Geo-graphy notes for grade 12 on Earthquakes
Earth’s
internal processes
Earth
Quakes
Earth quake is defined as
a violent tremor in the earth’s crust which sends out series of vibrating waves
in all directions.
Explanation of
terms
i.
Origin:
point at which begins. It is also called the focus.
ii.
Tremor: this is a vibration within the earth’s crust
produced by gentle waves. When this vibration occurs on ocean floor, they
produce tsunami (gigantic water wave up to 10m high).
iii.
Epicenter:
the is the region immediately above the focus where the shock wave first hits
the earth surface.
iv.
shock wave:
there are two types:
a. body wave: it travels through the earth
crust and are two types:
-
Primary wave:
it causes crustal rocks to move backward and forward in the direction of the
wave movement.
-
Secondary
wave causes crustal rocks to move from side to side at right angles in to the
direction of the wave.
b. Surface wave: this travel through surface
rocks. They are of two types:
-
Long wave:
it causes surface rocks to move from side to side at right angle to the wave
movement
-
Rayleigh
wave: this causes surface rocks to have a vertical circular movement
Causes and regions of earth quakes
Causes:
a.
The development of faults (cracks) in the
crust which results from the collision between tectonic plates
b.
The sudden release of stress which has
slowly built up along the plane.
Regions
of Earthquake
This is often
concentrated in belts marking boundaries of plates which includes the ocean
ridge, the ocean deeps and volcanic island and regions of crystal depression.
Some earthquakes in the
past
-
The great Lisbon Earthquake 1755 so
disastrous
-
Yokohoma and Tokyo Japan September,1st
1923
-
San Francisco 1906
-
Acra Ghana Earth tremor 1939 etc.
Effects of earth’s quakes
a.
displacement
of earth’s crust,
c.
rising and
lowering of coastal rocks, rising and lowering
d.
of ocean’s floor, landslides and cracks.
e.
Destruction of lives and properties
f.
Destruction of roads, building, telecommunication system etc.
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