Rock fragments with dark coatings in slope deposits of the Famenne region, southern Belgium

Quaternary slope deposits near the Lesse river in the Famenne region, south Belgium, contain scattered rounded rock fragments (5-15 cm diameter) that are typically characterized by a dark coating or patina. This dark surface resembles rock varnish occurrences. To establish the nature of the coatings...

Full description

Bibliographic Details
Main Authors: Dirk Goossens, Florias Mees, Eric Van Ranst, Pieter Tack, Laszlo Vincze, Jean Poesen
Format: Article
Language:English
Published: Société Royale Belge de Géographie and the Belgian National Committee of Geography 2015-12-01
Series:Belgeo
Subjects:
Online Access:http://journals.openedition.org/belgeo/17625
id doaj-c0bccb0bdcc44b87a8e14c320c5a5f08
record_format Article
spelling doaj-c0bccb0bdcc44b87a8e14c320c5a5f082021-04-02T13:51:28ZengSociété Royale Belge de Géographie and the Belgian National Committee of GeographyBelgeo1377-23682294-91352015-12-01410.4000/belgeo.17625Rock fragments with dark coatings in slope deposits of the Famenne region, southern BelgiumDirk GoossensFlorias MeesEric Van RanstPieter TackLaszlo VinczeJean PoesenQuaternary slope deposits near the Lesse river in the Famenne region, south Belgium, contain scattered rounded rock fragments (5-15 cm diameter) that are typically characterized by a dark coating or patina. This dark surface resembles rock varnish occurrences. To establish the nature of the coatings, chemical, mineralogical and petrographical analyses were performed. The coatings are essentially Fe/Mn oxide features, developed as surface deposits on the rock fragments with associated impregnation of the rock substrate. The Fe/Mn compounds are amorphous or at least poorly crystalline. The coating also shows enrichment in clay minerals compared to the matrix of the covered rock fragments. Some of these characteristics are typical for rock varnish, but the coating does not show a layered structure. We hypothesize that the coating was formed by precipitation of Mn and Fe supplied by water, after burial of the rock fragments in the surrounding slope deposits, and was not affected by atmospheric deposition. Despite its strong macroscopic resemblance to rock varnish the patina on the Famenne rocks must most likely be classified as a heavy-metal skin.http://journals.openedition.org/belgeo/17625rock coatingvarnishslope depositsFamenne
collection DOAJ
language English
format Article
sources DOAJ
author Dirk Goossens
Florias Mees
Eric Van Ranst
Pieter Tack
Laszlo Vincze
Jean Poesen
spellingShingle Dirk Goossens
Florias Mees
Eric Van Ranst
Pieter Tack
Laszlo Vincze
Jean Poesen
Rock fragments with dark coatings in slope deposits of the Famenne region, southern Belgium
Belgeo
rock coating
varnish
slope deposits
Famenne
author_facet Dirk Goossens
Florias Mees
Eric Van Ranst
Pieter Tack
Laszlo Vincze
Jean Poesen
author_sort Dirk Goossens
title Rock fragments with dark coatings in slope deposits of the Famenne region, southern Belgium
title_short Rock fragments with dark coatings in slope deposits of the Famenne region, southern Belgium
title_full Rock fragments with dark coatings in slope deposits of the Famenne region, southern Belgium
title_fullStr Rock fragments with dark coatings in slope deposits of the Famenne region, southern Belgium
title_full_unstemmed Rock fragments with dark coatings in slope deposits of the Famenne region, southern Belgium
title_sort rock fragments with dark coatings in slope deposits of the famenne region, southern belgium
publisher Société Royale Belge de Géographie and the Belgian National Committee of Geography
series Belgeo
issn 1377-2368
2294-9135
publishDate 2015-12-01
description Quaternary slope deposits near the Lesse river in the Famenne region, south Belgium, contain scattered rounded rock fragments (5-15 cm diameter) that are typically characterized by a dark coating or patina. This dark surface resembles rock varnish occurrences. To establish the nature of the coatings, chemical, mineralogical and petrographical analyses were performed. The coatings are essentially Fe/Mn oxide features, developed as surface deposits on the rock fragments with associated impregnation of the rock substrate. The Fe/Mn compounds are amorphous or at least poorly crystalline. The coating also shows enrichment in clay minerals compared to the matrix of the covered rock fragments. Some of these characteristics are typical for rock varnish, but the coating does not show a layered structure. We hypothesize that the coating was formed by precipitation of Mn and Fe supplied by water, after burial of the rock fragments in the surrounding slope deposits, and was not affected by atmospheric deposition. Despite its strong macroscopic resemblance to rock varnish the patina on the Famenne rocks must most likely be classified as a heavy-metal skin.
topic rock coating
varnish
slope deposits
Famenne
url http://journals.openedition.org/belgeo/17625
work_keys_str_mv AT dirkgoossens rockfragmentswithdarkcoatingsinslopedepositsofthefamenneregionsouthernbelgium
AT floriasmees rockfragmentswithdarkcoatingsinslopedepositsofthefamenneregionsouthernbelgium
AT ericvanranst rockfragmentswithdarkcoatingsinslopedepositsofthefamenneregionsouthernbelgium
AT pietertack rockfragmentswithdarkcoatingsinslopedepositsofthefamenneregionsouthernbelgium
AT laszlovincze rockfragmentswithdarkcoatingsinslopedepositsofthefamenneregionsouthernbelgium
AT jeanpoesen rockfragmentswithdarkcoatingsinslopedepositsofthefamenneregionsouthernbelgium
_version_ 1721563754846486528