Tibet: the geological history

Update: 2008-09-03

Description

A look at the geological history of Tibet and the Raymo Ruddiman hypothesis; that chemical weathering increased as the temperature dropped due to the rise in the plateau. Raymo and Ruddiman believed that the uplift of the Himalayas caused global cooling.

Comments

In Channel

Earth and Life

2010-04-1200:54

Daisyworld: James Lovelock and Gaia

2008-09-0302:39

Daisyworld: Gaia and Daisyworld

2008-09-0306:44

Daisyworld: Self regulation

2008-09-0307:27

Daisyworld: Gaia theory and the real world

2008-09-0306:21

Tibet: the Raymo-Ruddiman Hypothesis

2008-09-0305:57

Tibet: Berner's model of the carbon cycle

2008-09-0303:13

Tibet: the geological history

2008-09-0304:53

Tibet: The signifiicance of the strontium ratio

2008-09-0303:38

Tibet: evidence for and against the Raymo- Ruddiman Hypothesis

2008-09-0304:37

Tibet: Field trip conclusions

2008-09-0300:54

Volcanoes: eruptions and climatic effects

2008-09-0303:21

Volcanoes: How eruptions affect climate

2008-09-0301:10

Volcanoes: Historic eruptions and their climatic effects

2008-09-0303:23

Volcanoes: Effects of magma eruptions

2008-09-0302:34

Volcanoes: Flood Basalt and itys effects

2008-09-0307:19

Volcanoes: eruptions and mass extinctions

2008-09-0302:36

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Tibet: the geological history

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Tibet: the geological history

The Open University

Tibet: the geological history