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The Earth in Time

  • M. Vázquez
  • E. Pallé
  • P. Montañés Rodríguez
Chapter
Part of the Astronomy and Astrophysics Library book series (AAL)

Abstract

The history of our planet is 4,500 million years old. During this time, it has undergone multiple changes that have clearly affected its global properties as seen from space. In this chapter, after an introduction on the present structure of the planet, we make a journey from the early days of the Earth to the present day, in its current state of global warming. Dissipation of the internal energy has configured a variable aspect of the surface. Together with the changes in the solar output, the varying concentration of greenhouse gases in the atmosphere has produced several climate changes with different periods and amplitudes. The activities of life, both in the past and in the present, have played an active role in the global evolution of the planet. At the end of the chapter, we stress the importance of the current age, the Anthropocene, in which humans are starting to influence the global environment.

Keywords

Rayleigh Number Continental Crust Mantle Plume Plate Tectonic Benthic Foraminifera 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

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© Springer Science+Business Media, LLC 2010

Authors and Affiliations

  • M. Vázquez
    • 1
  • E. Pallé
    • 1
  • P. Montañés Rodríguez
    • 1
  1. 1.Instituto de Astrofísica de CanariasTenerifeSpain

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