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Relevant bibliographies by topics / Benue River Valley (Cameroon and Nigeria) / Journal articles

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Journal articles on the topic 'Benue River Valley (Cameroon and Nigeria)'

Author: Grafiati

Published: 4 June 2021

Last updated: 28 July 2025

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1

Wright, David K., Scott MacEachern, Jungyu Choi, Jeong-Heon Choi, Carol Lang, and Jean-Marie Datouang Djoussou. "Iron Age Landscapes of the Benue River Valley, Cameroon." Journal of Field Archaeology 42, no. 5 (2017): 394–407. http://dx.doi.org/10.1080/00934690.2017.1358017.

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2

Berns, Marla C., and Richard Fardon. "Central Nigeria Unmasked: Arts of the Benue River Valley." African Arts 44, no. 3 (2011): 16–37. http://dx.doi.org/10.1162/afar.2011.44.3.16.

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3

Shuaibu, Mohammed Lawal. "British Colonial Marine Transport Services in the Niger-Benue Confluence Area of Nigeria, 1914–1918." ABUAD Journal of Social and Management Sciences 3, no. 1 (2022): 1–11. http://dx.doi.org/10.53982/ajsms.2022.0301.01-j.

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This paper focuses on the British marine transport services in the Niger-Benue confluence area of Nigeria during the First World War. It posits that the flow of the Benue River through the Northern Nigeria/Cameroon border was a major way through which the British war resources were conveyed from the Niger-Benue confluence area to the battlefronts against the German Cameroon. The paper claims that the British authorities used lies as strategy by painting the Germans as land grabbers to get the locals’ commitment and support during the war at the expense of marine transport services. It reveals

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4

Anosike, Jude C., Anthony N. Okere, Bertram E. B. Nwoke, et al. "Endemicity of vesical schistosomiasis in the Ebonyi Benue River valley, South Eastern Nigeria." International Journal of Hygiene and Environmental Health 206, no. 3 (2003): 205–10. http://dx.doi.org/10.1078/1438-4639-00214.

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5

Umar, Nura, and Alison Gray. "A Comparative Study of Time Series and Decision Tree Models for Forecasting Water Levels on the River Benue, Nigeria." UMYU Scientifica 4, no. 2 (2025): 122–34. https://doi.org/10.56919/usci.2542.015.

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The river Benue is vulnerable to flood risks, partly due to the release of water from the Lagdo Dam in Cameroon into Nigeria, as well as high precipitation, resulting in substantial damage and economic losses. Improved flood event prediction is crucial for decision-makers and the population to effectively plan strategies for reducing flood-related losses. This paper presents a comparative study using time series SARIMA and decision tree models applied to monthly water level data for 2011-2016 from Ibi, Makurdi, and Umaisha water stations on the river Benue. Granger causality and correlation te

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6

Oragwa, Arthur Obinna, Faith Chinasa Oragwa, and Daniel Oladimeji Oluwayelu. "Serologic evidence of silent Rift Valley fever virus infection among occupationally exposed persons in northern Nigeria." Journal of Infection in Developing Countries 16, no. 05 (2022): 881–87. http://dx.doi.org/10.3855/jidc.15367.

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Introduction: Rift Valley fever (RVF) is a zoonotic disease caused by RVF virus (RVFV) and transmitted primarily by mosquitoes and contact with fluids and tissues of infected animals. First described in Kenya, it has spread to many African countries and beyond. In humans, it is sometimes misdiagnosed because the symptoms resemble those of influenza and/or malaria. Butchers, abattoir workers, and livestock keepers have the highest risk of infection. Methodology: In this study, serum samples collected between February and September 2019 from 196 individuals comprising of butchers (n = 121)

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7

Salaudeen, A., A. Ismail, B. K. Adeogun, and M. A. Ajibike. "Validating Gauge-based Spatial Surface Atmospheric Temperature Datasets for Upper Benue River Basin, Nigeria." March 2021 5, no. 1 (2021): 173–90. http://dx.doi.org/10.36263/nijest.2021.01.0259.

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Like most other countries of Africa, one of the main problems threatening effective impact modelling in Nigeria including Upper Benue river basin, dwells in lack of high-quality in-situ observation datasets at appropriate spatiotemporal scales. Gridded meteorological variables can serve as promising alternatives to in-situ measurements in data sparse regions, but then, require validations to assess quantitatively their level of accuracies and reliabilities. As a consequence, this study makes comparative analysis of two gauge-based, spatially interpolated surface atmospheric temperature dataset

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8

Ekeu-wei, Iguniwari, George Blackburn, and Philip Pedruco. "Infilling Missing Data in Hydrology: Solutions Using Satellite Radar Altimetry and Multiple Imputation for Data-Sparse Regions." Water 10, no. 10 (2018): 1483. http://dx.doi.org/10.3390/w10101483.

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In developing regions missing data are prevalent in historical hydrological datasets, owing to financial, institutional, operational and technical challenges. If not tackled, these data shortfalls result in uncertainty in flood frequency estimates and consequently flawed catchment management interventions that could exacerbate the impacts of floods. This study presents a comparative analysis of two approaches for infilling missing data in historical annual peak river discharge timeseries required for flood frequency estimation: (i) satellite radar altimetry (RA) and (ii) multiple imputation (M

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9

Mogaji, Hammed Oladeji, Olaitan Olamide Omitola, Adedotun Ayodeji Bayegun, Uwem Friday Ekpo, and Andrew W. Taylor-Robinson. "Livestock Reservoir Hosts: An Obscured Threat to Control of Human Schistosomiasis in Nigeria." Zoonotic Diseases 3, no. 1 (2023): 52–67. http://dx.doi.org/10.3390/zoonoticdis3010006.

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Schistosomiasis is one of the leading neglected tropical diseases in sub-Saharan Africa. Recorded case numbers of this chronic and debilitating helminth disease indicate Nigeria to be the most endemic country within this region. National control efforts have focused intensively on restricting human contact with freshwater sources of intermediate host snails. However, limited attention has been paid to the role of livestock as reservoir hosts and the prevalence of transmission of schistosomes to humans via farmed animals. The West African nations of Mali, Senegal, and the neighbouring Niger, Be

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10

Obiadi, B. N., I. M. Onuorah, P. U. Mbah, C. C. Okafor, and E. I. Kikanme. "Corrupt Government Practices, Regulatory Oversignt, Igorance and Negligence, the Key Factors Affecting Sustainable Urban and Rural Devlopments in Nigeria: Heance, Floodings." International Journal of Research and Scientific Innovation X, no. IX (2023): 39–60. http://dx.doi.org/10.51244/ijrsi.2023.10907.

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Human experiences of the urban spaces have been reshaped by events and how the public domain is framed have produced nagging quests for solutions. These are added to the hitherto baffling situations of how the sustainability of urban and rural spaces have often been affected and on many occasions preculded by the decaying urban fabrics, unplanned physical developments and poor space administration. The 2022 flooding in Nigeria, that partly resulted from corrupt government practices and regulatory oversight have destroyed more lives and properties in the country yet, not enough efforts have bee

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11

Bukar, Shettima, Mohammed Bukar, Asabe Kuku, Bintu Shettima, and Ishaku H. Kamale. "Incised Valley Depositional System of the Cretaceous Yolde Formation of the Gongola Sub-basin Northern Benue Trough N.E. Nigeria." European Journal of Engineering Research and Science 5, no. 8 (2020): 870–76. http://dx.doi.org/10.24018/ejers.2020.5.8.1999.

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This research was carried out in the Gongola Sub-basin of the Northern Benue Trough aimed at deciphering of the paleo-depositional environment of the Yolde Formation based on facies on facies analysis. Six lithofacies were identified to include trough crossbedded sandstone facies (St), massive bedded sandstone facies (Sm), planar crossbedded sandstone facies (Sp), ripple laminated sandstone facies (Sr), parallel sandstone facies (Sl) and mudstone facies (Fm). These build into two facies association of fluvial channel and tidally influenced fluvial channel facies associations. The fluvial succe

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12

Bukar, Shettima, Mohammed Bukar, Asabe Kuku, Bintu Shettima, and Ishaku H. Kamale. "Incised Valley Depositional System of the Cretaceous Yolde Formation of the Gongola Sub-basin Northern Benue Trough N.E. Nigeria." European Journal of Engineering and Technology Research 5, no. 8 (2020): 870–76. http://dx.doi.org/10.24018/ejeng.2020.5.8.1999.

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This research was carried out in the Gongola Sub-basin of the Northern Benue Trough aimed at deciphering of the paleo-depositional environment of the Yolde Formation based on facies on facies analysis. Six lithofacies were identified to include trough crossbedded sandstone facies (St), massive bedded sandstone facies (Sm), planar crossbedded sandstone facies (Sp), ripple laminated sandstone facies (Sr), parallel sandstone facies (Sl) and mudstone facies (Fm). These build into two facies association of fluvial channel and tidally influenced fluvial channel facies associations. The fluvial succe

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13

Parker, John. "Marla C. Berns, Richard Fardon and Sidney Littlefield Kasfir (eds): Central Nigeria Unmasked: Arts of the Benue River Valley. 607 pp. Los Angeles: Fowler Museum at UCLA, 2011. ISBN 978 0 9778344 6 4." Bulletin of the School of Oriental and African Studies 76, no. 1 (2013): 195–97. http://dx.doi.org/10.1017/s0041977x12001917.

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14

"Central Nigeria unmasked: arts of the Benue River valley." Choice Reviews Online 50, no. 02 (2012): 50–0666. http://dx.doi.org/10.5860/choice.50-0666.

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15

Akamba, Gilles Yvans, Joseph Belinga Ateba, and Jean Guy Dzana. "Hydrogeomorphology and flood mapping in the Bénué Plain (North-Cameroon)." Géomorphologie : relief, processus, environnement 31, no. 3 (2025). https://doi.org/10.4000/13a92.

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Hydrogeomorphology makes use of various data notably hydrology and topography, which are necessary to analyse the change in river courses. It lays the foundation of a flood mapping technique done either by delineating the various river beds or by identifying the various features. Following this approach, this paper analyses the flood hazard on the Cameroonian side of the upper Bénué valley, from the Lagdo dam moving downstream to the Bénué-Faro confluence. The uniform geomorphology of this plain and the increasing human dynamics prone to flood occurrence of increasing magnitude, accompanied mo

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