an anticline is a type of fold that is an arch-like shape and has its oldest beds at its core, whereas a syncline is the inverse of an anticline. A typical...

The Oxaya anticline is a large north–south aligned anticline and buckle in the Chilean Andes west of the Altiplano Plateau. The anticline is about 60 km...

A river anticline is a geologic structure that is formed by the focused uplift of rock caused by high erosion rates from large rivers relative to the...

is, lines connecting points of equal dip on adjacent folded surfaces: Anticline: linear, strata normally dip away from the axial center, oldest strata...

The Weald–Artois Anticline, or Wealden Anticline, is a large anticline, a geological structure running between the regions of the Weald in southern England...

The Mareuil Anticline, also called Mareuil-Meyssac Anticline, is a structural high within the sedimentary sequence of the northeastern Aquitaine Basin...

with younger layers closer to the center of the structure, whereas an anticline is the inverse of a syncline. A synclinorium (plural synclinoriums or...

Sheet or block and is the northern limb of the Powell Valley Anticline, a ramp anticline. The ridge exists because hard Lee-type sandstones of Early Pennsylvanian...

The Anticline Ridge is a ridge, southeast of Joaquin Ridge, declining from its 3,629 foot / 1,106 meter high point, Black Mountain in the north at 36°18′16″N...

Rollover anticlines are anticlines related to extensional normal faults. They must be differentiated from fault-propagation folds, which are associated...