INTERIOR OF THE EARTH Flashcards

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1
Q

Direct Sources of earths interior

A

Mining, drilling, volcanic eruption

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2
Q

InDirect Sources of earths interior

A

Analysis of temeperature and pressure, meteors, gravitation, magnetic field, and seismic activity

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3
Q

lithosphere refers to the portion of depth

A

up to 200 km from the

surface of the earth

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4
Q

Two types of body waves

A

p and s waves

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5
Q

waves are similar to sound waves. They travel

through gaseous, liquid and solid materials

A

The P-waves

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6
Q

Shadow zone of P waves

A

105 to 145

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7
Q

Shadow zone of s waves

A

beyonf 105

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8
Q

collapse earthquakes

A

In the areas of intense mining activity,
sometimes the roofs of underground
mines collapse causing minor tremors

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9
Q

explosion earthquakes.

A

Ground shaking may also occur due to the explosion of chemical or nuclear devices

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10
Q

Types of Earthquakes

A

tectonic earthquakes, volcanic earthquake. collapse earthquakes explosion earthquakes. reservoir induced earthquakes

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11
Q

The magnitude scale is known as the

A

Richter scale 0 to 10

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12
Q

The intensity scale is named after

A

Mercalli, 1 to 12

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13
Q

The mean thickness of

oceanic crust is

A

5 km

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14
Q

The mean thickness of the

continental is around

A

30 km

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15
Q

mean density of oceanic crust is

A

2.7g/cc

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16
Q

mean density of continental crust

A

3 g/cc

17
Q

type of rock in oceanic crust is

A

basalt

18
Q

The mantle extends from

A

Moho’s discontinuity to a depth of 2,900 km.

19
Q

The upper portion of the mantle is called

A

asthenosphere. extending upto 400 km.

20
Q

Main source of magma

A

asthenosphere.

21
Q

density in asthenosphere.

A

3.4g/cc higher than crust

22
Q

The crust and the uppermost part of the mantle are called

A

lithosphere. Its thickness ranges from 10-200 km

23
Q

The core mantle boundary is located at the depth of

A

2,900 km.

24
Q

Nife layer

A

core

25
Q

density at core mantle boundary

A

5 g/cc

26
Q

density at core centre

A

13g/cc

27
Q

magma.

A

The material in the upper mantle portion

28
Q

are the largest of all the volcanoes on the earth.

A

Shield volcanoes

29
Q

Shield volcanoes

A

basalt, very fluid, generally low explosivity

30
Q

cinder cone found in

A

Shield volcanoes

31
Q

characterised by eruptions of cooler and more viscous lavas than basalt and explosive eruptions

A

Composite Volcanoes

32
Q

These are the most explosive of the earth’s

volcanoes.

A

Calderas

33
Q

tend to collapse on themselves rather than building any tall structure. The collapsed depressions are called

A

calderas.

34
Q

Intrusive Volcanic Forms

A

Batholiths, Lacoliths, Lapolith, Phacolith and Sills, dykes

35
Q

These are large dome-shaped intrusive bodies

with a level base and connected by a pipe-like conduit from below

A

Lacoliths Karnataka plateau

36
Q

develops into a saucer shape, concave

to the sky body, it is called

A

lapolith

37
Q

A wavy mass of intrusive rocks, at times, is found at
the base of synclines or at the top of anticline
in folded igneous country.

A

phacoliths

38
Q

The near horizontal bodies of theintrusive igneous

rocks are called

A

sill or sheet (thinner)