L1 | Earthquakes Flashcards
(33 cards)
What causes/produces tremendous strain or directions to the Earth’s crust?
COOLING & SHRINKING OF ROCK LAYERS
forces that stretch or PULL rock layers TO opposite directions
TENSION FORCE
forces that PUSH rock layers FROM opposite directions
COMPRESSION FORCE
forces that pull rock layers IN DIFFERENT directions
SHEARING FORCE
vibrations or tremors on the Earth’s surface caused by the breaking slipping of rocks underneath
EARTHQUAKE
classifications of earthquakes
- TECTONIC
2. VOLCANIC
an earthquake where a sudden displacement of the Earth’s crust occurs along a fault or break in the rocks
TECTONIC EARHTQUAKE
source of great amounts of energy rapidly released resulting to the movement of the Earth’s crust
FOCUS or HYPOCENTER
point on the surface directly above the focus
EPICENTER
TRUE OR FALSE :
All earthquakes occur along the faults.
FALSE
CORRECT ANSWER : Most earthquakes occur along faults. However, earthquakes may also occur in places where many active volcanoes are located, that is, along the margins of the deep ocean floors.
earthquake originating from a volcanic activity
VOLCANIC EARTHQUAKE
areas in the circum-Pacific belt where it is more likely to experience shaking or sliding of the ground
RING OF FIRE
How are earthquakes described?
described by :
- INTENSITY
- MAGNITUDE
the strength of an earthquake & its corresponding possible effects on people, structures, and the environment
INTENSITY
indicates the observable destruction of the earthquake in a specific location relative to its distance from the origin
INTENSITY
developed by Italian volcanologist Giuseppe Mercalli in 1902 which lists the effects of an earthquake in relation to its intensity
INTENSITY SCALE or MERCALLI SCALE
the amount of energy released at the focus or origin of the earthquake
MAGNITUDE
instrument used to measure the magnitude, which records not only the strength but also the time of occurrence & direction of an earthquake
SEISMOGRAPH
developed in 1935 by American seismologist & physicist Charles Francis Richter, which measures the magnitude
RICHTER SCALE
observable effects of strong earthquakes on the Earth’s surface
- GROUND TREMORS
- LAND RUPTURES
- LAN SLIPPAGE
- LANDSLIDES
secondary effects of earthquakes
- TSUNAMIS
- FIRES
- LOSS OF PROPERTIES & LIVES
The earth’s crust shakes, and the strength of movement depends on the distance of an area from the focus and epicenter of the earthquake. If the place is near the focus and epicenter, the tremor would be strong. In contrast, if an area is several kilometers away from the origin of the earthquake, the tremor felt in the place would be less.
GROUND TREMORS
The shock near the epicenter can cause land surfaces to break open. Fissures or cracks can also be found in some distant areas from the epicenter. The tremors may even force water, mud, and sand out of the ground through these cracks because of the pressure caused by the movement of the underground rocks.
LAND RUPTURES
During an earthquake, side-by-side sliding movement of the ground may take place. Along the fault, rock layer sink or move down while the other slab moves up. This movement can be observed in things that seem to rise, bend, or twist after an earthquake. This creates high cliffs and sinking lowlands. Land surfaces bend or create waves of folds, forming small mounds or hills.
LAN SLIPPAGE