Chapter 8 - SchoolRack
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Transcript Chapter 8 - SchoolRack
Chapter 8
VOLCANOES
Section 1 - Volcanic Eruptions
There are two types of volcanic eruptions,
Nonexplosive and Explosive
1) NONEXPLOSIVE ERUPTIONS
When most people think about volcanic eruptions
they think of rivers of red-hot lava (lava flows)
Lava flows come from nonexplosive eruptions
These calm outpourings of lava can release a HUGE
amount of molten rock
Some of the LARGEST mountains in the world
grew from repeated lava flows over hundreds of
thousands of years
2) EXPLOSIVE ERUPTIONS
During this type of eruption clouds of hot debris and gases
SHOOT out of the volcano
This often happens at SUPERSONIC speeds
These eruptions do not produce lava flows
Instead molten rock is blown into millions of pieces that harden
in the air
The dust size particles can circle the Earth for years in the upper
atmosphere
This type of eruption can also blast millions of tons of solid
rock from the volcano itself
In a matter of minutes, an explosive eruption can demolish
rock formations that took thousands of years to build
In this case a volcano will actually shrink instead of grow
Cross Section of a Volcano
All volcanoes share the same basic features
Magma - hot liquid material (rock) that creates
volcanoes
Magma collects underground in Magma Chambers
Some chambers can be up to 160km below the surface
Vents - holes in the Earth through which magma
rises
Lava - magma that erupts and flows onto the Earth’s
surface
Pyroclastic Material - is magma that erupts as
fragments of molten material that solidify in the air
Volcano - a vent or group of vents combined with the
build up of lava and/or pyroclastic material
Magma
By comparing the composition of magma from
different types of eruptions, scientists have
determined that the composition of the magma
dictates whether an eruption will be nonexplosive,
explosive, or somewhere in between
Water
A volcano is more likely to erupt explosively if the magma
has a high water content
The more water there is in magma, the greater the pressure
(like a can of soda) and the greater chance that there will be
a violent eruption
Gases (steam) need more room than liquids (pressure)
Silica - Explosive eruptions are also caused by
magma that contains a large percentage of
silica
Silica rich magma is very thick and has a
tendency to harden inside the volcano
This causes magma and gases to get trapped
inside the volcano until so much pressure builds
up that the volcano goes BOOM !!!!!!
Low silica magma is runny which allows gases
to escape easily, keeping pressure low
What Erupts from a Volcano?
Nonexplosive eruptions produce mostly lava,
while explosive eruptions produce mostly
pyroclastic material
Over many years, a volcano may alternate
between eruptions that produce lava or
pyroclastic material
Eruptions of lava and pyroclastic material may also
occur as separate stages of a single eruption
event
Lava
Lava is magma that flows onto the Earth’s surface
Like magma lava ranges in consistency from thick
to thin
Blocky Lava is cool, stiff lava that cannot travel far
from the erupting vent
Blocky lava forms jumbled heaps of sharp edged chunks
Pahoehoe is lava that flows slowly, like wax
dripping from a candle forming a glassy surface
with round wrinkles that look like “ropes”
Aa is slightly stiffer lava that pours out quickly and
forms a brittle crust that can break and harden
into jagged pieces
Pillow Lava forms when lava erupts underwater
It forms rounded lumps that are the size and shape of
pillows
Pyroclastic Material
Pyroclastic material refers to the rock fragments created by
explosive volcanic eruption and is produced when magma
EXPLODES from a volcano and solidifies in the air. It can
come in a variety of sizes that include:
Volcanic Blocks - are the largest pieces upwards to the size of a
house
Volcanic blocks are large pieces of rock (not magma) from the
mountain
Volcanic Bombs - are large blobs of magma that harden in a
flattened, elongated shape, like a bomb
Volcanic bombs are greater than 64mm in diameter
Lapilli - which means “little stones” in Italian, are pebble like
bits of pyroclastic material between 2 and 64mm in diameter
Volcanic Ash - consist of particles that are less than 2mm in
diameter
Chapter 8 Quiz 1
1) __________ is the hot liquid material found deep
in the ground, and is the driving force that creates
volcanoes
2) __________ are holes in the Earth’s crust in
which the above material (#1) flows
3) __________ includes hot liquid material (#1) and
rock fragments that are BLASTED into the air
4) __________ are large pieces of rock (from the
mountain) that are blasted into the air, and can be
upwards of the size of a house
5)___________ is lava that hardens into jagged
pieces
Bonus) _________ forms when a magma chamber
collapses causing the “roof” above it to collapse
Section 2 - Volcanoes Effects on
Earth
The effects of volcanic eruptions can be seen
both on land (mountains, plateaus, etc.) and
in the air (ash and escaping gases)
Ash and escaping gases can affect global climate
patterns
An Explosive Impact
Because ash and gases can be ejected high into the
air it can have widespread effects on Earth, including
blocking out the sun for days and over thousands of
miles.
Ash can also blow down trees and knock down buildings
Flows - are clouds of hot ash that can flow rapidly
downhill like an avalanche, searing everything in its
path
Large amounts of ash can sometimes mix with water,
turning the flow into the consistency of wet cement
These flows can pick up boulders, trees, and buildings causing
MASSIVE destruction
Fallout - happens when volcanic ash falls back to the
ground
Buildings have been known to collapse under the weight of
accumulating ash
Ash can also dam up river valleys, resulting in MASSIVE
floods
Too much ash can smoother crops causing food shortages
and loss of livestock
Climatic Fluctuation - are changes in global
temperatures and moisture levels due to the release
of ash and sulfur rich gases that reach our upper
atmosphere
Temperature shifts can disrupt climates all over the world
causing milder wetter summers and longer harsher winters
resulting in starvation and disease
Different Types of Volcanoes
There are three basic types of volcanoes:
1) Shield Volcanoes - are volcanoes built out of layers of
lava from repeated nonexplosive eruptions
Because lava is runny it spreads out over a wide area, which
over time builds up to form volcanoes with wide bases and
gently sloping sides
Though their sides are not steep, shield volcanoes can be
enormous and include the largest mountain on Earth, Mauna
Kea in Hawaii
2) Cinder Cone Volcanoes - are small volcanic cones made
entirely of pyroclastic material from moderately explosive
eruptions
These volcanoes have narrow bases and steeper slopes
Cinder cone volcanoes usually erupt for a short period of time
and occur in clusters
These volcanoes erode quickly because the pyroclastic material
of the volcano is not cemented together by lava
3) Composite Volcanoes - form from explosive eruptions of
pyroclastic material, followed by quieter outpourings of lava
These are the most common types of volcanoes and are also known as
stratovolcanoes
These have broad bases and sides that get steeper toward the summit
Craters and Calderas
Crater - is a funnel shaped pit found at the
top of the central vent in most volcanoes
A craters funnels shape results from explosions of
material out of the vent, as well as the collapse of
material from the craters rim back into the vent
Caldera - forms when a magma chamber that
supplies material to a volcano empties and its
roof collapses
This causes the ground to sink, leaving a large
circular depression
Lava Plateaus
Most of the lava on Earth’s continents do
NOT come from volcanoes, but ooze from a
series of long cracks called fissures
Runny lava oozing from fissures can spread out
over thousand of square kilometers forming Lava
Plateau
i.e. The Columbia River Plateau formed about 15 million
years ago
Chapter 8 Quiz 2
1) _________ are clouds of hot ash that can
flow rapidly downhill like an avalanche
2) _________ are built out of layers of lava
from repeated nonexplosive eruptions
3)__________ are also referred to as
Statovolcanoes
4) __________ forms when a magma
chamber empties and its roof collapses
Bonus) _________ are places within tectonic
plates where columns of rising magma are
Section 3 - What Causes
Volcanoes
The Formation of Magma
The key to understanding why volcanoes erupt is
understanding how magma forms
All volcanoes begin when magma collects in pockets in the
deep regions of the Earth’s crust and uppermost layers of
the mantle
The zone of magma formation is between 25 - 160 km below
the surface
Although the rocks of the mantle are hot and pliable, it is
still not a liquid. Why?
The weight of the rock above the mantle exerts so much
PRESSURE that the atoms are forced close together
This increases the melting point (temperature point) at which
the rock will melt
Mantle rock will not melt (turn into magma) until the
temperature increases or the pressure on it releases
Because the temperature of the mantle is fairly constant,
pressure release is the main reason why rock melts
Where Volcanoes Form
Most volcanoes are found on tectonic plate
boundaries
These boundaries are where plates either collide
or separate from each other
The plate boundaries around the Pacific Ocean is called
the RING OF FIRE !!!!!!
At these types of boundaries it is easier for
magma to travel upward through the crust
When Tectonic Plates Separate
As two tectonic plates separate a deep crack, called a
rift, forms
Mantle material is then able to rise up, decreasing
the pressure on it, and causing it to melt and turn
into magma
Magma continuously rises up through the rift creating
new crust
Most divergent boundaries are found under the
oceans where they produce long underwater
mountain chains called mid-ocean ridges
When Tectonic Plates Collide
The place where two tectonic plates collide is called a
convergent boundary
The movement of one plate under another is called a
subduction zone
Convergent boundaries are commonly located where
oceanic plates collide with continental plates
As the oceanic plate slides under the continental
plate it sinks deeper into the mantle causing it to
melt
As the magma rises to the surface it cause the silica
rich continental crust to also melt becoming part of
the gooey lava that can cause an explosive eruption
Hot Spots
Not all magma develops along tectonic plate
boundaries
i.e. The Hawaiian Islands are formed over hot
spots
Hot Spots - are places within tectonic plates
that are directly above columns of rising
magma called mantle plumes