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Journal articles on the topic 'Lower Tchiri Valley (Malawi)'

Author: Grafiati
Published: 4 June 2021
Last updated: 1 February 2022

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1

Bessant, Leslie, and Elias C. Mandala. "Work and Control in a Peasant Economy: A History of the Lower Tchiri Valley in Malawi, 1849-1960." African Economic History, no. 19 (1990): 219. http://dx.doi.org/10.2307/3601929.

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2

McCracken, John, and Elias C. Mandala. "Work and Control in a Peasant Economy: A History of the Lower Tchiri Valley in Malawi, 1859-1960." American Historical Review 97, no. 1 (February 1992): 261. http://dx.doi.org/10.2307/2164682.

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3

Power, Joey, and Elias Mandala. "Work and Control in a Peasant Economy: A History of the Lower Tchiri Valley in Malawi 1859-1960." Canadian Journal of African Studies / Revue Canadienne des Études Africaines 28, no. 2 (1994): 332. http://dx.doi.org/10.2307/485744.

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4

Northrup, Nancy R., and Elias Mandala. "Work and Control in a Peasant Economy: A History of the Lower Tchiri Valley in Malawi, 1859-1960." International Journal of African Historical Studies 25, no. 1 (1992): 137. http://dx.doi.org/10.2307/220150.

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5

Guyer, Jane, and Elias C. Mandala. "Work and Control in a Peasant Economy: A History of the Lower Tchiri Valley in Malawi, 1859-1960." Ethnohistory 39, no. 2 (1992): 236. http://dx.doi.org/10.2307/482423.

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6

Roseberry, William. ": Work and Control in a Peasant Economy: A History of the Lower Tchiri Valley in Malawi, 1859-1960 . Elias C. Mandala." American Anthropologist 94, no. 3 (September 1992): 738. http://dx.doi.org/10.1525/aa.1992.94.3.02a00530.

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7

White, Landeg. "Working Lives in the Lower Shire - Work and Control in a Peasant Economy: A History of the Lower Tchiri Valley in Malawi, 1859–1960. By Elias C. Mandala. Madison, Wisconsin: University of Wisconsin Press, 1990. Pp. xxi+402. $49.50 (paperback $22.50)." Journal of African History 34, no. 1 (March 1993): 158–59. http://dx.doi.org/10.1017/s0021853700033132.

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8

Monjerezi, Maurice, and Cosmo Ngongondo. "Quality of Groundwater Resources in Chikhwawa, Lower Shire Valley, Malawi." Water Quality, Exposure and Health 4, no. 1 (February 24, 2012): 39–53. http://dx.doi.org/10.1007/s12403-012-0064-0.

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9

Mburu, Monicah M., Themba Mzilahowa, Benjamin Amoah, Duster Chifundo, Kamija S. Phiri, Henk van den Berg, Willem Takken, and Robert S. McCann. "Biting patterns of malaria vectors of the lower Shire valley, southern Malawi." Acta Tropica 197 (September 2019): 105059. http://dx.doi.org/10.1016/j.actatropica.2019.105059.

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10

Lumumba Mijoni, Patrick, and Yasamin O. Izadkhah. "Management of floods in Malawi: case study of the Lower Shire River Valley." Disaster Prevention and Management: An International Journal 18, no. 5 (November 6, 2009): 490–503. http://dx.doi.org/10.1108/09653560911003688.

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11

Merelo-Lobo, A. R., P. J. McCall, M. A. Perez, A. A. Spiers, T. Mzilahowa, B. Ngwira, D. H. Molyneux, and M. J. Donnelly. "Identification of the vectors of lymphatic filariasis in the Lower Shire Valley, southern Malawi." Transactions of the Royal Society of Tropical Medicine and Hygiene 97, no. 3 (May 2003): 299–301. http://dx.doi.org/10.1016/s0035-9203(03)90149-0.

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12

Adeloye, A. J., F. D. Mwale, and Z. Dulanya. "A metric-based assessment of flood risk and vulnerability of rural communities in the Lower Shire Valley, Malawi." Proceedings of the International Association of Hydrological Sciences 370 (June 11, 2015): 139–45. http://dx.doi.org/10.5194/piahs-370-139-2015.

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Abstract. In response to the increasing frequency and economic damages of natural disasters globally, disaster risk management has evolved to incorporate risk assessments that are multi-dimensional, integrated and metric-based. This is to support knowledge-based decision making and hence sustainable risk reduction. In Malawi and most of Sub-Saharan Africa (SSA), however, flood risk studies remain focussed on understanding causation, impacts, perceptions and coping and adaptation measures. Using the IPCC Framework, this study has quantified and profiled risk to flooding of rural, subsistent communities in the Lower Shire Valley, Malawi. Flood risk was obtained by integrating hazard and vulnerability. Flood hazard was characterised in terms of flood depth and inundation area obtained through hydraulic modelling in the valley with Lisflood-FP, while the vulnerability was indexed through analysis of exposure, susceptibility and capacity that were linked to social, economic, environmental and physical perspectives. Data on these were collected through structured interviews of the communities. The implementation of the entire analysis within GIS enabled the visualisation of spatial variability in flood risk in the valley. The results show predominantly medium levels in hazardousness, vulnerability and risk. The vulnerability is dominated by a high to very high susceptibility. Economic and physical capacities tend to be predominantly low but social capacity is significantly high, resulting in overall medium levels of capacity-induced vulnerability. Exposure manifests as medium. The vulnerability and risk showed marginal spatial variability. The paper concludes with recommendations on how these outcomes could inform policy interventions in the Valley.
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13

Monjerezi, Maurice, Rolf D. Vogt, Per Aagaard, and John D. K. Saka. "The hydro-geochemistry of groundwater resources in an area with prevailing saline groundwater, lower Shire Valley, Malawi." Journal of African Earth Sciences 68 (June 2012): 67–81. http://dx.doi.org/10.1016/j.jafrearsci.2012.03.012.

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14

Kalua, Khumbo. "The Epidemiology of Trachoma in the Lower Shire Valley of Southern Malawi and Implications for the “SAFE” Strategy." International Journal of TROPICAL DISEASE & Health 4, no. 5 (January 10, 2014): 494–508. http://dx.doi.org/10.9734/ijtdh/2014/7437.

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15

Monjerezi, Maurice, Rolf D. Vogt, Asfaw Gebretsadik Gebru, John D. K. Saka, and Per Aagaard. "Minor element geochemistry of groundwater from an area with prevailing saline groundwater in Chikhwawa, lower Shire valley (Malawi)." Physics and Chemistry of the Earth, Parts A/B/C 50-52 (2012): 52–63. http://dx.doi.org/10.1016/j.pce.2012.08.011.

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16

Mwale, F. D., A. J. Adeloye, and L. Beevers. "Quantifying vulnerability of rural communities to flooding in SSA: A contemporary disaster management perspective applied to the Lower Shire Valley, Malawi." International Journal of Disaster Risk Reduction 12 (June 2015): 172–87. http://dx.doi.org/10.1016/j.ijdrr.2015.01.003.

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17

Monjerezi, Maurice, Rolf D. Vogt, Per Aagaard, Asfaw Gebretsadik Gebru, and John D. K. Saka. "Using 87Sr/86Sr, δ18O and δ2H isotopes along with major chemical composition to assess groundwater salinization in lower Shire valley, Malawi." Applied Geochemistry 26, no. 12 (December 2011): 2201–14. http://dx.doi.org/10.1016/j.apgeochem.2011.08.003.

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18

Monjerezi, Maurice, Rolf D. Vogt, Per Aagaard, and John D. K. Saka. "Hydro-geochemical processes in an area with saline groundwater in lower Shire River valley, Malawi: An integrated application of hierarchical cluster and principal component analyses." Applied Geochemistry 26, no. 8 (August 2011): 1399–413. http://dx.doi.org/10.1016/j.apgeochem.2011.05.013.

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19

MOHAN, JOSEPH, JEFFERY R. STONE, and CHRISTOPHER J. CAMPISANO. "Three novel species of Bacillariophyta (Diatoms) belonging to Aulacoseira and Lindavia from the Pliocene Hadar Formation, Afar Depression of Ethiopia." Phytotaxa 272, no. 4 (September 2, 2016): 235. http://dx.doi.org/10.11646/phytotaxa.272.4.1.

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Paleolake Hadar was an expansive lake in the lower Awash Valley of Ethiopia’s Afar Depression that existed periodically through the Late Pliocene. The sedimentary deposits from this ancient lake (Hadar Formation) have broad importance because a significant number of hominin fossils have been recovered from the formation. Samples of the Hadar Formation lacustrine sequence were collected from sediment cores extracted as part of the Hominin Sites and Paleolakes Drilling Project (HSPDP). A paleoecological study of the HSPDP Northern Awash (Hadar Formation) material has unearthed three novel species of Bacillariophyta (diatoms) from diatomites that appear periodically in the cores. The Hadar Formation assemblage represents a newly revealed excerpt from the evolutionary history of freshwater diatoms in East Africa during the Piacenᴢian age (2.59–3.60 Ma). The HSPDP Northern Awash diatom species are compared to previously reported diatoms from Pliocene outcrops, modern and fossil core material from Lake Malawi, and extant species. Here we describe two new species of Aulacoseira and one of Lindavia. Taxonomic treatment of two diatom varieties reported by previous researchers as Melosira are transferred into Aulacoseira herein.
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20

Schoffeleers, Matthew. "The Zimba and the Lundu State in the Late Sixteenth and Early Seventeenth Centuries." Journal of African History 28, no. 3 (November 1987): 337–55. http://dx.doi.org/10.1017/s0021853700030073.

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This article is a partial answer to M. D. D. Newitt, who proposed that settled Maravi states were established only as a result of the rise of Muzura in the first half of the seventeenth century (cf. J. Afr. Hist., 1982, ii). Newitt thereby challenged the more orthodox view that a formal Maravi state system existed already by the middle of the sixteenth century, if not earlier. It is argued here that the orthodox view is still valid in the case of the Lundu state in the lower Shire valley, and perhaps also in the case of some of the neighbouring states. It is shown that around 1590 the then Lundu incumbent embarked on a course of strong state centralisation during which he appropriated the power of the traditional rain priests and thus became both the secular and the ritual leader of the country. It is also argued that this unusual degree of centralisation was achieved and could for a time be maintained with the help of the Zimba, an army of fugitives from the south bank of the Zambezi. However, the present article challenges Malawian historiographical orthodoxy on a very different point, by maintaining that Muzura is not to be identified with the Kalonga dynasty on the south-western shores of Lake Malawi, but with a separate state system in the western Shire Highlands, which gained prominence well before the Kalongas came to the fore.
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21

"Work and control in a peasant economy: a history of the lower Tchiri Valley in Malawi, 1859-1960." Choice Reviews Online 28, no. 09 (May 1, 1991): 28–5223. http://dx.doi.org/10.5860/choice.28-5223.

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22

"Elias C. Mandala. Work and Control in a Peasant Economy: A History of the Lower Tchiri Valley in Malawi, 1859–1960. Madison: University of Wisconsin Press. 1990. Pp. xxi, 402. Cloth $49.50, paper $22.50." American Historical Review, February 1992. http://dx.doi.org/10.1086/ahr/97.1.261.

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23

Grimason, AM, TK Beattie, SJ Masangwi, GC Jabu, SC Taulo, and KK Lungu. "Classification and quality of groundwater supplies in the Lower Shire Valley, Malawi – Part 2: Classification of borehole water supplies in Chikhwawa, Malawi." Water SA 39, no. 4 (July 10, 2013). http://dx.doi.org/10.4314/wsa.v39i4.17.

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24

Grimason, AM, TD Morse, TK Beattie, SJ Masangwi, GC Jabu, SC Taulo, and KK Lungu. "Classification and quality of groundwater supplies in the Lower Shire Valley, Malawi – Part 1: Physico-chemical quality of borehole water supplies in Chikhwawa, Malawi." Water SA 39, no. 4 (July 10, 2013). http://dx.doi.org/10.4314/wsa.v39i4.16.

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25

Malota, Mphatso, and Joshua Mchenga. "Revisiting dominant practices in floodwater harvesting systems: making flood events worth their occurrence in flood-prone areas." Applied Water Science 10, no. 1 (November 12, 2019). http://dx.doi.org/10.1007/s13201-019-1096-4.

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Abstract The lower Shire valley region in Malawi has long been characterized by floods which have accounted for many fatalities and disaster-related economic losses in the region. Rain-fed crop production has also been adversely affected by such floods, subsequently leading to the region registering the highest levels of poverty in the country due to low agricultural crop production. This study employed both qualitative and quantitative methods and based on what is practiced in the region and elsewhere, recommended strategies that would lower the risk of engaging in crop production under floodwater harvesting. Study results revealed that farmers in the region have sought to dig networks of water ponds and shallow wells as coping strategies to future water scarcity at a scheme level. The absence of well-designed networks of field waterways in the irrigation schemes results in an unequal distribution of floodwaters among field plots. The study concluded that in addition to digging a network of shallow wells and small water ponds to enhance infiltration of floodwaters and increasing groundwater recharge, a resilient and low-risk package of the floodwater harvesting system in the region must also include (1) construction of floodwater diversion structures to increase the chances of flooding even from relatively small rainfall storms, (2) construction of floodwater field distribution channel networks to facilitate field to field distribution of floodwaters, and (3) formulating water distribution rules to enhance equal floodwater distribution among field plots.
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