Detecting Transient Uplift at the Active Volcano Ol Doinyo Lengai in Tanzania With the TZVOLCANO Network

Author:

Daud Ntambila12ORCID,Stamps D. Sarah1ORCID,Ji Kang‐Hyeun3ORCID,Saria Elifuraha2,Huang Mong‐Han4ORCID,Adams Aubreya5ORCID

Affiliation:

1. Department of Geosciences Virginia Tech Blacksburg VA USA

2. Department of Geospatial Sciences and Technology Ardhi University Dar Es Salaam Tanzania

3. Korea Institute for Geoscience and Mineral Resources Daejeon South Korea

4. Department of Geology University of Maryland College Park MD USA

5. Department of Earth and Environmental Geosciences Colgate University Hamilton NY USA

Abstract

AbstractOver the last 7 years, geodetic data have detected periods of uplift and subsidence of the active volcano Ol Doinyo Lengai in Tanzania. Although numerous eruptions of the volcano have occurred historically, a systematic investigation of transient deformation using continuous Global Navigation Satellite System (GNSS) data has not been undertaken. We use the Targeted Projection Operator (TPO) to assess 7 years of continuous GNSS data from the TZVOLCANO network for transient signals and find rapid uplift spanning March 2022–December 2022 and then steady‐state uplift through August 2023. We conduct a nonlinear inversion of the GNSS velocities associated with the transient signal using dMODELS and find consistency with an inflating spheroidal source located 2.3 ± 0.6 km beneath the crater. Prior to March 2022, geodetic data indicated quiescence just below Ol Doinyo Lengai, thus detecting transient deformation with TPO allows for tracking changes in the magmatic system over time in the Natron Rift.

Funder

National Science Foundation

Ministry of Science and ICT, South Korea

Virginia Polytechnic Institute and State University

Korea Institute of Geoscience and Mineral Resources

Publisher

American Geophysical Union (AGU)

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