File:Rosso Verona Marble (Rosso Ammonitico Formation, Upper Jurassic; Verona Province, Venetia Region, Italy) (14802172801).jpg

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"Rosso Verona Marble" from the Jurassic of Italy.

In the commercial decorative stone trade, “marble” is used to refer to a wide variety of relatively soft rocks (H = 3 to 5) that will take a fine polish. These include true marbles and rocks that aren’t marbles, such as limestones, tectonic breccias, and serpentinites. True limestones are calcitic biogenic and ~chemical sedimentary rocks.

Rosso Verona Marble (a.k.a. “Red Verona Marble”) is a Jurassic-aged, hematitic, stylolitized, nodular limestone from Verona Province in northern Italy. The lighter-colored areas (nodules) have been attributed to soft-sediment deformation (Pivko, 2003). Some samples have fossil ammonite shells (Mollusca, Cephalopoda, Ammonoidea, Ammonitida). This limestone represents part of a condensed succession of sediments deposited on an ancient submarine plateau, the Trento Plateau.

Stratigraphy & Age: Rosso Ammonitico Superiore Member, Rosso Ammonitico Formation, Oxfordian Stage, lower Upper Jurassic.

Locality: commercial quarry near Caprino Veronese or Cerro Veronese or Erbezzo or Sant’Ambrogio di Valpolicella, Verona Province, western Veneto Region (Venetia Region), southern Alps, northern Italy
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Source Rosso Verona Marble (Rosso Ammonitico Formation, Upper Jurassic; Verona Province, Venetia Region, Italy)
Author James St. John

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This file is licensed under the Creative Commons Attribution 2.0 Generic license.
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This image was originally posted to Flickr by James St. John at https://flickr.com/photos/47445767@N05/14802172801 (archive). It was reviewed on 6 December 2019 by FlickreviewR 2 and was confirmed to be licensed under the terms of the cc-by-2.0.

6 December 2019

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Date/TimeThumbnailDimensionsUserComment
current03:55, 6 December 2019Thumbnail for version as of 03:55, 6 December 20192,330 × 2,261 (2.53 MB)Ser Amantio di Nicolao (talk | contribs)Transferred from Flickr via #flickr2commons

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