Jump to content

Asthenosphere

Frae Wikipedia, the free beuk o knawledge
Yird cutaway frae core tae crust, the asthenosphere lyin atween the upper mantle an the lithospheric mantle (detail nae tae scale)

The asthenosphere (frae Greek asthenēs 'weak' + sphere) is the heichly viscous, mechanically waik[1] an ductilely-defurmin region o the upper mantle o the Yird. It lies belaw the lithosphere, at depths atween ~80 an ~200 km (~ 50 an 124 mile) ablo the surface. The lithosphere-asthenosphere boondary is uisually referred tae as LAB. Asthenosphere is generally solit altho some its regions coud be meltit (e.g. belaw mid-ocean ridge). The lawer boondary o the asthenophere is nae well defined. The thickness o the asthenosphere depends mainly on the temperatur. For some regions asthenosphere coud extend as deep as 700 km (430 mi). It is considered the soorce region o mid-ocean ridge basalt (MORB).[2]

References

[eedit | eedit soorce]
  1. Barrel, J. The strength of the crust, Part VI. Relations of isostatic movements to a sphere of weakness - the astenosphere. J. Geol. 22, 655-683, 1914.
  2. Hofmann, A.W., 1997. Mantle geochemistry: the message from oceanic volcanism. Nature 385, 219-228.
pFad - Phonifier reborn

Pfad - The Proxy pFad of © 2024 Garber Painting. All rights reserved.

Note: This service is not intended for secure transactions such as banking, social media, email, or purchasing. Use at your own risk. We assume no liability whatsoever for broken pages.


Alternative Proxies:

Alternative Proxy

pFad Proxy

pFad v3 Proxy

pFad v4 Proxy