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A fact from Geology of Cyprus appeared on Wikipedia's Main Page in the Did you know column on 24 March 2013 (check views). The text of the entry was as follows:
This article is within the scope of WikiProject Cyprus, a collaborative effort to improve the coverage of Cyprus on Wikipedia. If you would like to participate, please visit the project page, where you can join the discussion and see a list of open tasks.CyprusWikipedia:WikiProject CyprusTemplate:WikiProject CyprusCypriot articles
Talk:Geology of Cyprus is part of WikiProject Geology, an attempt at creating a standardized, informative, comprehensive and easy-to-use geology resource. If you would like to participate, you can choose to edit this article, or visit the project page for more information.GeologyWikipedia:WikiProject GeologyTemplate:WikiProject GeologyGeology articles
Not particularly user-friendly: in "sediments become progressively more shallow marine, is "progressive" a spatial progress, outward from the Troopos Ophiolite, or progressive with geological time? The article does not say that the sediments were laid down before the Kyrenia Terrane (as it's spelled on the map) became stuck to the northern coast. There's no sense of the dynamic history. The terrane's arc shape might be discussed too. --Wetman (talk) 16:24, 24 March 2013 (UTC)[reply]
