2.1 Earthquakes and volcanoes Flashcards

1
Q

Crater def?

A

Depression at the top of a volcano following a volcanic eruption. It may contain a lake

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2
Q

Lava def?

A

Molten magma that has reached the Earth’s surface. It may be liquid or may have solidified

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3
Q

Shield volcano def?

A

Gently sloping volcano produced by very hot, runny lava

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4
Q

Cone volcano def?

A

Steeply sloping volcano produced by thick lava

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5
Q

Ash def?

A

Very fine-grained volcanic material

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6
Q

Cinders def

A

Small-sized rocks and coarse volcanic materials.

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7
Q

Magma def?

A

Molten rock within the Earth. When magma reaches the surface it is called lava

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8
Q

Magma chamber def

A

The reservoir of magma located deep inside the volcano

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9
Q

Pyroclastiques flow def

A

Super hot (700*c) flows of ash, pumice and steam at speeds of over 500km per hour.

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10
Q

Pumice def

A

Volcanic rock

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11
Q

Vent def

A

The channel through which volcanic material is ejected

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12
Q

Dormant def? (volcano)

A

Volcanoes which have not erupted for a very long time

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13
Q

Active def? (volcano)

A

A volcano currently showing signs of activity

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14
Q

Extinct def? (volcano)

A

A volcano which has shown no signs of volcanic activity in historic times

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15
Q

Intensity def?

A

The power of an earthquake, this is generally measured using the Richter Scale or sometimes the Mercalli scale

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16
Q

Richter Scale def?

A

An open ended scale to record magnitude of earthquakes - the higher the number on the scale, the greater the strength of the earthquake. There are more small earthquakes than large

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17
Q

Mercalli Scale def?

A

Relates ground movement to commonplace observations of, for example, light bulbs, bookcases and building damage

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18
Q

Epicentre def?

A

The point on Earths surface directly above the focus of an earthquake. The strength of the shock waves generally decrease away from the epicentre.

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19
Q

Focus def?

A

The position within the Earth where an earthquake occurs. Earthquakes may be divided into shallow-focus and deep-focus earthquakes depending on how far below the Earths surface they occur

20
Q

What’s the shape of a volcano dependent on?

A

Type of lava
Very hot, runny lava = shield volcano
Thick material = cone volcano

21
Q

Composite/cone (strato-volcanoes)

are?

A

Steep volcanoes
formed of viscous acidic lava, ash and cinders.
Found at Destructive plate margins
(may have more than one cone)

22
Q

What are shield volcanoes?

A

Low-angle volcanoes
formed of runny basaltic lava
found at constructive plate margins and hotspots.

23
Q

What is an earthquake?

A

A sudden, violent movement of the earth. It occurs after a build up of pressure causes rocks to give away

24
Q

Types of crust

A

Continental

Oceanic

25
Describe Continental crust
35-70km thickness very old, mainly over 1500 million years Lighter, with an avarage density of 2.6 Usually made up of granite
26
Describe oceanic crust
6-10km thickness younger rock, under 200 million years Heavier with an avarage density of 3 Mainly basalt
27
Describe the destructive boundary process
The oceanic crust moves towards continental. | Due to oceanic being more dense it sinks beneath it, deep sea trenches and island arcs are formed
28
Describe the Constructive boundary process
Two plates move apart from each other; new crust is formed, creating mid-ocean ridges, volcanic activity is common
29
Describe the collision process from two continental crusts
Two congenital crusts collide, as neither of them sink they are folded up into mountains
30
describe the Conservative boundary process
Two plates move sideways past each other but land is neither destroyed nor created
31
What causes most earthquakes
Nuclear testing the weight of large dams drilling for oil/fracking
32
Where do most earthquake occur?
Plate boundaries
33
How does an Earthquake happen
Release of pressure as two plates move in different direction or at different speeds
34
Where do volcanoes occur
Mainly at plate boundaries however some occur in the middle of a plate, at location known as hotspots
35
What causes eruption
Rising magma entering a magma chamber…when pressure in the chamber is great enough eruption occurs
36
Primary hazards of earthquakes
Ground shaking | Surface faulting
37
Secondary Hazards of earthquakes
Ground failure and soil liquefaction Landslides and rockfalls Debris flows and mudflows Tsunamis
38
impacts of earthquakes
Loss of life loss of livelihood Total or partial destruction of building structure interruption of water supplies Breakage of sewage disposal systems Loss of public utilities such as electricity
39
Volcanoes direct hazards
``` Volcanic bombs Lava flows Ass fallout Volcanic gas Lahars (mudflows) Earthquakes ```
40
Volcano indirect hazards
Atmospheric ash fallout Landslides Tsunamis Acid rainfall
41
Socio-economics impacts of volcanoes
``` Destruction of settlements Loss of life Loss of farmland + forrest’s Destruction of infrastructure Distrusting of communications Reduced tourist arrivals ```
42
Opportunity’s provided by volcanoes
Fertile soil New land and islands for people to live on mineral rich soil important as tourist destinations
43
Case study: Soufrière Hills, Montserrat
Thé Soufrière Hills volcanoes erupted in 1995 after being dormant for nearly 400 years. Killed 19 people. Evacuation of capital city Plymouth. Major redevelopment of housing, schools, hospitals and a new airport. Montserrat observatory set up to monitor changes… checks size and shape of volcano use seidmometers to check for internal changes within crust measure emissions of sulfur
44
How do you reduce impacts of earthquakes (main ways)
Better forecasting and warning Building location building design emergency procedures
45
How can you predict and moniter earthquakes
Small-scale ground surface changes ground tilt change in rock stress micro-earthquake activity (cluster of small quakes) changed in radon gas concentration unusual animal behaviour, especially toads
46
CASE STUDY: Nepal, 2015 - an earthquake in an LEDC
2015 Nepal Earthquake - magnitude 7.8 - 25tg April as a result of the indian plate colliding with the Eurasian plate. Epicentre of the earthquake was 80km north of Capital, shallow focus of 15km. Occurred around midday 9k deaths in main earthquake and 200 were killed in an aftershock of 7.3 Fatalities were less in rural parts as less buildings. Economic cost of 7billion dollars - 35% of Nepals GDP. Asian development bank provided 3 million grant for emergency relief, including shelter, food, blankets and cooking utensils