In structural geology , a
syncline is a fold with younger layers closer to the center of the structure. is a large
syncline with
Kaynak: SynclineThe Tetapaga
Syncline, also known as the Lake Tetapaga
Syncline, is a northeasterly trending
syncline in Northeastern Ontario , Canada ,
Kaynak: Tetapaga SynclineAnticlines are often flanked by
syncline s although faulting can complicate and obscure the relationship between the two. Folds often
Kaynak: AnticlineSyncline , in structural geology, a
syncline is a fold, with younger layers closer to the center of the structure. Synclinal, in alkane
Kaynak: Synclinal Pericline also refers to a doubly plunging anticline or
syncline . Pericline is a form of albite exhibiting elongate prismatic crystal.
Kaynak: Periclinedescribes the rocks of the English county of Hertfordshire which are a northern part of the great shallow
syncline known as the London Basin .
Kaynak: Geology of HertfordshireMore specifically, it is a typically lens-shaped pluton that occupies either the crest of an anticline or the trough of a
syncline .
Kaynak: PhacolithCoal-bearing strata are to be found across three
syncline s; the Donnington, Madeley and Coalport
synclines whilst the majority of the
Kaynak: Coalbrookdale CoalfieldThe largest
syncline in the basin, the Watchung
syncline, contains the greater portion of the Watchung flood basalts as they appear today
Kaynak: Watchung MountainsSome elongated structural basins are also known as
syncline s. Structural basins may also be sedimentary basin s, which are aggregations
Kaynak: Structural basinIt lies in the geological
syncline which also forms the Solent . This gives it a fairly constant and gentle gradient. Historical events
Kaynak: River Sommea core area of great ecological significance - the forests of the lowland karst
syncline - gazetted as the Pororari Ecological Area in 1979.
Kaynak: Paparoa National Park