The crust of the earth contains the highest mountains and deepest oceans.
The Earth is larger than what we can perceive from its surface. In fact, if you could split the Earth in two and hold it in your palm, you'd see that it has several layers. However, there are still many unanswered questions regarding the interior of our globe. The inside of our planet is still off-limits to humanity, despite the fact that we bravely investigate other planets and put satellites into orbit.
But because of developments in seismology, we now know a lot more about the Earth and the various strata that make it up. Numerous important planetaryprocesses are impacted by the features, content, and characteristics of each layer. The crust, the mantle, the outer core, and the inner core are them, going from the outside in. Let's examine them and see what is going on with them.
The interior of the Earth is distinct, much like all terrestrial planets. This indicates that it has layers, arrayed like the skin of an onion, making up its interior structure. Peel back one and you'll discover another that differs greatly from the first in terms of its chemical and geological characteristics as well as temperature and pressure.
Therefore, the crust of the earth contains the highest mountains and deepest oceans.
Read more about the layers of the earth, here
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The average rate of recession can be calculated by dividing the total distance receded by the number of years in each time span. The rate increased or decreased depending on these calculations.
To answer this question, we first need to know exactly how far the Saint Anthony Falls receded between the specified times. However, if we assume those distances are provided (in the form of the gaps on the map, expressed in feet), the student can calculate the rate of recession by dividing the total distance receded by the total number of years for each time span. For example, if the falls receded 86 feet between 1680 and 1766, that's 86 feet/86 years = 1 feet/year. If it receded 120 feet between 1856 and 1876, that's 120 feet/20 years = 6 feet/year. In this hypothetical example, the rate increased from the first time span to the next.
Again, it's crucial to know the exact distances receded (the lengths of the gaps on your map) to compute the accurate rates of recession.
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Answer:
The time span between 1680 and 1766 (lines 1 and 2) is 86 years: 1766 − 1680 = 86 years. During this time, the falls receded an average of 5.8 feet per year: 500 feet ÷ 86 years ≈ 5.8 feet per year.
The time span between 1856 and 1876 (lines 3 and 4) is 20 years: 1876 − 1856 = 20 years. During this time, the falls receded an average of 25 feet per year: 500 feet ÷ 20 years = 25 feet per year.
Explanation:
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B. The United States has a parliamentary system that holds general elections every four years.
C. The United States has a cabinet system that advises the prime minister on national issues.
tes has a federal government that handles national affairs and states that have their
own governments.
Answer:
The answer is Option D. The United States has a federal government that handles national affairs and states that have their own governments.
Explanation:
The United States has a presidential government system, whereas other countries like England have a parliamentary system. In a presidential system, the people choose the executive leader (the President) directly. In a parliamentary system, people vote for the party and technically it is the legislators who are a member of that party who chose their leader. So, in a parliamentary system voters do not select the leader directly like in a presidential system. The United States is also a federal system where power is shared in the national system and the individual states.
Answer:
D
Explanation:
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Answer:
Western coast of Australia
Explanation:
The Indian Ocean is the third largest ocean on the planet. It is located on both the Northern and Southern hemispheres. This ocean is located between Africa, Asia, and Australia, as well as the Southern Ocean. Africa is its western border, Asia its northern border, Australia the eastern border, and the Southern Ocean its southern border. This ocean facilitates connections between the western coast of Africa and the eastern coast of Australia, enabling much easier, cheaper, and quicker movement of goods, ideas, technology, and people between the two continents.