This report covers the mapping of the springs in the area of Sparafeld and Reichenstein, i.e. catchment areas Flitzengraben to Kalblinggatterl to Mödlinger Hütte and Kirchengraben as well as Treffnergraben between Mödlinger Hütte and Donner.
80 sources were located by GPS and examined with regard to water type, temperature and conductivity. The individual mapping areas are described in terms of location and geomorphology.
Except for a few pictures, the springs originate from partly very unstable steep trenches of the permoskythian limestone alpine base and from the metamorphic paleozoic of the greywaken zone. The mapped mountain waters are predominantly at 1,000 to 1.450 m above sea level and have consistently small quantities. Due to the diverse geology, a wide range of mineralisation can be found. Due to the diverse geology, a wide range of mineralisation can be found.
80 sources were located by GPS and examined with regard to water type, temperature and conductivity. The individual mapping areas are described in terms of location and geomorphology.
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