An integrated approach toward understanding our planet
Main Sustainable Development Goals for the Department of Earth Sciences.

In studying the system Earth and other planets, the Earth Sciences contribute to answers on social and economic questions that concern: 

  • the natural means of existence (water, energy, raw materials),
  • the terrestrial environment (including remediation of pollutions),
  • natural hazards and disasters (such as earthquakes, volcanic eruptions, and floods),
  • and the use of terrestrial space (specifically near surface and underground space).

Through our work, we contribute in particular to 4 of the 17 Sustainable Development Goals as set by the United Nations in 2015.

The Earth Sciences are a multidisciplinary science in which the principles and methods of physics, chemistry, geology, biology, mathematics, and computational sciences are integrated. We specifically develop new scientific hypotheses, methods of data analyses, and experimental and observational techniques that enable us to reconstruct and predict the interactive behaviour of the solid Earth, the biosphere, the hydrosphere, and the atmosphere, on scales ranging from seconds to billions of years, and from nanometers to the entire globe. We honour James Hutton’s early insight that "from what has actually been, we have data for concluding with regard to that which is to happen thereafter".

Our research focus is on 4 major aspects of the natural Earth:

News

Subduction zone
27 August 2018
An international team of Earth scientists showed that subduction zones form because tectonic changes elsewhere start pushing one plate below another.
20 August 2018
Caroline Slomp from Utrecht University presented her awarded Paul Gast Lecture as a plenary at the Goldschmidt Conference on Tuesday 14th August 2018 in Boston.
1 August 2018
The William Gilbert Award 2018 goes to Lennart de Groot and the Jason Morgan Early Career Award 2018 goes to Ylona van Dinther
30 July 2018
With his ERC grant Bijl will reconstruct the role of ocean conditions on fluctuations in the size of the Antarctic ice sheet for past warm climates.

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