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The recent eruption of Ethiopia’s Hayli Gubbi volcano has drawn significant attention in India as its ash plume drifts across the Arabian Sea towards the subcontinent. This guide explains the volcano, the eruption, ash transport, and India’s current measures.
Hayli Gubbi is located in Ethiopia’s Rift Valley, part of the East African Rift System, one of the world’s most active tectonic regions. The volcano sits in a zone where the African Plate is slowly splitting into two:
This rifting causes frequent volcanic activity.
It is a stratovolcano, known for strong ash emissions, explosive eruptions, and the ability to send ash plumes high into the atmosphere. Such volcanoes are common along major rifts and subduction zones.
While detailed scientific studies are ongoing, the eruption is linked to:
These are typical processes for East African Rift volcanoes, which are among the fastest-changing continental plate systems.
Early satellite images show:
Meteorological agencies classify the plume as significant but not catastrophic.
Upper-atmospheric wind patterns over the Arabian Sea are responsible. At this time of year, tropical easterly jets and westerly upper-tropospheric winds can transport ash clouds:
Ethiopia → Arabian Peninsula → Arabian Sea → Western India
This is similar to how dust from the Gulf region occasionally reaches western India.
Based on the IMD and global models, ash is initially seen over western Rajasthan and may move northeastwards, potentially spreading over central India, Delhi, parts of Bihar, northeastern states, and eastern Himalayan regions. Its movement depends on jet stream shifts and wind speed.
Volcanic ash contains sharp, glass-like particles that can:
This is why the DGCA has asked airlines to avoid affected air corridors and maintain safe altitudes.
The Directorate General of Civil Aviation (DGCA) has:
Ash concentration is expected to be very low when it reaches Indian cities. In general, volcanic ash can cause:
In this case, such risk is minimal.
The East African Rift is one of Earth’s major active geological features due to:
Famous volcanoes in the region include Nyiragongo, Erta Ale, Nabro, and Ol Doinyo Lengai.
This eruption demonstrates:
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