Research Article| February 01, 2002 Weathering rinds and rock coatings from an Arctic alpine environment, northern Scandinavia John C. Dixon; John C. Dixon 1Department of Geosciences, University of Arkansas, Fayetteville, Arkansas 72701, USA Search for other works by this author on: GSW Google Scholar Colin E. Thorn; Colin E. Thorn 2Department of Geography, University of Illinois, Urbana, Illinois 61801, USA Search for other works by this author on: GSW Google Scholar Robert G. Darmody; Robert G. Darmody 3Department of Natural Resources and Environmental Sciences, University of Illinois, Urbana, Illinois 61801, USA Search for other works by this author on: GSW Google Scholar Sean W. Campbell Sean W. Campbell 4Department of Geosciences, University of Arkansas, Fayetteville, Arkansas 72701, USA Search for other works by this author on: GSW Google Scholar Author and Article Information John C. Dixon 1Department of Geosciences, University of Arkansas, Fayetteville, Arkansas 72701, USA Colin E. Thorn 2Department of Geography, University of Illinois, Urbana, Illinois 61801, USA Robert G. Darmody 3Department of Natural Resources and Environmental Sciences, University of Illinois, Urbana, Illinois 61801, USA Sean W. Campbell 4Department of Geosciences, University of Arkansas, Fayetteville, Arkansas 72701, USA Publisher: Geological Society of America Received: 13 Jun 2000 Revision Received: 11 Sep 2001 Accepted: 19 Sep 2001 First Online: 01 Jun 2017 Online ISSN: 1943-2674 Print ISSN: 0016-7606 Geological Society of America GSA Bulletin (2002) 114 (2): 226–238. https://doi.org/10.1130/0016-7606(2002)114<0226:WRARCF>2.0.CO;2 Article history Received: 13 Jun 2000 Revision Received: 11 Sep 2001 Accepted: 19 Sep 2001 First Online: 01 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation John C. Dixon, Colin E. Thorn, Robert G. Darmody, Sean W. Campbell; Weathering rinds and rock coatings from an Arctic alpine environment, northern Scandinavia. GSA Bulletin 2002;; 114 (2): 226–238. doi: https://doi.org/10.1130/0016-7606(2002)114<0226:WRARCF>2.0.CO;2 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGSA Bulletin Search Advanced Search Abstract Coarse rock debris exposed in the subaerial environment of northern Sweden displays the development of a wide variety of surface coatings. These include weathering rinds as well as a great diversity of geochemical coatings, including those dominated by Ca, Fe, Si, and Al. Each of these types of rock coatings displays a high degree of geochemical complexity. The weathering rinds exhibit both geochemical and morphologic changes to the parent rock cores, including extensive dissolution, oxidation, and hydration as well as disaggregation, fracturing, and cementation by secondary geochemical coatings. Chemical breakdown of the rock to form weathering rinds includes loss of K, Si, Mg, and Ca and buildup of Fe. Weathering rinds are fundamentally the result of dissolution, as no clay minerals were identified in the rinds. Rock coatings are distinguished from rinds by their clear accretionary nature. Despite the distinction made between weathering rinds and rock coatings, it is important to note that often the two are intimately related. The presence of rock coatings as well as weathering rinds on rock surfaces amplifies the important role played by geochemical processes in the Arctic alpine climate of northern Sweden in particular, as well as its significance in landscape evolution in such environments in general. You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
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