muschelkalk	15.04.2024 08:30	396.18	6.40
GRAIN	SAD	Burg- und Blasensandstein (Sandsteinkeuper)	25.03.2024 13:40	360.78	12.34
HIRSCHAU/WALDMÜHLE AM-S-1	AS	Buntsandstein	09.04.2024 08:39	400.41	10.18
PENESLOHE AM-KMS-2	AS	Burg- und Blasensandstein (Sandsteinkeuper)	09.04.2024 08:58	439.83	10.73
GROSSALBERSHOF B1	AS	Burg- und Blasensandstein (Sandsteinkeuper)	09.04.2024 11:15	404.65	22.21
Gressenwöhr	AS	Kreide-Sandsteine	09.04.2024 13:32	399.88	-0.98
Mappach	SAD	Burg- und Blasensandstein (Sandsteinkeuper)	22.04.2024 11:08	370.90	64.94
TAUBENB.FORST B 937	AS	Weißer Jura / Malmkarst	02.04.2024 10:26	400.83	22.50
PFAFFENREUTH K1		Burg- und Blasensandstein (Sandsteinkeuper)	15.04.2024 13:05	472.07	25.96
GREUT/KIRCHENL. TB 994	BT	Benker Sandstein (Gipskeuper)	23.04.2024 10:00	458.35	-5.07

Explanations

Deep layer of groundwater

Measurement stations in the deep layer are supplied by infiltrating water from above lying aquifers. Fluctation of the waterlevel is damped and regeneration of the groundwater needs longer periods of time.

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