Answer:
The War of 1812 is sometimes called the second war for independence. The Americans fought for their rights; for the rights to neutral trade, which British government suspended because of the continental system of the French emperor Napoleon.
Explanation:
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*ok I'm Australian I'm just basing what I know of this from what I've read and heard from the musical* ok so basically Hamilton was in control of the capital and to raise it he needed tariffs (tax) from certain people, therefore tariff would help him get ahead of Jefferson and Madison who had control of the banks (I think)
<u>Advantages of a Janissary life:</u>
- They were young boys who were converted to Islam and were specially trained to guard the fortress and fight in wars.
- They were given privileges as they were Sultan's most truth worthy soldiers.
- They were constantly trained to be better fighters.
<u>Disadvantages of a janissary life:</u>
- They were not allowed to marry until their fighting days are not over.
- They were supposed to be always on foot and active to fight the danger.
It varies depending on the environment where it fossils and the type of organism:
1-Conservation of organs without modification or with discrete modifications (recrystallization). Is the usual case of hard parts (shells, bones, teeth, calcareous algae ...), and exceptionally soft parts in very particular conditions: ahem. mammoths conserved in icy soils of siberia or in hydrocarbons (ozokerites) north of the Carpathians, insects included in fossil resins (baltic amber).
2-Conservation of organs after their replacement by a different subject preserbando its structure with more or less detail. (It is a process called metasomatism) ahem. silicification of trunks of trees, vertebrate bones or the pyritization of ammonites.
3-Conservation in the form of mold of the organism, internal or external to it. It is often the case of ammonites, shells or conches.
The fossilization process is said to start at 100ºC and pressures above 1Kb (kilobar). Conyeva an exchange of atoms, between the original organism and the matter that surrounds it. They are called fossiligenetic processes. Some of the processes are: carbonation, silicification, phosphatization, pyritization, dissolution.
