Answer:
When you find the Earth's chemical structure, you can split the interior into <em>three layers: the crust, the mantle, and the core.</em>
- The crust is perhaps the lowest volume layer made up of several minerals formed from silicate.
- The mantle underneath the crust is the biggest layer which consists of more porous iron and silicate rock with magnesium.
- The core with high density is primarily metal (predominantly iron and nickel).
Through comparison, despite the Earth's physical features, how much the layers react to temperature and pressure, the Earth consists of five layers: <em>the lithosphere, the asthenosphere, the mesosphere, the outer center, and the inner centre.</em>
- The lithosphere is indeed the outermost layer of brittle rock which breaks when applying pressure.
- The asthenosphere is a porous layer; if a steady pressure is applied it flows.
- The mesosphere is below the asthenosphere (corresponding to the middle and lower mantle) and is solid because of the enhanced thickness tension.
- Underneath the mesosphere the outer core is liquid (capable of flowing), as well as the inner core is solid.
- The same as the mesosphere, as force is applied, the pressure on the inner core creates a hard layer which is unable to move.
Hello there,
Which factors add to the greenhouse effect and are caused by human activities? Check all that apply.
Answers:
a decrease in the amount of dust in the atmosphere
an increase in gases in the atmosphere that absorb heat
Answer: The berg winds are described as being dry because of extensive heat in South Africa.
Explanation:
When the air that has been heated on the extensive central plateau flows down the escarpment to the coast it undergoes further warming by adiabatic processes. This accounts for the hot and dry properties of these off-shore winds, wherever they occur along South Africa's coastline.
Terrestrial planets: Mercury, Venus, Earth and Mars.
Gas Giants: Jupiter and Saturn.
Ice Giants: Uranus and Neptune.