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Linea 1: [[Fasciculus:Gros Morne moho.jpg~~\|right~~\|thumb\|300px\|[[Ophiolites]] Ordovicianus in [[Reservatio Civitatis Gros Morne\|Reservatione Civitatis Gros Morne]], [[Newfoundlandia et Labrador\|Newfoundlandiae]]. Hoc saxum, per Moho conformatum, in superficie exponitur.]]▼ ~~{{Pagina non annexa}}~~ ▲[[Fasciculus:Gros Morne moho.jpg\|right\|thumb\|300px\|[[Ophiolites]] Ordovicianus in [[Reservatio Civitatis Gros Morne\|Reservatione Civitatis Gros Morne]], [[Newfoundlandia et Labrador\|Newfoundlandiae]]. Hoc saxum, per Moho conformatum, in superficie exponitur.]] [[Fasciculus:Slice earth.svg\|thumb\|Littera A discontinuitatem Mohorovicic in promptu ponit.]] '''Discontinuitas Mohorovicic,''' accuratius '''Discontinuitas Mohorovičić,''' vulgo '''Moho,''' est finis qui [[crusta (geologia)\|crustas]] [[Tellus (planeta)\|Telluris]] [[crusta oceanica\|oceanicas]] [[crusta continentalis\|continentalesque]] ab [[amiculum (geologia)\|amiculo]] separat. Discontinuitas circa 5 km sub [[alveus oceani\|alveo oceani]] et fere 30 ad 50 km sub [[crusta continentalis\|continentes]] iacetur; altissumum est sub [[Planities Tibetana\|Planitie Tibetana]], ubi circa 75 km sub superficie demergitur. Moho igitur maximam partem in [[lithosphaera]] iacet; solum quoque<!--modifies "solum," the word that precedes it; whis did you insert it here? (or at all?)--> definit finem inter lithosphaeram et [[asthenosphaera]]m sub [[iugum medium oceanicum]]. Haec discontinuitas primum reperta est anno [[1909]], ab [[Andreas Mohorovicic]], [[seismologo]] [[Croatia]]no, cum auctum abruptum velocitatis undarum [[terraemotu]]um (diserte [[unda P\|undarum P]]) observaret. [[Ophiolites]] sunt sectiones crustae oceanicae et fortasse saxi amiculi quae in crustam continentalem per [[orogenia\|concursūs patellarum]] [[obductio\|obductae]] sunt.<!--PLUS IN EN:-->▼ Discontinuitas circa 5 km sub [[alveus oceani\|alveo oceani]] et fere 30 ad 50 km sub [[crusta continentalis\|continentes]] iacetur; altissumum est sub [[Planities Tibetana\|Planitie Tibetana]], ubi circa 75 km sub superficie demergitur. Moho igitur maximam partem in [[lithosphaera]] iacet; solum quoque<!--modifies "solum," the word that precedes it; whis did you insert it here? (or at all?)--> definit finem inter lithosphaeram et [[asthenosphaera]]m sub [[iugum medium oceanicum]]. == Vide etiam ==▼ ▲Haec discontinuitas primum reperta est anno [[1909]], ab [[Andreas Mohorovicic]], [[seismologo]] [[Croatia]]no, cum auctum abruptum velocitatis undarum [[terraemotu]]um (diserte [[unda P\|undarum P]]) observaret. [[Ophiolites]] sunt sectiones crustae oceanicae et fortasse saxi amiculi quae in crustam continentalem per [[orogenia\|concursūs patellarum]] [[obductio\|obductae]] sunt.<!-- * [[Discontinuitas Gutenberg]]▼ * [[Discontinuitas Lehmann]]▼ * [[Kola Superdeep Borehole]]▼ * [[Zona transitionis fragilis-ductilis]]▼ == Bibliographia ==▼ During the late 1950s and early 1960s, there was a proposal taken up in the executive committee of the [[National Science Foundation]] to drill a hole through the ocean floor to reach this boundary. However the operation, named ''[[Project Mohole]]'', never received sufficient support and the proposal was canceled by [[US Congress]] in 1967. This remains as an important scientific objective, which is being addressed by [[scientific drilling]].{{Fact\|date=July 2008}} Simultaneous efforts were made by the Soviet Union at the [[Kola Superdeep Borehole\|Kola Institute]], who reached a depth of 12,260 meters (40,226 feet) over 15 years - the world's deepest hole to date - before that attempt was also abandoned.<ref>{{cite web \|url=http://www.wired.com/science/discoveries/multimedia/2008/08/gallery_kola_borehole \|title=How the Soviets Drilled the Deepest Hole in the World \|work=Wired \|date=2008-08-25 \|accessdate=2008-08-26}}</ref> * Dixon, Dougal. [[2000]]. ''Beginner's Guide to Geology.'' [[Novum Eboracum (urbs)\|Novi Eboraci]]: Bounty Books. ISBN ~~0-7537-0358-0~~0753703580.▼ * Harris, P. [[1972]]. "The composition of the earth." In ''Understanding the earth: a reader in the earth sciences.'' Ediderunt I. G. Gass et alii. [[Horshamia]]e: Artemis Press for the Open University Press. ISBN ~~0-85141-308-0~~0851413080.▼ * [http://www.glossary.oilfield.slb.com/default.cfm ''Schlumberger Oilfield Glossary,''] ~~inventum 17 Iulii 2008~~www.glossary.oilfield.slb.com▼ == Nexus externi ==▼ A more recent proposal considers a self-descending tungsten capsule heated by radiogenic heat to explore [[Structure of the Earth\|Earth’s interior]] near the Moho discontinuity and in the upper mantle.<ref>{{cite journal \|last=Ozhovan \|first=M. \|coauthors=F. Gibb, P. Poluektov and E. Emets \|year=2005 \|month=August \|title=Probing of the Interior Layers of the Earth with Self-Sinking Capsules \|journal=Atomic Energy \|volume=99 \|issue=2 \|pages=556–562 \|doi=10.1007/s10512-005-0246-y}}</ref> --> * Britt, Robert Roy. ''Hole Drilled to Bottom of Earth's Crust, Breakthrough to Mantle Looms'' http://www.livescience.com/technology/050407_earth_drill.html, inventum 17 Iulii 2008.<!--▼ ▲== Vide etiam == ▲* [[Discontinuitas Gutenberg]] ▲* [[Discontinuitas Lehmann]] ▲* [[Kola Superdeep Borehole]] ▲* [[Zona transitionis fragilis-ductilis]] ▲== Bibliographia == ▲* Dixon, Dougal. [[2000]]. ''Beginner's Guide to Geology.'' [[Novum Eboracum (urbs)\|Novi Eboraci]]: Bounty Books. ISBN 0-7537-0358-0. ▲* Harris, P. [[1972]]. "The composition of the earth." In ''Understanding the earth: a reader in the earth sciences.'' Ediderunt I. G. Gass et alii. [[Horshamia]]e: Artemis Press for the Open University Press. ISBN 0-85141-308-0. ▲* http://www.glossary.oilfield.slb.com/default.cfm ''Schlumberger Oilfield Glossary,'' inventum 17 Iulii 2008. ▲== Nexus externi == ▲* Britt, Robert Roy. ''Hole Drilled to Bottom of Earth's Crust, Breakthrough to Mantle Looms'' http://www.livescience.com/technology/050407_earth_drill.html, inventum 17 Iulii 2008.<!-- {{cite web \|url=http://www.nas.edu/history/mohole/ \|title=Digging a Hole in the Ocean: Project Mohole, 1958-1966 \|accessdate=2008-07-17 \|publisher=[[United States National Academy of Sciences\|National Academy of Sciences]]}} [http://www.igf.fuw.edu.pl/igf/index.php?option=com_content&view=article&id=292&Itemid=225&lang=pl Map of the Moho depth of the European plate] --> [[Categoria:Conformationes litoris et maris]] [[Categoria:Geologia]]

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