Answer:
I'll assume you have to match the name with their definitions.
1. aquifers
underground water sources
That's because of the presence of porous rocks that let water pass through them and reach an underground cavern that then acts as a tank.
2. delta
a broad, triangular-shaped land area at the mouth of a river
That's common especially in larger rivers that meet their destination point (usually the ocean).
3. oasis
a small fertile area in the desert, usually a place where water is close to the surface (plural - oases)
We all heard about oases in the desert, where human and animals alike gather to drink.
4. rain shadow
an area that receives less precipitation because of its location on the leeward side of a mountain
That's common in high mountains region where the mountains are so high they block the passage of clouds to the other side.
Answer: True
Explanation:
The rocky planets are the terrestrial planets these are composed of rocks, within the rocks hard metals core is present which is composed of metals like iron, nickel and other mineral metals. The example of rocky planets includes the Earth.
A gas giant is a giant planet which is composed mainly of gases like helium and hydrogen. Jupiter and Saturn are the gas giant planets of the solar system.
Answer:
Deltas are a landform created by a constructive force and are formed by several different processes. When a river weathers rocks into sediments, the sediments are carried away, or eroded. Then, the sediment is deposited at the mouth of the river and it forms a delta.
When a rock is buried deep in Earth and experiences the same force from all sides, it is under confining pressure. When a rock is subjected to tectonic forces and experiences stress that is not the same in all directions, it is under differential stress.
<h3>What is
confining pressure?</h3>
Generally, confining pressure is the tension or strain exerted on a layer of soil or rock by the weight of the underlying substance is referred to as confining pressure.
In conclusion, Differential stress is simply the variance between an object's maximum and minimum compressive stress.
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