Dodoma, the capital city of Tanzania, lies within the East African Rift System (EARS) prone to earthquake of moderate to strong ground shaking. In the recent years, Dodoma area has been hit by earthquakes with considerable damages to build environments as the case for the magnitude 5.5 earthquakes of November 2002 that induced several cracks to National Parliament building and brought several panics to Tanzanian Members of Parliament who was in the session. By revisiting the geologic setting of Dodoma, earthquake activities and the current technologies for earthquake monitoring in the urban areas, the study proposes the community earthquake monitoring network for Dodoma City and the nearby populations that are currently dwelling in backgr...
The southern East African rift system (EARS) is geologically rare considering its early-stage contin...
International audienceWell-constrained earthquake depth estimations are important for seismic hazard...
In lieu of comprehensive instrumental seismic monitoring, short historical records, and limited faul...
This paper presents the seismic hazard levels for the Northern Tanzania Divergence (NTD) and adjoini...
The Dodoma area (Tanzania) lies within the Tanzanian craton, in a region where the eastern branch of...
This work presents the evaluation of earthquake resistance of the Arusha International ConferenceCen...
The study was carried out to understand the risks posed by earthquakes in Karonga based on roles and...
Dodoma, the capital of Tanzania, was hit by a 5.5 magnitude (Mw) eathquake during a parliamentary se...
The central part of Tanzania, Dodoma, was hit by an Mw= 5.5 earthquake in November 4, 2002. It was p...
In November 4, 2002, an earthquake of Mb = 5.5 struck Dodoma, the capital city of Tanzania, in Centr...
Temporary broadband seismic networks deployed from 2007 to 2011 around the Afar triple junction of t...
Uganda is situated between the two seismically active branches of the East African Rift Valley Syste...
To cope with earthquakes, resistant housing is crucial. Too often essential construction techniques ...
Earthquakes of low to intermediate magnitudes are a commonly observed feature of continental rifting...
This article establishes existing knowledge on earthquakes and coping mechanisms employed in reducin...
The southern East African rift system (EARS) is geologically rare considering its early-stage contin...
International audienceWell-constrained earthquake depth estimations are important for seismic hazard...
In lieu of comprehensive instrumental seismic monitoring, short historical records, and limited faul...
This paper presents the seismic hazard levels for the Northern Tanzania Divergence (NTD) and adjoini...
The Dodoma area (Tanzania) lies within the Tanzanian craton, in a region where the eastern branch of...
This work presents the evaluation of earthquake resistance of the Arusha International ConferenceCen...
The study was carried out to understand the risks posed by earthquakes in Karonga based on roles and...
Dodoma, the capital of Tanzania, was hit by a 5.5 magnitude (Mw) eathquake during a parliamentary se...
The central part of Tanzania, Dodoma, was hit by an Mw= 5.5 earthquake in November 4, 2002. It was p...
In November 4, 2002, an earthquake of Mb = 5.5 struck Dodoma, the capital city of Tanzania, in Centr...
Temporary broadband seismic networks deployed from 2007 to 2011 around the Afar triple junction of t...
Uganda is situated between the two seismically active branches of the East African Rift Valley Syste...
To cope with earthquakes, resistant housing is crucial. Too often essential construction techniques ...
Earthquakes of low to intermediate magnitudes are a commonly observed feature of continental rifting...
This article establishes existing knowledge on earthquakes and coping mechanisms employed in reducin...
The southern East African rift system (EARS) is geologically rare considering its early-stage contin...
International audienceWell-constrained earthquake depth estimations are important for seismic hazard...
In lieu of comprehensive instrumental seismic monitoring, short historical records, and limited faul...