C. phyllite is the intermediate between slate and schist.
For much of South and Southeast Asia, winter is a period characterised by relatively dry conditions is "true" statement.
<h3>Reason for Dry condition in South and Southeast Asia:</h3>
The South and Southeast Asian winters is characterised by relatively dry conditions. This is because of the trade winds blowing from the Northeast to Southwest over the Pacific Ocean from the subtropical high-pressure belt towards the equatorial lows.
Some characteristics of South and Southeast Asia are-
- In general, Asia is demarcated by a continental climate in the interior parts of the continent.
- This means there is a strong heating up of the landmass during summer months and a strong chilling of the continent during winters.
- The relatively dry conditions as compared to summer is due to the dry wind which loses most of its moisture at the coasts while passing through the continental landmass.
Learn more about the main wind belts, here
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Answer:
Below
Explanation:
Salinity: Sink (increase in density)
Increase in temp: Rise (the molecules spread farther)
Freeze: Sink (water is becoming ice)
Dilution: Rise (Adding more)
Evaporation: Sink (taking water out)
Temperate climate zone, because big cities don't function well during the arctic winter, nor summer actually
