RSS feed source: USGS Earthquake Hazards Program
Time2025-09-15 00:06:35 UTC2025-09-15 00:06:35 UTC at epicenterLocation53.165°N 160.038°EDepth35.00 km (21.75 mi)
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RSS feed source: USGS Earthquake Hazards Program
Job ID: 262530
Research Fellow (Maritime Studies)
Nanyang Technological University
We are looking for a Research Fellow in Maritime Studies to work in the School of Civil and Environmental Engineering (CEE) at Nanyang Technological University (NTU) with a flexible start time. The appointment is for 1 year with a provision for further extensions, subject to good performance and availability of research funding.
Key Responsibilities:
Conduct research in maritime transport, maritime decarbonisation and digitalisation, methodology development and applications
Publish findings in top peer-reviewed journals and conference proceedings
Collaborate with other researchers on project discussions and joint deliverables
Coordinate the preparation of project reports and deliverables
Support the preparation of research proposals and grant applications
Job Requirements:
Must hold a
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RSS feed source: USGS Earthquake Hazards Program
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RSS feed source: USGS Earthquake Hazards Program
Background:
Volcán Popocatépetl, whose name is the Aztec word for smoking mountain, towers to 5426 m 70 km SE of Mexico City to form North America’s 2nd-highest volcano. The glacier-clad stratovolcano contains a steep-walled, 250-450 m deep crater. The generally symmetrical volcano is modified by the sharp-peaked Ventorrillo on the NW, a remnant of an earlier volcano.
At least three previous major cones were destroyed by gravitational failure during the Pleistocene, producing massive debris-avalanche deposits covering broad areas south of the volcano. The modern volcano was constructed to the south of the late-Pleistocene to Holocene El Fraile cone. Three major plinian eruptions, the most recent of which took place about 800 AD, have occurred from Popocatépetl since the mid Holocene, accompanied by pyroclastic flows and voluminous lahars that swept basins below the volcano. Frequent historical eruptions, first recorded in Aztec codices, have occurred since precolumbian
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