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  2. Asthenosphere - Wikipedia

    en.wikipedia.org/wiki/Asthenosphere

    The asthenosphere (from Ancient Greek ἀσθενός (asthenós) 'without strength') is the mechanically weak [1] and ductile region of the upper mantle of Earth. It lies below the lithosphere , at a depth between ~80 and 200 km (50 and 120 mi) below the surface, and extends as deep as 700 km (430 mi).

  3. Lithosphere–asthenosphere boundary - Wikipedia

    en.wikipedia.org/wiki/Lithosphere–asthenosphere...

    The lithosphere–asthenosphere boundary (referred to as the LAB by geophysicists) represents a mechanical difference between layers in Earth's inner structure. Earth's inner structure can be described both chemically (crust, mantle, and core) and mechanically. The lithosphere–asthenosphere boundary lies between Earth's cooler, rigid ...

  4. Convergent boundary - Wikipedia

    en.wikipedia.org/wiki/Convergent_boundary

    Convergent boundary. A convergent boundary (also known as a destructive boundary) is an area on Earth where two or more lithospheric plates collide. One plate eventually slides beneath the other, a process known as subduction. The subduction zone can be defined by a plane where many earthquakes occur, called the Wadati–Benioff zone. [1]

  5. Mohorovičić discontinuity - Wikipedia

    en.wikipedia.org/wiki/Mohorovičić_discontinuity

    The Mohorovičić discontinuity (/ ˌmoʊhəˈroʊvɪtʃɪtʃ / MOH-hə-ROH-vih-chitch; Croatian: [moxorôʋiːtʃitɕ]) [1] – usually called the Moho discontinuity, Moho boundary, or just Moho – is the boundary between the crust and the mantle of Earth. It is defined by the distinct change in velocity of seismic waves as they pass through ...

  6. CityVille Space Needle: Everything you need to know - AOL

    www.aol.com/2012/07/14/cityville-space-needle

    Rather than looking like the real world Space Needle, this structure is unique in appearance containing bright colors and lots of CityVille Space Needle: Everything you need to know Skip to main ...

  7. Core–mantle boundary - Wikipedia

    en.wikipedia.org/wiki/Core–mantle_boundary

    The core–mantle boundary (CMB) of Earth lies between the planet's silicate mantle and its liquid iron–nickel outer core, at a depth of 2,891 km (1,796 mi) below Earth's surface. The boundary is observed via the discontinuity in seismic wave velocities at that depth due to the differences between the acoustic impedances of the solid mantle ...

  8. Plate tectonics - Wikipedia

    en.wikipedia.org/wiki/Plate_tectonics

    t. e. Plate tectonics (from Latin tectonicus, from Ancient Greek τεκτονικός (tektonikós) 'pertaining to building') [1] is the scientific theory that Earth 's lithosphere comprises a number of large tectonic plates, which have been slowly moving since 3–4 billion years ago. [2][3][4] The model builds on the concept of continental ...

  9. File:Aerial photo of Space Needle under construction, 1961.jpg

    en.wikipedia.org/wiki/File:Aerial_photo_of_Space...

    English: Aerial photo of Space Needle under construction, 1961, in preparation for the Century 11 Exposition (1962 Seattle World's Fair). Item 167461 , Engineering Department Photographic Negatives (Record Series 2613-07), Seattle Municipal Archives .

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