Abstract
Geophysical and geological studies of an Ethiopian maar, Haro Maja, demonstrate that its eruptive history is more complex than surface geology alone suggests. The crater is 750 m by 1000 m in diameter and varies in depth from 70 m to 110 m. A strong magnetic anomaly is caused by a central basaltic mound, but a broader crater-wide anomaly is best modelled by a 50 m thick frozen lava lake, 30 m below the crater floor. The central mound was not erupted directly onto the lava lake, but was extruded onto top of the sedimentary infill after a quiescent depositional interval. Electrical resistivity measurements further indicate that other basaltic intrusions failed to reach the surface during that eruptive period.
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Cole, J. W., 1969,Gariboldi Volcanic Complex, Ethiopia. bull. Volcanol.,33, p. 566–578.
Dakin, F. M., (in prep.),Geology of the Debre Zeit Crater Field.
Di Paola, G. M., 1972,Geology of the Corbetti Caldera (Main Ethiopian Rift Valley). Bull. Volcanol.,35, p. 497–506.
Emilia, D. A. andList, B. J., 1977,A study of Sq Variation at Addis Ababa. J. Atmos. Terr. Phys.,39, p. 375–381.
Gibson, I. L., 1967,Preliminary Account of the Volcanic Geology of Fantale, Shoa. Bull. Geophys. Obs. Addis Ababa,10, p. 59–67.
Gouin, P. andMohr, P. A., 1964,Gravity Traverses in Ethiopia. Bull. Geophys. Obs., Addis Ababa,7, p. 185–239.
Gupta, V. K. andFitzpatrick, M. M., 1971,Evaluation of Terrain Effects in Ground Magnetic Surveys. Geophysics,36, p. 582–589.
Kim, C. K., 1968,Gravity and Magnetic Surveys of the Hole-in-the-Ground Crater, Lake County, Central Oregon. Univ. of Oregon M. S. thesis, 66 pp.
Lorenz, V., 1973,On the Formation of Maars. Bull. Volcanol.,37, p. 183–204.
--,McBirney, A. R. andWilliams, H., 1970,An Investigation of Volcanic Depression, Part III. Maars, Tuff Rings, Tuff Cones, and Diatremes. NASA Progress Report (NGR-38-003-012), Houston, Texas, 198 pp.
Makris, J., Menzel, H. andZimmermann, J., 1972,A Preliminary Interpretation of the Gravity Field of Afar, Northern Ethiopia. Tectonophysics,15, p. 31–39.
Mohr, P. A., 1961,The Geology, Structure, and Origin of the Bishoftu Explosion Craters, Bull. Geophys. Obs. Addis Ababa,2, p. 65–101.
——, 1967,Further Notes on the Explosion Craters of Bishoftu. Bull. Geophys. Obs., Addis Ababa,10, p. 99–112.
Ollier, C. D., 1967,Maars, Their Characteristics, Varieties, and Definition. Bull. Volcanol.,31, p. 45–73.
Searle, R. andGouin, P., 1972,A Gravity Survey of the Central Part of the Ethiopian Rift Valley. Tectonophysics,15, p. 41–52.
Thrall, R., 1975,Gadamsa Caldera, Ethiopia. Bull. Geophys. Obs., Addis Ababa,15, p. 71–82.
Waters, A. C. andFisher, R. V., 1970,Maar Volcanoes, Proc. 2nd Columbia River Basalt Symp. 1969, Cheney, Wash. Eastern Wash. State College Press.
Wood, C. A., 1974,Reconnaissance Geophysics and Geology of the Pinacate Craters, Sonora, Mexico. Bull. Volcanol.,38, p. 149–172.
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Work done while the authors were at Addis Ababa University, Ethiopia.
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Emilia, D.A., Last, B.J., Wood, C.A. et al. Geophysics and geology of an explosion crater in the Ethiopian rift valley. Bull Volcanol 40, 133–140 (1977). https://doi.org/10.1007/BF02596995
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DOI: https://doi.org/10.1007/BF02596995