bishops<span>, </span>priests<span>, and </span><span>deacons</span>
The Paleolithic Era <span>or </span>Old Stone Age<span> is a period of prehistory from about 2.6 million years ago to around 10000 years ago. The </span>Neolithic Era<span> or </span>New Stone Age<span> began around 10,000 </span>BC<span> and ended between 4500 and 2000 BC in various parts of the world. In the Paleolithic era, there were more than one human species but only one survived until the Neolithic era. Paleolithic humans lived a nomadic lifestyle in small groups. They used primitive stone tools and their survival depended heavily on their environment and </span>climate<span>. Neolithic humans discovered agriculture and animal husbandry, which allowed them to settle down in one area. The Mesolithic era followed the Paleolithic era but the period of the Paleolithic—Mesolithic boundary varies by </span>geography<span> by as much as several thousand years.</span>
Answer: Easy
Explanation: We get a day off so who cares if he discoverd the cuban islands
There were a number of reasons Federalists opposed the Louisiana Purchase. One can assume some opposed it just because it was Jefferson who made the purchase, out of a kind of reflex. Others had heard wild stories about the land purchased, and thought the purchase a bad bargain. Some thought that the inclusion of Louisiana as the treaty was written would undercut the power of the states by not having each state vote, thus undercutting Federalist power. (Some Federalists in the eastern states specifically feared a shift in power to the west.)
http://www.enotes.com/homework-help/why-did-some-federalists-oppose-louisiana-purchase-21441
Comments if you have any questions. :)
Scientists can determine if oxygen existed in Earth’s Archean atmosphere by looking for oxidized iron in rock. In the beginning, there was only a little to no oxygen in the atmosphere. The oxygen that are being produced by cyanobacteria is only enough for the weathering process. There will only enough oxygen that shall remain in the atmosphere when the rocks at the surface are properly and adequately oxidized. However, as time goes by, evidences said that the amount of oxygen in the Archean atmosphere is actually increasing in a slow steady pace.
