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Volcano
An opening in the
Earth's crust
where
lava
, molten rocks, and gaseous materials are forced out
Volcanoes
Vary in different
sizes
- some are low-lying depressions, some are small, some are
tall
How a volcanic eruption occurs
1.
Tectonic plates
collide
2. Massive
rocks
underground deform
3.
Temperature
and
pressure
build up
4.
Rocks
melt to become
magma
5.
Magma rises
to the surface and
volcanoes
erupt
Crater
The
opening
of a
volcano
Magma chamber
Deeply under the
crater
, where the
magma
is located
Volcanic vent
The cylindrical channel that connects the
crater
to the
magma chamber
Volcanic
eruption
When magma is released from the
crater
Lava
The
magma
that flows out on the
surface
Secondary vent
or
siphon
Another way out for the
magma
when a
volcano
erupts
Types of volcanic eruptions
Explosive
Non-explosive
Explosive eruption
Large amounts of
pyroclastic
materials (lava, ash, volcanic gas, rocks) are
ejected
into the air
Pyroclastic materials
Lava
, ash,
volcanic gas
, and rocks
Non-explosive eruption
Lava
just flows out of the crater and gaps along the side of the
volcano
Types of volcanoes by activity
Active
Dormant
Extinct
Active volcano
Currently erupting or showing regular signs of activity like
earthquakes
and significant
gas emission
Dormant volcano
Has erupted in the past but has entered a long period of
inactivity
Extinct volcano
Has not shown signs of activity for a long period of time and has
no records
of
volcanic eruptions
in the past thousand years
Volcanic
eruptions
Can cause
damage
to plants,
animals
, people, and properties
Volcanic
eruptions
Can also have beneficial effects in
nature
and for
people
Negative effects of volcanic
eruptions
Hot lava flow can burn anything in its path
Mud flow or lahar can cause
landslides
, flooding, and damage to
buildings
and farms
Volcanic ash and dust can irritate
lungs
and cause
health problems
Strong eruptions can trigger
earthquakes
and damage
buildings
Positive effects of volcanic eruptions
Pyroclastic
materials can make soil fertile for
planting
and farming
Geothermal
steam from
fumaroles
can generate electricity
Produce industrial materials like
pumice
and
sulfur
Rocks from
volcanoes
help scientists study the Earth's
interior
Crust
The
outer cool
layer on which we live
Crust
Covered with
landforms
, air and
water
Mantle
The layer
below
the crust
Mantle
Very hot
Consists of rocks in
molten
form
Core
The layer located just below the
Mantle
Core
Divided into two parts:
outer
core (in
liquid
state) and inner core (in solid state)
Metals in the Core
Nickel
Iron
Sometimes, hot melted rocks called
lava
come out to the surface of the earth. Such places are called
volcanoes.
Formation of Earth
1. Very hot
2. Rains and thunderstorms cooled the
outer
portion
3. Different life forms started
originating
Layers of the Earth
Crust
Mantle
Inner Core
Outer Core
Crust
Thin
outer layer of the Earth where we
live
3-5
miles thick in the
ocean floor
25
miles thick on
land
Made of
solid rock
and
minerals
Mantle
Thicker
than the crust at almost
1900
miles deep
Makes up about
85
% of the Earth's weight
Solid rock
but not completely hard
Made of slightly different silicate rocks with more
iron
and
magnesium
Tectonic plates
Combination of the outer
mantle
and the
crust
Move very
slowly
about a couple of inches per year
The place where the plates touch each other is known as the
fault
Tectonic plates move and the boundaries bump up against each other
May cause an
earthquake
Outer Core
Made up of hot liquid
iron
and
nickel
About
1400
miles thick
Creates a
magnetic field
and a
protective barrier
around the Earth
Inner Core
Made up of
solid iron
and
nickel
About
1500
miles thick
As
hot
as the sun's surface, around
9000-13000
degrees Fahrenheit
Earthquakes
are caused by the release of energy that generate waves which travel in all directions causing the
shaking
of earth's surface
Tectonic plates
Jigsaw puzzles of around
19
to
20
pieces that make up the earth
Tectonic plates are placed on a hot partially molten layer of earth's
mantle
, which is the reason why these pieces are
continuously
moving
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