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gegra 3
gegra 3
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prady cieplne- prondy konwekcyjne
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powtsaja w wyniku stalei wymiany ciepla miedzy goraacym jadrem a chlodniejszym plaszczem ziemi
co powoduja prady cieplne
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powoduja ruch magmy i docieraja do skorupy ziemskiej
dwie odmiany skorupy ziemnskiej
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oceaniczna i kontynentalna
oceanoczna
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grubosc dochodzi do 12km
kontynentalna
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grubosc przekracza 50km
jak powstJe litosfera
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sklrupa ziemska +zewnetrzna czesc plaszcza gornego=litosfera
magma
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goraca masa slalna znajduje sie w glebi ziemio
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