EPICLINAL Meaning and
Definition
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Epiclinal is an adjective that is used to describe geological features or processes that occur along or across the slope of a rock stratum or the bending or contortion of rock layers. The term is derived from the combination of two words, "epicline" and "line". An epicline refers to a fold in stratified rock that occurs parallel to the dip or inclination of the rock layers. The suffix "-al" is added to form the adjective epiclinal.
In geological terms, epiclinal features or processes commonly occur due to various tectonic forces, such as folding, faulting, or displacement of rock layers. These forces can cause the layers of rocks to bend, curve, or slope along the pre-existing inclination of the stratified rocks. Epiclinal structures can range from subtle folds to more pronounced contortions, depending on the intensity of the tectonic forces at play.
The term epiclinal is often used in the fields of structural geology, sedimentology, and geophysics to describe and analyze the deformation and geological history of rock formations. Understanding the epiclinal nature of the rocks can help geologists decipher the complex geological processes that have shaped the Earth's crust over millions of years.
Overall, epiclinal refers to the specific conditions and features found within rocks where the layers exhibit bending, contortion, or inclination parallel to the original slope of the strata.
Common Misspellings for EPICLINAL
- wpiclinal
- spiclinal
- dpiclinal
- rpiclinal
- 4piclinal
- 3piclinal
- eoiclinal
- eliclinal
- e-iclinal
- e0iclinal
- epuclinal
- epjclinal
- epkclinal
- epoclinal
- ep9clinal
- ep8clinal
- epixlinal
- epivlinal
- epiflinal
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