Lithosphere in a sentence

Due to its lower density, hot oceanic lithosphere will not lie as deep as old, cool oceanic lithosphere.

In a paper published to Nature Communications, the team showed that large portions of the African tectonic plate – otherwise known as the lithosphere – have disappeared over the past 200m years.

The thickness of the crust and mantle lithosphere is not to scale.

Another theory is that the mantle flows neither in cells nor large plumes but rather as a series of channels just below the Earth's crust, which then provide basal friction to the lithosphere.

As oceanic lithosphere is formed at spreading ridges from hot mantle material, it gradually cools and thickens with age (and thus adds distance from the ridge).

Average oceanic lithosphere is typically convert thick;sfn its thickness is a function of its age: as time passes, it conductively cools and subjacent cooling mantle is added to its base.

CD-ROM Working Group, Structure and Evolution of the Lithosphere Beneath the Rocky Mountains: Initial Results from the CD-ROM Experiment.

Deep-focus earthquakes occur at a depth where the subducted lithosphere should no longer be brittle, due to the high temperature and pressure.

Failing an ocean, the icy lithosphere may be somewhat thicker, up to about 300 km.

For Callisto, the outer conductive layer corresponds to the cold and rigid lithosphere with a thickness of about 100 km.

Geologists attribute the arcuate structure to the rigidity of the descending plate, and island arc cusps relate to tears in the descending lithosphere.

In periods with relatively large areas of new lithosphere, the ocean floors come up, causing the eustatic sea level to rise.

It includes the study of the atmosphere, hydrosphere, lithosphere, and biosphere.

Long residence in the cratonic lithosphere allows diamond crystals to grow larger.

Mechanically, the lithosphere is cooler and more rigid, while the asthenosphere is hotter and flows more easily.

Multi-ring structures probably originated as a result of a post-impact concentric fracturing of the lithosphere lying on a layer of soft or liquid material, possibly an ocean.

Oceanic crust is also part of tectonic plates, but it is denser than continental lithosphere, so it floats low on the mantle.

Somehow, this energy must be transferred to the lithosphere for tectonic plates to move.

Tectonic lithosphere plates consist of lithospheric mantle overlain by either or both of two types of crustal material: oceanic crust (in older texts called sima from silicon and magnesium ) and continental crust ( sial from silicon and aluminium ).

Tectonic plates main The mechanically rigid outer layer of Earth, the lithosphere, is broken into pieces called tectonic plates.