Use of lithosphere in Sentences. 29 Examples
The examples include lithosphere at the start of sentence, lithosphere at the end of sentence and lithosphere in the middle of sentence
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lithosphere at the end of sentence
- The tremendous weight of the ice sheet loaded and depressed that part of the lithosphere.
- The heavy oceanic lithosphere descends into the mantle, beneath the lighter continental lithosphere.
- Oceanic lithosphere, however, is young and effectively of uniform age relative to continental lithosphere.
- The time scale over which uplift takes place depends upon the way in which heat is transferred through the lithosphere.
- Back-arc spreading may be initiated within the volcanic arc because the high heat flux from below weakens the lithosphere.
- Other evidence supports the idea of a lack of major deformation within plates, at least over plates composed of oceanic lithosphere.
lithosphere in the middle of sentence
- This occurs because rifting of the lithosphere allows hot mantle rock to move towards the surface.
- The lithosphere is broken into about a dozen large rigid plates, each plate moving as a distinct unit.
- Oceanic lithosphere has a mean density rather close to that of the immediately underlying asthenosphere.
- In other words the lithosphere experiences flexure, just as a springboard does when a diver walks along it.
- Perhaps more significant is the thickening of oceanic lithosphere as it moves away from mid-oceanic ridges.
- In his original model McKenzie assumed, for ease of calculation, that the lithosphere is stretched instantaneously.
- For example, while heating of the lithosphere may account for uplift, subsidence may result from lithospheric cooling.
- Subduction of oceanic lithosphere beneath a plate carrying continental crust gives rise to a continental-margin orogen.
- Such mountain belts develop when the oceanic lithosphere originally lying between two continents is eventually consumed.
- Warming occurs so slowly that the descending lithosphere retains its high density characteristics for a very long time.
- This is because thick lithosphere will tend to be more resistant to the effects of heat conduction and penetrative magmatism.
- A second reason for isostatic anomalies is that the lithosphere is not capable of adjusting instantaneously to a change in load.
- To attain hydrostatic equilibrium the position of the lithosphere adjusts vertically in accordance with its density and thickness.
- The hydrosphere, atmosphere, pedosphere, lithosphere, biosphere, and energy circle in an ecosystem are also in a dynamic balance.
- Convergent boundaries between oceanic lithosphere are marked by an oceanic trench, a volcanic island arc and a Wadati-Benioff zone.
- Cool, thick, old oceanic lithosphere is gravitationally unstable as it is generally denser than the asthenosphere over which it lies.
- One reason is that the lithosphere is not divided into small discrete blocks able to move freely up and down with respect to each other.
- The sequence of continental-margin orogen development begins with the subduction of oceanic lithosphere at, or close to, a continental margin.
- But if the lithosphere along the margin has sufficient rigidity the resulting imbalance in load will be accommodated through flexural isostasy.
- Where oceanic lithosphere is subducted beneath another oceanic part of a plate the associated volcanic activity and produce an intra-oceanic island arc.
- Continental lithosphere stands higher than oceanic lithosphere because continental crust is both of greater thickness and lower density than oceanic crust.
- Each of these areas of continental lithosphere are thought to have overridden regions of hot asthenosphere associated with former mid-oceanic spreading ridges.
- Panxi Rift with the dome-shaped volcano pattern has undergone three evolutionary processes: the lithosphere dome by mantle bulge, the continental crust dome and the subvolcano-dome.
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