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Roof pendant pinnacles.
The roof pendants occur as isolated pieces of the surrounding rock within the intrusive mass.
In structural geology a roof pendant which also known as a pendant is a mass of country rock that projects downward into and is entirely surrounded by an igneous intrusion such as a batholith or other pluton in lay terminology sometimes rock hat is used.
Consist of thin roof pendants or remnants occurring sporadically over the denuded batholith.
A roof pendant is an erosional remnant that was created by the removal by erosion of the overlying country rock that formed the roof of.
The crystalline limestone is slightly more resistant.
The intrusions that most commonly contain roof pendants are relatively shallow stocks or batholiths.