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
Section: Chapter Questions
Problem 1LR
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Question
LET US REMEMBER
LET US PRACTICE MORE
Directions: Supply the missing information in the paragraphs.
Choose from the words inside the box.
• According to the plate tectonics model, the
entire lithosphere of the Earth is broken into
numerous segments called plates.
• Each plate is slowly but continuously moving.
tectonic plates
Continental crust
Oceanic crust
thicker
heavier
The Earth's crust is divided up into chunks of solid rock called
They vary in size and the Earth's surface can be likened
1.
to that of a boiled egg which has been cracked. The major plates include
the Pacific, Eurasian, African, Antarctic, North American, South American,
and the Indo-Australian. There are other smaller plates however, such as
the Philippines and Coco plates. The plates are made up of different
materials, and there are 2 broad types:
LET US APPRECIATE
is 3.
, older, and lighter, and is
composed mainly of granite. It is 22 mi (35 km) thick on average and less
dense than oceanic crust,
of about 3 mi (4.8 km) above that of the ocean floor. Continental crust is
more complex than oceanic crust in its structure and origin and is formed
primarily at subduction zones at destructive plate margins.
Directions: Answer the question briefly.
nich acco
for its mean
ation
What are the uses of natural resources like granite, gabbro,
and basalt?
is younger, 5.
composed of basalt and gabbro. It is mainly formed at constructive
and is mainly
margins or spreading mid-ocean ridges.
7
8
Transcribed Image Text:LET US REMEMBER LET US PRACTICE MORE Directions: Supply the missing information in the paragraphs. Choose from the words inside the box. • According to the plate tectonics model, the entire lithosphere of the Earth is broken into numerous segments called plates. • Each plate is slowly but continuously moving. tectonic plates Continental crust Oceanic crust thicker heavier The Earth's crust is divided up into chunks of solid rock called They vary in size and the Earth's surface can be likened 1. to that of a boiled egg which has been cracked. The major plates include the Pacific, Eurasian, African, Antarctic, North American, South American, and the Indo-Australian. There are other smaller plates however, such as the Philippines and Coco plates. The plates are made up of different materials, and there are 2 broad types: LET US APPRECIATE is 3. , older, and lighter, and is composed mainly of granite. It is 22 mi (35 km) thick on average and less dense than oceanic crust, of about 3 mi (4.8 km) above that of the ocean floor. Continental crust is more complex than oceanic crust in its structure and origin and is formed primarily at subduction zones at destructive plate margins. Directions: Answer the question briefly. nich acco for its mean ation What are the uses of natural resources like granite, gabbro, and basalt? is younger, 5. composed of basalt and gabbro. It is mainly formed at constructive and is mainly margins or spreading mid-ocean ridges. 7 8
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