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Soils in collu vłal materiał

K    Colluvial Sand.

L    Colluvial Loam.

L4 Colluvial Loam. Gley- or rust phenomena less than 40 cm. deep.

L5 Colluvial Loam. Gley- or rust phenomena less than 40 cm. deep.

M Colluvial Clay.

M4 Colluvial Clay. Gley- or rust phenomena between 40 and 120 cm.

M5 Colluvial Clay. Gley- or rust phenomena less than 40 cm. deep.

Soils in allu vial materiał

N4 Alluvial Sand. Gley- or rust phenomena between 40 and 120 cm.

N5 Alluvial Sand. Gley- or rust phenomena less than 40 cm. deep.

04    Alluvial Loam. Gley- or rust phenomena between 40 and 120 cm.

05    Alluvial Loam. Gley- or rust phenomena less than 40 cm. deep.

P5 Alluvial Clay. Gley- or rust phenomena less than 40 cm. deep.

Plateau soils

AC Clay produced by weathering of Arietenschichten. Shallow soil.

Ad Clay produced by weathering of Arietenschichten. Very shallow soil.

Ae Clay produced by weathering of Arietenschichten. Very shallow soil. Chalk layer less than 40 cm. deep.

JAc Clay produced by weathering of Arietenschichten. Shallow soil. Up to maximal 40 cm. deep, covered with aeolian loam.

1 Ac Clay produced by weathering of Arietenschichten. Shallow soil. Up to maximal 40 cm. deep, covered with colluvial loam.

lAe Clay produced by weathering of Arietenschichten. very shallow soil. Chalk layer less than 40 cm. deep. Up to maximal 40 cm. deep, covered with colluvial loam.

AB Clay produced by weathering of Arietenschichten, between 40 and 120 cm. deep, on sand produced by weathering of Luxemburg sandstone.

Ba Sand produced by weathering of Luxemburg sandstone. Deep soil.

Bb    Sand    produced    by    weathering    of    Luxemburg    sandstone.    Moderately deep soil.

Bc    Sand    produced    by    weathering    of    Luxemburg    sandstone.    Shallow soil.

Bd    Sand    produced    by    weathering    of    Luxemburg    sandstone.    Very shallow    soil.

Bla    Sand    produced    by    weathering    of    Luxemburg    sandstone.    Band rich in    iron.    Deep soil.

Bib Sand produced by weathering of Luxemburg sandstone. Band rich in iron. Moderately deep soil.

Blc Sand produced by weathering of Luxemburg sandstone. Band rich in iron. Shallow soil.

B2b Sand produced by weathering of Luxemburg sandstone. Band rich in iron and clay. Moderately deep soil.

B2c Sand produced by weathering of Luxemburg sandstone. Band rich in iron and clay. Shallow soil.

B3 Sand produced by weathering of Luxemburg sandstone. Bleached eluvial band.

Bqd Sand produced by weathering Of Luxcmb\irg sandstone. Loamy variation. Very shallow soil.

Bs Sand produced by weathering of Luxemburg sandstone. Coarse sandy variation.

jB2 Sand produced by weathering of Luxemburg sandstone. Up to maximal 40 cm. deep, covered with aeolian loam. Band rich in iron and clay.

Slope soils

C Sand produced by weathering of Luxemburg sandstone.

kDq Materiał produced by weathering of Psilonontenschichten. Loamy variation. Up to maximal 40 cm. deep, covered with colluvial sand.

lDr Materiał produced by weathering of Psilonotenschichten. Clayey variation. Up to maximal 40 cm. deep, covered with colluvial loam.

1E Clay produced by weathering of red siatę. Up to maximal 40 cm. deep, covered with colluvial loam.

lFq Materiał produced by weathering of RhSt sandstone. Loamy variation of the Rhat. Up to maximal 40 cm. deep, covered with colluvial loam.

lFr Materiał produced by weathering of black foliated marł. Clayey variatlon of the Rhat. Up to maximal 40 cm. deep, covered with colluvial loam.

Gc    Clay    produced    by    weathering    of stone marł Keuper. Shallow    soil.

Gd    Clay    produced    by    weathering    of stone marł Keuper.    Very    shallow soil.

H    Clay    produced    by    weathering    of red gypsum marł.

I    Sand    produced    by    weathering    of Schilf sandstone.

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