Mohorovičić discontinuity

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World map showing the depth of the Moho.

The Mohorovičić discontinuity (Croatian pronunciation: [moxoroʋitʃitɕ]), 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.[1]

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.[2]

Nature[edit]

Earth cross-section showing location of the Mohorovičić discontinuity (labelled as 2)
Two paths of a P-wave, one direct and one refracted as it crosses the Moho.[1]
Ordovician ophiolite in Gros Morne National Park, Newfoundland. This rock which formed the Ordovician Moho is exposed on the surface.

Immediately above the Moho, the velocities of primary seismic waves (P-waves) are synonymous with those through basalt (6.7–7.2 km/s), and below they are similar to that of peridotitic or dunitic (7.6–8.6 km/s).[3] That suggests the Moho marks a change of composition, but the interface appears to be too even for any believable sorting mechanism within the Earth. Near-surface observations suggest such sorting produces an irregular surface.[4]

Exploration[edit]

During the late 1950s and early 1960s the executive committee of the U.S. National Science Foundation funded drilling a hole through the ocean floor to reach this boundary. However the operation, named Project Mohole, never received sufficient support and was mismanaged[citation needed]; the United States Congress canceled it in 1967. Soviet scientists at the Kola Institute pursued the goal simultaneously; after 15 years they reached a depth of 12,260 metres (40,220 ft), the world's deepest hole, before abandoning their attempt in 1989.[5]

Reaching the discontinuity remains an important scientific objective. A more recent[when?] proposal considers a rock-melting radionuclide-powered capsule with a heavy tungsten needle that can propel itself down to the Moho discontinuity and explore Earth's interior near it and in the upper mantle.[6] The Japanese project Chikyu Hakken ("Earth Discovery") also aims to explore this general area with the drilling ship, Chikyū, built for the Integrated Ocean Drilling Program (IODP).

See also[edit]

Notes[edit]

  1. ^ a b Andrew McLeish (1992). Geological science (2nd ed.). Thomas Nelson & Sons. p. 122. ISBN 0-17-448221-3. 
  2. ^ James Stewart Monroe, Reed Wicander (2008). The changing Earth: exploring geology and evolution (5th ed.). Cengage Learning. p. 216. ISBN 0-495-55480-4. 
  3. ^ RB Cathcart & MM Ćirković (2006). Viorel Badescu, Richard Brook Cathcart, Roelof D. Schuiling, ed. Macro-engineering: a challenge for the future. Springer. p. 169. ISBN 1-4020-3739-2. 
  4. ^ Benjamin Franklin Howell (1990). An introduction to seismological research: history and development. Cambridge University Press. p. 77 ff. ISBN 0-521-38571-7. 
  5. ^ "How the Soviets Drilled the Deepest Hole in the World". [[Wired (magazine)|]]. 2008-08-25. Retrieved 2008-08-26. 
  6. ^ Ozhovan, M.; F. Gibb, P. Poluektov and E. Emets (August 2005). "Probing of the Interior Layers of the Earth with Self-Sinking Capsules". Atomic Energy 99 (2): 556–562. doi:10.1007/s10512-005-0246-y. 

References[edit]

External links[edit]