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PANGANI BASIN WATER BOARD

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C.2 Industrial interests<br />

Probably the largest industrial interest in the Pangani River Basin (PRB) is power generation. The main<br />

supplier in this regard is the state-owned Tanzania Electric Supply Co. [sic.] (TANESCO), which owns<br />

four hydropower facilities on the Pangani River. These are Nyumba ya Mungu (NYM) (with an 8 MW<br />

capacity), Hale (21 MW), and New Pangani Falls (68 MW. All the power plants are connected to the<br />

national grid and they contribute about 17% to the total hydropower production of the country (Ngula,<br />

2002). The firm discharge through the power plants is about 24 m 3 /s, whereas the maximum designed<br />

discharge is 45 m 3 /s. Old Pangani (17.5 MW) operates only occasionally, crippled by lack of adequate<br />

water (Lugeiyamu, pers. comm.).<br />

In the dry season, water shortages may cause power generation within the basin to drop to as low as 32<br />

MW (Sarmett and Kamugisha, 2002).<br />

There are extensive mining interests in the Pangani River Basin. These include tin mining in Korogwe,<br />

tanzanite and phosphate mines in the Arusha Region, and limestone mines in the Tanga Region (Mkuula,<br />

1993). Genstones are also an important quest, and 80% of the world’s known tanzanite reserves are to<br />

be found at Merelani, 100 km northeast of Arusha. Sand mining for building purposes is common along<br />

riverbanks, and in Kenyan parts of the Basin, ruby mining is carried out.<br />

Other industry within the basin is that associated with farming, such as sugar refineries and sisal<br />

processing plants. In Kenya’s Taita – Taveta District, sisal production is the main agricultural activity.<br />

C. 3 Farming interests<br />

The Chagga peoples have lived on Mt. Kilimanjaro’s slopes for between 300 – 450 years. Their farmland<br />

is divided into two types of tenure. The first is ‘shamba’, and is typically restricted to the lower slopes of<br />

the mountain where rainfall is much less reliable, and irrigation commensurately more important. The<br />

use of shamba land was overseen by Chagga chiefs, who would allocate parcels of land to farmers on<br />

a seasonal basis. While a farmer might exploit the land for a long period of time, it was never his to own<br />

(Johnston, 1946). The second type of Chagga land tenure is the ‘kihamba’, which was set aside for the<br />

private use of Chagga denizens. Kihamba was – and still is – farmed with remarkable intensity. Even<br />

in the 1940s, at the time of Johnston’s (1942) writing, there was very little kihamba land left that could<br />

be used as pasture, and most livestock was stall-fed. In those areas where farming intensities became<br />

too high, and no additional kihamba land was available, Chagga chiefs were obliged to convert shamba<br />

land to kihamba. In effect, this gesture served to siphon off excess farming from the upper slopes to the<br />

lower slopes of the mountain. The Chagga could not expand up the mountain because this was already<br />

set aside as forest reserve, and they could not expand into the middle slope areas because this was<br />

‘alienated’ land for European settlers (Lein, 2002).<br />

Against this background of high farming intensity, the Chagga devised furrow systems to deliver water<br />

from natural watercourses to their crops. This system is said to be one of the oldest (thought to have<br />

started in the 18 th Century (Gillingham, 1999)) and most extensive furrowbased irrigation systems in<br />

Africa (Røhr et al. n.d.). To obtain such furrow water, a Chagga had to be a member of a furrow board,<br />

which was governed by furrow elders whose instructions farmers had to follow on pain of fines or<br />

prohibition from using furrow water (Johnston, 1946). Furrow board members were also expected to play<br />

a part in the maintenance of the furrows. Furrow members who abstracted water from furrows owned by<br />

individuals or claims had to pay fees to do so.<br />

Despite the apparent farming intensity and population pressure on kihamba land, traditional institutions of<br />

governance and conflict prevention appear to have been effective. Johnston (1942) commented that “…it is<br />

remarkable that, with a big and complicated furrow system in the kihamba land, so well are matters run by the<br />

furrow elders, that the number of cases arising out of disputes over water rights are relatively few” (p. 4).<br />

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