A syncline is the opposite of an anticline. It is a downward fold or "dip" in underground strata. The anticline is the upward fold in a layer of strata. If you can picture a layer of subterranean strata that goes "across" in a straight or flat line, then comes to a plunging U-shaped dip, then you've got the syncline pictured. The opposite for the anticline. Sometimes we see the two together, as in side by side. Use the link below to see a drawing and get more information. The picture alone is worth the "click" to get to the Wikipedia post.
syncline: Saou in Europe
anticline: Nittany valley in Pennsylvania
anticline
Syncline
In an anticline, the fold is at the top, called the crest. The syncline, in contrast, is the trough of the "wave."
An upward (U-shaped) fold is called a syncline. a downward (n-shaped) fold is called an anticline. The way I always remember it is that a SYNCline SINKs in the middle.
If the downfold is the syncline, then the upfold is the anticline i think.
Everest is an anticline
monocline syncline anticline well they mostly have a cline at the end funny right?
anticline
A syncline is a fold with younger layers closer to the center of the structure whereas an anticline has older layers closer to the center. A syncline vaguely resembles a smile(you would smile if you were committing a sin[syn]) and an anticline is the opposite, vaguely like an "A"
An anticline
anticline and syncline
Syncline
An Anticline is the upward or top part of folded rock It is the opposite of a syncline.
The two types of folding that come about as a result of earth movement: syncline and anticline. Syncline folds are down-curving, layers of earth bent downwards, pushing the folds of earth around it upwards. The upwards folds are the anticline folds. ^ <- Anticline v <-Syncline
Syncline. However unless you know which way up the rocks are the correct term to use should be Antiform (not anticline) and Syform (not syncline).
Anticline, Syncline, Monocline.
In an anticline, the fold is at the top, called the crest. The syncline, in contrast, is the trough of the "wave."