Browsing by Author "Gaduputi, Sankaranna"

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    Identification of potential groundwater recharge zones at Makutupora basin, Dodoma Tanzania
    (Taylor & Francis, 2021) Mseli, Zaina Hussein; Mwegoha, William John; Gaduputi, Sankaranna
    This paper presents results of identifying potential groundwater recharge zones at the Makutupora basin using GIS and remote sensing techniques. The study was based on integration of seven factors known to contribute towards groundwater existence, namely lineaments and drainage density, elevation, slope, lithology, rainfall, and land use/land cover. For each factor, a thematic layer was prepared, reclassified into five classes, and assigned weight based on its contribution to groundwater existence. All weighted thematic layers were overlaid by the weighted sum analysis method using spatial analyst tool in ArcGIS 10.4® to produce spatial distribution of potential groundwater recharge zones. The potential groundwater recharge zones were classified into five classes, ranging from not suitable to more suitable. This study reveals coverage of potential groundwater recharge as: 2% very good zone, 11% good, 40% average, 45.5% poor, and 1.6% very poor. The Southwest, Northeast, and some small sections of the North of the basin are predominantly between good and very good groundwater recharge potential; while the rest of the basin ranges from poor to very poor. These results have provided some useful information to enable exploration of groundwater wells and foster sustainable planning and use of groundwater resources in this area.
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    The late quaternary eruptive history of Meru volcano, northern Tanzania
    (Elsevier, 2021) Kisaka, Mary; Fontijn, Karen; Shemsanga, Ceven; Tomašek, Ines; Gaduputi, Sankaranna; Debaille, Vinciane; Delcamp, Audray; Kervyn, Matthieu
    Mt. Meru, in the northern Tanzania divergence zone within the East African Rift System, is a historically active volcano, with its last eruption in 1910 CE. The flank deposits of Meru are dominated by lava flows, debris avalanche deposits as well as major pyroclastic formations indicative of Plinian-style eruptions. The stratigraphy, spatial extent, and chronology of these pyroclastic deposits have, however, not been systematically studied. Here we report on the detailed reconstruction of the stratigraphy and eruptive dynamics of Late Quaternary Meru explosive eruptions, based on field investigations, geochronological and geochemical analyses. The findings indicate that Meru had at least three moderate-to-large-scale explosive eruptions over the past 40,000 years. The oldest Meru explosive event we recognize (MXP1) generated pyroclastic density currents (PDCs), while the second (MXP2) and the third, most intense explosive event (MXP3) generated both pyroclastic fallout and PDCs. Conventional radiocarbon dating of 6 palaeosols underlying MXP2 and MXP3, dated at ~34.1–38.5 ka cal BP and ~31.5–36.9 ka cal BP respectively, suggest these two eruptions may have followed each other relatively close in time. The compositional range of pumice lapilli of both MXP2 and MXP3 is limited to tephriphonolite-phonolite. Dispersal and thickness data of the better preserved and larger MXP3 deposits suggest a minimum bulk volume of 2.5 km3 of pumice fallout and 1.2 km3 of PDCs, respectively, which corresponds to a total erupted mass of at least 2.7 × 1012 kg and a magnitude of 5.4. Similar large-scale eruptions in the future would have a considerable impact on the nearby large urban population in Arusha city and its suburbs. This new information is, therefore, vital for the long-term volcanic hazard assessment in Northern Tanzania.