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OBJECTIVE:
Describe the
Internal
structure of
the Earth.
(S10ES-Ia-j-36.5)
EARTH’S INTERIOR
SPELLING
TIME!
ASTHENOSPHERE
MANTLE
UPWARD
DENSITY
CONVECTION
CURRENT
OBJECTIVE:
Describe the
process of
Convection
Current in the
mantle.
(S10ES-Ia-j-36.5)
CONVECTION
CURRENT
COMPOSITION OF THE EARTH’S INTERIOR
CRUST
OUTER
CORE
MANTLE
INNER
CORE
40 km
thickness
2900 km
thickness
2200 km
thickness
1278 km
thickness
Illustration above shows the relative thickness of the different layers of the
Earth.
CRUST
CONTINENTAL CRUST
Si, O, Al, Ca, Na,
and K
35-40 kilometers thick
Less dense rocks - Granite
OCEANIC CRUST
7-10 kilometers thick
which its average
thickness is 8
kilometers
Denser rocks - Basalt
MANTLE
MANTLE
Silicate rocks
Extends to about 2900
kilometers from the
Earth’s surface.
Fe, Si, Mg, and O
MANTLE
Lower part of the mantle
consists of more iron than the
upper part.
The lower mantle is denser than
the upper portion.
MANTLE
Beneath the lithosphere lies the
soft, weak layer, made of hot molten
material. Its temperature is about
300 – 800˚C. Facilitates the
movement of the lithospheric plates.
ASTHENOSPHERE
SIMULATING
PLASTICITY
The ability of the
asthenosphere to
flow slowly.
PLASTICITY
QUIZ
TIME!!!
1. What makes up the Lithosphere?
a. Continental crust
b. Crust and the Upper mantle
c. Oceanic and Continental crust
d. Upper mantle
2. It is the ability of the asthenosphere to
flow slowly.
a. Convection current
b. Plasticity
c. Pressure Freezing
d. Subduction
3. The thickest layer of the Earth.
a. Crust
b. Mantle
c. Outer core
d. Inner core
4. What element has the most abundant
percentage in the Earth’s crust?
a. Aluminum
b. Oganesson
c. Oxygen
d. Silicon
5. Soft, weak layer, made of hot molten
material on the upper mantle.
a. Molten Iron and Nickel
b. Magma
c. Lithosphere
d. Asthenosphere
LET’S
CHECK!
1. What makes up the Lithosphere?
a. Continental crust
b. Crust and the Upper mantle
c. Oceanic and Continental crust
d. Upper mantle
2. It is the ability of the asthenosphere to
flow slowly.
a. Convection current
b. Plasticity
c. Plate tectonics
d. Subduction
3. The thickest layer of the Earth.
a. Crust
b. Mantle
c. Outer core
d. Inner core
4. What element has the most abundant
percentage in the Earth’s crust?
a. Aluminum
b. Oganesson
c. Oxygen
d. Silicon
5. Soft, weak layer, made of hot molten
material on the upper mantle.
a. Molten Iron and Nickel
b. Magma
c. Lithosphere
d. Asthenosphere
CORE
Subdivided into 2 Layers:
OUTER CORE
INNER CORE
OUTER CORE
Fe, Ni (molten/liquid)
2900 kilometers below the
Earth’s surface
2250 kilometers thick
2000˚C temperature
OUTER CORE
The outer core is mainly
made up of iron and
nickel moving around the
solid inner core, creating
Earth’s magnetic field
(magnetism).
INNER CORE
Fe, Ni (solid) 1300
kilometers
thick
Iron and nickel are believed to have
solidified as a result of pressure freezing,
which is common to liquids subjected under
tremendous pressure.
5000˚C temperature
What tells us that the
inner core is made up of
iron?
Some clues that the inner core and the outer core
are made up of iron include the following:
 Iron and nickel
are both dense
and magnetic.
Some clues that the inner core and the outer core
are made up of iron include the following:
 The overall density of the
earth is much higher than
the density of the rocks in
the crust. This suggests
that the inside must be
made up of something
denser than rocks.
Some clues that the inner core and the outer core
are made up of iron include the following:
Meteorite analysis have revealed
that the most common type is
chondrite. Chondrite contains iron,
silicon, magnesium and oxygen;
some contains nickel. The whole
earth and the meteorite roughly have
the same density, thus the Earth’s
mantle rock and a meteorite minus
its iron, have the same density.
QUIZ
TIME!!!
1. Miners dig into the Earth in search for
precious rocks and minerals. In which layer
is the deepest explorations made by miners?
a. Crust
b. Mantle
c. Outer core
d. Inner core
2. The layer which is made up of molten
(liquid) Iron and Nickel?
a. Crust
b. Mantle
c. Outer core
d. Inner core
3. Iron and nickel are believed to have
solidified because of under tremendous
pressure which is common to liquids.
a. Convection current
b. Plasticity
c. Pressure Freezing
d. Subduction
4. A layer which is made up of iron and
nickel moving around, creating Earth’s
magnetic field (magnetism).
a. Crust
b. Mantle
c. Outer core
d. Inner core
5. How do you compare the densities of the
Earth’s crust, mantle and core?
a. The mantle is less dense than the core but
denser than the crust.
b. The mantle is less dense than both the core
and the crust.
c. The mantle is denser than the core but less
dense than the crust.
d. The mantle is denser than both the core
and the crust.
LET’S
CHECK!
1. Miners dig into the Earth in search for
precious rocks and minerals. In which layer
is the deepest explorations made by miners?
a. Crust
b. Mantle
c. Outer core
d. Inner core
2. The layer which is made up of molten
(liquid) Iron and Nickel?
a. Crust
b. Mantle
c. Outer core
d. Inner core
3. Iron and nickel are believed to have
solidified because of under tremendous
pressure which is common to liquids.
a. Convection current
b. Plasticity
c. Pressure Freezing
d. Subduction
4. A layer which is made up of iron and
nickel moving around, creating Earth’s
magnetic field (magnetism).
a. Crust
b. Mantle
c. Outer core
d. Inner core
5. How do you compare the densities of the
Earth’s crust, mantle and core?
a. The mantle is less dense than the core but
denser than the crust.
b. The mantle is less dense than both the core
and the crust.
c. The mantle is denser than the core but less
dense than the crust.
d. The mantle is denser than both the core
and the crust.
Here is where your presentation begins
End of the
Lesson
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RESULTS
ANALYSIS
METHODOLOGY
CONCLUSIONS
OBJECTIVES
TABLE OF CONTENTS
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01
03
02
04
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INTRODUCTIO
N
-SOMEONE FAMOUS
“This is a quote, words full of wisdom that
someone important said and can make
the reader get inspired.”
AWESOM
E WORDS
VENUS
MARS
MERCURY
STUDY OBJECTIVES
It’s the closest planet to the
Sun and the smallest one
in the Solar System
Despite being red, Mars is
actually a cold place. It’s
full of iron oxide dust
Venus has a beautiful
name and is the second
planet from the Sun
THEORY 1 THEORY 2
LITERATURE REVIEW
Mercury is the closest planet to
the Sun and the smallest one in
the Solar System. The name
has nothing to do with the liquid
metal
Venus has a beautiful name
and is the second planet from
the Sun. It’s hot and is the
second-brightest natural object
in the night sky
VENUS SATURN MARS
NEPTUN
E
SCHEDULE
01 02 03 04
Venus is the second
planet from the Sun
Saturn is composed of
hydrogen and helium
Despite being red,
Mars is actually a cold
place
Neptune is the farthest
planet from the Sun
METHODOLOGY
Despite being red,
Mars is very cold
Neptune is far away
from Earth
Mercury is the
smallest planet
INFORMATION
DATA STUDY
COMPARISON
THESIS
Saturn is a gas giant
with rings
AUTHORS
RESEAR
CH
ANALYSI
S
TABLE
EARTH
LAYER
DESCRIPTIO
N
DEPTH TEMPERATU
RE
MARS
Despite being red,
Mars is very cold
100 km 1,600 F°
MERCURY
Mercury is the
smallest planet
400 km 3,000 F°
VENUS
Venus has a
beautiful name
5,000 km 4,000 F°
SATURN
Saturn is a gas
giant with rings
10,000 km 9,000 F°
35%
40%
25%
RESULTS ANALYSIS
Saturn is composed of
hydrogen and helium
Despite being red, Mars
is actually a cold place
Neptune is the farthest
planet from the Sun
Follow the link in the graph to modify its data and then
paste the new one here. For more info, click here
MARS
NEPTUN
E
SATURN
MAP
Despite being red,
Mars is cold
Venus is the second
planet from the Sun
Saturn is a gas giant
with rings
MARS
VENUS
SATURN
A PICTURE IS WORTH A
THOUSAND WORDS
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REINFORCES
THE CONCEPT
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MARS
SATURN
NEPTUNE
VENUS
CONCLUSIONS
Despite being red, Mars
is actually a cold place
Neptune is the farthest
planet from the Sun
Saturn is composed of
hydrogen and helium
Venus is the second
planet from the Sun
Big numbers catch your audience’s attention
6,000,000
Is the distance between Earth and the Moon
Earths is the Sun’s mass
333,000
386,000 km
NEPTUNE
MARS
SATURN
VENUS
JUPITER
MERCURY
Jupiter is the biggest
planet of them all
MINERAL CHARACTERISTICS
Mercury is the smallest
planet of them all
Venus is the second
planet from the Sun
Saturn is composed of
hydrogen and helium
Despite being red, Mars is
actually a cold place
Neptune is the farthest
planet from the Sun
BIBLIOGRAPHICAL REFERENCES
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● AUTHOR (YEAR). Title of the publication. Publisher
● AUTHOR (YEAR). Title of the publication. Publisher
● AUTHOR (YEAR). Title of the publication. Publisher
● AUTHOR (YEAR). Title of the publication. Publisher
● AUTHOR (YEAR). Title of the publication. Publisher
● AUTHOR (YEAR). Title of the publication. Publisher
● AUTHOR (YEAR). Title of the publication. Publisher
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Earths Internal Structure for Grade 10 Learners.pptx

  • 3.
  • 4.
  • 11. OBJECTIVE: Describe the process of Convection Current in the mantle. (S10ES-Ia-j-36.5)
  • 13. COMPOSITION OF THE EARTH’S INTERIOR CRUST OUTER CORE MANTLE INNER CORE 40 km thickness 2900 km thickness 2200 km thickness 1278 km thickness Illustration above shows the relative thickness of the different layers of the Earth.
  • 14. CRUST
  • 15. CONTINENTAL CRUST Si, O, Al, Ca, Na, and K 35-40 kilometers thick Less dense rocks - Granite
  • 16. OCEANIC CRUST 7-10 kilometers thick which its average thickness is 8 kilometers Denser rocks - Basalt
  • 17.
  • 19. MANTLE Silicate rocks Extends to about 2900 kilometers from the Earth’s surface. Fe, Si, Mg, and O
  • 20. MANTLE Lower part of the mantle consists of more iron than the upper part. The lower mantle is denser than the upper portion.
  • 21. MANTLE Beneath the lithosphere lies the soft, weak layer, made of hot molten material. Its temperature is about 300 – 800˚C. Facilitates the movement of the lithospheric plates. ASTHENOSPHERE
  • 23. The ability of the asthenosphere to flow slowly. PLASTICITY
  • 25. 1. What makes up the Lithosphere? a. Continental crust b. Crust and the Upper mantle c. Oceanic and Continental crust d. Upper mantle
  • 26. 2. It is the ability of the asthenosphere to flow slowly. a. Convection current b. Plasticity c. Pressure Freezing d. Subduction
  • 27. 3. The thickest layer of the Earth. a. Crust b. Mantle c. Outer core d. Inner core
  • 28. 4. What element has the most abundant percentage in the Earth’s crust? a. Aluminum b. Oganesson c. Oxygen d. Silicon
  • 29. 5. Soft, weak layer, made of hot molten material on the upper mantle. a. Molten Iron and Nickel b. Magma c. Lithosphere d. Asthenosphere
  • 31. 1. What makes up the Lithosphere? a. Continental crust b. Crust and the Upper mantle c. Oceanic and Continental crust d. Upper mantle
  • 32. 2. It is the ability of the asthenosphere to flow slowly. a. Convection current b. Plasticity c. Plate tectonics d. Subduction
  • 33. 3. The thickest layer of the Earth. a. Crust b. Mantle c. Outer core d. Inner core
  • 34. 4. What element has the most abundant percentage in the Earth’s crust? a. Aluminum b. Oganesson c. Oxygen d. Silicon
  • 35. 5. Soft, weak layer, made of hot molten material on the upper mantle. a. Molten Iron and Nickel b. Magma c. Lithosphere d. Asthenosphere
  • 36. CORE Subdivided into 2 Layers: OUTER CORE INNER CORE
  • 37. OUTER CORE Fe, Ni (molten/liquid) 2900 kilometers below the Earth’s surface 2250 kilometers thick 2000˚C temperature
  • 38. OUTER CORE The outer core is mainly made up of iron and nickel moving around the solid inner core, creating Earth’s magnetic field (magnetism).
  • 39. INNER CORE Fe, Ni (solid) 1300 kilometers thick Iron and nickel are believed to have solidified as a result of pressure freezing, which is common to liquids subjected under tremendous pressure. 5000˚C temperature
  • 40. What tells us that the inner core is made up of iron?
  • 41. Some clues that the inner core and the outer core are made up of iron include the following:  Iron and nickel are both dense and magnetic.
  • 42. Some clues that the inner core and the outer core are made up of iron include the following:  The overall density of the earth is much higher than the density of the rocks in the crust. This suggests that the inside must be made up of something denser than rocks.
  • 43. Some clues that the inner core and the outer core are made up of iron include the following: Meteorite analysis have revealed that the most common type is chondrite. Chondrite contains iron, silicon, magnesium and oxygen; some contains nickel. The whole earth and the meteorite roughly have the same density, thus the Earth’s mantle rock and a meteorite minus its iron, have the same density.
  • 44.
  • 45.
  • 46.
  • 47.
  • 49. 1. Miners dig into the Earth in search for precious rocks and minerals. In which layer is the deepest explorations made by miners? a. Crust b. Mantle c. Outer core d. Inner core
  • 50. 2. The layer which is made up of molten (liquid) Iron and Nickel? a. Crust b. Mantle c. Outer core d. Inner core
  • 51. 3. Iron and nickel are believed to have solidified because of under tremendous pressure which is common to liquids. a. Convection current b. Plasticity c. Pressure Freezing d. Subduction
  • 52. 4. A layer which is made up of iron and nickel moving around, creating Earth’s magnetic field (magnetism). a. Crust b. Mantle c. Outer core d. Inner core
  • 53. 5. How do you compare the densities of the Earth’s crust, mantle and core? a. The mantle is less dense than the core but denser than the crust. b. The mantle is less dense than both the core and the crust. c. The mantle is denser than the core but less dense than the crust. d. The mantle is denser than both the core and the crust.
  • 55. 1. Miners dig into the Earth in search for precious rocks and minerals. In which layer is the deepest explorations made by miners? a. Crust b. Mantle c. Outer core d. Inner core
  • 56. 2. The layer which is made up of molten (liquid) Iron and Nickel? a. Crust b. Mantle c. Outer core d. Inner core
  • 57. 3. Iron and nickel are believed to have solidified because of under tremendous pressure which is common to liquids. a. Convection current b. Plasticity c. Pressure Freezing d. Subduction
  • 58. 4. A layer which is made up of iron and nickel moving around, creating Earth’s magnetic field (magnetism). a. Crust b. Mantle c. Outer core d. Inner core
  • 59. 5. How do you compare the densities of the Earth’s crust, mantle and core? a. The mantle is less dense than the core but denser than the crust. b. The mantle is less dense than both the core and the crust. c. The mantle is denser than the core but less dense than the crust. d. The mantle is denser than both the core and the crust.
  • 60. Here is where your presentation begins End of the Lesson
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  • 62. RESULTS ANALYSIS METHODOLOGY CONCLUSIONS OBJECTIVES TABLE OF CONTENTS You can describe the topic of the section here You can describe the topic of the section here You can describe the topic of the section here You can describe the topic of the section here 01 03 02 04
  • 63. You can give a brief description of the topic you want to talk about here. For example, if you want to talk about Mercury, you can say that it’s the smallest planet in the entire Solar System INTRODUCTIO N
  • 64. -SOMEONE FAMOUS “This is a quote, words full of wisdom that someone important said and can make the reader get inspired.”
  • 66. VENUS MARS MERCURY STUDY OBJECTIVES It’s the closest planet to the Sun and the smallest one in the Solar System Despite being red, Mars is actually a cold place. It’s full of iron oxide dust Venus has a beautiful name and is the second planet from the Sun
  • 67. THEORY 1 THEORY 2 LITERATURE REVIEW Mercury is the closest planet to the Sun and the smallest one in the Solar System. The name has nothing to do with the liquid metal Venus has a beautiful name and is the second planet from the Sun. It’s hot and is the second-brightest natural object in the night sky
  • 68. VENUS SATURN MARS NEPTUN E SCHEDULE 01 02 03 04 Venus is the second planet from the Sun Saturn is composed of hydrogen and helium Despite being red, Mars is actually a cold place Neptune is the farthest planet from the Sun
  • 69. METHODOLOGY Despite being red, Mars is very cold Neptune is far away from Earth Mercury is the smallest planet INFORMATION DATA STUDY COMPARISON THESIS Saturn is a gas giant with rings AUTHORS RESEAR CH ANALYSI S
  • 70. TABLE EARTH LAYER DESCRIPTIO N DEPTH TEMPERATU RE MARS Despite being red, Mars is very cold 100 km 1,600 F° MERCURY Mercury is the smallest planet 400 km 3,000 F° VENUS Venus has a beautiful name 5,000 km 4,000 F° SATURN Saturn is a gas giant with rings 10,000 km 9,000 F°
  • 71. 35% 40% 25% RESULTS ANALYSIS Saturn is composed of hydrogen and helium Despite being red, Mars is actually a cold place Neptune is the farthest planet from the Sun Follow the link in the graph to modify its data and then paste the new one here. For more info, click here MARS NEPTUN E SATURN
  • 72. MAP Despite being red, Mars is cold Venus is the second planet from the Sun Saturn is a gas giant with rings MARS VENUS SATURN
  • 73. A PICTURE IS WORTH A THOUSAND WORDS
  • 74. A PICTURE ALWAYS REINFORCES THE CONCEPT You can replace the image on the screen with your own work. Just right-click on it and select “Replace image”
  • 75. MARS SATURN NEPTUNE VENUS CONCLUSIONS Despite being red, Mars is actually a cold place Neptune is the farthest planet from the Sun Saturn is composed of hydrogen and helium Venus is the second planet from the Sun
  • 76. Big numbers catch your audience’s attention 6,000,000
  • 77. Is the distance between Earth and the Moon Earths is the Sun’s mass 333,000 386,000 km
  • 78. NEPTUNE MARS SATURN VENUS JUPITER MERCURY Jupiter is the biggest planet of them all MINERAL CHARACTERISTICS Mercury is the smallest planet of them all Venus is the second planet from the Sun Saturn is composed of hydrogen and helium Despite being red, Mars is actually a cold place Neptune is the farthest planet from the Sun
  • 79. BIBLIOGRAPHICAL REFERENCES ● AUTHOR (YEAR). Title of the publication. Publisher ● AUTHOR (YEAR). Title of the publication. Publisher ● AUTHOR (YEAR). Title of the publication. Publisher ● AUTHOR (YEAR). Title of the publication. Publisher ● AUTHOR (YEAR). Title of the publication. Publisher ● AUTHOR (YEAR). Title of the publication. Publisher ● AUTHOR (YEAR). Title of the publication. Publisher ● AUTHOR (YEAR). Title of the publication. Publisher ● AUTHOR (YEAR). Title of the publication. Publisher ● AUTHOR (YEAR). Title of the publication. Publisher ● AUTHOR (YEAR). Title of the publication. Publisher
  • 80. You can replace the image on the screen with your own work. Just right-click on it and select “Replace image” MOCKUP
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  • 84. RESOURCES Did you like the resources on this template? Get them for free at our other websites: PHOTOS: ● Green tree in front of rocky mountain against blue sky ● Full frame shot of rock VECTORS: ● Earth exploration isometric structure of globe soil layers scientific laboratory geological ● Isometric geology collection with outdoor landscape illustration
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  • 90.
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  • 92. JANUARY FEBRUARY MARCH APRIL MAY JUNE PHASE 1 PHASE 2 Task 1 Task 2 Task 1 Task 2 JANUARY FEBRUARY MARCH APRIL PHASE 1 Task 1 Task 2
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  • 102. Add the title here Text 1 Text 2 Text 3 Text 4 Text 5 Text 6 2016 2017 2018 2019 2020 “Despite being red, Mars is actually a very cold place” “Mercury is closest planet to the Sun and the smallest” “Neptune is the farthest-known planet from the Sun” “Saturn is a gas giant and has several rings” “Venus has a beautiful name and is the second planet” Premium infographics
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Editor's Notes

  1. The Earth’s composition tells a story about itself. It gives us clues to its past and proofs about the gradual and slow changes that it has undergone for over 4.6 billion years.
  2. The crust is the thinnest and the outermost layer of the Earth that extends from the surface to about 32 kilometers below. Underneath some mountains, the crust’s thickness extends to 72 kilometers. The Earth’s crust, as gleaned from Figure, is subdivided into two regions: the continental crust and the oceanic crust.
  3. The continental crust is mainly made up of silicon, oxygen, aluminum, calcium, sodium, and potassium. The thickness of the continental crust is mostly 35-40 kilometers. Continental crust, found under land masses, is made of less dense rocks such as granite. The oceanic crust is around 7-10 kilometers thick which its average thickness is 8 kilometers. It is found under the ocean floor and is made of dense rocks such as basalt. The oceanic crust is heavier than the continental crust. The crust consists of two layers. The upper layer is composed of granite and is only found in the continental crust. Below the granite is a layer made mainly of basalt. This is found on both under the continents and the oceans.
  4. The oceanic crust is around 7-10 kilometers thick which its average thickness is 8 kilometers. It is found under the ocean floor and is made of dense rocks such as basalt. The oceanic crust is heavier than the continental crust. The crust consists of two layers. The upper layer is composed of granite and is only found in the continental crust. Below the granite is a layer made mainly of basalt. This is found on both under the continents and the oceans.
  5. The oceanic crust is around 7-10 kilometers thick which its average thickness is 8 kilometers. It is found under the ocean floor and is made of dense rocks such as basalt. The oceanic crust is heavier than the continental crust. The crust consists of two layers. The upper layer is composed of granite and is only found in the continental crust. Below the granite is a layer made mainly of basalt. This is found on both under the continents and the oceans.
  6. Extends to about 2900 kilometers from the Earth’s surface. It makes up about 80% of the Earth’s total volume and about 68% of its total mass. The mantle is mainly made up of silicate rocks, and contrary to common belief, is solid, since both S-waves and P-waves pass through it.
  7. Extends to about 2900 kilometers from the Earth’s surface. It makes up about 80% of the Earth’s total volume and about 68% of its total mass. The mantle is mainly made up of silicate rocks, and contrary to common belief, is solid, since both S-waves and P-waves pass through it.
  8. This explains that the lower mantle is denser than the upper portion. The temperature and the pressure increase with depth. The high temperature and pressure in the mantle allows the solid rock to flow slowly.
  9. Extends to about 2900 kilometers from the Earth’s surface. It makes up about 80% of the Earth’s total volume and about 68% of its total mass. The mantle is mainly made up of silicate rocks, and contrary to common belief, is solid, since both S-waves and P-waves pass through it.
  10. Extends to about 2900 kilometers from the Earth’s surface. It makes up about 80% of the Earth’s total volume and about 68% of its total mass. The mantle is mainly made up of silicate rocks, and contrary to common belief, is solid, since both S-waves and P-waves pass through it.
  11. Extends to about 2900 kilometers from the Earth’s surface. It makes up about 80% of the Earth’s total volume and about 68% of its total mass. The mantle is mainly made up of silicate rocks, and contrary to common belief, is solid, since both S-waves and P-waves pass through it.
  12. The core is subdivided into two layers: the inner and the outer core.
  13. 2900 kilometers below the Earth’s surface. It is 2250 kilometers thick and is made up of iron and nickel. The temperature in the outer core reaches up to 2000oC at this very high temperature, iron and nickel melt.
  14. 2900 kilometers below the Earth’s surface. It is 2250 kilometers thick and is made up of iron and nickel. The temperature in the outer core reaches up to 2000oC at this very high temperature, iron and nickel melt.
  15. The inner core is made up of solid iron and nickel and has a radius of 1300 kilometers. Its temperature reaches to about 5000˚C. The extreme temperature could have molten the iron and nickel but it is believed to have solidified as a result of pressure freezing, which is common to liquids subjected under tremendous pressure.
  16. The inner core is made up of solid iron and nickel and has a radius of 1300 kilometers. Its temperature reaches to about 5000oC. The extreme temperature could have molten the iron and nickel but it is believed to have solidified as a result of pressure freezing, which is common to liquids subjected under tremendous pressure.
  17. Some clues that the inner core and the outer core are made up of iron include the following.
  18. Some clues that the inner core and the outer core are made up of iron include the following.
  19. Some clues that the inner core and the outer core are made up of iron include the following.