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winds blow in from the west and lose their moisture upon hitting the region's mountains. Average rainfall per year ranges from 1,000 mm to 2,000 mm. High elevations give the region a cooler climate than the rest of
Cameroon. For example, the average temperature at
330:
The
Western High Plateau was once heavily forested. However, repeated cutting and burning by human beings has forced the forest back to areas along the waterways and has allowed grasslands to expand into the area.
296:. This means that the rivers experience a long, high-water period during the wet season and a short, low-water period during the dry season. The region's rivers ultimately empty into the
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181:. The plateau rises in steps from the west. To the east, it terminates in mountains that range from 1,000 metres to 2,500 metres in height, terminating in the
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346:—and short shrubs and trees that shed their foliage during the dry season as a defence against brush fires and dry weather.
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covers this. Vulcanism has created fertile black and brown soils. Erosion played a large role.
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292:. These rivers follow a Cameroon regime, a subtype of the equatorial regime of other southern
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forms the dominant vegetation. This consists of grassfields—leading to the name
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Gwanfogbe, Mathew; Meligui, Ambrose; Moukam, Jean; Nguoghia, Jeanette (1983).
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on its lower course. The region gives rise to important tributaries to the
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of the
Cameroon type. The area experiences two major seasons: A long,
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in the northeast. The region is characterised by accidented relief of
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The
Western High Plateau's relief and high rainfall make it a major
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characterised by high relief, cool temperatures, heavy rainfall and
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dot the plateau, the result of dead volcanoes filling with water.
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and mountains. The
Western High Plateau features several dormant
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to the northeast, which is a larger but less accidented region.
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is 20°C. Toward the north, rainfall levels are reduced as the
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to the northeast and the
Cameroon coastal plain to the south.
30:"Cameroon Highlands" redirects here. Not to be confused with
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of three months. During the wet season, humid, prevailing
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for
Cameroon. Important rivers in the region include the
300:. The area's accidented geography gives rise to several
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157:in the southwestern part of the plateau to the
153:, a series of volcanic swells running from the
573:Modern Geography of the Republic of Cameroon
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149:The Western High Plateau lies along the
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62:
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36:
227:
14:
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312:in the West Region is 80 metres high.
192:The core of the plateau is made up of
113:vegetation. The region lies along the
350:grow in the valleys and depressions.
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24:
556:. Hong Kong: Macmillan Education.
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89:from the mountain road into town.
185:. The plateau gives way to the
13:
1:
633:Cameroonian Highlands forests
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326:Cameroonian Highlands forests
280:on its lower course, and the
240:of nine months, and a short,
208:. The base rock is primarily
27:Mountainous area in Cameroon
7:
575:. Bamenda: Neba Publishers.
232:The plateau experiences an
10:
649:
545:
323:
32:Cameron Highlands District
29:
133:. The region borders the
319:
284:, which is known as the
304:along these waterways.
183:South Cameroon Plateau
145:Topography and geology
137:to the southeast, the
135:South Cameroon Plateau
90:
79:
60:
45:
554:Geography of Cameroon
524:Gwanfogbe et al. 1983
512:Gwanfogbe et al. 1983
500:Gwanfogbe et al. 1983
476:Gwanfogbe et al. 1983
449:Gwanfogbe et al. 1983
434:Gwanfogbe et al. 1983
422:Gwanfogbe et al. 1983
410:Gwanfogbe et al. 1983
369:Gwanfogbe et al. 1983
272:, which rises in the
261:becomes predominant.
196:, which is ringed by
85:
66:
51:
40:
623:Plateaus of Cameroon
571:Neba, Aaron (1999).
228:Climate and drainage
95:Western High Plateau
595: /
342:around the city of
340:Bamenda grassfields
274:Bamboutos Mountains
171:Bamboutos Mountains
103:Bamenda Grassfields
294:Cameroonian rivers
234:equatorial climate
218:Precambrian period
216:that dates to the
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80:
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46:
18:Bamileke Highlands
436:, pp. 16–17.
400:, pp. 23–24.
99:Western Highlands
16:(Redirected from
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599:6.500°N 10.500°E
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276:and becomes the
206:metamorphic rock
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117:and consists of
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187:Adamawa Plateau
159:Adamawa Plateau
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139:Adamawa Plateau
119:mountain ranges
105:is a region of
59:on the plateau.
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324:Main article:
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298:Atlantic Ocean
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200:. The base is
155:Atlantic Ocean
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259:Sudan climate
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220:. A layer of
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198:plutonic rock
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194:volcanic rock
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151:Cameroon line
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115:Cameroon line
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68:Menchum Falls
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348:Raffia palms
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314:Crater lakes
290:Sanaga River
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131:igneous rock
102:
98:
94:
92:
602: /
286:Wouri River
278:Cross River
255:West Region
202:crystalline
127:crystalline
76:Benue River
57:crater lake
617:Categories
354:References
310:Nkongsamba
306:Ekon Falls
302:waterfalls
242:dry season
238:wet season
179:Mount Kupe
628:Highlands
536:Neba 1999
488:Neba 1999
461:Neba 1999
398:Neba 1999
386:Neba 1999
266:watershed
175:Mount Oku
167:volcanoes
123:volcanoes
72:tributary
44:grassland
125:made of
107:Cameroon
53:Lake Oku
42:Bamileke
590:10°30′E
546:Sources
344:Bamenda
336:savanna
253:in the
251:Dschang
246:monsoon
214:granite
163:massifs
111:savanna
87:Bamenda
74:of the
587:6°30′N
560:
222:basalt
210:gneiss
333:Sudan
320:Flora
308:near
270:Manyu
70:is a
55:is a
558:ISBN
282:Nkam
212:and
204:and
177:and
129:and
121:and
93:The
101:or
619::
468:^
441:^
376:^
361:^
173:,
97:,
566:.
78:.
34:.
20:)
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