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Chapter 10
The Sea Floor and Continental Margins
| Question | Answer |
|---|---|
| What is a continental shelf | The edge of a continent that lies under the ocean |
| Which features CANNOT be observed on a seismic-reflection profile | Orientation of rock layers, shape of the seafloor, folds, and faults |
| What information can be determined directly by analyzing drill cores? | The type of sediment on the seafloor, the type of rock on the seafloor, the rate of sediment deposition. |
| Which of the following is associated with mid-ocean ridges? | As two oceanic plates move apart, solid rock and magma rise to occupy the space between the plates |
| What is an abyssal plane? | An abyssal plain is one that occurs underwater, generally just along the edge of a continent and is almost entirely flat. |
| The deepest parts of the seafloor are | Ocean trenches |
| The shallowest parts of the seafloor are | Mid-ocean ridges |
| What rock type forms oceanic plateaus? | Basalt |
| What do the island chains of Hawaii, Tahiti, and Tristan de Cunha have in common | They formed from hot spots |
| Example of island arc | Japanese islands |
| What processes can occur in front of or behind some island arcs? | A trench rollback or back-arc rifting |
| Island arcs form in association with what type of tectonic setting? | Ocean-ocean convergent |
| Sea formed when subduction jumped or shifted outward from the continent | Bering Sea |
| The Sea of Japan formed as a deep basin between Asia and Japan because of: | Back-arc seafloor spreading |
| What sea was formed by rifting or seafloor spreading? | Red Sea |
| What sea was formed by loading of thrust sheets of the Zagros Mountains? | Persian Gulf |
| Why did the Great Barrier Reef in Australia grow upward, forming the largest organic structure on Earth? | The sea level rose |