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Leya [2.2K]
3 years ago
8

Immigrant populations in low-income countries are growing.

Geography
2 answers:
DENIUS [597]3 years ago
8 0
The answer for your question is true not false
Tom [10]3 years ago
4 0

Answer:

its :true

Explanation: i googled it  ._______________________.

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The Hawaiian islands appear to be older at one end of the island chain than the
andrew11 [14]

Answer:

2

Explanation:

3 0
3 years ago
The alps and Pyrenees of Western Europe and the Ural Mountains of Russia were created primarily by
disa [49]

Answer:Ural, mountain range forming a rugged spine in west-central Russia and the major part of the traditional physiographic boundary between Europe and Asia. Extending some 1,550 miles (2,500 km) from the bend of the Ural River in the south to the low, severely eroded Pay-Khoy Ridge, which forms a 250-mile (400-km) fingerlike extension to the northern tip of the Urals proper, the mountains constitute the major portion of the Uralian orogenic belt, which stretches 2,175 miles (3,500 km) from the Aral Sea to the northernmost tip of Novaya Zemlya.

Explanation:

5 0
3 years ago
What characteristics describe the ethiopian highlands region
Juliette [100K]

Answer:

The Ethiopian Highlands is a rugged mass of mountains in Ethiopia, situated in northeast part of Africa. It forms the largest continuous area of its elevation in the continent, with little of its surface falling below 1,500 m (4,900 ft), while the summits reach heights of up to 4,550 m (14,930 ft).

Hope this helps!!

5 0
4 years ago
The science that specifically attempts to determine Earth's shape and size by surveys and mathematical means is called:_________
kipiarov [429]
Surveying
Is the explain to exusnshsbs
6 0
3 years ago
The term used to describe large rock masses such as Half Dome in Yosemite National Park whose surface consists of imperfect curv
Vlad1618 [11]

Answer:

The answer is Batholithic intrusions

Explanation:

The Half Dome is an isolated mass suspended within the batholithic intrusions. Developed due to  vertical jointing, exfoliation, and some glacial activity. Steep face of half dome began to take shape as thin slabs of rock b/w parallel vertical joints were loosened by weathering and mass wasting and fell away layer by layer. Tenaya Glacier cleared away exfoliation debris and talus flowing in direction parallel to trend of vertical joints, removed sheets of rock by plucking . Rounded back of Half Dome formed as curved shells of rock exfoliated

8 0
4 years ago
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