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What is another word for anticlinal?

Pronunciation: [ˌantɪklˈɪnə͡l] (IPA)

Anticlinal is a geologic term used to describe a fold in rock layers that slopes downward on both sides from a central crest. There are several synonyms for the word anticlinal, including arched, uplifted, folded, domed, and peaked. The word arched implies a smooth, curved shape, while uplifted suggests a rise in elevation. Folded and domed both suggest the bending or curving of rock layers, while peaked refers to the pointed or cone-like shape of an anticlinal fold. Regardless of the synonym used, the term refers to a geological formation that commonly plays an essential role in the formation of oil and gas reserves.
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Synonyms for Anticlinal:

What are the hypernyms for Anticlinal?

A hypernym is a word with a broad meaning that encompasses more specific words called hyponyms.

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What are the opposite words for anticlinal?

Antonyms for the word "anticlinal" are "synclinal" and "periclinal". Synclinal refers to rock formations where the strata dips inward, towards the center. This is often the opposite of anticlinal formations, where the strata dips outward. Periclinal, on the other hand, refers to planes that run parallel to the outer surface of a developing tissue or organ. It is also considered an antonym for anticlinal due to its perpendicular orientation. These terms are often used in geology and botany to describe the different aspects of strata and plant growth. By understanding these antonyms, researchers can gain a better understanding of the structures and phenomena they are studying.

What are the antonyms for Anticlinal?

Usage examples for Anticlinal

The ridge trended north-west, as most others did in this extensive basin; and this direction being nearly parallel to that of the coast ranges further northward, seemed to afford additional reason for expecting to find anticlinal and synclinal lines, and, consequently, rivers, much in the same direction.
"Journal of an Expedition into the Interior of Tropical Australia In Search of a Route from Sydney to the Gulf of Carpentaria (1848) by Lt. Col. Sir Thomas Livingstone Mitchell Kt. D.C.L. (1792-1855) Surveyor-General of New South Wales"
Thomas Mitchell
When we reflect upon the fact that all the inclined strata which crop out at the surface of the ground are but the truncated portions of beds that were once continuous, and formed complete anticlinal arches or curves, we must be impressed with the degree of denudation, or wearing-away, which the solid strata have experienced.
"Geology"
James Geikie
anticlinal and Synclinal Curves.
"The Student's Elements of Geology"
Sir Charles Lyell

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