INTERIOR OF THE EARTH Flashcards

(38 cards)

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

17
Q

type of rock in oceanic crust is

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

24
Q

Nife layer

25
density at core mantle boundary
5 g/cc
26
density at core centre
13g/cc
27
magma.
The material in the upper mantle portion
28
are the largest of all the volcanoes on the earth.
Shield volcanoes
29
Shield volcanoes
basalt, very fluid, generally low explosivity
30
cinder cone found in
Shield volcanoes
31
characterised by eruptions of cooler and more viscous lavas than basalt and explosive eruptions
Composite Volcanoes
32
These are the most explosive of the earth’s | volcanoes.
Calderas
33
tend to collapse on themselves rather than building any tall structure. The collapsed depressions are called
calderas.
34
Intrusive Volcanic Forms
Batholiths, Lacoliths, Lapolith, Phacolith and Sills, dykes
35
These are large dome-shaped intrusive bodies | with a level base and connected by a pipe-like conduit from below
Lacoliths Karnataka plateau
36
develops into a saucer shape, concave | to the sky body, it is called
lapolith
37
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.
phacoliths
38
The near horizontal bodies of theintrusive igneous | rocks are called
sill or sheet (thinner)