Answer:
I believe that The European Union is a good thing because in times of war, the countries most likely will not go to war against each other, and also because it allows the countries in the EU to become iron allies, which could prove useful in both war and times of hardship. Speaking of hardship, if any of the countries in the EU is faced with hardship or a hard decision, that country can ask the other countries in the European Union for help or for advice. And, if anybody in one of the nations within the EU travels to another country that is in the EU can use the same form of money, without the worry of having to convert it to the type of money that is used there, because every country in the European Union uses the same type of currency, the euro. For instance, if someone in, say, France, travels to maybe Greece for vacation, then that person could use the same form of money in Greece as used in France, which is a big worry taken off the mind. Plus, it gives the countries reasons why not to go to war over each other, and so they countries probably won't go to war against each other for a small reason, such as a steel mine or the sort. The European Union lets the citizens of the countries in the EU have freedom and human dignity, which is more than most countries have to offer to their citizens. The EU is a surprisingly good method of maintaining peace in the European countries, or, at least for the ones in the EU, such as Belgium, Germany, Greece, or Italy. So, in conclusion, I believe that the European Union is a good thing, for many reasons.
Explanation:
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Brainlest Please!</em></u></h2>
Answer:
Study the map of Phnom Penh, capital city of Cambodia and write a reflection on why so many factories are concentrated in one
Explanation:
Moderate is your answer hope this helps!
I would have to go with Europe.
Answer:
B. DIVERGENT
Explanation:
Ridge push (also known as gravitational sliding) or sliding plate force is a proposed driving force for plate motion in plate tectonics that occurs at mid-ocean ridges as the result of the rigid lithosphere sliding down the hot, raised asthenosphere below mid-ocean ridges.
