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Updated: Oct 14, 2025

Kinematic History of a Salient-recess Junction Explored through a Combined Approach of Field Data and Analog Sandbox Modeling
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Catching the Main Ethiopian Rift evolving towards plate divergence.

Eugenio Nicotra1, Marco Viccaro2,3, Paola Donato4

  • 1Dipartimento di Biologia Ecologia e Scienze della Terra, Università della Calabria, Arcavacata di Rende, Cosenza, Italy. eugenio.nicotra@unical.it.

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|November 9, 2021
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Magmatism in the Northern Main Ethiopian Rift (NMER) shows a transition from older scoria cones to recent fissure eruptions. This shift indicates increased tensile conditions and magma ascent directly from the crustal base, suggesting mature rifting.

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Area of Science:

  • Geology
  • Geophysics
  • Volcanology

Background:

  • Magmatism is associated with divergent plate boundaries but its role before continental breakup is unclear.
  • The Northern Main Ethiopian Rift (NMER) exhibits magmatism but lacks current volcanism and clear tectono-magmatic links to adjacent rift segments.

Purpose of the Study:

  • To define the magmatic behavior in the NMER.
  • To understand the relationship between eruptive fissures (EF) and monogenetic scoria cones (MSC).
  • To investigate the transition towards mature rifting.

Main Methods:

  • Chemical analysis of basaltic lavas from EF and MSC.
  • Petrographic analysis of volcanic products.
  • Geochemical modeling to infer parental melt composition and magma evolution.

Main Results:

  • Recent EF basalts are aphyric with higher Ti content than older, porphyritic, plagioclase-rich MSC basalts.
  • Both EF and MSC products share a similar parental melt, indicating different evolutionary paths.
  • MSC magmas were stored at intermediate crustal levels, while EF magmas ascended directly from the crustal base without contamination.

Conclusions:

  • The NMER shows a transition from central polygenetic volcanism to linear fissure volcanism.
  • This transition suggests increased tensile conditions and direct magma supply from the crustal base.
  • The observed magmatic behavior indicates a progression towards mature continental rifting.