Question: Jasminum multipartitum is native to what landlocked country located in southern Africa, between the Zambezi and Limpopo Rivers?

Context articles: Limpopo River
Gaza Empire
Zimbabwe
Tsonga people
Jasminum multipartitum
Kingdom of Mutapa
Kingdom of Mapungubwe
Zimbabwe Craton
List of companies of Zimbabwe
Geography of Zimbabwe

The Limpopo River rises in central southern Africa, and flows generally eastwards to the Indian Ocean.
 The term Limpopo is the modified version of the original Sepedi name "diphororo tša meetse", meaning "gushing strong waterfalls".
 The river is approximately 1750 km long, with a drainage basin 415000 km2 in size.
 The mean discharge measured over a year is 170 m/s (6,200 cu ft/s) at its mouth.
 The Limpopo is the second largest river in Africa that drains to the Indian Ocean, after the Zambezi River.
The Gaza Empire (1824–1895) was an African empire established by the powerful general Soshangane and was located in southeastern Africa in the area of southern Mozambique and southeastern Zimbabwe.
 The Gaza Empire, at its height in the 1860s, covered all of Mozambique between the Zambezi and Limpopo rivers.
Zimbabwe ( ), officially the Republic of Zimbabwe, is a landlocked country located in southern Africa, between the Zambezi and Limpopo Rivers.
 It is bordered by South Africa to the south, Botswana to the west and southwest, Zambia to the northwest, and Mozambique to the east and northeast.
 Although it does not border Namibia, less than 200 metres of the Zambezi River separates it from that country.
 The capital and largest city is Harare.
 A country of roughly 16 million people, Zimbabwe has 16 official languages, with English, Shona, and Ndebele the most commonly used.
Tonga, Thonga or Tsonga people (Tsonga: "Vatsonga" ) and languages span most of southern Africa, notable countries being South Africa, Swaziland, Mozambique, Malawi, Zambia and Zimbabwe.
 In these countries, there are regions where one or more languages and/or dialects are more dominant.
 For example, in South Africa, Tsonga people are mainly found in the Limpopo, Mpumalanga, KwaZulu-Natal and Gauteng provinces, with smaller populations in North-West and Free State.
 Within these provinces, there are towns and cities where they are most prevalent, although this is continually changing in the new South Africa as black people can now move freely.
 Most or all of southern Mozambique is inhabited by Tsonga people, variously named as Copi, Rhonga, Ndzawu, Tonga, Shangana, and Tshwa.
 Historically and currently the Tsonga people in Mozambique are between the Limpopo and Save rivers.
 Their density lowers between Save and Zambezi, where the Tsonga/Shona group of Ndau starts to dominate.
 The provinces are Maputo, Maputo City, Inhambane, Manica, Gaza, and Sofala.
Jasminum multipartitum (Starry Wild Jasmine or Imfohlafohlane) is a species of jasmine, in the family Oleaceae, that is native to Mozambique, Zimbabwe, Swaziland and South Africa.
The Kingdom of Mutapa - sometimes referred to as the Mutapa Empire, Mwenemutara, (Shona: "Mwene we Mutapa" or more commonly and modern "Munhumutapa"; Portuguese: "Monomotapa" ) - was a Kalanga kingdom which stretched from the Zambezi through the Limpopo rivers to the Indian Ocean in southern Africa, in what are the modern states of Zimbabwe, South Africa, Lesotho, Swaziland, Mozambique and parts of Namibia and Botswana; stretching well into modern Zambia.
 Its founders are descendants of the builders who constructed Great Zimbabwe.
The Kingdom of Mapungubwe (1075–1220) was a pre-colonial state in Southern Africa located at the confluence of the Shashe and Limpopo rivers, south of Great Zimbabwe.
 The name is derived from either Venda or Shona.
 The name may mean "Hill of Jackals" - see below.
 The kingdom was the first stage in a development that would culminate in the creation of the Kingdom of Zimbabwe in the 13th century, and with gold trading links to Rhapta and Kilwa Kisiwani on the African east coast.
 The Kingdom of Mapungubwe lasted about 80 years, and at its height its population was about 5000 people.
 The Mapungubwe Collection is a museum collection of artifacts found at the archaeological site and is housed in the Mapungubwe Museum in Pretoria.
The Zimbabwe Craton is an area in Southern Africa of ancient continental crust, being a part of the ancient continent of Western Gondwana, with rocks dating back to the early Archean Eon, possibly as early as 3.46 billion years ago (Ga.).
 The craton is named after the country of Zimbabwe where the majority of the craton is located.
 The rocks of the Zimbabwe Craton are separated from the rocks of the Kaapvaal Craton to the southeast by the 250 km wide Limpopo Belt of granulite facies tectonites.
 The Limpopo belt formed contemporaneously with the Zimbabwe and Kaapvaal cratons, but remained geologically active until much later.
 It was only in the late Archean, ca. 2.8-2.5 Ga., that the two cratons were stabilized together and that high-grade metamorphism ceased in the Limpopo Belt.
 North of the Zimbabwe Craton is the Zambezi Belt.
Zimbabwe is a landlocked sovereign state located in southern Africa, between the Zambezi and Limpopo Rivers.
 It borders South Africa to the south, Botswana and Namibia to the west, Zambia to the northwest, and Mozambique to the east and northeast.
 The capital and largest city is Harare.
 A country of roughly 13 million people, Zimbabwe has 16 official languages, with English, Shona, and Ndebele the most commonly used.
Zimbabwe is a landlocked country in southern Africa lying wholly within the tropics.
 It straddles an extensive high inland plateau that drops northwards to the Zambezi valley where the border with Zambia is and similarly drops southwards to the Limpopo valley and the border with South Africa.