The best option in terms of the Gentleman’s Agreement of 1907 would be that "<span>The United States would not segregate Japanese immigrants, and Japan would not allow further emigration to the United States," although it had less to do with segregation and more to do with not allowing more Japanese into the US. </span>
Explanation:
1. Why begin this article with a quote from the Old Testament and one from John Locke?
2. Why use Clyde Ross, a resident of North Lawndale in particular, to illustrate much of this article?
3. Just considering housing as a topic, how does housing policy illustrate systematic racism?
4. "We invoke the words of Jefferson and Lincoln because they say something about our legacy and our traditions.
We do this because we recognize our links to the past - at least when they flatter us. But black history does not
flatter American democracy; it chastens it.... White supremacy is not merely the work of hotheaded
demagogues, or a matter of false consciousness, but a force so fundamental to America that it is difficult to
imagine the country without it." From Coates' evidence, explain this.
5. What would "paying reparations" to American blacks look like to Coates?
R8 Coates The Case for Reparations - The Atlantic cory.pdf
Answer:
The success of the cotton gin led to increased production of short-staple cotton throughout the South. In Texas, Austin offered land bounties to colonists willing to grow cotton and to blacksmiths and carpenters willing to build cotton gins. As early as 1825 primitive gin manufacturing took place near San Augustine.
Explanation:
Answer:
Historians generally recognize three motives for European exploration and colonization in the New World: God, gold, and glory. Motives for Exploration For early explorers, one of the main motives for exploration was the desire to find new trade routes to Asia. By the 1400s, merchants and crusaders had brought many goods to Europe from Africa, the Middle East, and Asia. Demand for these goods increased the desire for trade.
<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>
