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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.
A syncline fold is concave downward, meaning the youngest rock layers are found in the center of the fold and the oldest rock layers are found on the outer edges of the fold.
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.
Syncline.
The youngest rock layers are in the center of a syncline fold. This is because syncline folds form when rock layers are bent downward in the middle and upward on the sides, causing the youngest layers to be in the center.
...known as syncline
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).
Synclines are downward-folding rock layers in which the youngest rocks are in the center of the fold. They are part of the larger geological structure known as a fold, where layers of rock are bent in response to stress in the Earth's crust. Synclines often form in association with anticlines, which are upward-folding rock layers.
Layers of rock that bend can produce a downward fold known as a syncline. This type of fold typically has the youngest rocks in the center surrounded by older rocks on either side. Synclines are common features in folded mountain ranges.
A syncline is a downward curving fold in a rock formation, where the strata dip toward the center of the structure. An anticline is an upwardly curving fold, with the strata rise upward toward the center of the structure.
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.