Mapping faults around Adama Town: Implication for future earthquake triggering potential

The unique structural and morphological feature of Adama area studied to infer local paleo-stress direction and to further evaluate their earthquake triggering potential. Kinematic analysis on standard field based structural data performed and integrated with geomorphological results. N 1120 E dire...

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Main Authors: Asfaw Erbello Doelesso, Hassen Shube
Format: Article
Language:English
Published: Adama Science and Technology University 2019-05-01
Series:Ethiopian Journal of Science and Sustainable Development
Subjects:
Online Access:https://ejssd.astu.edu.et/index.php/EJSSD/article/view/51
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spelling doaj-80ba30154b354226bd79ecf6b57104292020-11-25T03:52:05ZengAdama Science and Technology UniversityEthiopian Journal of Science and Sustainable Development1998-05312663-32052019-05-016110.20372/ejssdastu:v6.i1.2019.51Mapping faults around Adama Town: Implication for future earthquake triggering potentialAsfaw Erbello DoelessoHassen Shube The unique structural and morphological feature of Adama area studied to infer local paleo-stress direction and to further evaluate their earthquake triggering potential. Kinematic analysis on standard field based structural data performed and integrated with geomorphological results. N 1120 E directed stress inferred from kinematic analysis technique. The result is statistically similar with the current stress inferred from geophysical monitoring (~ N 1050 E) .The result shows minor deflection to the south. This deflection could be resulted due to crustal strength heterogeneity and /or local stress change. Morphological analysis using stream profile index indicate active fault signatures .These signatures are mainly common in the west of the study area. Integration of structural and geomorphological data mainly from the western side of the town further confirms active fault characteristics. Pilot study on ground cracks around the town shows a significant relationship with faults of the area. This correlation indicate the current tectonic stress of the area has a significant control on the frequently occurring ground cracks in the area https://ejssd.astu.edu.et/index.php/EJSSD/article/view/51Fault kinematics, tectonic stress, paleo-stress, ground crack.
collection DOAJ
language English
format Article
sources DOAJ
author Asfaw Erbello Doelesso
Hassen Shube
spellingShingle Asfaw Erbello Doelesso
Hassen Shube
Mapping faults around Adama Town: Implication for future earthquake triggering potential
Ethiopian Journal of Science and Sustainable Development
Fault kinematics, tectonic stress, paleo-stress, ground crack.
author_facet Asfaw Erbello Doelesso
Hassen Shube
author_sort Asfaw Erbello Doelesso
title Mapping faults around Adama Town: Implication for future earthquake triggering potential
title_short Mapping faults around Adama Town: Implication for future earthquake triggering potential
title_full Mapping faults around Adama Town: Implication for future earthquake triggering potential
title_fullStr Mapping faults around Adama Town: Implication for future earthquake triggering potential
title_full_unstemmed Mapping faults around Adama Town: Implication for future earthquake triggering potential
title_sort mapping faults around adama town: implication for future earthquake triggering potential
publisher Adama Science and Technology University
series Ethiopian Journal of Science and Sustainable Development
issn 1998-0531
2663-3205
publishDate 2019-05-01
description The unique structural and morphological feature of Adama area studied to infer local paleo-stress direction and to further evaluate their earthquake triggering potential. Kinematic analysis on standard field based structural data performed and integrated with geomorphological results. N 1120 E directed stress inferred from kinematic analysis technique. The result is statistically similar with the current stress inferred from geophysical monitoring (~ N 1050 E) .The result shows minor deflection to the south. This deflection could be resulted due to crustal strength heterogeneity and /or local stress change. Morphological analysis using stream profile index indicate active fault signatures .These signatures are mainly common in the west of the study area. Integration of structural and geomorphological data mainly from the western side of the town further confirms active fault characteristics. Pilot study on ground cracks around the town shows a significant relationship with faults of the area. This correlation indicate the current tectonic stress of the area has a significant control on the frequently occurring ground cracks in the area
topic Fault kinematics, tectonic stress, paleo-stress, ground crack.
url https://ejssd.astu.edu.et/index.php/EJSSD/article/view/51
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AT hassenshube mappingfaultsaroundadamatownimplicationforfutureearthquaketriggeringpotential
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