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 (4)

Label Occurrences
Gutenberg discontinuity canonical 2
Earth’s outer core 1
Lehmann discontinuity 1

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 Lehmann discontinuity ⓘ
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 (5)

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 → Mohorovičić discontinuity ⓘ
linked to: Gutenberg discontinuity
Gutenberg discontinuity → isDistinctFrom → Lehmann discontinuity ⓘ
linked to: Gutenberg discontinuity
Earth’s magnetic field → generatedBy → Earth’s outer core ⓘ
linked to: Gutenberg discontinuity