GDP is important because it is a leading indicator of a country's economic health. It gives economists an idea of the nation's financial viability. <span>The GDP calculates the economic value of all produced goods and services generated by the country. Keeping track of it you would know or maybe predict the future trends of the economy of a country. Hope this answers the question.</span>
Answer:
Julius Caesar began to reshape the Roman Republic by beginning to give himself authority over certain aspects other officials would get. For example, Caesar gained control of the consul (which were supposed to be two that held the "most" authority), the praetor (which were the replacements of the consuls), and other positions slowly without outright saying he was overruling their authority. He frequently ignored the suggestions of the Senate when it came to war and other affairs, and he basically did as much as he could to gain absolute power without everyone suspecting so. He even declared a civil war against Rome because his enemy, General Pompey, was rivalling his power. I hope this helps, Julius Caesar is a very interesting character!
I did something super similar to this but I forgot
Answer:
Because to the Hispanic people,it is a big thing to be 15,cos u r only 15 once. And lyk in the English people like us , it's sweet sixteen.
Explanation:
I don't really know if u understand what am trying to say..................
<span><span><span>The crust: low density silicate rock, 5-70 km thick. There are two distinct types of crust.<span><span>Continental crust is variable in thickness and composition. Thickness ranges from 5-70 km. The composition ranges from mafic to felsic.</span><span>Oceanic crust is uniform in thickness and composition. It is 5-6 km thick and is mafic in composition.</span><span>The differences in thickness and density between continental and oceanic are responsible for the existence of ocean basins due to isostatic balance as the crust floats on the more dense mantle.</span></span></span><span>The mantle: high density, ultramafic silicate rock which can flow when subjected to long duration stresses. The mantle is over 2900 km thick and makes up over 80% of the volume of the Earth. The mantle is not molten!</span></span><span>The core: iron and nickel, liquid outer region with a solid center. The core is just over half the diameter of the Earth.</span></span>
