anticline
Quick Summary
An anticline is an arch of stratified rock where layers bend downward in opposite directions from the crest. This geological formation is essentially an upfold of strata, appearing as an inverted V-shape on geologic maps. Anticlines are a type of fold, which are undulations or waves in the Earth's crustal rocks that were originally deposited horizontally.123
These structures are significant in geology, particularly in the formation of structural traps for petroleum and natural gas. Approximately 80 percent of the world's petroleum has been discovered in anticlinal traps, which are formed by tectonic events like folding.2
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mountainAlpine- (or Himalayan-)type belts…into linear, regularly spaced folds—alternating anticlines and synclines—and thrust on top of one another. The Valley and Ridge province of Pennsylvania, which was formed during the collision of Africa and North America near the end of Paleozoic time (about 240,000,000 years ago), is a classic example.
Read More…into linear, regularly spaced folds—alternating anticlines and synclines—and thrust on top of one another. The Valley and Ridge province of Pennsylvania, which was formed during the collision of Africa and North America near the end of Paleozoic time (about 240,000,000 years ago), is a classic example.
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PamirsGeology of Pamirs…the whole represents a huge anticline, or series of stratified arches. The central zone of the Pamirs contains limestone, sandstone, and shale rocks of the Jurassic, Triassic, and Permian periods (about 300 to 145 million years ago) and also red-coloured rocks of the Early Cretaceous Period (145 to 100 million…
Read More…the whole represents a huge anticline, or series of stratified arches. The central zone of the Pamirs contains limestone, sandstone, and shale rocks of the Jurassic, Triassic, and Permian periods (about 300 to 145 million years ago) and also red-coloured rocks of the Early Cretaceous Period (145 to 100 million…
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Rocky MountainsPhysiographyThe granitic core of the anticlinal mountains often has been upfaulted, and many ranges are flanked by Paleozoic sedimentary rocks (e.g., shales, siltstones, and sandstones) that have been eroded into hogback ridges. This same mountain-building process is occurring today in the Andes Mountains of South America. Most mountain building in…
Read MoreThe granitic core of the anticlinal mountains often has been upfaulted, and many ranges are flanked by Paleozoic sedimentary rocks (e.g., shales, siltstones, and sandstones) that have been eroded into hogback ridges. This same mountain-building process is occurring today in the Andes Mountains of South America. Most mountain building in…
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