Science Lecture Summary, Lecture notes of Earth science

Summary of 1st quarter lessons in Science for grade 10/4th year highschool

Typology: Lecture notes

2021/2022

Available from 01/13/2023

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SCIENCE
1st Quarter
Earth’s Interior
The earth has 3 layers: crust,
mantle, and core.
Crust
2 types of Crust
Continental crust
- Granite is the main rock in
continental crust
Oceanic crust
- thinner and denser than
the continental crust
- Basalt is the rock found in
oceanic crust
Mantle
- is the thickest layer of Earth
Moho - located between the crust
and upper mantle
Lithosphere
- Uppermost mantle + crust
How do scientists know what’s inside
the Earth??
Studying seismic waves
- Waves produced by
earthquakes, machines
or explosions
- P-waves and S-waves
- Bends and changes
speed at interfaces
between different
materials
- Reach different parts of
Earth at different times
Drilling holes
- Kola Hole in Russia - 12
km
Studying materials brought up
to the surface by volcanic
eruptions
Plate Tectonic Theory
Earth’s surface is made up of
separate slabs of rigid rocks
called plates that moves slowly
over Earth's upper mantle, and
are constantly changing in shape
and size.
Each plate may contain
Oceanic crust/ continental
crust/ both
Solid uppermost mantle
Together they consist the
Lithosphere
Separated and interact along
plate boundaries
3 types of Plate Boundaries
Convergent boundaries
- Where to plates are
colliding
Divergent boundaries
- Where two plates are
moving apart
Transform boundaries
- Where plates slide past
each other
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1st Quarter

Earth’s Interior

● The earth has 3 layers: crust, mantle, and core.

Crust

2 types of Crust ● Continental crust

  • Granite is the main rock in continental crust ● Oceanic crust
  • thinner and denser than the continental crust
  • Basalt is the rock found in oceanic crust

Mantle

  • is the thickest layer of Earth ● Moho - located between the crust and upper mantle ● Lithosphere
    • Uppermost mantle + crust How do scientists know what’s inside the Earth?? ● Studying seismic waves
  • Waves produced by earthquakes, machines or explosions
  • P-waves and S-waves
  • Bends and changes speed at interfaces between different materials
  • Reach different parts of Earth at different times ● Drilling holes
  • Kola Hole in Russia - 12 km ● Studying materials brought up to the surface by volcanic eruptions

Plate Tectonic Theory

● Earth’s surface is made up of separate slabs of rigid rocks called plates that moves slowly over Earth's upper mantle, and are constantly changing in shape and size. ● Each plate may contain ❖ Oceanic crust/ continental crust/ both ❖ Solid uppermost mantle ❖ Together they consist the Lithosphere ● Separated and interact along plate boundaries

3 types of Plate Boundaries

➢ Convergent boundaries

  • Where to plates are colliding ➢ Divergent boundaries
  • Where two plates are moving apart ➢ Transform boundaries
  • Where plates slide past each other

1st Quarter

Convergent Boundary

  • towards each other
  • trench
  • volacones can be formed as well as mountains ● Formation of trenches - deep groove due to the bending of oceanic crust ● The denser plate sinks below the buoyant plate ● Oceanic plate sinks below continental crust (O-C) O-C ● Older oceanic crust sinks below younger oceanic crust (O-O) O-O ● Destruction of one of the plates ● When two continental plates of equal density collide, there is no subduction (C-C) C-C ● In oceanic-continental collision, the rising magma forms continental volcanic arc (Andes Mountains) ● In an oceanic-oceanic collision, the rising magma forms island volcanic arc (Mariana Islands) ● In continental-continental collision, a mountain range with no volcanic activity is formed (Himalayas Mountain) ❖ The continental crust are folded, buckled and metamorphosed

Divergent Boundary

Process ● Magma is buoyant and rises up through cracks in the crust ● This causes the crust to spread apart ● An ocean ridge forms as the seafloor spreads apart. (Mid-ocean ridge if it is at the center) ● A long, narrow depression called a rift valley forms ● New oceanic crust is formed as lava fills in the rift valley Occurrences ● Addition of new oceanic crust on both sides of the ridge ● Pushing of older rocks away from the ridge (ridge-push)

1st Quarter

Fuca plate with the Cascadian subduction zone KEY VOCAB WORDS ● Seismic Waves

  • vibrations that travel through Earth carrying the energy released during an earthquake ● Epicenter
  • point on Earth’s surface directly above an earthquake’s focus ● Earthquake
  • sudden and violent movement or trembling of ground caused by release of energy when plates along the fault slide past one another, movements within the earth’s crust or volcanic action ❖ Why isn’t the Earth’s diameter/size increasing if the new crust is being added all the time at the divergent plate boundary?? ➔ It is because of the subduction in divergent boundaries. As they transfer the newly formed oceanic crust, they are slowly moving away from each other. The rate of increase of the earth is also slow because of this.