Voorbeelden van het gebruik van Lithosphere in het Engels en hun vertalingen in het Nederlands
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The layer below the lithosphere is called the‘asthenosphere'.
They have to understand, the species has burrowed into the Lithosphere.
Cut a little groove on the lithosphere as the locating point.
The tunnel leads to a vault 1. 6 kilometers inside the Earth's lithosphere.
The mantle part of the lithosphere consists largely of peridotite.
Some lithospheric plates consist of both continental and oceanic lithosphere.
Earth's mechanically rigid outer layer, the lithosphere, is divided into tectonic plates.
The phosphorus cycle describes the movement of phosphorus through the lithosphere,….
The Earth's outer solid layer, the lithosphere, is made of rock.
Biogeology is the study of the interactions between the Earth's biosphere and the lithosphere.
The lithosphere is cooler
hydrosphere, lithosphere and biosphere.
Due to its lower density, hot oceanic lithosphere will not lie as deep as old, cool oceanic lithosphere.
For this reason, stones in the asthenosphere can move around far easier than those in the lithosphere.
Which is limited to a determined zone at the surface of the lithosphere"” in his 1926 book, The Biosphere.
After the lithosphere drilled, if it needs to pull the drilling tool out,
This refers to whether a crustal boundary between oceanic lithosphere and continental lithosphere is a plate boundary or not.
The Earth's lithosphere is broken up According to the theory of plate tectonics, into seven large and many minor tectonic plates.
grabens together with basaltic volcanism resulted in the creation of new oceanic lithosphere.
Could go right through to lithosphere and, yes, Yes, the ocean crust is thin enough that the blast it could conceivably push the planet back into alignment.
cryosphere, lithosphere, and biosphere.
When a piece of lithosphere that was heated and stretched cools again, its density rises,
terrestrial biosphere, lithosphere, and the atmosphere.
In periods with relatively large areas of new lithosphere, the ocean floors come up, causing the eustatic sea level to rise.
Where the lithosphere moves upward(tectonic uplift),
mantle, lithosphere, crust, and by interactions with possible ocean and atmosphere.
In terms of heat transfer, the lithosphere loses heat by conduction,
where oceanic lithosphere of the Rheic Ocean subducted beneath the Mid-German/Normannian highs.
the angle of the drill into lithosphere is moderate,
the movements of a larger number of smaller plates of the Earth's lithosphere, since tectonic processes began on Earth between 3