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Mozambique · Landforms

Mountain Ranges, Deserts and Landforms of Mozambique

Africa is the largest of the 5 mountain ranges, deserts and other landforms recorded for Mozambique, at 29.41M km², ahead of Great Rift Valley at 163,247 km². The full list follows.

How this list is built: Ranked by mapped area. Covers mountain ranges, deserts, plateaus, named glaciers, plains, basins, peninsulas and capes. One that crosses a border is listed under every country it lies in, with the area of the whole feature. It covers the mountain ranges, deserts and other landforms indexed in YearMaps, drawn from open geospatial data, and is not an exhaustive national register.

Landforms Listed
5
Top Ranked
29.41M km²
Africa
Second
163,247 km²
Great Rift Valley
Profiled Below
2
Photo, encyclopedia text and figures
Mountain Ranges, Deserts and Landforms of Mozambique
#NameArea
1Africa29.41M km²
2Great Rift Valley163,247 km²
3Inyanga Mountains58,492 km²
4Lebombo Mountains17,406 km²
5Zambezi Delta15 km²

The Landforms of Mozambique in Detail

The 2 mountain ranges, deserts and other landforms above that have an encyclopedia article, in the same order, each with its photograph, figures and the places around it.

Inyanga Mountains
Image via Wikimedia Commons (author and licence on the file page).

Inyanga Mountains

Range/mtn · 58,492 km²

Inyanga Mountains is a range/mtn in Africa, covering an estimated 58,492 km². It extends across Zimbabwe and Mozambique.

Mount Nyangani (formerly Mount Inyangani) is the highest mountain in Zimbabwe at 2,592 metres or 8,504 feet. The mountain is located within Nyanga National Park in Nyanga District, about 110 km (68 mi) north-northeast of Mutare. The summit lies atop a small outcrop of rock around 40 metres or 130 feet 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 2,200 millimetres or 87 inches) but long spells of dry weather occur during the winter period of May to August. Due to its relatively low elevation and tropical location, snowfall is very rare; the last recorded snowfall occurred in August 1935.

Adapted from Wikipedia: Mount Nyangani (CC BY-SA 4.0).

Feature class
Range/mtn
Mapped extent
58,492 km²
Size rank
#73 of 216 mountain ranges
Region
Africa
Countries
Zimbabwe, Mozambique
Coordinates
-17.5018°, 32.5704°
Adjacent ranges:
Lebombo Mountains (Africa), Witwatersrand (Africa)
Settlements:
Chimoio (33 km), Dondo (177 km), Beira (199 km)

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Lebombo Mountains
Image via Wikimedia Commons (author and licence on the file page).

Lebombo Mountains

Range/mtn · 17,406 km²

Lebombo Mountains is a range/mtn in Africa, covering an estimated 17,406 km². It extends across Mozambique, South Africa and Swaziland.

The Lebombo Mountains, also called Lubombo Mountains, Rivombo Mountains (Portuguese: Montes Libombos), are an 800 km-long (500 mi), narrow range of mountains in Southern Africa. They stretch from Hluhluwe in KwaZulu-Natal in the south to Punda Maria in the Limpopo Province in South Africa in the north. Parts of the mountain range are also found in Mozambique and Eswatini.

Adapted from Wikipedia: Lebombo Mountains (CC BY-SA 4.0).

Feature class
Range/mtn
Mapped extent
17,406 km²
Size rank
#129 of 216 mountain ranges
Region
Africa
Countries
Mozambique, South Africa, Swaziland
Coordinates
-26.1330°, 32.0367°
Adjacent ranges:
Witwatersrand (Africa), Drakensberg (Africa)
Settlements:
Matola (96 km), Maputo (100 km), Macia (103 km)

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More about Lebombo Mountains

Description

Geologically, the range is considered a monocline; part of a rifted volcanic margin. The Lebombo monocline was aligned with the Explora Escarpment off-shore Dronning Maud Land, Antarctica, before the break-up of Gondwana. The Lebombo monocline strikes N-S and dips to the east. It is composed of a sequence of Jurassic age volcanic rock, both basaltic lavas and rhyolitic flows and tuffs. The sequence rests on essentially horizontal Karoo Supergroup sedimentary rocks of the Kalahari Craton to the west and is overlain by Cretaceous to recent sediments to the east. The alternating resistant rhyolite and easily eroded basalts produce a series of parallel sharp cuesta ridges separated by savanna plains.

Sections adapted from Wikipedia: Lebombo Mountains (CC BY-SA 4.0).

Lebombo Mountains: Key Facts

Key facts about Lebombo Mountains
Length800 km

Facts from Wikidata Q1501766 (CC0).

More on Mozambique

Quick Answers

What is the largest landform in Mozambique?
Africa, at 29.41M km². Great Rift Valley is second at 163,247 km². Rankings cover the mountain ranges, deserts and other landforms indexed in YearMaps.
How many mountain ranges, deserts and other landforms are there in Mozambique?
YearMaps lists 5 mountain ranges, deserts and other landforms for Mozambique. This is the number mapped in the atlas, not an official national count.