File:Rendzina flachgruendig Heufeld Schwaebische-Alb.jpg

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Deutsch: Rendzina auf der Ebene des „Heufeldes“, ein typischer, weit verbreiteter, Boden, Mittlere Schwäbische Alb. Diese Ebene ist die größte, zusammenhängende Fläche der vor dem Albtrauf liegenden, so genannten Schichtflächenalb (Weißer Jura beta, bereits bis auf die Wohlgeschichte Kalk-Formation, ox2, abgetragen). Die Rendzina ist ein sehr flachgründiger, zu Trockenheit neigender Boden. Unter dürftigem, 10-15 cm stark humosem Feinboden folgt bereits der nahezu unverwitterte Kalkstein. Der Boden ist durch Erosion aus einem erdgeschichtlich viel früher entwickeltem, tieferen Profil hervorgegangen. Verbreitet treten auch Rendzinen mit 20-30 cm Oberboden auf. Auch das ist immer noch flachgründig. Unter Wald zeigen sich Übergänge zur Braunerde.

English: Rendzina, extremely thin topsoil on the plain „Heufeld”, middleSwabian Alb. The plain Heufeld is completely cultivated by villagers of Ringingen (community of Burladingen). The plain, next to the northern cuesta, is the largest closed area of the so called “Schichtflächenalb”, the second lowest of 8 layers of the upper lithostratigraphic unit of the South German Jurassic, (ox2). Rendzina is a humous, fine soil, with only little decarbonization, tending to drought, which developed very slowly by a mere 10-20 cm in tenthousand years. Soil on woods tends to become Brown Earth.
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Author K. Rilling
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(Reusing this file)		 explicit permission by E-Mail as of May 3th, 2016

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