Anticlines form an 'A' shape in rocks. They are folds where the apex points up, toward the sky. Generally, they fold where the oldest rocks form the core of the fold.
Anticlines and Synclines typically form during crustal deformation as the result of compression that accompanies orogenic mountain building.
The large anticlines form the fold mountain and the dome mountains. This is usually as a result of jointing, folding and faulting.
dome con
compression
anticlines and synclines
Syncline
Anticlines and Synclines typically form during crustal deformation as the result of compression that accompanies orogenic mountain building.
gradpoint: anticlines
The large anticlines form the fold mountain and the dome mountains. This is usually as a result of jointing, folding and faulting.
The most common of these are anticlines and synclines; anticlines are the "crests", while synclines are the "troughs".
dome con
compression
yes
yes
anticlines, synclines, and monoclines
anticlines and synclines
gradpoint: anticlines