Type: | Soil Diffuse Emission |
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Description: | Main Ethiopian Rift (MER) is the Eastern Rift of the East African Rift System (EARS). Degassing in the MER is concentrated in discrete areas of volcanic and off‐edifice activity,and locations of hot springs and fumaroles along the rift show numerous geothermal areas away from volcanic edifices. |
Point of contact for this site:
Tamsin Mather, Tamsin.Mather@earth.ox.ac.uk (Department of Earth Science, University of Oxford)
Measurement | date (d/m/y) | Added by | Added on |
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Habilo-HF1_01062016 | 1/6/2016 | Emanuela Bagnato | May 29, 2020 |
Habilo-HF3_01062016 | 1/6/2016 | Emanuela Bagnato | May 29, 2020 |
Habilo-HF6_01062016 | 1/6/2016 | Emanuela Bagnato | May 29, 2020 |
Hunt Jonathan A., Amdemichael Zafu, Tamsin A. Mather , David M. Pyle, Peter H. Barry, 2017,Spatially variable CO2 degassing in the Main Ethiopian Rift: Implications for magma storage, volatile transport and rift-related emissions, Geochemistry, Geophysics, Geosystems, vol.18, pp. 3714–3737, DOI: https://doi.org/10.1002/2017GC006975