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Molodets [167]
3 years ago
11

How were countries formed​

Geography
1 answer:
True [87]3 years ago
3 0

Answer:

Some were established as a result of geographic isolation, such as England. Others were created as the result of emigration, such as Australia, often displacing existing nations. And still others were created from the breakup of larger empires or from peace treaties, such as Croatia.Explanation:

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Describe two specific examples of devolution each from a different world region.​
slamgirl [31]

Answer:

Devolution, the transfer of power from a central government to subnational (e.g., state, regional, or local) authorities. Devolution usually occurs through conventional statutes rather than through a change in a country’s constitution; thus, unitary systems of government that have devolved powers in this manner are still considered unitary rather than federal systems, because the powers of the subnational authorities can be withdrawn by the central government at any time (compare federalism).

Explanation:

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3 years ago
Which diagram could be used to prove △ABC ~ △DEC using similarity transformations?
Elena-2011 [213]

Explanation:

triangle ABC is reflected across A C and then is dilated to form smaller triangle D C E

3 0
2 years ago
How did geography protect the United States and Canada during World War I and World War II?
nikklg [1K]
We were far away from Germany, Italy and Japan. Water seperated the U.S. from the attacking countries so it was harder for them to attack the U.S.
6 0
3 years ago
what is the length of a diagonal of a cube with a side length of 3cm? A. square root 18 cm B. square root 27 cm C. square root 3
galina1969 [7]

Answer: b. square root of 27 cm

Explanation:

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5 0
3 years ago
Read 2 more answers
QUESTION 5 The elevation at which a parcel of air cools to its dew point temperature is called the a lifting condensation level
AleksandrR [38]

Answer:

A. condensation level

Explanation:

  • What usually happens when a parcel of air cools more slowly the air in motion, leads to the formation of clouds as moisture accumulation takes place. Thus the vertical ascent of air reduces its capacity to store or hold water and hence condensation occurs at dew point.
  • The rising parcel of air cools and descents down the original dew point and results in net condensation. Thus the lifted parcel of air reaches o its 100% concerning Adiabatic cooling.
5 0
3 years ago
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