What is another word for flexure?

Pronunciation: [flˈɛkʃʊ͡ə] (IPA)

Flexure is a term often used in engineering to describe a bending or curving movement. When describing flexure in an object, engineers may use synonyms such as bend, curve, twist, contort, or flex. These words can all be used to convey the same idea of a change in shape or position due to an applied force. Additionally, the word flexure may also be replaced with words such as deformation, deflection, or distortion, which all describe the same concept of a change in shape or position. The use of synonyms for flexure allows engineers to find the perfect word to describe a particular aspect of an object's movement or deformation.

Synonyms for Flexure:

What are the paraphrases for Flexure?

Paraphrases are restatements of text or speech using different words and phrasing to convey the same meaning.
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What are the hypernyms for Flexure?

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

What are the opposite words for flexure?

The word "flexure" refers to a bend or curve, but its opposite or antonym can be a straight line. Other antonyms for flexure include stiffness, rigidity, straightness, and inflexibility. These opposite terms describe a situation where an object or structure cannot be easily bent or curved. For example, a metal rod is rigid and cannot be flexed or curved easily, while a rubber band is flexible and can be easily bent or stretched. In engineering and architecture, flexibility and flexure can be desirable for some structures, while others require rigid and inflexible materials for stability and durability.

What are the antonyms for Flexure?

Usage examples for Flexure

Connection of Fracture and flexure of Rocks.
"The Student's Elements of Geology"
Sir Charles Lyell
These rules may often be of great practical utility; for the different degrees of dip occurring in the two cases represented in Figures 66 and 67 may occasionally be encountered in following the same line of flexure at points a few miles distant from each other.
"The Student's Elements of Geology"
Sir Charles Lyell
But it is now admitted that this structure has been owing to movements of the earth's crust of upheaval and subsidence, and that the flexure and inclination of the beds has no connection with the original geographical configuration of the district.
"The Student's Elements of Geology"
Sir Charles Lyell

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