Answer:
Based on Figure 2, we can conclude that, as the concentration of carbon dioxide (CO2) increases, the temperature in Antarctica increases, as well. It's the same the other way around - when the CO2 concentration decreased, so did the temperature.
We can see two spikes - about 125,000 years ago and in the present. In the present, there are almost 400 mean parts of CO2 per million. Because of this, the mean temperature increased to about two degrees Celsius. About 25,000 years ago, the temperature was about - 8 degrees, which is a very significant change, showing us how strongly the concentration of CO2 affects our climate.
Okay, so you take the length of your hypotenuse (17) and plug it into the pythagorean theorem as C. And then plug the given side (15) into A or B (doesn't matter which). So:
<span><span>a2</span>+<span>152</span>=<span>172</span></span>
<span><span>a2</span>+225=289</span>
Now isolate a^2 by subtracting 225 from both sides of the equation.
<span><span>a2</span>=64</span><span>
Find the square root of both sides to find the missing value.
a = 8</span>
Latitude: <span>It's in the northern hemisphere
</span>
Proximity to Water: <span>It's 300 miles from the sea</span>
Answer:
C. Hinduism
Explanation:
Buddhism is an offshoot of Hinduism. Its founder, Siddhartha Gautama, started out as a Hindu. For this reason, Buddhism is often referred to as an offshoot of Hinduism. ' With this, Gautama became known as Buddha, and his message spread to much of the Asian world.
Answer:
<em>D. Isostasy is reached with the lithosphere is neither sinking nor rising relative to the asthenosphere.</em>
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Explanation:
Isostasy refers to the principle of buoyancy in which an object immersed in a fluid is buoyed with a force equal to the weight of the displaced fluid. This means that a state of gravitational equilibrium has been reached between the lithosphere and the asthenosphere such that the lithosphere "floats" at an elevation that depends on its thickness and density. In Isostasy, the lithosphere is neither rising or sinking, and therefore in any region undergoing a change in vertical position, isostasy can provide a 'view' of the processes that are happening in such regions.
