QUESTION IMAGE
Question
- look at the picture on the left. about how long ago did the continents appear this way? ~ 250 million years
- what two pieces of evidence did wegener discover that supported the idea of pangaea?
- what does “pangaea” mean in greek? “all earth”/“all lands”
- what two major landmasses broke apart from pangaea?
- what does the modern theory of plate tectonics state?
- write one observation you made as you completed this activity.
- compare the thickness of continental crust and oceanic crust.
- which type of crust is usually the oldest?
- what is the border between two tectonic plates called?
in the table below, describe each type of boundary and draw a picture of the boundary.
- convergent
- divergent
- transform
Brief Explanations
- The continents have appeared in their current - like form about 250 million years ago due to the process of continental drift.
- Wegener's evidence for Pangaea included the fit of the continents (like puzzle pieces) and the distribution of similar fossils across different continents.
- In Greek, "Pangaea" means "all Earth" or "all land".
- The two major landmasses that broke apart from Pangaea were Laurasia and Gondwana.
- The modern theory of plate tectonics states that the lithosphere is broken into tectonic plates that move constantly, which explains earthquakes, volcanic activity, and the formation of mountains.
- An observation could be that the shapes of the continents can be fitted together to form a super - continent, similar to a jigsaw puzzle.
- Continental crust is thicker (about 30 - 70 km) than oceanic crust (about 5 - 10 km).
- Continental crust is usually the oldest because oceanic crust is constantly being recycled at subduction zones.
- The border between two tectonic plates is called a plate boundary.
- Convergent boundary: Plates move towards each other. Can cause subduction (oceanic - continental or oceanic - oceanic) or mountain building (continental - continental). [A simple drawing could show two plates colliding, with one plate going under the other in the case of subduction or mountains forming in the case of continental - continental collision].
- Divergent boundary: Plates move away from each other. Magma rises to fill the gap, creating new crust. [A simple drawing could show two plates moving apart with magma welling up].
- Transform boundary: Plates slide past each other horizontally. Can cause earthquakes. [A simple drawing could show two plates sliding side - by - side].
Snap & solve any problem in the app
Get step-by-step solutions on Sovi AI
Photo-based solutions with guided steps
Explore more problems and detailed explanations
- About 250 million years ago.
- Fit of continents and fossil distribution.
- "All Earth"/"All land".
- Laurasia and Gondwana.
- The lithosphere is broken into moving tectonic plates.
- Continents can be fitted like a jigsaw puzzle.
- Continental crust is thicker than oceanic crust.
- Continental crust.
- Plate boundary.
- Plates move towards each other; [Drawing description as above].
- Plates move away from each other; [Drawing description as above].
- Plates slide past each other horizontally; [Drawing description as above].