tectonic plates Continental crust Oceanic crust thicker heavier The Earth's crust is divided up into chunks of solid roc - They vary in size and the Earth's surface can be that of a boiled egg which has been cracked. The major plates e Pacific, Eurasian, African, Antarctic, North American, South Ar nd the Indo-Australian. There are other smaller plates however, e Philippines and Coco plates. The plates are made up of aterials, and there are 2 broad types: older, and lighte is 3. omposed mainly of granite. It is 22 mi (35 km) thick on average ense than oceanic crust, which accounts for its mean surface about 3 mi (4.8 km) above that of the ocean floor. Continental ore complex than oceanic crust in its structure and origin and i imarily at subduction zones at destructive plate margins. 2. is younger, 5. omposed of basalt and gabbro. It is mainly formed at con: 4. and is
tectonic plates Continental crust Oceanic crust thicker heavier The Earth's crust is divided up into chunks of solid roc - They vary in size and the Earth's surface can be that of a boiled egg which has been cracked. The major plates e Pacific, Eurasian, African, Antarctic, North American, South Ar nd the Indo-Australian. There are other smaller plates however, e Philippines and Coco plates. The plates are made up of aterials, and there are 2 broad types: older, and lighte is 3. omposed mainly of granite. It is 22 mi (35 km) thick on average ense than oceanic crust, which accounts for its mean surface about 3 mi (4.8 km) above that of the ocean floor. Continental ore complex than oceanic crust in its structure and origin and i imarily at subduction zones at destructive plate margins. 2. is younger, 5. omposed of basalt and gabbro. It is mainly formed at con: 4. and is
Applications and Investigations in Earth Science (9th Edition)
9th Edition
ISBN:9780134746241
Author:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Chapter1: The Study Of Minerals
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