In the Lesser Sunda Islands there are two geologically different groups of islands.[2] The northern group is volcanic. It is made up of Bali, Lombok, Sumbawa, Flores and Wetar. Some of the volcanoes, like Mount Rinjani on Lombok, are still active. However, there are some other volcanoes, such as Kelimutu on Flores, which are extinct. The northern group of islands started forming during the Pliocene, about 15 million years ago. They formed because of the collision between the Australian and the Asiantectonic plates.[2]
The southern group of islands include Sumba, Timor and Babar. They are not volcanic and are probably part of the Australian plate.[3]
Since colonial times in Indonesia, people have been studying the geographical history of the islands. However, we still do not fully understand how the islands were formed. Ideas of how the islands were formed changed in many ways during the last decades of the 20th century.[4]
At the point where two tectonic plates collide, the Lesser Sunda Islands are some of the most geologically complex and active regions in the world.[4] There are several volcanoes located on the Lesser Sunda Islands.[5]
Ecology
The Lesser Sunda Islands are different from the large islands of Java or Sumatra because there are many small islands. These small islands are sometimes divided by deep oceanic trenches. Because flora and fauna cannot move between the islands easily, there are many localised species like the Komodo dragon.[4] In The Malay Archipelago, Alfred Wallace writes about the "Wallace Line" that passes between Bali and Lombok, along the deep waters of the Lombok Strait. In this imaginary line between Bali and Lombok, even when sea levels were lower, the sea stopped flora and fauna from moving between islands. The islands east of the Lombok Strait are part of Wallacea, and have wildlife of Asian and Australasianorigin.[6] In the Lesser Sundas, there are many plants and animals that come from Asia, because Weber's Line, which separates the parts of Wallacea that have both Asian and Australasian species, is east of the Lesser Sundas. These islands have the driest climate in Indonesia.
Deciduous forests
Some of the islands east of the Wallace line, from Lombok and Sumbawa east to Flores and Alor, have original vegetation of dry forest and not the rain forest that covers most parts of Indonesia. These islands have been designated by the World Wildlife Fund as the Lesser Sundas deciduous forests ecoregion.[7] The higher slopes of the islands contain forests of tall Podocarpus conifers and Engelhardias with an undergrowth of lianas, epiphytes, and orchids such as Corybas, Corymborkis, and Malaxis (Adder's Mouth). The islands' coastal plains used to be savanna grasses like the savanna with Borassus flabelliferpalm trees on the coasts of Komodo, Rincah and Flores. While most of the vegetation on these islands is dry forest there are small areas of rainforest on these islands too, especially in lowland areas and riverbanks on Komodo. There is also a special area of dry thorny forest on the southeast coast of Lombok. Thorn trees used to be more common in coastal areas of the islands but have mostly been cleared.
Many unique species live on the Lesser Sundas. They include seventeen endemic birds (of the 273 birds found on the islands). The endemic mammals are the endangeredFlores Shrew(Suncus mertensi), the vulnerableKomodo Rat(Komodomys rintjanus), and Lombok Flying Fox(Pteropus lombocensis), Sunda Long-eared Bat(Nyctophilus heran) while the carnivorous Komodo dragon, which is the world's largest lizard, is found on Komodo, Rincah, Gili Motang, and the coast of northwestern Flores.
Threats and preservation
More than half of the original vegetation of the islands are cleared. This is because people cleared the forest to grow food, like rice, for settlements or because there were forest fires. Only Sumbawa now contains a large area of intact natural forest, while Komodo, Rincah and Padar are now protected as Komodo National Park.
General observations[8] about small islands that can be applied to Nusa Tenggara include:[9]
↑ 2.02.1Audley-Charles, M.G. (1987) "Dispersal of Gondwanaland: relevance to evolution of the Angiosperms" In: Whitmore, T.C. (ed.) (1987) Biogeographical Evolution of the Malay Archipelago Oxford Monographs on Biogeography 4, Clarendon Press, Oxford, pp. 5–25, ISBN0-19-854185-6
↑Veevers, J.J. (1991) "Phanerozoic Australia in the changing configuration of ProtoPangea through Gondwanaland and Pangea to the present dispersed continents" Australian Systematic Botany 4: pp. 1–11
↑ 4.04.14.2Monk, K.A.; Fretes, Y. and Reksodiharjo-Lilley, G. (1996). The Ecology of Nusa Tenggara and Maluku. Hong Kong: Periplus Editions Ltd. p. 9. ISBN962-593-076-0.{{cite book}}: CS1 maint: multiple names: authors list (link)
↑Beller, W., P. d'Ayala, and P. Hein. 1990. Sustainable development and environmental management of small islands. Paris and New Jersey: United Nations Educational, Scientific, and Cultural Organisation and Parthenon Publishing Group Inc.; Hess, A, 1990. Overview: sustainable development and environmental management of small islands. In Sustainable development and environmental management of small islands. eds W. Beller, P. d'Ayala, and P. Hein, Paris and New Jersey: United Nations Educational, Scientific, and Cultural Organisation and Parthenon Publishing Group Inc. (both cited in Monk)
Monk, K.A.; Fretes, Y. and Reksodiharjo-Lilley, G. (1996). The Ecology of Nusa Tenggara and Maluku. Hong Kong: Periplus Editions Ltd. ISBN962-593-076-0.{{cite book}}: CS1 maint: multiple names: authors list (link)