What is an Upridge?

Upridge is a term used in geology and mining to describe a type of fault or structural feature where a layer of rock is pushed upwards along a linear structure, such as a fault line.

In an upridge, the upper layer of rock is displaced upwards relative to the lower layer, creating a step-like structure. This can occur due to tectonic forces that cause the rocks to stretch and thin, resulting in the formation of a ridge or plateau.

Upridges are often found in areas where there has been significant tectonic activity, such as along fault lines or at the boundaries between tectonic plates. They can also be formed by other geological processes, such as folding or faulting.

In mining, upridges can be important features to identify and map, as they can indicate the presence of valuable mineral deposits. For example, gold and copper deposits are often found in areas where there has been significant tectonic activity, such as along fault lines and upridges.