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WELCOME TO
OUR SCIENCE
CLASS!
`
PROCEDURE:
1. Drop a small amount of liquid below their
names.
2. Slowly lift your paper in a slant position.
3. Count 3 seconds and place it on your
arm chair.
4. Observe.
Q1.Which liquid is most viscous? How do
you know?
Q2.Which liquid is least viscous? How do
you know?
Q3.Compare how these liquid flow with
how you think lava flows.
At the end of the discussion, the students can:
a. define viscosity; and
b. identify the type of magma and
its temperature.
√ It is the resistance to flow (opposite of fluidity).
√ It depends primarily on the composition of the
magma, and temperature.
VISCOSITY
Volcanic Eruptions
√ caused by magma expelled
onto the Earth's surface
1. Basaltic magma
Silicon dioxide (SiO2) 45-55 wt%, high in Iron (Fe),
Magnesium (Mg), Calcium (Ca), low in Potassium (K),
Sodium (Na)
2. Andesitic magma
Silicon dioxide (SiO2) 55-65 wt%, intermediate. in
Iron (Fe), Magnesium (Mg), Calcium (Ca), low in Potassium
(K), Sodium (Na)
3. Rhyolitic magma
Silicon dioxide (SiO2) 65-75%, low in Iron (Fe),
Magnesium (Mg), Calcium (Ca) high in Potassium (K),
Sodium (Na).
• Basaltic magma - 1000 to 1200℃
• Andesitic magma - 800 to 1000℃
• Rhyolitic magma - 650 to 800℃
Basaltic magma
Andesitic magma
Rhyolitic magma
• Mostly water vapor & some carbon dioxide
• Minor amounts of Sulfur, Chlorine, and
Fluorine gases
MAGMA TYPE CHEMICAL
COMPOSITION
TEMPERATURE
Basaltic
Magma
Andesitic
Magma
Rhyolitic
Magma
Criteria:
Content 10 pts
Delivery/Presentation 5 pts
Teamwork 5 pts
TOTAL 20 pts
IDENTIFICATION:
____1. It has a temperature of 1000℃ to 1200℃ and with the
composition of Silicon dioxide (SiO2) 45-55 wt %, high in
Iron (Fe), Magnesium (Mg), Calcium (Ca), low in
Potassium (K), Sodium (Na)
___ 2. It is caused by magma that has expelled onto the Earth's
surface.
____3. This magma has a temperature of 650℃ to 800℃.
____4. This describe the resistance to flow (opposite of fluidity)
and depends primarily on the composition of the magma,
and temperature.
____5. What is the important property in determining the eruptive
behaviour of magmas.
:

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JHAM PPT- SESSION 4_1.pptx

  • 2.
  • 3.
  • 4.
  • 5.
  • 6. `
  • 7. PROCEDURE: 1. Drop a small amount of liquid below their names. 2. Slowly lift your paper in a slant position. 3. Count 3 seconds and place it on your arm chair. 4. Observe.
  • 8. Q1.Which liquid is most viscous? How do you know? Q2.Which liquid is least viscous? How do you know? Q3.Compare how these liquid flow with how you think lava flows.
  • 9. At the end of the discussion, the students can: a. define viscosity; and b. identify the type of magma and its temperature.
  • 10. √ It is the resistance to flow (opposite of fluidity). √ It depends primarily on the composition of the magma, and temperature. VISCOSITY
  • 11. Volcanic Eruptions √ caused by magma expelled onto the Earth's surface
  • 12. 1. Basaltic magma Silicon dioxide (SiO2) 45-55 wt%, high in Iron (Fe), Magnesium (Mg), Calcium (Ca), low in Potassium (K), Sodium (Na) 2. Andesitic magma Silicon dioxide (SiO2) 55-65 wt%, intermediate. in Iron (Fe), Magnesium (Mg), Calcium (Ca), low in Potassium (K), Sodium (Na)
  • 13. 3. Rhyolitic magma Silicon dioxide (SiO2) 65-75%, low in Iron (Fe), Magnesium (Mg), Calcium (Ca) high in Potassium (K), Sodium (Na).
  • 14. • Basaltic magma - 1000 to 1200℃ • Andesitic magma - 800 to 1000℃ • Rhyolitic magma - 650 to 800℃
  • 18. • Mostly water vapor & some carbon dioxide • Minor amounts of Sulfur, Chlorine, and Fluorine gases
  • 19.
  • 21. Criteria: Content 10 pts Delivery/Presentation 5 pts Teamwork 5 pts TOTAL 20 pts
  • 22. IDENTIFICATION: ____1. It has a temperature of 1000℃ to 1200℃ and with the composition of Silicon dioxide (SiO2) 45-55 wt %, high in Iron (Fe), Magnesium (Mg), Calcium (Ca), low in Potassium (K), Sodium (Na) ___ 2. It is caused by magma that has expelled onto the Earth's surface. ____3. This magma has a temperature of 650℃ to 800℃. ____4. This describe the resistance to flow (opposite of fluidity) and depends primarily on the composition of the magma, and temperature. ____5. What is the important property in determining the eruptive behaviour of magmas. :