англ 4-5

англ 4-5

University

20 Qs

quiz-placeholder

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19 Formation Characteristics

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англ 4-5

англ 4-5

Assessment

Quiz

English

University

Hard

Created by

Айсат Жумажанов

FREE Resource

20 questions

Show all answers

1.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

How are Igneous rocks formed?

biologically

formed by the accumulation or deposition of small particles and subsequent cementation of mineral or organic particles

form only at the high temperatures and pressures associated with the process of metamorphism

formed from cooling rocks

formed by hot, molten rock crystallizes and solidifies

2.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What's she doing?

She goes to the country

He is printing the syllabus

She is sewing a new dress

He was doing home task

They have a dictation

3.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

How are Sedimantary rocks formed?

Formed by the accumulation or deposition of small particles and subsequent cementation of mineral or organic particles

From when hot, molten rock crystallizes and solidifies

Form only at the high temperatures and pressures associated with the process of metamorphism

Formed from cooling rocks

Unknown

4.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

The unproductive rocks, usually igneous and metamorphic rocks underlying the sedimentary rocks, are called -

aggregates

sourse rocks

minerals

basement rocks

cementation     

5.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

How are Metamorphic rocks formed?

formed  by exposion of  igneous and  Sedimantary  rocks at the high  temperatures and  pressures

formed by the accumulation or deposition of small particles and subsequent cementation of mineral or organic particles

from when hot, molten rock crystallizes and solidifies.

formed from cooling rocks

biologically

6.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is formed when the molten melt is cooled?

Oil and gas

Igneous rock

Igneous rock

One rock

Plutonic rock

7.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Organic sediments are formed -

by the breakdown of rocks

by the precipitation of salt out of water

biologically

by the processes of cementation

by high heat and pressure

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