Plate Tectonics
Across
- 1. a boundary in which two plates move apart, resulting in upwelling of material from the mantle to create new seafloor.
- 4. deep canyonlike structure
- 6. a hypothesis, first proposed in the 1960s by Harry Hess, which suggested that new oceanic crust is produced at the crests of mid-ocean ridges, which are the sites of divergence.
- 9. a chain of volcanic islands generally located a few hundred km from a trench where there is active subduction of one oceanic plate beneath another.
- 11. were formed when India “rammed” into Asia.
- 13. an elongated depression
- 15. a hypothesis which suggested that all present continents once existed as a single supercontinent.
- 18. is the primary driving force for movement of tectonic plates.
- 19. supercontinent containing all of the existing continents.
- 20. older, denser portion of oceanic lithosphere descend into mantle at a rate equal to seafloor production.
Down
- 2. wrote a book titled The Origin of Continents and Oceans that outline his continental drift hypothesis.
- 3. processes that deform Earth’s crust to create major structural features, such as mountains, continents, and ocean basins.
- 5. a well-tested theory proposing that Earth’s outer shell consists of individual plates that interact in various ways and thereby produce earthquakes, volcanoes, mountains, and the crust itself.
- 7. linear zone of irregular topography on the deep-ocean floor that follows transform faults and their inactive extensions.
- 8. elevated areas of the seafloor characterized by high heat flow and volcanism.
- 10. occurs when igneous rocks melt over a temp range.
- 12. a boundary in which two plates move together resulting in oceanic lithosphere being thrust beneath an overriding plate, eventually to be reabsorbed into the mantle; could also create a mountain system.
- 14. a boundary in which two plates slide past one another without creating or destroying lithosphere.
- 16. a narrow, elongated depression of the seafloor
- 17. a continuous elevated zone on the floor of all the major ocean basins and varying in width from 500 to 5,000km 300-3,000 miles.