Kalkstein wird aus den Überresten von Meeresorganismen gebildet.
Das ist an den Kuhtritt-Muscheln („Megalodonten“) zu erkennen, deren dicke Schalen heute noch sichtbar zu Tage treten.
Die ehemaligen Kalkbänke finden sich im Gesäuse in der Buchstein- und Hochtorgruppe.
www.nationalpark-partner.atLimestone is composed of the remains of marine organisms.
This is revealed in the fossilized bivalve molluscs (megalodonts) whose thick shells are clearly visible even today.
In the Gesäuse, ancient limestone banks are found in the Buchstein and the Hochtor Group.
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