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Answer:
920 metres.
Explanation:
As one goes down under water, one additional atmosphere of pressure will be added for each metre descended. This is because water is much denser than our atmosphere.
Due to the incredibly high density of the Venusian atmosphere, the surface pressure is much higher than that of Earth's atmosphere. The atmospheres themselves are quite different, with that of Venus being made up mostly of carbon dioxide instead of the nitrogen of Earth's gaseous layer.
It is the pressure, however, that really sets these two worlds apart. Surface pressure on Venus is over 90 times sea-level pressure on Earth and even probes require submarine-like designs.
Minerals that grow as crystals in cooling lava can become magnetized if they contain iron.
Igneous rocks are composed of minerals that crystallise at a variety of different temperatures. This explains how a cooling magma could contain some crystals while still being primarily liquid. The Bowen reaction series is the pattern of mineral crystallisation from a magma.
Individual plagioclase crystals can be zoned from more sodium-rich around the exterior to calcium-rich in the centre when cooling occurs reasonably quickly. Because it controls how long the reaction can last before all the silica is consumed, the initial magma's composition is crucial to the crystallisation of magma.
Know more about crystals here
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And pushes them over. I would just put Spread
