MONOCLINE Meaning and
Definition
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A monocline refers to a geological structure characterized by a single, steeply inclined flexure or fold in otherwise relatively horizontal rock layers or strata. This type of fold typically occurs on a large scale and displays a distinct change in the dip or slope of the affected rocks. Monoclines commonly form as a result of tectonic forces, such as crustal compression or extension, which cause the rocks to buckle or bend.
In a monocline, a gently dipping limb of rock strata is displaced by a steeper, inclined limb. The relatively flat-lying strata on one side of the fold are referred to as the "dip slope," while the side with the steeper incline is known as the "scarp" or "cliff face." The change in slope between these two limbs is typically abrupt and can be quite pronounced.
Monoclines are often found in regions with extensive geological deformation, such as mountainous areas or basins that have undergone significant tectonic activity. They can be several kilometers in length and may reveal layers of different rock types or periods of deposition. Monoclines play a crucial role in understanding the geological history and dynamics of an area, as they provide insights into the forces and processes that have shaped the Earth's crust over time.
Common Misspellings for MONOCLINE
Etymology of MONOCLINE
The word "monocline" is derived from the Greek words "mono" meaning "single" and "klinein" meaning "to lean". In geology, a monocline refers to a fold in rock layers where the strata slopes in one direction and remains relatively horizontal in the other direction. The name "monocline" was coined in the 19th century to describe this specific geological feature based on its appearance of a single continuous slope or lean.
Similar spelling words for MONOCLINE
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