Lecture10
Table of Contents
- Motion Inside Earth
- Why study Earth's internal motion?
- Why study Earth's internal motion?
- Why study Earth's internal motion?
- Why study Earth's internal motion?
- Why study Earth's internal motion?
- Why study Earth's internal motion?
- Why study Earth's internal motion?
- Why study Earth's internal motion?
- Why study Earth's internal motion?
- 10.1 How does convection work?
- Convection
- 10.1 How does convection work?
- 10.1 How does convection work?
- 10.1 How does convection work?
- 10.1 How does convection work?
- 10.1 How does convection work?
- 10.1 How does convection work?
- 10.2 What does mantle convection look like?
- 10.2 What does mantle convection look like?
- 10.2 What does mantle convection look like?
- 10.2 What does mantle convection look like?
- 10.2 What does mantle convection look like?
- 10.2 What does mantle convection look like?
- 10.2 What does mantle convection look like?
- 10.2 What does mantle convection look like?
- 10.2 What does mantle convection look like?
- 10.3 How does outer-core convection generate the magnetic field?
- 10.3 How does outer-core convection generate the magnetic field?
- 10.3 How does outer-core convection generate the magnetic field?
- 10.3 How does outer-core convection generate the magnetic field?
- 10.3 How does outer-core convection generate the magnetic field?
- 10.3 How does outer-core convection generate the magnetic field?
- 10.3 How does outer-core convection generate the magnetic field?
- 10.3 How does outer-core convection generate the magnetic field?
- 10.4 How do we know ... Earth's core is a dynamo?
- 10.4 How do we know ... Earth's core is a dynamo?
- 10.4 How do we know ... Earth's core is a dynamo?
- 10.4 How do we know ... Earth's core is a dynamo?
Text and Images from Slide
10.2 What does mantle convection look like?
- Convection and decompressive melting are what generate magma
- Convecting hot rock that cools only slightly can get to a pressure low enough to allow it to melt while rock around it at similar temperature (but differing composition) remains solid.