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asthenosphere

American  
[as-then-uh-sfeer] / æsˈθɛn əˌsfɪər /

noun

Geology.
  1. the region below the lithosphere, variously estimated as being from fifty to several hundred miles (eighty-five to several hundred kilometers) thick, in which the rock is less rigid than that above and below but rigid enough to transmit transverse seismic waves.


asthenosphere British  
/ əsˈθiːnəˌsfɪə, -ˈθɛn- /

noun

  1. a thin semifluid layer of the earth (100–200 km thick), below the outer rigid lithosphere, forming part of the mantle and thought to be able to flow vertically and horizontally, enabling sections of lithosphere to subside, rise, and undergo lateral movement See also isostasy

"Collins English Dictionary — Complete & Unabridged" 2012 Digital Edition © William Collins Sons & Co. Ltd. 1979, 1986 © HarperCollins Publishers 1998, 2000, 2003, 2005, 2006, 2007, 2009, 2012

asthenosphere Scientific  
/ ăs-thĕnə-sfîr′ /
  1. The upper part of the Earth's mantle, extending from a depth of about 75 km (46.5 mi) to about 200 km (124 mi). The asthenosphere lies beneath the lithosphere and consists of partially molten rock. Seismic waves passing through this layer are significantly slowed. Isostatic adjustments (the depression or uplift of continents by buoyancy) take place in the asthenosphere, and magma is believed to be generated there.

  2. Compare atmosphere hydrosphere lithosphere


Etymology

Origin of asthenosphere

First recorded in 1910–15; from Greek asthen(ḗs) “frail, weak, sickly” + -o- + -sphere; see asthenia

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Example Sentences

Examples are provided to illustrate real-world usage of words in context. Any opinions expressed do not reflect the views of Dictionary.com.

This difference in water content between the two layers constituting the LAB can explain the sharp velocity drops as well as the near constant attenuation observed over a wide frequency range in the asthenosphere.

From Science Daily • Sep. 27, 2023

This layer appears to glide over a weaker region below called the asthenosphere, characterized by high seismic attenuation and low shear wave velocity.

From Science Daily • Sep. 27, 2023

These observations suggest that the oceanic asthenosphere must contain water.

From Science Daily • Sep. 27, 2023

Unlike the lithosphere that consists of multiple plates, the asthenosphere is relatively unbroken.

From Textbooks • Jan. 1, 2017

Rocks in the asthenosphere are under so much pressure that they move in and out of solid form—sometimes they are solid rocks, sometimes liquid magma.

From "Meltdown" by Deirdre Langeland

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