Gutenberg discontinuity

E377370

The Gutenberg discontinuity is the seismic boundary within the Earth that marks the transition between the solid mantle and the liquid outer core.

All labels observed (3)

How this entity was disambiguated

Statements (32)

Predicate Object
instanceOf geophysical boundary
seismic discontinuity
aboveLayer lower mantle
affects P-wave velocities
S-wave propagation
associatedWith global seismic wave shadow zones
belowLayer outer core
causes disappearance of S-waves in the outer core
characterizedBy sharp change in seismic wave velocities
discoveredUsing seismology
evidenceFor liquid state of Earth's outer core
fieldOfStudy geophysics
seismology
hasApproximateDepthRange 2890 to 2910 kilometers
hasCoordinateSystem measured by depth from Earth's surface
hasPhysicalPropertyChange composition change
density increase
phase change from solid to liquid
identifiedBy analysis of seismic wave travel times
isBoundaryBetween mantle and core
isDistinctFrom Gutenberg discontinuity self-linksurface differs
surface form: Lehmann discontinuity

Gutenberg discontinuity self-linksurface differs
surface form: Mohorovičić discontinuity
isPartOf core–mantle system
locatedAtDepth approximately 2900 kilometers
locatedWithin Earth's interior
marksTransitionBetween liquid outer core
solid mantle
namedAfter Beno Gutenberg
partOf Earth's internal structure
separates Earth's mantle
Earth's outer core
typeOf core–mantle boundary

How these facts were elicited

Referenced by (4)

Full triples — surface form annotated when it differs from this entity's canonical label.

Beno Gutenberg notableWork Gutenberg discontinuity
Beno Gutenberg eponymOf Gutenberg discontinuity
Gutenberg discontinuity isDistinctFrom Gutenberg discontinuity self-linksurface differs
this entity surface form: Mohorovičić discontinuity
Gutenberg discontinuity isDistinctFrom Gutenberg discontinuity self-linksurface differs
this entity surface form: Lehmann discontinuity