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Richat Structure
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{{Short description|Circular geological feature in the Sahara desert}} {{Infobox landform | water = | name = Richat Structure | other_name = ''Tagense''<ref name="Richard-Molard1952a" /> | type = [[Dome (geology)|Dome]] | photo = Richat Structure ISS030-E-12516.jpg | photo_width = 250px | photo_alt = | photo_caption = Image from the [[International Space Station]], 17 December 2011 | map = Mauritania#Africa | map_width = | map_caption =Location within [[Mauritania]]##Location within [[Africa]] | map_alt = | relief = yes | label = | label_position = | mark = | marker_size = | location = [[Adrar Plateau]] of the [[Sahara]] | grid_ref = | coordinates ={{coord|21.114700|-11.394300|format=dms|region:MR_type:landmark_dim:50000|display=inline,title}} | coordinates_ref = | range = | part_of =[[Adrar Region]], Mauritania | water_bodies = | elevation_ft = <!-- or |elevation_m = --> | elevation_ref = | surface_elevation_ft = <!-- or |surface_elevation_m = --> | surface_elevation_ref = | highest_point = | highest_elevation = | highest_coords = | length = | width = | area = <!-- {{Convert|NN|ha|acres}} --> | depth = | drop = | formed_by = | geology = <!-- or |type = --> | age = | orogeny = | topo = | operator = | designation = | free_label_1 = | free_data_1 = | free_label_2 = | free_data_2 = | website = <!-- {{URL|example.com}} --> | embed = | native_name = {{native name|ar|قلب الريشات|parensize=90%}} }} {{Use dmy dates|date=January 2023}} The '''Richat Structure''', or '''''Guelb er Richât''''' ({{langx|ar|قلب الريشات|Qalb ar-Rīšāt}}, {{IPA|mey|galb er.riːʃaːt|lang|LL-Q56231 (mey)-Tidjani Saleh-گلب الريشات.wav}}), is a prominent circular geological feature in the [[Adrar Plateau]] of the [[Sahara]]. It is located near [[Ouadane]] in the [[Adrar Region]] of [[Mauritania]]. In [[Hassaniya Arabic]], ''rīšāt'' means ''feathers'' and it is also known locally in Arabic as ''tagense'', referring to the circular opening of the leather pouch that is used to draw water from local wells.<ref name="Richard-Molard1952a">{{Cite journal |last=Richard-Molard |first=J. |year=1952 |title=The Pseudo-boutonniers of Richat |journal=Gouvernement Général de l'Afrique Occidentale Française Bulletin de la Direction des Mines |volume=15 |issue=2 |pages=391–401}}</ref> It is an eroded [[Dome (geology)|geological dome]], {{convert|40|km|mi}} in diameter, caused by a subsurface [[igneous intrusion]] deforming the overlying [[sedimentary rock]] layers, causing the rock to be exposed as concentric rings with the oldest layers exposed at the centre of the structure. [[Igneous rock]] is exposed inside and there are [[rhyolite]]s and [[gabbro]]s that have undergone [[hydrothermal alteration]], and a central [[Breccia|megabreccia]]. The structure is also the location of exceptional accumulations of [[Acheulean]] [[Paleolithic]] stone tools. It was selected as one of the 100 geological heritage sites identified by the [[International Union of Geological Sciences]] (IUGS) to be of the highest scientific value.<ref name="IUGS2022a">{{Cite web |title=The First 100 IUGS Geological Heritage Sites |url=https://iugs-geoheritage.org/videos-pdfs/iugs_first_100_book_v2.pdf |access-date=3 November 2022 |website=IUGS International Commission on Geoheritage |publisher=IUGS}}</ref>
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