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Proses Pergerakan Kerak Bumi

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Proses Pergerakan Kerak Bumi

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Permainan ini dicipta sebagai tujuan untuk menguji tahap penguasaan murid mengingati proses berlakunya kesan pergerakan kerak bumi.

Created by

Yusra Yusri
Yusra Yusri
Malaysia

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Proses Pergerakan Kerak Bumi
 

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Proses Pergerakan Kerak BumiOnline version

Permainan ini dicipta sebagai tujuan untuk menguji tahap penguasaan murid mengingati proses berlakunya kesan pergerakan kerak bumi.

by Yusra Yusri
1

bertentangan pertembungan mampatan banjaran

Pergerakan dan plat bumi akan menyebabkan berlakunya pembentukan gunung lipat . Daya menjadi punca utama terhadap pergerakan dan pertembungan tersebut .
Tolakan serta himpitan dua plat dari arah akan menyebabkan kerak bumi bertembung sehingga terbentuknya gunung lipat .

2

sempadan gelinciran tegangan sesaran

Proses gelinciran yang berlaku di plat bumi berpunca daripada pengaruh daya atau mampatan . Proses pergerakan kerak bumi ini juga dikenali sebagai proses . Terdapat satu ciri lanskap penting untuk menentukan pembentukan gunung bongkah seperti lurah .

3

rekahan lava terjunam magma benam

Pertembungan dua plat yang mewujudkan zon menyebabkan berlakunya gunung berapi . Plat yang ke bawah akan bertemu lapisan mantel sehingga membentuk dan . Pertembungan tersebut akan membentuk gunung dan rekahan . Letusan gunung berapi terjadi apabila cecair magma keluar memenuhi pada plat bumi .

4

tekanan himpitan lautan tsunami gegaran

Daya akibat pertembungan dan antara plat bumi menyebabkan berlakunya gempa bumi . Proses ini boleh menghasilkan di kawasan sempadan plat . Istilah gempa bumi sering digunakan jika proses ini berlaku di bahagian daratan , manakala istilah jika di bahagian .

 
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