Die Steinbrüche im Stadtwald sind ehemalige Steinbrüche im Gebiet der Stadt Fürth. Sie entstanden durch den Abbau von Buntsandstein und sind im gesamten Stadtwald verteilt. Markante Stellen findet man an der Alten Veste, bei der Eschenau, oberhalb Weiherhof, hinter der Stadtförsterei, nördlich des Waldkrankenhauses (Steinbruch Rennbock), nördlich des Waldheims Sonnenland (Steinbruch Katzenstein) sowie oberhalb des Felsenkellers.
Die über das gesamte Gebiet verteilten Sandsteinbüche sind ein eingetragenes Naturdenkmal der Stadt Fürth und vom Bayerischen Landesamt für Umwelt ausgewiesenes Geotop (563A001[1]). In den Stadtwald-Steinbrüchen wurde der Burgsandstein bis ins Mittelalter als wichtiger Baustoff abgebaut. Ein größeres Steinbruchgebiet mit Informationstafel befindet sich in der Nähe des Rangaublicks oberhalb der Waldgaststätte Felsenkeller.
Zusätzlich existierten auch unterirdische Steinbrüche, bei denen der gewünschte Sandstein im Untertagebau gewonnen wurde. Ein noch erhaltener unterirdischer Steinbruch ist der Felsenkeller im Bereich der Waldgaststätte Felsenkeller.
Im Winterrangen mit Kanzel und alter Schmiede
Steinbruch im Winterrangen, ehemalige Feldschmiede
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Am Steinbruckweg
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Am Krummweg
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Steinbruch am Krummweg. Deutlich sichtbare Bearbeitungsspuren
In den Weiherhofer Hängen
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Steinbruch in den Weiherhofer Hängen
Am Trinkwasserhochbehälter
Steinbruch am Trinkwasserhochbehälter nach Rodungsarbeiten im Sommer 2020
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Am ehemaligen Waldkrankenhaus
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Im Katzenstein
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Steinbruch im Katzenstein, sog. Summstein
Am Eschenaubuck
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Literatur
- Hans Werner Kress: Die Sandsteinbrüche des Cadolzburger Höhenzuges vom Dillenberg zur Alten Veste. In: Fürther Heimatblätter, 1993/2, S. 49 - 54
- Hans Werner Kress: Die Sandsteinbrüche des Cadolzburger Höhenzuges vom Dillenberg zur Alten Veste Teil - II(I). In: Fürther Heimatblätter, 1994/4, S. 85 - 110
Siehe auch
Einzelnachweise
Bilder
