1. What is the Asthenosphere? There are many misconceptions about the Asthenosphere

2. Asthenosphere (s) ; Asthenospheres (pl) 1

3. The Asthenosphere lies beneath the lithosphere

4. The lithosphere rides on the Asthenosphere

5. What are synonyms for Asthenosphere?

6. Synonyms for Asthenosphere in Free Thesaurus

7. The lithosphere rides on the Asthenosphere.

8. Asthenospheres meaning Plural form of asthenosphere.

9. The concept of the Asthenosphere came in 1926.

10. Beneath the Asthenosphere is the mesosphere, another strong layer

11. The Asthenosphere is the ductile part of the earth just below the lithosphere, including the upper mantle.The Asthenosphere is about 180 km thick.

12. The asthenosphere corresponds approximately to the low - velocity zone.

13. The asthenosphere is the middle layer and the Centrosphere is the region from the asthenosphere all the way to the center of the earth

14. The differential movement of lithosphere and Asthenosphere causes the …

15. The Asthenosphere is the bottom half of the mantle

16. 3 words related to Asthenosphere: layer, crust, Earth's crust

17. The Asthenosphere is a solid but it can flow, like toothpaste.

18. Examples of Asthenosphere in a sentence, how to use it

19. The mesosphere comprises the rest of the mantle below the asthenosphere.

20. Asthenosphere and Lithosphere constitute the outmost concentric layers of our earth

21. The Asthenosphere lies beneath the lithosphere and consists of partially molten rock

22. Learn about the two distinct regions of the Mantle, the lithosphere and Asthenosphere

23. Forty-five miles beneath the surface, the layer known as the asthenosphere begins.

24. The differential movement of lithosphere and asthenosphere causes the Neozoic deformation of Tianshan.

25. The Asthenosphere is found between 50 to a few hundred miles below the lithosphere

26. The boundary where the lithosphere and Asthenosphere meet is referred to as the LAB

27. ♦ The Asthenosphere is composed of matter in the molten or semi-molten state

28. The Okinawa Trough is a back arc basin still driven by the converging asthenosphere.

29. The Asthenosphere extends from 100 km depth to 660 km beneath the Earth's surface

30. Most of the Asthenosphere is solid but could be melted depending on its location.

31. The Asthenosphere is the region of the upper earth considered to be mechanically weak

32. The rocks in the Asthenosphere are not as dense as the rocks in the lithosphere.

33. Oceanic lithosphere has a mean density rather close to that of the immediately underlying asthenosphere.

34. 1 Characteristics 2 Historical 3 References 4 External links The Asthenosphere is a portion of

35. Definition of Asthenosphere : a zone of a celestial body (such as the earth) which lies beneath the lithosphere and within which the material is believed to yield readily to persistent stresses Other Words from Asthenosphere Example Sentences Learn More …

36. Alternatively, subducted oceanic crust may be able to pull adjacent continental crust down into the asthenosphere.

37. 10 It presents a decided signification that the asthenosphere rised to the forming of big petroliferous regions.

38. Asthenosphere, zone of Earth’s mantle lying beneath the lithosphere and believed to be much hotter and more fluid than the lithosphere. The Asthenosphere extends from about 100 km (60 miles) to about 700 km (450 miles) below Earth’s surface

39. The Asthenosphere is solid upper mantle material that is so hot that it behaves plastically and can flow

40. The Asthenosphere is the depth in the earth where heat from the core begins to melt the crust

41. The lithosphere is made of the brittle crust and uppermost mantle and lies on the plastic Asthenosphere

42. The Asthenosphere is solid upper mantle material that is so hot that it behaves plastically and can flow

43. As nouns the difference between mantle and Asthenosphere is that mantle is a piece of clothing somewhat like an open robe or cloak, especially that worn by orthodox bishops while Asthenosphere is (geology) the zone of the earth's upper mantle, below the lithosphere

44. The layer of earth that is just below Lithosphere and goes deeper inside the surface is known as Asthenosphere

45. Asthenospheres asthenospheric astheny asthma asthma-weed asthma attack: asthma attacks asthma crystals asthmalike asthmas asthmata asthmatic; Literary usage of Asthenosphere

46. The Asthenosphere is mostly solid except for a few regions that have half molten rocks and are thus semi-fluid

47. The rise of the asthenosphere , the position of Moho and mantle plume are the indication of the mantle convection.

48. This would drag the underlying asthenosphere along and promote a compensatory upward movement within the mantle under mid-oceanic ridges.

49. The Lithosphere-Asthenosphere boundary is defined by a difference in response to stress: the lithosphere remains rigid for very long periods of geologic time in which it deforms elastically and through brittle failure, while the Asthenosphere deforms viscously and accommodates strain through plastic deformation.

50. Deep-zone earthquakes, i.e., those that occur in the Asthenosphere or below it, may be caused by crustal plates sinking into

51. Basaltic magmas that form the oceanic crust of Earth are generated in the asthenosphere at a depth of about 70 kilometres

52. The Asthenosphere lies beneath the lithosphere and consists of partially molten rock. Seismic waves passing through this layer are significantly slowed

53. As the ice retreats, the load on the lithosphere and asthenosphere is reduced and they rebound back towards their equilibrium levels.

54. The Asthenosphere In Plate Tectonic Theory The Asthenosphere is now thought to play a critical role in the movement of plates across the face of Earth's surface. According to plate tectonic theory, the lithosphere consists of a relatively small number of very large slabs of rocky material.

55. According to the previous studies, the uplifting of the asthenosphere could be correlated with lithosphere thinning resulted from an E-W extension.

56. The Asthenosphere is a mechanically weak layer beneath the lithosphere characterized by low seismic wave velocities and high attenuation (Karato, 2012)

57. The Asthenosphere (from Greek asthenēs 'weak' + sphere) is the mechanically weak ductily-deforming region of the upper mantle of the Earth

58. Asterted asterting asterts asthenia asthenias asthenic (current term) asthenic personality asthenic personality disorder asthenic type asthenics: asthenies asthenopia asthenopic asthenosphere asthenospheres asthenospheric

59. Isostatic adjustments (the depression or uplift of continents by buoyancy) take place in the Asthenosphere, and magma is believed to be generated there

60. Isostatic adjustments (the depression or uplift of continents by buoyancy) take place in the Asthenosphere, and magma is believed to be generated there

61. Lithospheric plates are exerted by a fluid pressure, since they immediately overlie the asthenosphere . We define this fluid pressure as Asthenospheric Static Push (ASP).

62. Asthenosphere (a:without; stheno:strength) is the weak and easily deformed layer of the Earth that acts as a “lubricant” for the tectonic plates to slide over

63. The Asthenosphere, in its capacity as a quasi-liquid, has convection currents that extend throughout its whole surface, under the entire area of the plates

64. 29 Lithospheric plates are exerted by a fluid pressure, since they immediately overlie the asthenosphere . We define this fluid pressure as Asthenospheric Static Push (ASP).

65. Mantle plumes induced asthenosphere upwelling and development of magma chambers along deep-sited faults, and thus resulted in fracture eruption of flood basalts on large scale.

66. As the plates spread apart, the lithosphere, or crust, is moved aside like a lid, allowing molten rock from the liquid asthenosphere to seep through.

67. In Mesozoic, the most important interaction occurred between the crust and the mantle, whereas in the older and Cenozoic it did between the lithosphere and the asthenosphere .

68. Seamounts form from magmatic eruptions, which occur when lava seeps up to the crust through the partially-melted sub-layer, known as the asthenosphere, in the mantle.

69. The parental magma for pyroxenite xenoliths could be derived from the partial melting of the asthenosphere with continental crust material involvement and of the upper lithospheric mantle.

70. Batholithic mantle lithosphere (SBML) which was produced in Cretaceous time and which included elements of the ancient (Proerozoic) North American SCLM, tectonically accreted oceanic lithosphere mantle, and asthenosphere

71. Asthenosphere uplift indicates the deep adjustment process during the interaction of plates, and also shows the adjusting process of gravitational equilibrium between upper layer of crust and mantle

72. Asthenosphere uplift indicates the deep adjustment process during the interaction of plates, and also shows the adjusting process of gravitational equilibrium between upper layer of crust and mantle.

73. The mantle convection is the primary driving force for the formation and evolution of sedimentary basins, and manifested in the position of the asthenosphere, Moho discontinuity and mantle plume.

74. At the dawn of plate tectonics the concept of a weak Asthenosphere layer sandwiched between strong overlying plates and more viscous underlying mantle was widely accepted, albeit vaguely defined

75. Asthenosphere - the lower layer of the crust layer - a relatively thin sheetlike expanse or region lying over or under another crust, Earth's crust - the outer layer of the Earth

76. THE GREATEST SHOW ON EARTH The Asthenosphere, in its capacity as a quasi-liquid, has convection currents that extend throughout its whole surface, under the entire area of the plates.

77. Asthenosphere (n.) layer of the Earth's upper mantle, 1914, literally "sphere of weakness" (by comparison with the lithosphere), from Greek asthenes "weak" (see asthenia) + sphere.

78. This paper has proposed a hypothesis of magma tides in the asthenosphere to interpret 6 year earthquake cycles in major seismic regions of the world which was discovered by the author.

79. This hot molasses substance will be forced into the lithosphere causing the liquid to cool off into rock, only to be forced back into the Asthenosphere causing the rock to melt

80. Then his study achievement, as the key of solve the problem of continental geosphere structure which has the same structure as asthenosphere, has found a series of new idea and pattern.