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The Seafloor.

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Presentation on theme: "The Seafloor."— Presentation transcript:

1 The Seafloor

2 Types of Crust Two types of crust 1. oceanic 2. continental
Deepest part of ocean is Marianas Trench in Pacific Ocean (just over 11 km deep!)

3 Continental Crust Continental crust is land that we live on and can see

4 Oceanic Crust Oceanic crust is covered by water

5 Ocean Floor Topography
Maps show underwater ridges have deep-sea trenches near them

6 Mid-Ocean Ridges Most common features of the ocean basins
Mid-ocean ridges often have volcanic eruptions and earthquake activity

7 Mid-Ocean Ridges of the World

8 Seafloor Spreading Henry Hess explained data collected Seafloor spreading theory – new ocean crust is formed at ocean ridges and destroyed at deep-sea trenches

9 Seafloor Spreading Magma is less dense than surrounding rocks. It is forced upwards towards the crust along an ocean ridge and fills the gap that is created. When magma hardens, a small amount of new ocean floor is added to Earth’s surface. The sections of ocean floor slowly move away from the ridge.


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