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gptkbp:instance_of
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gptkb:region
|
|
gptkbp:affects
|
the propagation of seismic waves
|
|
gptkbp:can_detect
|
seismic reflection methods
|
|
gptkbp:discovered_by
|
gptkb:Andrija_Mohorovičić
|
|
gptkbp:feature
|
the Earth's lithosphere
|
|
gptkbp:has_a_focus_on
|
geological mapping
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|
https://www.w3.org/2000/01/rdf-schema#label
|
Mohorovičić discontinuity
|
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gptkbp:is_a_boundary_that_influences
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gptkb:volcanic_activity
|
|
gptkbp:is_a_boundary_that_marks
|
the transition from crust to mantle
|
|
gptkbp:is_associated_with
|
the transition from solid to semi-solid material
|
|
gptkbp:is_characterized_by
|
a change in seismic wave velocity
|
|
gptkbp:is_critical_for
|
geological surveys
|
|
gptkbp:is_divided_into
|
Earth's mantle
Earth's crust
|
|
gptkbp:is_essential_for
|
understanding Earth's internal structure
|
|
gptkbp:is_found_beneath
|
oceanic and continental crusts
|
|
gptkbp:is_involved_in
|
the study of earthquakes
|
|
gptkbp:is_located_at
|
approximately 5 to 70 kilometers below the Earth's surface
|
|
gptkbp:is_related_to
|
the Earth's thermal structure
|
|
gptkbp:is_relevant_to
|
mineral exploration
|
|
gptkbp:is_significant_for
|
plate tectonics
|
|
gptkbp:is_studied_in
|
geophysics
earth sciences
|
|
gptkbp:key_feature
|
seismology
|
|
gptkbp:known_as
|
Moho
|
|
gptkbp:named_after
|
a Croatian seismologist
|
|
gptkbp:was_identified_in
|
1909
|
|
gptkbp:bfsParent
|
gptkb:Andrija_Mohorovičić
|
|
gptkbp:bfsLayer
|
6
|