Rinjani Mountain
Potential Park. Mount Rinjani area was part of the tropical rain forest, located in West Nusa Tenggara. It consists of various types of ecosystems and complete vegetation ranging from lowland tropical forests (semi-evergreen) rainforest to the mountains (1500 to 2000 masl) consisting of prime forest, forest and sub-casurina vegetation alphine (> 2.00 masl ). at an altitude of 1000 masl many types of trees and shrubs. such as the banyan (ficus Benyamina), stinging nette (laportea stimulants), guava (sygium sp), wild nutmeg (Myritica fatna), Buni Forest (Antdesma so), Neem (Azadiracta indica), bajur (Pterospermium hptophilla), terep (artocarplus elastica), harending (Melasotama sp) and Pandan (Pandanus tectorius) tree.At masl height from 1.00 to 2.00 maslthis where many species of flora can be seen as Orchid (Vanda, Sp), Meniran (Calicarpa Sp), wood jakut (Syzigium sp), Sentul (Aglaia sp), deduren (Aglaia Argentia), Pandan (psandanus tectorius), bird-nest fern (Asplenium nidus), glagah (spontaius saccharum), coarse grass (Imperata cylenca), ferns ( Cyclocorus sp), edeweiss (Anaphalis Visida), beard Algae (Unsea sp) and Bigg rattan (Daemonorops sp), you can also find various types of mammals that lived on Mount Rinjani, the main types are: Wild pig (Sus scrofa), gray gray monkeys (Macaca fascicularis), Black leaf monkey (Trcypphitecus auratus cristatus), a small Ganggarangan (Vivvericula indica), Javan pangolin (Manis javanica), rinjani Palm civets (Paradoxuurus hermaproditus rindjanicus), Leleko Congkok (bengelensis felis javanensis) Deers deer ( Cervus timorensis floresiensis), and porcupine (hystrix javanica). too many birds, such as sulfur crested cockatoo (Cacatua sulphures parvula), Koakiau (Philemon buceroides negelcus), shest red perkici (Trichoglosus haematodus), Honeyeater (Lichmera lomokia), Black-headed thrush (Zootera interpress).
Based on information provided by the Ministry of Mines and Energy of the Province of West Nusa Tenggara, the height of Mount Rinjani never reached approximately; 5000 m above sea level. also, the western part recently from Mount Rinjani, at the pre quarter era (1.8 million years ago), only the sediment. Later in the Pleistocene era (1.8 million then) there was volcanic activity as a result of tectonic volcanic action, which permeates through the surface in the form of activities or melted lava explosions.Mt. Climbing Rinjani is one of the main tourist attractions. Mount Rinjani is the second highest mountain in Indonesia.