The American Revolutionary War, the Declaration of Independence, and the birth of the two-party system — this is a pivotal period in American history.
Guam, Texas, parts of mexico, cuba (for a bit), philipines until after ww2, puerto rica, us virgin islands and I think that's it
Answer:
Explanation:
Well if was a few things, first was the idea of why are we fighting to protect the democracy of a country have way across the world especially when many South Vietnamese government seemed on the edge of collapse and was oppressing the Buddhist majority, then fact that we had a draft here, however politicians refused to activate the reserve and the national guard so many young people who were forced to serve were upset, then many people believed the Vietnamese people had the right to self determination.
but the many TL DR reason was just how many Americans were being killed in the pointless war and how many Americans were captured, also in 1967 and 1968 when it seemed like we couldn't win the war, and when documents were released saying that LBJ didn't think we could win either that really hurt support for the war
It would be "traditional forms of poetry" that was not characteristic of the beat movement and the beat generation, since much of this movement had to do with "doing away" with tradition in many different aspects of life.
<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>
