Last modified: 16 Nov 2016 18:26
This course delves into the environmental changes that have occurred since the end of the last ice age 14,000 years ago (the Lateglacial and the Holocene). We will explore the evidence used to reconstruct past environments from proxy records preserved in archives such as peat bogs and the ice cores that suggest that climate and environmental conditions have been far from stable. Our discussion of the evidence will show that the Lateglacial and Holocene are characterised by a series of major but short-lived climatic oscillations as well as permanent transformations as a result of increasing pressure as human population has developed.
|Session||Second Sub Session||Credit Points||15 credits (7.5 ECTS credits)|
This is the total time spent in lectures, tutorials and other class teaching.