- Info & Contacts
The Global Volcanism Program has no activity reports for Tepi.
The Global Volcanism Program has no Weekly Reports available for Tepi.
The Global Volcanism Program has no Bulletin Reports available for Tepi.
The densely forested Tepi basaltic shield volcano, morphologically unmodified in a region of high rainfall, is capped by prominent cinder cones and small craters. Three satellitic centers are located along an E-W line north of the main shield, whose 2728-m-high summit forms Ethiopia's highest Holocene volcano. Lava flows have traveled down pre-existing valleys. Tepi lies at the northern end of the Turkana rift, about 300 km west of the center of the main Ethiopian rift and was constructed along a zone of ENE-trending faults that extends in line with the Gulf of Aden. Tepi has associated active hot springs and was considered by Davidson (1983) to be of probable Holocene age.
The Global Volcanism Program is not aware of any Holocene eruptions from Tepi. If this volcano has had large eruptions (VEI >= 4) prior to 10,000 years ago, information might be found on the Tepi page in the LaMEVE (Large Magnitude Explosive Volcanic Eruptions) database, a part of the Volcano Global Risk Identification and Analysis Project (VOGRIPA).
This compilation of synonyms and subsidiary features may not be comprehensive. Features are organized into four major categories: Cones, Craters, Domes, and Thermal Features. Synonyms of features appear indented below the primary name. In some cases additional feature type, elevation, or location details are provided.
|Feature Name||Feature Type||Elevation||Latitude||Longitude|
|Bishan Waka||Pit crater|
|The densely forested Tepi basaltic shield volcano lies about 300 km west of the Ethiopian Rift in southern Ethiopia. A small crater near the center of this NASA Landsat image (with north to the top) is one of many satellite features on this broad volcano, whose 2728-m-high summit forms Ethiopia's highest Holocene volcano. Lava flows have traveled down pre-existing valleys. Active hot springs are found on Tepi, Ethiopia's highest Holocene volcano. The smoke plume at the right is from a vegetation fire.
NASA Landsat7 image (worldwind.arc.nasa.gov)
The following references have all been used during the compilation of data for this volcano, it is not a comprehensive bibliography. Discussion of another volcano or eruption (sometimes far from the one that is the subject of the manuscript) may produce a citation that is not at all apparent from the title.
Davidson A, 1983. The Omo River project - reconnaissance geology and geochemistry of parts of Ilubabor, Kefa, Gemu Gofa, and Sidamo, Ethiopia. Ethiopian Inst Geol Surv Bull, 2: 1-89.