MAGMATISM, PARTIAL MELTING, AND TECTONIC SETTING.pptx
The document discusses magma, defined as molten rock beneath the Earth's surface, highlighting its composition, characteristics, and the processes of magmatism. It explains how magma is formed through partial melting due to increased temperature, reduced pressure, and the addition of volatiles. Key objectives include describing magma, identifying its components, and understanding its formation processes.
Magma
I kept myself
Ihid to deep
Burned myself, with my own heat
I must go out, must go with the flow
My red tears shouted pain, as it glows
So as I am, later on it would be tough
I freed my burning self and I'll go reach the top
2
5
OBJECTIVES
Describe thecharacteristics of magma.
Identify the substances/elements
present in magma;
Explain the processes involved in the
formation of magma.
6.
What is magma?
▪is defined as molten rock found below
the earth's surface. It's a Greek word
which means 'thick ointment.’
▪ Magma is found in the magma
chamber of the volcano.
▪ This molten state, when solidified,
creates igneous rocks found on the
surface of the Earth.
6
What is magmatism?
▪is a process under the
earth’s crust where
formation and movement
of magma occur. These
happen in the lower part
of the Earth’s crust and in
the upper portion of the
mantle, known as
asthenosphere. 9
10.
What is magmatism?
▪is a process under the
earth’s crust where
formation and movement
of magma occur. These
happen in the lower part
of the Earth’s crust and in
the upper portion of the
mantle, known as
asthenosphere. 10
11.
How is magmaformed?
▪ The magma present in the lower crust
and upper mantle of the Earth is formed
or generated through the process of
partial melting. In this process, different
minerals in rock melt at different
temperature and pressure.
11
12.
12
The solid rock
containsthe
minerals quartz,
feldspar, biotite,
and hornblende.
The first minerals
that melt are quartz
and some types of
feldspar. The
background
represents magma.
Minerals such as
biotite and hornblende
generally melt last,
which changes the
composition of
magma.
13.
Melting in theMantle
▪ 1. AN INCREASE IN TEMPERATURE:
Conduction in mantle happens when
heat is transferred from hotter molten
rocks to the Earth’s cold crust. As
magma rises, it is often hot enough to
melt the rock it touches. This is called
heat transfer melting. It happens at
convergent boundaries, where
tectonic plates are crashing together. 13
14.
▪ Rocks arecomposed of minerals. These
rocks start to melt once the temperature
in the lower crust and upper mantle
increases or exceeds the melting point
of minerals. The temperature of mantle
is around 1200 degrees Celsius. Rock
minerals such as quartz and feldspar
begin to partially melt at around 650-850
degrees Celsius. 14
Melting in the Mantle
15.
▪ Rocks arecomposed of minerals. These
rocks start to melt once the temperature
in the lower crust and upper mantle
increases or exceeds the melting point
of minerals. The temperature of mantle
is around 1200 degrees Celsius. Rock
minerals such as quartz and feldspar
begin to partially melt at around 650-850
degrees Celsius. 15
Melting in the Mantle
16.
▪ 2. ADECREASE OF PRESSURE:
Mantle rocks remain solid when exposed
to high pressure. However, during
convection, these rocks tend to go
upward (shallower level) and the pressure
is reduced. This triggers the melting of
magma. This is known as
decompression melting. This process
occurs at the Mid-Ocean Ridge, an 16
Melting in the Mantle
17.
Melting in theMantle
▪ 2. A DECREASE OF PRESSURE:
Mantle rocks remain solid when exposed
to high pressure. However, during
convection, these rocks tend to go
upward (shallower level) and the pressure
is reduced. This triggers the melting of
magma. This is known as
decompression melting. This process
occurs at the Mid-Ocean Ridge, an
underwater mountain system. 17
18.
▪ 3. ADDITIONOF VOLATILES:
▪ When water or carbon dioxide is added to
hot rocks, flux melting occurs. The
melting points of minerals within the rocks
decrease. If a rock is already close to its
melting point, the effect of adding these
volatiles can be enough to trigger partial
melting. It occurs around subduction
zones. 18
Melting in the Mantle
19.
▪ 3. ADDITIONOF VOLATILES:
▪ When water or carbon dioxide is added to
hot rocks, flux melting occurs. The
melting points of minerals within the rocks
decrease. If a rock is already close to its
melting point, the effect of adding these
volatiles can be enough to trigger partial
melting. It occurs around subduction
zones. 19
Melting in the Mantle
37
1. What termshould be used to describe a semi-
liquid hot molten rocks located beneath the
Earth?
A. lava C. rocks
B. sand D. magma
2. In what part of the earth does magmatism
happen?
A. Asthenosphere C. Earth’s core
B. Earth’s crust D. Lithosphere
27.
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3. Which ofthe following is NOT a factor of
partial melting?
A. addition of volatiles C. increase in pressure
B. decrease in pressure D. increase in temperature
4. What is the most abundant element in
magma?
A. Oxygen C. Aluminum
B. Silicon D. Iron
28.
39
5. What happensto the temperature of rocks
during partial melting?
A. It decreases.
B. It increases
C. It remains the same
D. All of the above
#4 Give three descriptions about the picture.
What is the material being extruded by Mount Mayon? Where do you think did this material come from?
#7 When magma reaches the earth surface, it changes its name to lava. Magma and lava are both molten rocks. However, they differ in location. Magma is found in the magma chamber of the volcano while lava is found on the surface of earth once the volcano erupts.
#8 Crater - mouth of volcano, varies in shape
Conduit – underground passage thorough which magma travels
Magma Chamber – large underground pool of liquid rock, home of magma
#10 Asthenosphere extends from 100 km to 700 km below the Earth’s surface.
Continental lithosphere has a thickness from about 40 km to 100 km. The upper 30 to 50 km is the crust. Whereas, oceanic lithosphere is typically 50 – 140 thick.
#14 There are three contributing factors why partial melting happens in the mantle.
#19 Flux melting – lowers the melting point of substances
Volatiles -
#20 Flux melting – lowers the melting point of susbtances
#21 Where tectonic plates dive back into the mantle
#24 1. How will you relate these images to magmatism?
#25 1. How will you relate these images to magmatism?
#36 1. How will you relate these images to magmatism?