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- Q194259 subject Q2945759.
- Q194259 subject Q7215285.
- Q194259 abstract "The Mohorovičić discontinuity (Croatian pronunciation: [moxorôʋiːt͡ʃit͡ɕ]), usually referred to as the Moho, is the boundary between the Earth's crust and the mantle. Named after the pioneering Croatian seismologist Andrija Mohorovičić, the Moho separates both the oceanic crust and continental crust from underlying mantle. The Moho lies almost entirely within the lithosphere; only beneath mid-ocean ridges does it define the lithosphere–asthenosphere boundary. The Mohorovičić discontinuity was first identified in 1909 by Mohorovičić, when he observed that seismograms from shallow-focus earthquakes had two sets of P-waves and S-waves, one that followed a direct path near the Earth's surface and the other refracted by a high-velocity medium.The Mohorovičić discontinuity is 5 to 10 kilometres (3–6 mi) below the ocean floor, and 20 to 90 kilometres (10–60 mi), with an average of 35 kilometres (22 mi), beneath typical continents.".
- Q194259 thumbnail Mohomap.png?width=300.
- Q194259 wikiPageExternalLink default.cfm.
- Q194259 wikiPageExternalLink 050407_earth_drill.html.
- Q194259 wikiPageExternalLink mohole.
- Q194259 wikiPageExternalLink index.php?option=com_content&view=article&id=292&Itemid=225&lang=pl.
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- Q194259 wikiPageWikiLink Q2945759.
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- Q194259 wikiPageWikiLink Q7215285.
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- Q194259 wikiPageWikiLink Q83371.
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- Q194259 comment "The Mohorovičić discontinuity (Croatian pronunciation: [moxorôʋiːt͡ʃit͡ɕ]), usually referred to as the Moho, is the boundary between the Earth's crust and the mantle. Named after the pioneering Croatian seismologist Andrija Mohorovičić, the Moho separates both the oceanic crust and continental crust from underlying mantle. The Moho lies almost entirely within the lithosphere; only beneath mid-ocean ridges does it define the lithosphere–asthenosphere boundary.".
- Q194259 label "Mohorovičić discontinuity".
- Q194259 depiction Mohomap.png.