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What is another word for Monoclinal?

Pronunciation: [mˈɒnə͡ʊklˌɪnə͡l] (IPA)

Monoclinal is a term used in geology to describe a fold where the strata are inclined in only one direction. It is often used interchangeably with the term monocline. However, there are other synonyms that can be used for this term, including simple fold, steep dip, and flexure. These synonyms describe a particular geological formation where a layer of rock has been tilted or folded, often due to tectonic activity. Being familiar with these synonyms can help geologists and other researchers identify and describe geological formations accurately, advancing our understanding of the earth's history and the processes that have shaped it.
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Synonyms for Monoclinal:

What are the hypernyms for Monoclinal?

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

  • Other hypernyms:

    geology, geological structure, geological feature.

What are the opposite words for Monoclinal?

Monoclinal is a term used in geology to describe rocks that slope in one direction. The antonyms for this word would be "cumulative," "sinuate," "undulating," "zigzag," "serpentine," or "hilly." Cumulative refers to the gradual accumulation of material, while sinuate and undulating both suggest a series of smooth curves or waves. Zigzag and serpentine both describe rocks that change direction frequently, while hilly indicates a terrain with multiple hills and dips. These antonyms provide a variety of descriptive words that convey a different type of geological formation compared to those that are monoclinal.

What are the antonyms for Monoclinal?

Usage examples for Monoclinal

On the east it descends four thousand feet by a Monoclinal fold, which passes into a fault towards the north.
"The Elements of Geology"
William Harmon Norton
But that the trough is a true valley of fracture is proved by the fact that on either side it is bounded by fault scarps and Monoclinal folds.
"The Elements of Geology"
William Harmon Norton
The intercanyon valleys of this portion of the Grand Canyon extend back from three to seven miles west of the river, and are eroded in the crest of the Monoclinal fold that forms the eastern margin of the Kaibab Plateau.
"The-Grand-Canyon-of-Arizona-how-to-see-it"
James, George Wharton

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