Every second integer is odd. (The ones in between them are even.)
If you promise that 'n' is odd, then the next odd ones
are (n+2), (n+4), and (n+6) .
We need to add them all up:
n + (n+2) + (n+4) + (n+6) = <u>4n + 12</u>
Now you're telling me that the sum is 56. Knowing that, I can
figure out what 'n' is, and once I know 'n', I can fiugure out all
four of the numbers.
<u>4n + 12 = 56</u>
Subtract 12 from each side: 4n = 44
Divide each side by 4 : <u>n = 11</u>
The four consecutive odd integers are:
n . . . . . <em>11</em>
n+2 . . . <em>13</em>
n+4 . . . <em>15</em>
n+6 . . . <em>17</em> .
Check the answer:
Add up (11 + 13 + 15 + 17) = <em><u>56</u></em> yay !
Answer:
Explanation:
Japan: Constitutional monarchy
A form of government in which a non elected monarch functions as the head of the state but within the limits of a constitution is called constitutional monarchy. The power is shared between a government and the monarch. e.g Britain.
Korea: One person Dictatorship
The from of government in which a small group or a person have the absolute power and there are no constitutional limitations on them is called Dictatorship. African nations such as Zimbabwe, Uganda and Asian nation North Korea and Eastern countries such as Syria are dictatorships.
Philippines: Republic democracy
A Presidential system is a a republican and democratic form of government in which the legislative branch is separate form the executive branch and the head of the government leads the executive branch. The head of state is called president and it is a ceremonial post.
Answer:
I'm unsure what the latter part of this question is asking (what do you mean by <em>Ion?</em>), but some landforms that are the result of weathering, erosion, and deposition include canyons, arches, and deltas. There are some like sinkholes which are formed by things like acid, too. Hope this helps! ♥
Marine waters cover 70.8% of the earth’s surface. And, if we substract the 5.5% area of the continental shelf, 65.3% of the earth’s surface is occupied by continental slope and rise, and deep-sea parts (data after Dietrich and Kalle 1957). The deep sea can be subdivided into several topographical units. There are deep-sea grabens<span> (15 in number), which cut deeper than 6,000 m. Deep-sea grabens are restricted to tectonic active regions near the foot of continental slopes.</span>
