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Definitions and images to illustrate geological terms, links to images and website articles. A syncline is a concave geological fold, with layers that dip downward toward the center of the structure. This arrangement is opposite to that of an arching anticline.
There each mountain-ridge corresponds to an anticline, and each valley to a syncline, or trough-shaped arrangement of strata. Fragments of Earth Lore James Geikie The whole mountain is part of a syncline, the beds dipping into it from the north-west and south-east. Encyclopaedia Britannica, 11th Edition, Volume 5, Slice 3 Various. A downfold, where the strata dip from either side toward the axis of the trough, is called a syncline (Fig. 170). The Elements of Geology William Harmon Norton Hence the anticline noses out to the north and the syncline to the south. Encyclopaedia Britannica, 11th Edition, Volume 10, Slice 5 Various On the north shore of the Island the strata rise slightly on the northern side of the syncline.