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Textbook Solutions: The Interior of the Earth | Window on the Word Class 7: Solutions, Notes & Worksheets PDF Download

A. Choose the correct answer

1.
Ans: 
(a)

2.
Ans: 
(c)

3.
Ans:
(d)

4.
Ans:
(c)

B. Fill in the blanks

1. Sial is another name for the___________________ . It contains the minerals _____________ and ___________
Ans: Sial is another name for the continental crust. It contains the minerals silica and aluminium.

2. The innermost layer of the Earth is called the ________.
Ans: 
The innermost layer of the Earth is called the core.

3. Rock made of cooled magma is known as _________ rock.
Ans: Rock made of cooled magma is known as igneous rock.

4. Hot, molten magma flowing onto the surface of the Earth is called __________ .
Ans: 
Hot, molten magma flowing onto the surface of the Earth is called lava.

5. ___________ rocks contain fossils.
Ans: 
Sedimentary rocks contain fossils.

C. Answer in one or two sentences.

1.
Ans: 
The three layers of the Earth are the crust, the mantle and the core.

2.
Ans:
The mantle is composed of the minerals silica, iron, magnesium and aluminium, and most of it is made up of semi-solid molten rock, also known as magma.

3.
Ans:
The inner core is different from the outer core as the outer core is liquid, while the inner core is solid because it is under extremely high pressure.

4.
Ans: 
Intrusive rocks are formed when magma gets trapped under the crust, cools down and solidifies.

5.
Ans:
Iron ore is the main mineral used in the production of steel.

D. Answer in a paragraph.

1.
Ans:
The oceanic crust differs from the continental crust in several ways. Firstly, the oceanic crust is thinner and denser than the continental crust, extending to a depth of 5 km to 10 km compared to the 35 to 70 km depth of the continental crust. Secondly, the oceanic crust is composed mainly of silica and magnesium, and it forms the ocean floor, whereas the continental crust is composed mainly of silica and aluminium and forms the continents.

2.
Ans: The three types of rocks are igneous, sedimentary and metamorphic rocks. Igneous rocks are formed when magma rises to the crust, cools down and solidifies. Sedimentary rocks are formed when rocks break down into small fragments known as sediment, which is then transported and deposited in different places by wind and water, and over time, gets compressed and hardened under pressure and varying temperatures. Metamorphic rocks are formed when igneous and sedimentary rocks transform or metamorphose under heat and pressure to form new kinds of rocks.

3.
Ans: 
Extrusive rocks are formed when magma, known as lava when it reaches the surface, cools and solidifies quickly on the Earth's surface after a volcanic eruption, resulting in very finely grained or even glassy rocks. Conversely, intrusive rocks are formed when magma gets trapped under the crust and cools down and solidifies very slowly, forming large crystals and a coarse structure. Examples of extrusive rocks include basalt and pumice, while granite and gabbro are examples of intrusive rocks.

4.
Ans: 
The rock cycle starts with magma cooling down to form igneous rocks. These rocks are brought to the Earth's surface due to earth movements like folding and faulting. Over millions of years, the rocks break down due to weathering and erosion to form sediments. These sediments are transported by water, wind or ice to different places, where they are deposited in layers. Over time, the sediments build up, until they are eventually compressed and hardened to form sedimentary rocks. Sometimes, when they are subject to conditions of high temperature and pressure, igneous and sedimentary rocks are transformed into metamorphic rocks. Movements of the Earth can push metamorphic rocks deep into the mantle, where they change back to molten magma, which can again solidify to form igneous rocks. This continuous cycle, through which one form of rock is changed into another, is called the rock cycle.

5.
Ans: 
Minerals are different naturally occurring substances that compose rocks, each with a unique chemical composition and definite physical properties. Examples of minerals include iron ore, copper, bauxite, limestone, mica, and kaolinite. Minerals are useful as they are the source of several important metals, such as iron, gold, aluminium, copper, and silver, which are used in various industries. Non-metallic minerals are used in various industries, for instance, limestone is used to make cement.

6.
Ans:
Fossil fuels are important sources of energy found in sedimentary rocks, formed as a result of the decomposition of fossils, which are plants and animals that died millions of years ago and got buried deep in the Earth's crust. Fossil fuels are used for various activities, including cooking, driving vehicles, and running factories, and most of the energy we use comes from fossil fuels.

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FAQs on Textbook Solutions: The Interior of the Earth - Window on the Word Class 7: Solutions, Notes & Worksheets

1. How do scientists study the interior of the Earth?
Ans. Scientists study the interior of the Earth using various methods such as seismic waves, drilling, and studying rocks brought up from deep within the Earth's crust.
2. What are the different layers of the Earth's interior?
Ans. The Earth's interior is divided into several layers including the crust, mantle, outer core, and inner core.
3. How does the temperature change as you move deeper into the Earth's interior?
Ans. The temperature increases as you move deeper into the Earth's interior due to the heat generated from the radioactive decay of minerals and the immense pressure within the Earth.
4. What role does the Earth's interior play in shaping the surface of the Earth?
Ans. The Earth's interior plays a significant role in shaping the surface of the Earth through processes such as plate tectonics, volcanic eruptions, and earthquakes.
5. How does the composition of the Earth's interior impact its overall structure and properties?
Ans. The composition of the Earth's interior, including the presence of different types of rocks and minerals, influences its density, temperature, and magnetic field, which in turn affects the planet's overall structure and properties.
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