How to use in-sentence of “lithosphere”:
– As a result, oceanic lithosphere is much younger than continental lithosphere: the oldest oceanic lithosphere is about 200 million years old, while parts of the continental lithosphere are billions of years old.
– Another distinguishing characteristic of the lithosphere is its flow properties.
– When a continental plate comes together with an oceanic plate, at a subduction zones, the oceanic lithosphere always sinks beneath the continental.
– A plate is also one of the broken pieces of lithosphere of the Earth.
– Under the lithosphere is the asthenosphere, the weaker, hotter, and deeper part of the upper mantle.
– Below the lithosphere is the asthenosphere.
– Due to its lower density, hot oceanic lithosphere does not lie so deep as old, cool oceanic lithosphere.
– In geology, a rift is caused by tectonic plates in the Earth’s lithosphere moving apart.
Example sentences of “lithosphere”:
– Oceanic lithosphere is made up of mostly basalt and gabbro.
– Cratonic lithosphere is much older than oceanic lithosphere – up to 4 billion years versus 180 million years.
– The lithosphere is divided into plates, some of which are very large and can be entire continents.
– The lithosphere IPA: lith’usfēr, from the Greek languageGreek for “rocky” sphere is the solid shell of the planet “Earth”.
– Here an unstable portion of cold root of the lithosphere drips down into the mantle, decreasing the density of the lithosphere and causing buoyant uplift.
– The lithosphere is broken up into tectonic plates that can move.
– The lithosphere is divided into tectonic plates, which move gradually relative to one another.
– The lithosphere provides a conductive lid atop the convecting mantle: it reduces heat transport through the Earth, A lithosphere is the rigid, outermost shell of a terrestrial-type planet or natural satellite that is defined by its rigid mechanical properties.
– Ocean lithosphere varies in thickness.
– New oceanic lithosphere is constantly being produced at mid-ocean ridges and is recycled back to the mantle at subduction zones.
- Oceanic lithosphere is made up of mostly basalt and gabbro.
- Cratonic lithosphere is much older than oceanic lithosphere – up to 4 billion years versus 180 million years.
- The lithosphere is divided into plates, some of which are very large and can be entire continents.