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Endogenic
Processes:
Plutonism and
Volcanism
Lesson 3
What’s New
Read the poem silently, then
identify the properties of magma.
Write your answer on a separate
sheet of paper.
What is Magma?
by: Razel M. Ferrer
Magma is a combination of molten rocks
And gases of the Earth’s mantle and cores
Temperature ranges from 600-1300 degree Celsius
And comprises of mineral mixtures.
Magma varies widely in composition
But in general, only 8 elements are on
Namely oxygen, silicon, aluminum and iron
Potassium, sodium, magnesium and calcium.
The most abundant element in magma is oxygen
Which comprises a little less than half of the
total And over one quarter, followed by silicon
The other one quarter is for other elements in all.
Vast amount of heat causes magma’s temperature to rise
In that case, melting point may reach for some minerals
But pressure also plays an important role as well
For materials to melt partial this way.
Magma’s properties and composition
Are truly impressive and awesome
But what happens after it was formed?
That’s a question, I want to be informed.
Endogenic Process
An endogenic process is a geological process
that was formed, originated, and located below
the surface of the earth. It involves geologic
activities such as tectonic movements,
metamorphism, seismic activities and
magmatism.
How is magma
formed?
Magma
Magma is formed under
certain circumstances in
special location deep in the
crust or in the upper mantle.
Magma forms from partial
melting of mantle rocks.
Rocks undergo partial melting because
the minerals that compose them melt at
different temperature. Partial melting
takes place because rocks are not pure
materials.
As temperature rises, some
minerals melt and others remain
solid. If the same conditions are
maintained at any given
temperature, the same mixture of
solid and melted rock is
maintained.
To understand melting, pressure
is also considered. Pressure
increases with depth as a result
of the increased weight of
overlying rock.
Geologists found out that as they
melted rocks under various
pressures, higher pressure led to
higher melting points.
According to Bayo-ang, et.al (2016), the
two main mechanisms through which
rocks melt are decompression melting
and flux melting.
DECOMPRESSION
Decompression melting
takes place within Earth
when a body of rock is
held at approximately
the same temperature
but the pressure is
reduced.
DECOMPRESSION
This happens because the rock is being
moved toward the surface, either at a mantle
plume (a.k.a., hot spot), or in the upwelling
part of a mantle convection cell.
DECOMPRESSION
If a rock that is hot enough which is close to
its melting point is moved toward the surface,
the pressure is reduced, and the rock can
pass to the liquid side of its melting curve. At
this point, partial melting starts to take place.
Flux melting happens if a
rock is close to its melting
point and some water or
carbon dioxide is added to
the rock, the melting
temperature is reduced and
partial melting starts.
FLUX MELTING
As the magma moves toward the surface,
and especially when it moves from the
mantle into the lower crust, it interacts with
the surrounding rock. This typically
leads to partial melting of the surrounding
rock because most such magmas are
hotter than the melting temperature of a
crustal rock.
Crustal Rock
What happens after
magma is formed?
Cuarto (2016) described that magma
escaped in two forms: intrusion and
extrusion.
Intrusion
An intrusion is magma that moves up into a
volcano without erupting. Like a
balloon, this causes the volcano to grow on
the inside. What is meant by the intrusion of
magma is the inclusion of the rock layers
forming the earth's crust (magma does
not get out).
PLUTONISM
● Plutonism refers to all sorts of igneous geological
activities taking place below the Earth's surface.
● In cases where magma infiltrates the Earth's crust
but fails to make it to the surface, the process of
magma differentiation gives birth to ideal conditions
for metallogenesis and that is a kind of Plutonism.
● This is the exact process that gives birth to
magma, when the presence of various oxides,
fluorine, sulfur, and chlorine compounds that are
necessary for the creation of magma is
guaranteed.
● The solidification and crystallization of magma
takes place mainly inside the Earth's interior.
When the process of crystallization takes place
inside the crust, the magmatic rocks produced are
called plutonites, which is another major category
of igneous rock formation.
Plutonites are igneous rock formations that are
created when the process of crystallization and
solidification of magma takes places below the
Earth's surface and particularly in the crust.
Magma that came out to
the surface of the earth is
called the eruption.
Magma that came to the
surface of the earth is
called lava.
Volcanism
● Volcanism is used to describe all geological
phenomena that occurs on the natural
terrestrial surface, such as the creation of
volcanoes and hot springs. (Grotzinger et.al
,2008)
Volcanism
● It refers to all sorts of geological
activities correlated with the flow and
transportation of igneous material from
the planet's interior towards the natural
terrestrial surface.
EA-L3.pdf................................

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EA-L3.pdf................................

  • 2. What’s New Read the poem silently, then identify the properties of magma. Write your answer on a separate sheet of paper.
  • 3. What is Magma? by: Razel M. Ferrer Magma is a combination of molten rocks And gases of the Earth’s mantle and cores Temperature ranges from 600-1300 degree Celsius And comprises of mineral mixtures. Magma varies widely in composition But in general, only 8 elements are on Namely oxygen, silicon, aluminum and iron Potassium, sodium, magnesium and calcium.
  • 4. The most abundant element in magma is oxygen Which comprises a little less than half of the total And over one quarter, followed by silicon The other one quarter is for other elements in all. Vast amount of heat causes magma’s temperature to rise In that case, melting point may reach for some minerals But pressure also plays an important role as well For materials to melt partial this way.
  • 5. Magma’s properties and composition Are truly impressive and awesome But what happens after it was formed? That’s a question, I want to be informed.
  • 6. Endogenic Process An endogenic process is a geological process that was formed, originated, and located below the surface of the earth. It involves geologic activities such as tectonic movements, metamorphism, seismic activities and magmatism.
  • 7.
  • 9. Magma Magma is formed under certain circumstances in special location deep in the crust or in the upper mantle. Magma forms from partial melting of mantle rocks.
  • 10. Rocks undergo partial melting because the minerals that compose them melt at different temperature. Partial melting takes place because rocks are not pure materials.
  • 11. As temperature rises, some minerals melt and others remain solid. If the same conditions are maintained at any given temperature, the same mixture of solid and melted rock is maintained.
  • 12. To understand melting, pressure is also considered. Pressure increases with depth as a result of the increased weight of overlying rock. Geologists found out that as they melted rocks under various pressures, higher pressure led to higher melting points.
  • 13. According to Bayo-ang, et.al (2016), the two main mechanisms through which rocks melt are decompression melting and flux melting.
  • 14. DECOMPRESSION Decompression melting takes place within Earth when a body of rock is held at approximately the same temperature but the pressure is reduced.
  • 15. DECOMPRESSION This happens because the rock is being moved toward the surface, either at a mantle plume (a.k.a., hot spot), or in the upwelling part of a mantle convection cell.
  • 16. DECOMPRESSION If a rock that is hot enough which is close to its melting point is moved toward the surface, the pressure is reduced, and the rock can pass to the liquid side of its melting curve. At this point, partial melting starts to take place.
  • 17.
  • 18. Flux melting happens if a rock is close to its melting point and some water or carbon dioxide is added to the rock, the melting temperature is reduced and partial melting starts. FLUX MELTING
  • 19. As the magma moves toward the surface, and especially when it moves from the mantle into the lower crust, it interacts with the surrounding rock. This typically leads to partial melting of the surrounding rock because most such magmas are hotter than the melting temperature of a crustal rock.
  • 21. What happens after magma is formed? Cuarto (2016) described that magma escaped in two forms: intrusion and extrusion.
  • 22. Intrusion An intrusion is magma that moves up into a volcano without erupting. Like a balloon, this causes the volcano to grow on the inside. What is meant by the intrusion of magma is the inclusion of the rock layers forming the earth's crust (magma does not get out).
  • 23.
  • 24. PLUTONISM ● Plutonism refers to all sorts of igneous geological activities taking place below the Earth's surface. ● In cases where magma infiltrates the Earth's crust but fails to make it to the surface, the process of magma differentiation gives birth to ideal conditions for metallogenesis and that is a kind of Plutonism.
  • 25. ● This is the exact process that gives birth to magma, when the presence of various oxides, fluorine, sulfur, and chlorine compounds that are necessary for the creation of magma is guaranteed. ● The solidification and crystallization of magma takes place mainly inside the Earth's interior.
  • 26.
  • 27. When the process of crystallization takes place inside the crust, the magmatic rocks produced are called plutonites, which is another major category of igneous rock formation. Plutonites are igneous rock formations that are created when the process of crystallization and solidification of magma takes places below the Earth's surface and particularly in the crust.
  • 28. Magma that came out to the surface of the earth is called the eruption. Magma that came to the surface of the earth is called lava.
  • 29. Volcanism ● Volcanism is used to describe all geological phenomena that occurs on the natural terrestrial surface, such as the creation of volcanoes and hot springs. (Grotzinger et.al ,2008)
  • 30. Volcanism ● It refers to all sorts of geological activities correlated with the flow and transportation of igneous material from the planet's interior towards the natural terrestrial surface.