Mount Nyangani Explained

Mount Nyangani
Other Name:Mount Inyangani
Elevation M:2592
Elevation Ref:[1]
Prominence M:1515
Map:Zimbabwe
Label Position:left
Listing:Country high point
Ultra
Location:Zimbabwe
Coordinates:-18.3°N 32.8417°W
Easiest Route:Hike

Mount Nyangani (formerly Mount Inyangani) is the highest mountain in Zimbabwe at 25920NaN0. The mountain is located within Nyanga National Park in Nyanga District, about 110km (70miles) north-northeast of Mutare. The summit lies atop a small outcrop of rock around 40-1NaN-1 above the surrounding area. The remainder of the peak is a broad moor of mainly rolling hills and plateau with an area of about 8 km2. The edges of this plateau then fall steeply to the east and west sides. The mountain vegetation is largely composed of heath around the summit plateau with evergreen forest along the wetter eastern slopes and grassland to the western side. Annual rainfall totals are high (around 22000NaN0) but long spells of dry weather occur during the winter period of May to August. Due to its relatively low altitude and tropical location, snowfall is very rare, last recorded in August 1935.[2]

Geology

The mountain is composed of an upper sill of dolerite and sandstone, with the harder dolerite forming cliffs and ridges. The dolerite sill and the sediments underlying it are probably part of the Umkondo Group.[3] The Umkondo Group dolerite sill north of Nyangani, on the Kwaraguza Road, has been dated at 1099 Ma [4]

Access

The mountain can be accessed from four base points within Nyanga National Park:

(1) The official car park, at the base of the Tourist Route. This is reached from Circular Drive.

(2) The Mountain Club of Zimbabwe hut, on the Kwaraguza Road, accessed via Circular Drive.

(3) Nyazengu Substation of Nyanga National Park, accessed via a road which goes south from just before the official car park.

(4) Gleneagles Substation of Nyanga National Park, accessed via the Circular Drive, Kwaraguza Road and the Gleneagles road or from Troutbeck via Nyafaru.

Mountain hikes

The peak can be reached within 1–3 hours by anyone of average fitness. This ascent brings the hiker to an altitude of about 2200-1NaN-1 and the remainder is mostly walking across the gentler gradients of the summit plateau. The hazards here are produced by bewilderingly fast weather changes that can switch from sunny skies to thick fog, and under these conditions several fatalities have occurred due to hikers losing their way and falling down ravines. There are three ascents that follow paths:

The mountain can also be ascended using the following routes which do not have paths or markings:

The above are all walks or scrambles, without rock climbing involved. However, caution is advised, especially on unmarked routes, as the weather may change very rapidly: descent of cloud can result in visibility of less than 50-1NaN-1. This may well be the cause for a number of disappearances on the mountain, such as that of two teenage children of the then Minister of Finance, Tichaendepi Masaya.[5]

Rivers and waterfalls

Three rivers have their sources on Mount Nyangani: the Nyamuziwa River, the (Kairezi) Gairezi River and the Pungwe River. The first two are tributaries of the Mazowe River, which is itself a tributary of the Zambezi River.

The Nyama River, a tributary of the Kayirezi, falls off the main plateau in a waterfall on the northeast of the mountain and the Gairezi Falls are located on the east edge of the main plateau.

Fauna

The fauna of the area is described under Nyanga National Park. Additional information:

Flora

Archaeology

Iron Age ruins have been found on Little Nyangani and on a hill west of the summit, the latter better-preserved,[9] but not on the summit plateau itself.

In popular culture

The film Mysteries of Mount Inyangani looks at some of the mysteries and myths about the mountain.[10]

See also

External links

Notes and References

  1. http://peaklist.org/WWlists/ultras/africa.html "Africa Ultra-Prominences"
  2. http://www.worldclimate.com/sources.htm GHCN
  3. Web site: Love, D.. February 2002. The geology of Nyangani Mountain: a preliminary report . University of Zimbabwe Earth Science Research Seminar Series . https://web.archive.org/web/20070926224746/http://www.uz.ac.zw/science/geology/davidlove/Nyangani-prelim%20abs.pdf . 2007-09-26 . 2011-08-20.
  4. Wingate, M.T.D.. 2001. SHRIMP baddeleyite and zircon ages for an Umkondo dolerite sill, Nyanga Mountains, eastern Zimbabwe. South African Journal of Geology. 104. 13–22. 2009-02-06. 10.2113/104.1.13. 1.
  5. Web site: Mount Nyangani. 2009-12-30.
  6. Butler, J.R.A. . Marshall, B. . amp . 1996. Resource Use Within the Crab-Eating Guild of the Upper Kairezi River, Zimbabwe. 12. 475–490. 0266-4674. 4. 10.1017/S0266467400009718. Journal of Tropical Ecology. 2560302.
  7. Amietia inyangae
  8. Web site: CJB - African plant database - Detail . 2020-06-19 . www.ville-ge.ch.
  9. Book: Garlake, P.S.. 1965. A guide to the antiquities of Inyanga. Historical Monuments Commission of Rhodesia. B0007JZPWM.
  10. Ingrid Sinclair, Joel Phiri. Mysteries of Mount Inyangani. Zimbabwe. 1999. dead. https://web.archive.org/web/20110720004955/http://www.africanmedia.msu.edu/php/showfilm.php?id=24181. 2011-07-20.