IPA: /ˈaɪsəˌklaɪn/
KK: /ˈaɪsəˌklaɪn/
A geological term referring to a type of fold in rock layers where the two sides are almost parallel due to tight folding, resembling an anticline or syncline.
The geologist explained how the isocline formed during the mountain-building process.
Isocline → It is formed from "iso-" (meaning equal) and "cline" (from Greek "klinein", meaning to lean or slope). The word describes a line on a map connecting points of equal value, such as temperature or pressure, indicating equality in a gradient.
Think of 'equal' ('iso-') slopes or lines ('cline') that connect points of the same value.