Jump to content

Red Verona marble

From Wikipedia, the free encyclopedia

This is an old revision of this page, as edited by 2600:387:5:803::ba (talk) at 18:48, 16 November 2019. The present address (URL) is a permanent link to this revision, which may differ significantly from the current revision.

[[File:Bergamo Basilica Santa Maria Maggiore Protiro di Giovanni De Campione.jpg|thumb|240px|Column-bearing lions in Red Verona Marble. Santa Maria Maggiore, Bergamo.]] Red Verona Marble is a variety of limestone rock which takes its name from Verona in Northern Italy.

It includes internal skeletons of ammonites and belemnoidea rostra in a fecal pellets matrix. It has been quarried from Red Ammonitic facies of Verona or the sedimentary Scaglia Rossa, both in the Lessinia geographical area of the northern Veneto Prealps.

References

  • Korus, Jesse T., ed. (Sep 2014). Geologic Field Trips Along the Boundary Between the Central Lowlands and Great Plains: 2014 Meeting of the Gsa North-Central Section (Field Guide). Geological Society of America. p. 47. ISBN 978-0813700366. Retrieved 26 April 2015.