EARTHQUAKE Flashcards

1
Q

is the vibration of earth’s surface caused by waves coming from a source of disturbance inside the earth

A

EARTHQUAKE

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2
Q

The typical characteristics of earthquake depends on

A
  1. Stress drop during the slip
  2. Total fault displacement
  3. Size of slipped area
  4. Roughness of the slipping process
  5. Fault shape (Normal fault, Reverse fault, Strike slip fault)
  6. Proximity of the slipped area to the ground surface
  7. Soil condition
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3
Q

As the waves radiate from the fault, they undergo geometric ________________ due to loss of energy in the rocks.

A

SPREADING AND ATTENUATION

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4
Q

These vibrations travel through the rocks in the form of

A

ELASTIC WAVES

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5
Q

there are three types of waves associated with propagation of an elastic stress wave generated by an earthquake.

A

primary (P) waves, secondary (S) waves and surface waves

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6
Q

These waves propagate by longitudinal or compressive action, which mean that the
ground is alternately compressed and dilated in the direction of propagation

A

PRIMARY WAVES

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7
Q

are transverse or shear waves, which mean that
the ground is displaced perpendicularly to the direction of propagation

A

SECONDARY WAVES

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8
Q

are tension-compression waves similar to the P-waves expect that their amplitude diminishes with distance below the surface of the ground.

A

RAYLEIGH WAVES

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9
Q

are the counterpart of the “S” body waves

A

LOVE WAVES

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10
Q

the rupture causing earthquakes initiates from a point

A

HYPOCENTER OR FOCUS

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11
Q

point on earth’s surface diametrically opposite to the epicenter

A

ANTI-CENTER

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12
Q

An imaginary line which joins the points at which the earthquake waves have arrived at the earth’s surface at the same time is called a

A

CO-SEISMAL

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13
Q

The instruments measure the ground displacements and are called

A

SEISMOGRAPH

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14
Q

The record obtained from a seismograph is called a

A

SEISMOGRAM

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15
Q

The seismograph has three components

A

the sensor, the recorder and the timer

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16
Q

The devises that measure the ground accelerations are called

A

ACCELEROMETER

17
Q

This scale is more comprehensive and describes the intensity of earthquake more precisely.

A

Mendvedev-Spoonheuer-Karnik scale (MSK 64)

18
Q

Numerous intensity scales have been developed over the last several hundred years to evaluate the effects of earthquakes, the most popular is

A

MODIFIED MERCALLI INTENSITY SCALE (MMI)

19
Q

In the Philippines, we use the __________________________ which composed of 10 increasing levels of
intensity.

A

PHIVOLCS Earthquake Intensity Scale (PEIS)

20
Q

Perceptible to people under favorable circumstances. Delicately balanced objects are disturbed slightly. Still Water in containers oscillates slowly.

A

INTENSITY I - SCARCELY PERCEPTIBLE

21
Q

Felt by few individuals at rest indoors. Hanging objects swing slightly. Still Water in containers oscillates noticeably.

A

INTENSITY II - SLIGHTLY FELT

22
Q

Felt by many people indoors especially in upper floors of buildings. Vibration is felt like one passing of a light truck. Dizziness and nausea are experienced by some people. Hanging objects swing moderately. Still water in containers oscillates moderately.

A

INTENSITY III - WEAK

23
Q

Felt generally by people indoors and by some people outdoors. Light sleepers are awakened. Vibration is felt like a passing of heavy truck. Hanging objects swing considerably. Dinner, plates, glasses, windows and doors rattle. Floors and walls of wood framed buildings creak. Standing motor cars may rock slightly. Liquids in containers are slightly disturbed. Water in containers oscillate strongly. Rumbling sound may sometimes be heard.

A

INTENSITY IV - MODERATELY STRONG

24
Q

Generally felt by most people indoors and outdoors. Many sleeping people are awakened. Some are frightened, some run outdoors. Strong shaking and rocking felt throughout building. Hanging objects swing violently. Dining utensils clatter and clink; some are broken. Small, light and unstable objects may fall or overturn. Liquids spill from filled open containers. Standing vehicles rock noticeably. Shaking of leaves and twigs of trees are noticeable.

A

INTENSITY V - STRONG

25
Q

Many people are frightened; many run outdoors. Some people lose their balance. motorists feel like driving in flat tires. Heavy objects or furniture move or may be shifted. Small church bells may ring. Wall plaster may crack. Very old or poorly built houses and man-made structures are slightly damaged though well-built structures are not affected. Limited rockfalls and rolling boulders occur in hilly to mountainous areas and escarpments. Trees are noticeably shaken.

A

INTENSITY VI - VERY STRONG

26
Q

Most people are frightened and run outdoors. People find it difficult to stand in upper floors. Heavy objects and furniture overturn or topple. Big church bells may ring. Old or poorly-built structures suffer considerable damage. Some well-built structures are slightly damaged. Some cracks may appear on dikes, fish ponds, road surface, or concrete hollow block walls. Limited liquefaction, lateral spreading and landslides are observed. Trees are shaken strongly. (Liquefaction is a process by which loose saturated sand lose strength during an earthquake and behave like liquid).

A

INTENSITY VII - DESTRUCTIVE

27
Q

People are panicky. People find it difficult to stand even outdoors. Many well-built buildings are considerably damaged. Concrete dikes and foundation of bridges are destroyed by ground settling or toppling. Railway tracks are bent or broken. Tombstones may be displaced, twisted or overturned. Utility posts, towers and monuments mat tilt or topple. Water and sewer pipes may be bent, twisted or broken. Liquefaction and lateral spreading cause man- made structure to sink, tilt or topple. Numerous landslides and rockfalls occur in mountainous and hilly areas. Boulders are thrown out from their positions particularly near the epicenter. Fissures and faults rapture may be observed. Trees are violently shaken. Water splash or stop over dikes or banks of rivers.

A

INTENSITY VIII - VERY DESTRUCTIVE

28
Q

People are forcibly thrown to ground. Many cry and shake with fear. Most buildings are totally damaged. bridges and elevated concrete structures are toppled or destroyed. Numerous utility posts, towers and monument are tilted, toppled or broken. Water sewer pipes are bent, twisted or broken. Landslides and liquefaction with lateral spreadings and sandboils are widespread. the ground is distorted into undulations. Trees are shaken very violently with some toppled or broken. Boulders are commonly thrown out. River water splashes violently on slops over dikes and banks.

A

INTENSITY IX - DEVASTATING

29
Q

Practically all man-made structures are destroyed. Massive landslides and liquefaction, large scale subsidence and uplifting of land forms and many ground fissures are observed. Changes in river courses and destructive seiches in large lakes occur. Many trees are toppled, broken and uprooted.

A

INTENSITY 10 - COMPLETELY DEVASTATING

30
Q

the logarithm to the base 10 of the largest displacement of a standard seismograph

A

magnitude