The Chinese have had restrictions in the amount of children that a family can have, for few decades it was one child, now it is two. Even thought the limit is increased to two children per family, it is a number that will allow the nation to keep it's population on a status quo level.
India, has it worst, the government has not been able to make a solid plan that can be implemented, the wast majority of the population is uneducated, and there's still the pride in having more children, so the population is still growing very fast.
The Kenyan government made a long term development plan, which as a main goal has to achieve a high quality life for all Kenyans that is sustainable with available resources. Also contraceptive coverage, and educating the population with videos, presentations, talks.
B.) "Equator" <span>divides our planet into the northern hemisphere and the southern hemisphere
Hope this helps!</span>
Food chains?????? I guess
Answer:
Sedimentary rocks are formed on or near the Earth's surface, in contrast to metamorphic and igneous rocks, which are formed deep within the Earth. The most important geological processes that lead to the creation of sedimentary rocks are erosion, weathering, dissolution, precipitation and lithification.
Explanation:
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Denudation was an important geological phenomenon in the Precambrian and Paleozoic ages in the Horn of Africa.
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What were the Precambrian and paleozoic epochs like?</h3>
The Precambrian (or Pre-Cambrian, or Cryptozoic) period of Earth's history before the present Phanerozoic Eon. The Precambrian is called after the Precambrian epoch, which preceded the Cambrian. The Precambrian period encompasses 88 percent of Earth's geologic history.
PALEOZOIC
The Paleozoic (or Palaeozoic) Era is the first of the Phanerozoic Eon's three geologic periods. The Cambrian, Ordovician, Silurian, Devonian, Carboniferous, and Permian epochs span 541 to 251.902 million years ago.
Thus, a major geological process of that era was denudation in the horn of Africa.
Learn more about the Paleozoic eras:
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