EARTH
SCIENCE!
Magma
I kept myself
I hid 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
MOUNT MAYON
3
MAGMATISM
5
OBJECTIVES
 Describe the characteristics of magma.
 Identify the substances/elements
present in magma;
 Explain the processes involved in the
formation of magma.
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
7
Magma
Chamber
Crater
Conduit
Composition of Magma
▪ Magma is mainly
composed of oxygen
(46.6%) and silicon
(27.7%).
8
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
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
How is magma formed?
▪ 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
The solid rock
contains the
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.
Melting in the Mantle
▪ 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
▪ Rocks are composed 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
▪ Rocks are composed 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
▪ 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 16
Melting in the Mantle
Melting in the Mantle
▪ 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
▪ 3. ADDITION OF 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
▪ 3. ADDITION OF 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
An area
where two
plates meet
where there
is often
earthquake
Subduction Zone
21
22
CONCEPT MAP
Directions: Complete the concept
map about Magmatism. Choose your
answers from the word pool.
23
24
WORD POOL
36
QUIZ
Directions:
Choose the letter of the best answer.
Write the chosen letter on your paper.
37
1. What term should 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
38
3. Which of the 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
39
5. What happens to the temperature of rocks
during partial melting?
A. It decreases.
B. It increases
C. It remains the same
D. All of the above
40
ASSIGNMENT
Use the word
MAGMATISM as an
acronym. Use each letter
to describe your most
favorite person.
M –
A –
G –
M –
A –
T –
I –
S –
M –
QUOTATION
“Look for the heat in your
life. And always be
inspired by that heat to
move forward.”
41
Thank
You!

MAGMATISM, PARTIAL MELTING, AND TECTONIC SETTING.pptx

  • 1.
  • 2.
    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
  • 3.
  • 4.
  • 5.
    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
  • 7.
  • 8.
    Composition of Magma ▪Magma is mainly composed of oxygen (46.6%) and silicon (27.7%). 8
  • 9.
    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
  • 20.
    An area where two platesmeet where there is often earthquake Subduction Zone
  • 21.
  • 22.
    22 CONCEPT MAP Directions: Completethe concept map about Magmatism. Choose your answers from the word pool.
  • 23.
  • 24.
  • 25.
    36 QUIZ Directions: Choose the letterof the best answer. Write the chosen letter on your paper.
  • 26.
    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.
    38 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
  • 29.
    40 ASSIGNMENT Use the word MAGMATISMas an acronym. Use each letter to describe your most favorite person. M – A – G – M – A – T – I – S – M –
  • 30.
    QUOTATION “Look for theheat in your life. And always be inspired by that heat to move forward.” 41
  • 31.

Editor's Notes

  • #3 What is the message of the poem?
  • #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?