PERICLINIA Meaning and
Definition
-
Periclinia is a term commonly used in geology and structural geology to describe a specific type of geological fold or deformation. It refers to a group of rocks that have undergone deformation by a process known as "fold bending". This process occurs when rocks are subjected to intense pressure and are forced to bend or fold.
The term "periclinia" specifically refers to a type of fold that has a distinct cylindrical or tubular shape, with the axis of the fold nearly vertical. This type of fold often occurs in areas of high tectonic activity, such as mountain ranges or along plate boundaries.
Periclinia can vary in size and shape, ranging from small-scale, localized folds to larger, regional-scale structures. They are often characterized by the presence of distinct layers or bands of rock that have been deformed and folded into the cylindrical shape.
The presence of periclinia can provide valuable information about the geological history and tectonic processes that have shaped an area. By studying the orientation and distribution of these folds, geologists can gain insights into the forces and pressures that have acted upon the rocks, as well as the direction and magnitude of the stresses involved.
In summary, periclinia are cylindrical or tubular folds in rocks that form due to intense pressure and tectonic forces. They are important structures in understanding the deformation and geological history of an area.
Common Misspellings for PERICLINIA
Infographic
Add the infographic to your website:
