Geohazards Flashcards

1
Q

geohazard def

A

a geological condition that is dangerous/ potentially to enviro or people who live within it

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2
Q

examples of geohazards

A

earthquakes
vol eruptions
tsunamis
landslides
subsidence
avalanche
cliff fall

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3
Q

what is the focus and epicentre of an earthquake

A

focus-where movement occurred

point within the earth at which the earthquake og as movement occurs along fault plane

sesmic waves radiate away from it in all directions

epicentre point on surface above focus

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4
Q

how is stored elastic strain energy released?

A

stress = forces
strain = reaction

relative movement of rock on either side of fault applies stress

rock undergoes strain

this process transfers energy and increases elastic strain stored in rock

energy releases and elastic energy decreases

energy released due to movement

released as heat and seismic waves (greater amp greater energy)

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5
Q

amplitude def

A

maximum extent of displacement of an oscillation from the position of rest

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6
Q

what does amplitude show

A

greater the amp = greater energy released

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7
Q

what happens to amp as waves move away from focus

A

reduces as energy released and transferred to surrounding rock

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8
Q

attenuation of seismic waves

A

loss of energy experienced by a wave shown as reduction in amp as it propagates through material

waves faster through rigid as transfer is easier so attenuation is reduced in more rigid rocks

amp decreases with distance from focus

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9
Q

Mercalli scale

A

magnitude scale for measuring earthquakes

empirical

gives 12 categories earthquake can fall into based on destruction and how people felt it
instrumental to cataclysmic

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10
Q

Mercalli scale pros and cons

A

pros-
don’t need specific equation
don’t need formal training to understand

cons-
empirical (based on observation/experience )

subjective

not comparable - e.g. all observation relate to building but they are diff in each country

may not remember experience

intensity decreases from focus but mag doesn’t

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11
Q

different earthquake measurement systems in time order

earliest to oldest

A

Mercalli- Richter- moment mag

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12
Q

Richter scale

A

measures energy output of the earthquake

1-10

use seismogram:
lag time - time diff between P and S waves tells us distance from focus
height of greatest S wave

plot on richter scale graph tells mag

should give same value no matter where

log so 1= 10x amp

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13
Q

Pros and cons of Richter scale

A

Pros:
Maths equ so less subjective
but also has desc for public

Cons:
assume same rock type

larger is underrepresented and less accurate the larger it gets (seismologists only measured at certain frequencies)

outdated

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14
Q

moment magnitude scale

A

What is used now

when waves arrive at seismometer measure:
lag time - tells us distance from focus
amplitude and waves
actual displacement of rock at quake site (new, not in richter)

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15
Q

Pros of moment mag

A

interpret broader range of seismic frequencies- determines more accurate e from large earthquake

accounts for rock type and rigidity

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16
Q

moment mag equ
(given to us)

A

Mw= 2/3logE-6.1

17
Q

different wave types

A

P- primary
S- secondary
L-love
R-rayleigh

18
Q

features of P waves and effect on buildings

SEE BOOKLET FOR DIAGRAM

A

features-
travel through L and S

body waves

arrive first- fastest

longitudinal

effect on building-
least dangerous

19
Q

features of S waves and effect on buildings

SEE BOOKLET FOR DIAGRAM

A

features-
can travel through S

body waves

arrive second- second fastest

shear waves - transverse

effect on buildings-
S waves more destructive than P
as greater amp

horizontal worse than vertical

20
Q

features of L waves and effect on buildings

SEE BOOKLET FOR DIAGRAM

A

Features-
Surface waves do the most damage

shear wave where shearing motion is confined to horizontal plane at earths surface (oscillate)

effect on buildings-
responsible for most damage

greatest effect- sideways movement is more effective

21
Q

features of R waves and effect on buildings

SEE BOOKLET FOR DIAGRAM

A

features- surface waves are most destructive

slowest

earths surface moves in a vertical elliptical path parallel to wave movement

effect on building-
worse than P and S

most movement with R- up and down so less destructive

22
Q

effect on ground movement on built environment

A

L waves cause most damage to buildings

lose objects thrown upwards

buildings fracture
pancake

freeways collapse

brick and stonework seperate along motar

sects of utility pipes separate

23
Q

how does rock competency affect how e is transferred and effect on buildings

A

comp rocks allow easier propergation of seismic waves and move on

less e dissipated to rock

less movement

also moves quicker through comp rock

24
Q

liquefaction and effect on buildings

A

saturated or partially saturated unconsolidated material losing strength and rigidity in response to applied stress

e.g. Earthquake

unconsolidated and incompetent rock holds more H2O in pore spaces

when rock compressed due to seismic waves, pore spaces reduce and H2O comes up and out

loss of strength makes buildings tip and sink

25
Q

where are developments banned

A

soft unconsol rock or incomp

on fault zone

nearby fault zones

26
Q

earthquake engineering ideas

A

reenforce concrete with steel

base isolation

tuned mass damper- giant pendulum near top of building brings back to centre by swing in opp direction (Taipei 101)

Crossbracing- X shaped brackets transfer seismic forces back to ground reducing lateral movement

seismic damper- absorb energy

emergency shut off switch

rubber/flexi pipes

metal plates around building- easier to move through than building as more rigid reduces impact on building)