earth 2 Flashcards
Fall of chimneys. Cracks in the walls of the building.
VIII. Damaging tremor
Describe how much energy an earthquake releases by assigning the earthquake a number from 1 to 10. The number indicates how strong the earthquake is.
Describe the strength or magnitude of an earthquake
Devised in 1935, Charles Richter, American Seismologist and Physicist
RICHTER SCALE
General awakening of those asleep. General ringing of bells. Oscillation of chandeliers, stopping of clocks, visible agitation of trees and shrubs. Some startled persons leaving their dwellings.
VI.Strong tremor.
Late 1700’s, used it as rough estimate of the size and the strength of an earthquake
Gives the idea how strong or weak the shaking is.
Tells how much a certain area was shaken when the earthquake reach that area
Can be determine by observing the effects of the earthquake in different places.
✓Houses, buildings, and other structures are inspected.
✓People are interviewed about what they saw (the cabinet fell over), how they felt (I was frightened), or what they did (I ran out of the house)
INTENSITY (I, II, III)
Recorder by a single seismograph or by the seismograph of the same model, but not by several seismograph of different kinds. The shock felt by an experienced observer.
I.Microseismic tremor
Overthrow of movable objects, fall of paster, ringing of church bells. General panic. Moderate to heavy damage buildings
VII. Very strong tremor.
Recorded by several seismograph of different kind. Felt by a small number of persons at rest
II.Extremely feeble tremor
. Felt by several persons at rest. Strong enough for the direction or duration to be appreciable.
III.Febble tremor
Felt by persons in motion. Disturbance of movable objects, doors, windows, cracking of ceilings.
IV.Slightly tremor
Felt generally by everyone. Disturbance of furniture, ringing of some bells.
V.moderate temor
Describe the strength of an earthquake.
Total amount of energy released by the earthquake at the focus as estimated from seismogram reading.
magnitude
➢ developed between 1879 and 1883 by Michele Stefano Conte de Rossi of Italy and François-Alphonse Forel of Switzerland.
✓used for about two decades until the introduction of the Mercalli intensity scale in 1902.
✓ use in some countries, such as
the Philippines until 1996 when it was replaced by the PHIVOLCS Earthquake Intensity Scale
ROSSI-FOREL SCALE
. Partial or total destruction of buildings.
IX. Devastating tremor
Great disaster, ruins, disturbance of the strata, fissures in the ground, rock falls from mountains
X. Extremely high intensity tremor.
✓ Very strong earthquake produces higher intensity ratings compared to weaker one.
FACTORS TO CONSIDER:
FACTORS TO CONSIDER: (1-7)
- Population
- Type of earthquake based on the depth from focus
- Presence of communities,
- Local soil
- Rock types underlying the area,
- Type and strength of the building present
- Duration of the shaking