Africa's ups and downs

The East African Rift is an area where two tectonic plates are moving apart, making it a region of high geological activity, home to a number of volcanoes.

This animation shows how satellite radars – like the one flown on Envisat – can detect surface displacement with centimetre accuracy from an altitude of about 800 km.

Interferometric Synthetic Aperture Radar – or InSAR – is a remote sensing technique where two or more over the same area are combined to detect slight surface changes between them.

Tiny changes on the ground cause changes in the radar signal and lead to rainbow-coloured in the combined image, known as a 'SAR interferogram'. These interferograms can then show how land is uplifting or subsiding.

For example, Envisat found that the dormant Mount Longonot in Kenya rose by 9 cm from 2004 to 2006. Tectonic activity such as the movement of magma underground may have caused this deformation of the surface above.

Radars can also identify fault lines – such as the radar on the Japanese ALOS satellite. Ground displacement following a series of earthquakes around Karonga, Malawi, was detected in the interferogram, revealing details of a fault line. The visualisations are based on results by Juliet Biggs from the University of Bristol in the UK.

Animation of geological activity of the East African Rift as observed by radars on the Envisat and ALOS satellites. This animation is based on a study by Juliet Biggs from the University of Bristol, UK, as part of ESA’s STSE Changing Earth Science Network Initiative. Credit: Planetary Visions/NERC-COMET/JAXA/ESA

Measurements like those seen in this animation are helping scientists to understand plate tectonics. They provide insights into patterns and consequences of activity that can help to get a clearer picture of a volcano's behaviour.


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Citation: Africa's ups and downs (2013, August 8) retrieved 28 February 2020 from https://phys.org/news/2013-08-africa-ups-downs.html
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