cross anticline
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Cross Mountain (Pennsylvania) — Cross Mountain Cross Mountain (note the tower on the summit) Elevation 2,062 ft (628 m) … Wikipedia
Anticline — In structural geology, an anticline is a fold that is convex up and has its oldest beds at its core. The term is not to be confused with antiform , which is a purely descriptive term for any fold that is convex up. Therefore if age relationships… … Wikipedia
Mareuil Anticline — The Mareuil Anticline, also called Mareuil Meyssac Anticline, is a structural high within the sedimentary sequence of the northeastern Aquitaine Basin. The northwest southeast trending anticline was caused by tectonic movements probably starting… … Wikipedia
Coalinga Oil Field — The Coalinga Oil Field in Central California. Other oil fields are shown in gray. The Coalinga Oil Field is a large oil field in western Fresno County, California, in the United States. It surrounds the town of Coalinga, about half way between… … Wikipedia
поперечная антиклиналь — (геол.) [http://slovarionline.ru/anglo russkiy slovar neftegazovoy promyishlennosti/] Тематики нефтегазовая промышленность EN cross anticline … Справочник технического переводчика
Orex Exploration — Inc. Type Public (TSX V: OX) Industry Mining Founded 1987 … Wikipedia
Marcellus Formation — Stratigraphic range: Middle Devonian … Wikipedia
Fold (geology) — For other uses, see Fold (disambiguation). Very tight folds. Formation near Moruya, New South Wales, Australia … Wikipedia
fold — fold1 foldable, adj. /fohld/, v.t. 1. to bend (cloth, paper, etc.) over upon itself. 2. to bring into a compact form by bending and laying parts together (often fol. by up): to fold up a map; to fold one s legs under oneself. 3. to bring (the… … Universalium
List of English back-formations — Back formation refers to either the process of creating a new lexeme (less precisely, a new word ) by removing actual or supposed affixes, or to the neologism formed by such a process. Back formations are shortened words created from longer words … Wikipedia
Weald — The Weald (PronEng|wɪəld) is the name given to a physiographic area in south east England situated between the parallel chalk escarpments of the North and the South Downs. It should be regarded in two separate parts: the sandstone High Weald in… … Wikipedia
