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Географическая кора Земли

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Географическая кора Земли

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Изучение состава и толщины коры

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Google G
Google G
Uzbekistan

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Географическая кора Земли
 

Географическая кора ЗемлиOnline version

Изучение состава и толщины коры

by Google G
1

Толщина океанической коры примерно 5–10 км.

2

Граница между корой и мантий называется границей Нептуна.

3

Кора является верхней частью земной оболочки над мантией.

4

Океаническая кора моложе и обновляется чаще, чем континентальная.

5

Континентальная кора состоит преимущественно из гранитоподобных пород.

6

Континентальная кора толще океанической около 100 км.

7

Толщина континентальной коры примерно 30–50 км.

8

Плотность континентальной коры около 2,7 г/см³, океанической около 3,0 г/см³.

9

На границе коры и мантии расположен Мо́хо — граница между ними.

10

Кора Земли делится на континентальную и океаническую.

11

Возраст океанической коры в среднем около 200 млн лет.

12

Континентальная кора толще океанической по толщине.

13

В коре встречаются месторождения металлов и минералов.

14

Океаническая кора состоит преимущественно из базальтовых пород.

 
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