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...

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

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...

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 Eskdale Anticline is a dip-slip fault at Whitby in North Yorkshire, England. The anticline was thought to have stretched for approximately 20 kilometres...

a few meters from the Franco-Spanish border. It is an example of an anticline, a convex fold of strata, the centre of which is occupied by the oldest...

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

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...

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