They are exposed by erosion of the overlying rock.
Roof pendants are.
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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.
Definition of roof pendant.
Mcgraw hill dictionary of scientific technical terms 6e copyright 2003 by the mcgraw hill companies inc.
Roof pendants can be read more.
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A dictionary of earth sciences.
Answer to question 16 1 pts roof pendants are characteristic of metamorphism which occurs at metamorphic grade.
The roof pendants occur as isolated pieces of the surrounding rock within the intrusive mass.
A downward projection or sag of the roof of a batholith.
The photo below shows the cretaceous granite below light colored rock and the dark colored sedimentary now metamorphic rock above.
Bateman a roof pendant is a mass of metamorphic rock that is entirely surrounded by plutonic rock and presumed to be a downward projection of rocks that overlaid the plutonic rocks before erosion in this report an overview of the roof pendants within the sierra nevada range is given.
If this downward protruding mass of roof rock still has a connection to the main surrounding mass of country rock they are known by structural geologists as either septa or screens.
The presence of roof pendants indicates that the igneous body is being observed near its upper surface.
These older rocks that are intruded by the granite are called roof pendants because they show the roof of the batholith.
In lay terminology sometimes rock hat is used.
Rüf pen dənt geology downward projection or sag into an igneous intrusion of the country rock of the roof.
Roof pendant downward extension of the surrounding rock that protrudes into the upper surface of an igneous intrusive body.
The removal of roof rocks by erosion may leave remnants of roof pendants which resemble xenoliths in the intruding rock.
Defined by paul c.
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 igneous intrusion that encloses it.
The intrusions that most commonly contain roof pendants are relatively shallow stocks or batholiths.
Also known as pendant.