I believe the answer you're looking for is Southwest Asia, looking at a climate map, the drier areas are located to the southwest.
Answer:
1. Continental-continental convergence are both <em>continental crust</em> plates.
2. Buoyancy basically means these plates are light float on top of the Asthenosphere.
Explanation:
1. To go a little more into detail, this type of convergence ocurrs when two plates made of continental crust (not oceanic) collide. In the case of ocean-continent convergence, the denser oceanic crust sinks underneath the lighter continental crust.
In this scenario, we have two plates, neither of which want to sink, so instead of going down they just crumple and fold and keep colliding. This collision creates very high mountain ranges such as the Himalaya and usually doesn't contain any volcanic activity because no magma is capable of penetrating through so much crustal material.
2. As for why continental crust is buoyant and doesn't sink has much to do with its composition. Continental crust is made mostly of silicate material. This is very different from oceanic crust which is made of basaltic rocks and is therefore heavier. The term buoyancy refers to the 'floating action' of the continental crust on top of the uppermost mantle.
Answer:
<h2>The answer is option B</h2>
Explanation:
Humidity is defined as the amount of water in the Earth's atmosphere. It is measured by the wet and dry bulb hygrometer.
When humidity is low, land organisms and trees tend to loose more water than when it's high. Plants loose water from parts such as leaves and bark and land organisms loose water from their their skin.
Hope this helps you
