Ruvuma River, formerly also known as the Rovuma River, is a river in the African Great Lakes region. During the greater part of its course, it forms the border between Tanzania and Mozambique. The river is 998 km (620 mi) long, with a drainage basin of ~155,000 km2 (60,000 sq mi) in size. Its mean annual discharge is 475 m3/s (16,800 cu ft/s) to 2,286 m3/s (80,700 cu ft/s) at its mouth.[4][2]

Ruvuma
Rovuma
Map of the Ruvuma River drainage basin.
Location
CountryTanzania, Mozambique
Physical characteristics
Source 
 • locationRuvuma Region, Tanzania
 • coordinates10°45′00″S 35°40′00″E / 10.75000°S 35.66667°E / -10.75000; 35.66667
 • elevation1,000 m (3,300 ft)
Mouth 
 • location
Indian Ocean
 • coordinates
10°28′28″S 40°26′13″E / 10.47444°S 40.43694°E / -10.47444; 40.43694
 • elevation
0 m (0 ft)
Length998 km (620 mi)
Basin size154,727.4 km2 (59,740.6 sq mi)[1] to 155,316.4 km2 (59,968.0 sq mi)[2]
Discharge 
 • locationNear mouth
 • average(Period: 1979–2015)55.94 km3/a (1,773 m3/s)[3]

(Period: 1971–2000)2,286.3 m3/s (80,740 cu ft/s)[2]

(Period: 1982–2013)890.8 m3/s (31,460 cu ft/s)[1]
Basin features
River systemRovuma River
Tributaries 
 • leftMlongasi, Likonde, Muhawesi, Lumesule, Mbangala
 • rightMessinge, Lucheringo, Chinlezi, Lugenda

Discharge

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Average and maximum discharge of the Rovuma River (11°9′53.9532″S 39°15′37.8072″E / 11.164987000°S 39.260502000°E / -11.164987000; 39.260502000):[5]

VIC modeled (1999–2008) MFR estimated flows (1999–2008) UNH-GRDC historical period (1957–1999)
Average discharge
1,864 m3/s (65,800 cu ft/s) 1,866 m3/s (65,900 cu ft/s) 1,838 m3/s (64,900 cu ft/s)
Maximum discharge
22,365 m3/s (789,800 cu ft/s) 22,630 m3/s (799,000 cu ft/s) 22,053 m3/s (778,800 cu ft/s)

Average monthly discharge of the Rovuma River (11°9′53.9532″S 39°15′37.8072″E / 11.164987000°S 39.260502000°E / -11.164987000; 39.260502000), UNH-GRDC historical period (1957–1999):[5]

Month Discharge

(m3/s)

JAN 3,340
FEB 4,040
MAR 5,390
APR 3,880
MAY 1,780
JUN 780
JUL 350
AUG 160
SEP 50
OCT 80
NOV 270
DEC 1,940

Tributaries

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The largest tributaries of the Rovuma River:[2]

Left

tributary

Right

tributary

Length

(km)

Basin size

(km2)

Average discharge

(m3/s)

Rovuma 760 155,316.4 1,773
Kitama 70 1,065.8 12.3
Matiu 100 1,920.1 26.1
Mwiti 80 994.2 14
Ninga 100 1,572.8 19.8
Miesi 80 946.7 12.5
Mbangala 160 3 598.2 44.4
Lugenda 650 60,990.4 752.1
Lukwika 100 1,331.5 16.3
Manjesi 90 1,084.2 16.3
Lumesule 180 2,342.8 28.9
Muhuwesi 240 10,319.6 137.3
Mzinieva 100 1,285.4 22.5
Chimovero 638.3 11.2
Licombe 60 975.7 16
Lukembule 1,234.6 21.6
Chiluezi 3,544.9 55.1
Lopele 763.1 13.3
Luvingo 80 592.4 10.3
Ludimilé 1,129.4 20.7
Sasawara 90 2,322.8 37.3
Msangesi 120 1,614.1 23.8
Lipapa 753.5 14.2
Lussanhando 2,863.2 51.9
Lucheringo 250 9,288.1 200.5
Lualece 60 611.9 11
Miongosi 50 964.3 11.6
Likonde 150 5,914.8 61.2
Mlongasi 100 960.8 11.9
Messinge 238 7,525.4 174.8
Lunyere 190 6,210.1 78.7

Overview

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The lower Ruvuma river is formed by the junction at 11° 25′ S, 38° 31′ E of two branches of nearly equal importance, the longer of which, the Lujenda, comes from the south-west, the other, which still bears the name Ruvuma, from the west. Its source lies on an undulating plateau, 1,000 m (3,300 ft) high, immediately to the east of Lake Nyasa, at 10° 45′ S, 35° 40′ E, the head-stream flowing first due west before turning south and east.

In its eastward course, the Ruvuma flows near the base of the escarpment of an arid sandstone plateau to the north, from which direction the streams, which have cut themselves deep channels in the plateau edge, have almost all short courses.

On the opposite bank the Ruvuma receives, besides the Lujenda, the Msinje River and Luchulingo River, flowing in broad valleys running from south to north. The Lujenda rises in proximity to Lake Chilwa, in the small Lake Chiuta (520 m, 1,700 ft), the swamps to the south of this being separated from Chilwa only by a narrow wooded ridge. The stream which issues from Chiuta passes by a swampy valley into the narrow Lake Amaramba, from which the Lujenda River finally issues as a stream 80 yards (73 m) wide.

Lower down it varies greatly in breadth, containing in many parts long wooded islands which rise above the flood level, and are often inhabited. The river is fordable in many places in the dry season. At its mouth it is about 1 mile (1.6 km) wide.

The lower Ruvuma, which is often 12 mile (0.8 km) wide but generally shallow, flows through a swampy valley flanked by plateau escarpments containing several small backwaters of the river. The mouth is near 10° 28′ S, 40° 30′ E, the boundary near the coast being formed by the parallel of 10° 40′ S. The length of the Ruvuma is about 500 miles (800 km).

Bridge

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A bridge called Unity Bridge across the river between Mozambique and Tanzania was proposed as early as 1975, and although construction was started, the project was abandoned due to lack of funds. In 2002 the two national governments made a formal agreement to build a new 600 metre bridge across the river, and this was finally opened in a ceremony on 25 May 2010. The bridge is located at Negomano, 200 km (120 mi) inland and 100 km (62 mi) from the nearest surfaced road in Mozambique. The site was agreed between Presidents Machel and Nyerere because this was the site of the first entry into Mozambique by Frelimo forces in the Mozambican War of Independence on 25 September 1964. Negomano was also the location where the German forces crossed the Rovuma river on 25 November 1917.[6] First foundation stones were laid on the Tanzanian and Mozambique sides on October 10, 2005. Construction was completed early 2010 and cost US$28 million. It used to be possible to cross the river with rafts (located at the Tanzanian side) that could carry 3 jeeps. The ferry sank in 2008 and has not been replaced. At low water the river is sometimes fordable with a good 4-wheel drive.

A smaller bridge called Unity Two was also completed in 2007 on the upper Rovuma close to Matchedge in Niassa Province.

Notes

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  1. ^ a b Development of Master Plan for Water Resources Management in Mozambique (PDF; 10,0 MB)
  2. ^ a b c d "Central East Coast".
  3. ^ "GEF TWAP - Transboundary Waters Assessment Programme — GEF TWAP".
  4. ^ Nakayama, Mikiyasu (2003). International Waters in Southern Africa. United Nations University Press. p. 9. ISBN 92-808-1077-4.; online at Google Books
  5. ^ a b M.R., Minihane (2012). "Evaluation of streamflow estimates for the Rovuma River". Physics and Chemistry of the Earth. 50–52: 14–23. doi:10.1016/j.pce.2012.09.003.
  6. ^ Paice, Edward, 2008, Tip & Run, Phoenix, p. 339 ISBN 978-0753823491

References

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  This article incorporates text from a publication now in the public domainChisholm, Hugh, ed. (1911). "Rovuma". Encyclopædia Britannica. Vol. 23 (11th ed.). Cambridge University Press. p. 782.