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gradpoint: anticlines
The most common of these are anticlines and synclines; anticlines are the "crests", while synclines are the "troughs".
yes
anticlines and synclines
The stress that causes strike-slip faults is produced by a shearing force and so is called shear stress.
If a rock undergoes horizontal stress, Anticlines and Synclines will form.
its the circulation of the rock and when it pushes together
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 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.