The crystalline limestone is slightly more resistant.
Roof pendant pinnacles.
The intrusions that most commonly contain roof pendants are relatively shallow stocks or batholiths.
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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.
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.
Outcrops are seldom more than a few hundred feet long and thicknesses of more than 20 feet are unusual.
Consist of thin roof pendants or remnants occurring sporadically over the denuded batholith.