Postgrad LIVE! Study Fairs

Birmingham | Edinburgh | Liverpool | Sheffield | Southampton | Bristol

Wellcome Trust Featured PhD Programmes
Imperial College London Featured PhD Programmes
King’s College London Featured PhD Programmes
University of St Andrews Featured PhD Programmes
University of Manchester Featured PhD Programmes

PhD in Geographical and Earth Sciences – Decoding tectonics and climate effects in incipient mountains: the Sierra Nevada (southern Spain) case study


Project Description

This project aims to constrain the evolving topography of mountain belts and to understand how mountains grow. Constraining how topography of mountains change with time, therefore, is crucial for understanding sediment delivery to the basins and changes in atmospheric circulation. Evidence of the early history of mountain belts is limited, both onshore because of poor preservation of the sediments and offshore where the sedimentary record may be incomplete and/or complicated by other processes, such as onshore temporary storage and sediment reworking.

The Sierra Nevada (Spain) began to emerge above sea-level about 10 Myr. The mountain front, especially on the western side, is defined by active normal faults that have generated river knickpoints that propagate upstream, deeply incising the mountain flank. Upstream of the knickpoints, erosion rates are two orders of magnitude lower than in the steep river valleys, creating stable, gently sloping headwaters and mountain tops. It has been suggested that this low-relief morphology represents a relict landscape that is not affected by rapid erosion, because the limited river discharge at high elevations provides insufficient energy for the knickpoints to propagate further. An important implication of this hypothesis is that the plateau-like morphology of the headwaters is a direct result of erosion efficiency and, therefore, of climate. The fact that this morphology is common to many non-glaciated mountains in arid environments supports this hypothesis, which, however, has never been tested.

This project will test the above hypothesis by constraining the spatial variation of erosion rates as the mountain block of Sierra Nevada evolved through time by analysing the sediments of the Granada basin and the deposits of one of the alluvial fans that overlies the Granada Basin using the burial dating technique.

Funding Notes

Funding is available to cover tuition fees for Home/EU students, as well as paying a stipend at the Research Council rate (estimated £14,999 for Session 2019-20).

For a student to be eligible to receive a IAPETUS2 scholarship, they must meet the NERC’s student eligibility criteria (www.rcuk.ac.uk/funding/grantstcs). These criteria requires all students to be UK or EU domiciled, and only allows for EU students to receive a full maintenance grant if they have been resident in the UK for the last 3 years prior to the commencement of the studentship.

Related Subjects

Email Now

Insert previous message below for editing? 
You haven’t included a message. Providing a specific message means universities will take your enquiry more seriously and helps them provide the information you need.
Why not add a message here
* required field
Send a copy to me for my own records.

Your enquiry has been emailed successfully





FindAPhD. Copyright 2005-2018
All rights reserved.