Environmental Change on Geological Timescales
Course, Master's level, 1GE055
Expand the information below to show details on how to apply and entry requirements.
Autumn 2025
Autumn 2025,
Uppsala, 33%, On-campus, English
- Location
- Uppsala
- Pace of study
- 33%
- Teaching form
- On-campus
- Instructional time
- Daytime
- Study period
- 1 September 2025–2 November 2025
- Language of instruction
- English
- Entry requirements
-
120 credits with 90 credits in earth science and Dynamics of Earth Systems - Global Chang, 10 credits. Proficiency in English equivalent to the Swedish upper secondary course English 6.
- Selection
-
Higher education credits in science and engineering (maximum 240 credits)
- Fees
-
If you are not a citizen of a European Union (EU) or European Economic Area (EEA) country, or Switzerland, you are required to pay application and tuition fees.
- First tuition fee instalment: SEK 12,083
- Total tuition fee: SEK 12,083
- Application deadline
- 15 April 2025
- Application code
- UU-18126
Admitted or on the waiting list?
- Registration period
- 25 July 2025–31 August 2025
- Information on registration from the department
Autumn 2025
Autumn 2025,
Uppsala, 33%, On-campus, English
For exchange students
- Location
- Uppsala
- Pace of study
- 33%
- Teaching form
- On-campus
- Instructional time
- Daytime
- Study period
- 1 September 2025–2 November 2025
- Language of instruction
- English
- Entry requirements
-
120 credits with 90 credits in earth science and Dynamics of Earth Systems - Global Chang, 10 credits. Proficiency in English equivalent to the Swedish upper secondary course English 6.
Admitted or on the waiting list?
- Registration period
- 25 July 2025–31 August 2025
- Information on registration from the department
About the course
The transition to Quaternary ice age conditions is marked by numerous major climatic changes. This course considers debates about the nature and forcing of these fundamental shifts in the Earth system over multi-millennial and tectonic timescales. We will discuss and engage in environmental change reconstruction using studies of key long-term archives such as loess and marine sediments as well as consider the proposed tectonic forcing mechanisms that shape our current climate epoch.