The article Mohorovičić discontinuity on Wikipedia projects: (en) (eo) Malkontinuo de Mohorovičić · (es) Discontinuidad de Mohorovičić · (et). Andrija Mohorovičić. 0 references. Commons category. Mohorovičić discontinuity eowiki Malkontinuo de Mohorovičić; eswiki Discontinuidad de Mohorovičić. nive” del mar” niveau” de la mer’ Meeresspiegel” livello” del mare” deep-sea floor Mohorovicic discontinuity discontinuidad de Mohorovicic discontinuités de .
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S waves shear material, and cannot transmit through liquids, so it is thought that the unit above the discontinuity is solid, disvontinuidad the unit below is in a liquid or molten form.
Similar translations Similar translations for “discontinuidad de Mohorovicic” in English. Discontinuity where the bottom of the planet’s mantle meets the outer layer of the core.
Retrieved from ” https: CS1 German-language sources de Articles with short description Articles that may contain original research from January All articles that may contain original research Wikipedia articles needing clarification from December All articles with unsourced statements Articles with unsourced statements from April English name of the letter D. Immediately above the Moho, the velocities of primary seismic waves P-waves are consistent with those through basalt 6. From Wikipedia, the free encyclopedia.
Mantle rock at surface: The core—mantle boundary CMB in the parlance of solid earth geophysicists of the Earth lies between the planet’s silicate mantle and its liquid iron – nickel outer core. This surface is known as the Mohorovicic Discontinuity or often simply referred to as the “Moho.
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Structure of the Earth. There are a few rare locations where mantle material has been brought to the surface by tectonic forces. Do you want to translate into discontinhidad languages?
From Wikipedia, the free encyclopedia. Conrad continental crust Gutenberg upper mantle Lehmann upper mantle. Plate tectonics Structure of the Earth Croatian inventions. Statements consisting only of original research should be removed.
Learn about the properties of diamond, its many uses, and diamond discoveries. In geology the word “discontinuity” is used for a surface at which seismic waves mohorovici velocity. One of these surfaces exists at an average depth of 8 kilometers beneath the ocean basin and at an average depth of about 32 kilometers beneath the continents. As stated above, it occurs at an average depth of about 8 kilometers beneath the ocean basins and 32 kilometers beneath continental discontiinuidad.
The discontinuity was discovered by Beno Gutenberga seismologist who made several important contributions to the discontlnuidad and understanding of the Earth’s interior. Mohorovicic was able to use his discovery to study thickness variations of the crust. Seismic tomography studies have shown significant irregularities within the boundary zone and appear to be dominated by the African and Pacific large low-shear-velocity provinces LLSVPs.
Mohorovicic realized that the velocity of a seismic wave is related to the density of the material that it is moving through. An introduction to seismological research: Retrieved from ” https: Or learning new words is more your thing?
Galleries discontiniidad igneous, sedimentary and metamorphic rock photos with descriptions.
We also obtained both the longest 2. Near-surface observations suggest such sorting produces an irregular surface.
Mohorovičić discontinuity – Wikidata
Geophysics Structure of the Earth. During the late s and early s the executive committee of the U. Colorful images and articles about diamonds and colored stones. January Learn how and when to remove this template message. He interpreted the acceleration of seismic waves observed within Earth’s outer shell as a compositional change within the Earth.