Details of Award
NERC Reference : NE/I013210/1
Tempo of post-glacial volcanism in southern Chile
Grant Award
- Principal Investigator:
- Professor D Pyle, University of Oxford, Earth Sciences
- Grant held at:
- University of Oxford, Earth Sciences
- Science Area:
- Terrestrial
- Earth
- Overall Classification:
- Earth
- ENRIs:
- Global Change
- Environmental Risks and Hazards
- Science Topics:
- Volcanic Processes
- Quaternary Science
- Geohazards
- Climate & Climate Change
- Abstract:
- The only way to understand what volcanoes might do in the future, is to understand how they have behaved in the past. This project focusses on a large area of southern Chile - one of the most volcanically active regions of the world - in order to try and work out how many times the volcanoes of this area have erupted over the past few thousand years. In this part of Chile, historical records of eruptions only go back to about the early 1800's; and even these are unlikely to be complete. So the only way to find out about older eruptions is look for places where ash and pumice from earlier eruptions is stored: and in Chile, this is mainly in lakes. Many of the volcanoes of southern Chile were covered in ice at the time of the last glaciation (about 20,000 years ago). Many of these mountain glaciers fed long tongues of ice which extended onto the plains in front of (or to the west of) these volcanoes; and as the glaciers retreated, they left behind a series of large, naturally dammed lakes. These lakes have been collecting volcanic ash and other sedimentary rocks for the past 18,000 years. Scientists from Belgium have been collecting long cores of mud from these lakes, and have started to use them to read the records of past climate, and past earthquakes, from the stripy layers of mud. The idea of this new project is to collect the layers of volcanic ash from each of these cores. Then we will try and match them to other examples of the same volcanic ash layer which are either found on land (e.g. near the volcanoes; or in road cuttings; or in peat bogs and marshes; or even in some of the remaining glaciers), or in other lake cores. Once we have started to match the layers (using a combination of factors, such as what they look like and what their composition is), then we will be able to put together a time-map for the region of these major eruptions. At the same time, we will date small samples of carbon (charcoal) to get a better idea of when the eruptions happened. When all of the information is put together, we will have a very detailed record of climate, volcanism and earthquakes in southern Chile, from the end of the last glaciation to the present day. The end result will be that we will be able to see exactly how rates of volcanic activity have changed over the past 18,000 years in southern Chile - and this is what we need, to start to think about how volcanic activity might continue into the future.
- NERC Reference:
- NE/I013210/1
- Grant Stage:
- Completed
- Scheme:
- Standard Grant (FEC)
- Grant Status:
- Closed
- Programme:
- Standard Grant
This grant award has a total value of £494,611
FDAB - Financial Details (Award breakdown by headings)
| DI - Other Costs | Indirect - Indirect Costs | Exception - Other Costs | DA - Investigators | DI - Staff | DA - Estate Costs | Exception - Staff | DI - Equipment | DI - T&S | DA - Other Directly Allocated |
|---|---|---|---|---|---|---|---|---|---|
| £56,873 | £136,076 | £17,184 | £20,317 | £127,398 | £34,779 | £42,425 | £14,889 | £41,616 | £3,057 |
If you need further help, please read the user guide.