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Question
- what is continental drift theory?
2 - 5. what are the four pieces of evidence of the continental drift theory?
bell work (tuesday)
define/ explain each piece of evidence of the continental drift theory:
1.
2.
3.
4.
bell work (wednesday)
- what causes the movement of the tectonic plates?
- describe the divergent plate boundary.
- describe the convergent plate boundary.
- describe the transform plate boundary.
bell work (thursday)
- what are plates?
2 what is the theory of plate tectonics?
- what are faults in geology?
- what are the three types of convergent boundaries?
bell work (friday)
- give 3 features or products of divergent plate movement.
- give 3 features or products of convergent plate movement.
- what is a hotspot in geology?
- what are 3 types of stress in plate tectonic movements?
- Continental Drift Theory: Proposed by Alfred Wegener, it states that the Earth's continents have moved relative to each other over geological time, seemingly "drifting" across the ocean bed.
2 - 5. Four pieces of evidence of the Continental Drift Theory:
- Fossil Distribution: Similar fossils are found on different continents now separated by oceans, suggesting those continents were once connected. For example, the Mesosaurus fossil is found in South America and Africa.
- Rock - Strata Matching: Identical rock formations and mountain ranges are found on different continents. The Appalachian Mountains in North America match with the Caledonian Mountains in Scotland.
- Paleoclimate Evidence: Evidence of glaciation in areas that are now tropical and coal deposits in areas that are now cold suggest that the continents were once in different positions on the Earth.
- Coastline Fit: The coastlines of some continents, like South America and Africa, appear to fit together like pieces of a jigsaw puzzle.
For Wednesday's Bell Work:
- Movement of tectonic plates: Convection currents in the Earth's mantle cause the movement of tectonic plates. The heat from the Earth's interior makes the semi - molten rock in the mantle move in a circular pattern, which in turn moves the plates above.
- Divergent Plate Boundary: A place where two tectonic plates move away from each other. Magma rises from the mantle to fill the gap, creating new oceanic crust. Mid - ocean ridges are examples of divergent plate boundaries.
- Convergent Plate Boundary: A boundary where two tectonic plates move towards each other. This can result in subduction (where one plate is forced under the other), mountain building, or volcanic activity.
- Transform Plate Boundary: A boundary where two tectonic plates slide past each other horizontally. Earthquakes are common at transform plate boundaries, such as the San Andreas Fault in California.
For Thursday's Bell Work:
- Plates: Tectonic plates are large, rigid slabs of the Earth's lithosphere (the crust and upper mantle) that move relative to one another.
- Theory of Plate Tectonics: It is the scientific theory that describes the large - scale motion of the Earth's lithosphere. It combines the ideas of continental drift and seafloor spreading and explains the formation of mountains, earthquakes, and volcanoes.
- Faults in Geology: A fault is a fracture or zone of fractures between two blocks of rock. Faults allow the blocks to move relative to each other, and this movement can cause earthquakes.
- Three types of convergent boundaries: Ocean - continent convergence (where an oceanic plate subducts under a continental plate), ocean - ocean convergence (where one oceanic plate subducts under another), and continent - continent convergence (where two continental plates collide and form mountains).
For Friday's Bell Work:
- Features of divergent plate movement: Mid - ocean ridges, rift valleys (on land), and volcanic activity.
- Features of convergent plate movement: Mountains (e.g., the Himalayas from continent - continent convergence), volcanic arcs (from ocean - continent or ocean - ocean convergence), and deep - sea trenches (from oceanic subduction).
- Hotspot in Geology: A hotspot is a place in the Earth's mantle where magma rises up in a narrow column. As the tectonic plate moves over the hotspot, a chain of volcanic islands or seamounts can form, like the Hawaiian Islands.
- Three types of stress in plate tectonic movements: T…
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- The Continental Drift Theory states that the Earth's continents have moved relative to each other over geological time.
2 - 5. Fossil distribution, rock - strata matching, paleoclimate evidence, coastline fit.
Wednesday:
- Convection currents in the mantle cause plate movement.
- A place where two plates move away from each other, creating new crust.
- A place where two plates move towards each other, causing subduction, mountain building, or volcanic activity.
- A place where two plates slide past each other horizontally, causing earthquakes.
Thursday:
- Large, rigid slabs of the Earth's lithosphere that move relative to one another.
- The scientific theory that describes the large - scale motion of the Earth's lithosphere.
- A fracture or zone of fractures between two blocks of rock where movement can occur.
- Ocean - continent, ocean - ocean, and continent - continent convergence.
Friday:
- Mid - ocean ridges, rift valleys, volcanic activity.
- Mountains, volcanic arcs, deep - sea trenches.
- A place in the mantle where magma rises in a narrow column, forming volcanic features as the plate moves over it.
- Tension, compression, shear.