(c) Rachaimer stylolites
lime of Oxford
Ortenberg / Deilingen
collection georolf
stylolites formed by chemical dissolution of the solid limestone by pressure solution. The clay residue solution forms a thin membrane that separates the rock in peg-like structures. Vertikalstylolithen interlocking layers together. In the bevel of the cross section through the jagged stylolites show strong, almost fractal lines, known for its similarity to the cranial sutures (sutures) as Drucksuturen. Beautiful to see this often in the "Jura marble from the one window sills made. G EORG W AGNER has described the formation of the stylolites beautiful.
Literature:
W AGNER , G.: Introduction to Earth and Landscape History 2 with particular reference to southwestern Germany
Ed Öhringen 1950
M URAWSKI , H.: Geology Dictionary
6th erg and ext. Ed Enke Stuttgart 1972
Literature:
W AGNER , G.: Introduction to Earth and Landscape History 2 with particular reference to southwestern Germany
Ed Öhringen 1950
M URAWSKI , H.: Geology Dictionary
6th erg and ext. Ed Enke Stuttgart 1972
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