A Syncline is where lays of rock bend downwards and then curve up.
An Anticline is the opposite: layers of rock bend upwards and then down.
Syncline.
An anticline. This is a geological feature where the layers of rock are bent upward in an arch shape, forming a convex structure.
the three main types of folds are anticlines, synclines, and monoclines.
A downward fold in a rock is called a syncline. It is a type of fold in which the rock layers are bent downward in a trough-like shape.
The two most common types of linear folds are syncline (downward fold) and anticline (upward fold). These fold structures are formed as a result of compressional forces acting on rock layers, causing them to deform and bend.
Syncline.
...known as syncline
An anticline. This is a geological feature where the layers of rock are bent upward in an arch shape, forming a convex structure.
the three main types of folds are anticlines, synclines, and monoclines.
An anticline is a type of fold where the layers of rock bend downwards to form an inverted U shape. This fold represents an upward convex fold in rock layers and is characterized by older rocks in the center and younger rocks on the sides.
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A fold in geology is a bend in rock layers caused by tectonic forces. The two main types of folds are anticlines (upward-arched rock layers) and synclines (downward-arching rock layers).
A fold
Fold
A downward fold in a rock is called a syncline. It is a type of fold in which the rock layers are bent downward in a trough-like shape.
A syncline is comprised of downward folding layers of rock.
This geological formation is called a syncline. It is a downward fold in the rock layers where the youngest layers are in the center and the oldest are on the outside.