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Mount Ungaran
Mount Ungaran is a deeply eroded stratovolcano, located in the south of Semarang, Central Java, Indonesia. There are no historical records about the mountain's activities. Two active fumarole fields are found on the southern flanks. The town of Ungaran is located on the eastern side of the volcano, whereas Ambarawa lays of its southern wing. Bandungan and surroundings, including the Gedong Songo temple complex, are tourist attractions on the volcano. The lake of Rawa Pening is located southeast of the volcano. Endemic fauna includes '' Philautus jacobsoni'', a tree frog that has not been seen for decades. See also * List of volcanoes in Indonesia The geography of Indonesia is dominated by volcanoes that are formed due to subduction zones between the Eurasian plate and the Indo-Australian plate. Some of the volcanoes are notable for their eruptions, for instance, Krakatoa for its globa ... References Stratovolcanoes of Indonesia Volcanoes of Central Java { ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ambarawa
Ambarawa is a town (and administratively, a district of the Semarang Regency) located between the city of Semarang and Salatiga in Central Java, Indonesia. Administratively, it is bordered by the districts of Banyubiru to the south, Jambu to the west, Bandungan to the north, and Bawen to the east. During colonial times, Ambarawa was an important railway hub connecting through regions in Java as far as Yogyakarta and Magelang. The Semarang-Ambarawa-Magelang line was fully operational until 1977. It is the site of the Indonesian Railway Museum (''Museum Kereta Api Ambarawa''), which features a section of rack railway between Ambarawa to Bedono on the former Ambarawa-Magelang mainline. The 19th-century Fort Willem I penitentiary complex and military barrack is also located in Ambarawa. Japanese internment camps Ambarawa was the site of Japanese internment camps where up to 15,000 Europeans had been held during the Japanese occupation during World War II. Following Japanese ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Volcanoes In Indonesia
The geography of Indonesia is dominated by volcanoes that are formed due to subduction zones between the Eurasian plate and the Indo-Australian plate. Some of the volcanoes are notable for their eruptions, for instance, Krakatoa for its global effects in 1883, the Lake Toba Caldera for its supervolcanic eruption estimated to have occurred 74,000 years before present which was responsible for six years of volcanic winter, and Mount Tambora for the most violent eruption in recorded history in 1815. Volcanoes in Indonesia are part of the Pacific Ring of Fire. The 150 entries in the list below are grouped into six geographical regions, four of which belong to the volcanoes of the Sunda Arc trench system. The remaining two groups are volcanoes of Halmahera, including its surrounding volcanic islands, and volcanoes of Sulawesi and the Sangihe Islands. The latter group is in one volcanic arc together with the Philippine volcanoes. The most active volcano is Mount Merapi on Java. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Philautus Jacobsoni
''Philautus jacobsoni'' is a species of frog in the family Rhacophoridae. It is endemic to Java, Indonesia. It is known only from Mount Ungaran, Central Java, Indonesia. There is only one preserved specimen held at the Naturalis Biodiversity Center in Leiden, Netherlands that was collected in the 1930s. Its status in the wild is currently unknown and could possibly be extinct, as it has not been recently found. Its natural habitats are subtropical or tropical moist lowland forests and subtropical or tropical moist montane forests. It is threatened by habitat loss Habitat destruction (also termed habitat loss and habitat reduction) is the process by which a natural habitat becomes incapable of supporting its native species. The organisms that previously inhabited the site are displaced or dead, thereby .... References jacobsoni Amphibians of Indonesia Endemic fauna of Java Taxa named by Pieter Nicolaas van Kampen Amphibians described in 1912 Taxonomy articles crea ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fauna
Fauna is all of the animal life present in a particular region or time. The corresponding term for plants is ''flora'', and for fungi, it is '' funga''. Flora, fauna, funga and other forms of life are collectively referred to as '' biota''. Zoologists and paleontologists use ''fauna'' to refer to a typical collection of animals found in a specific time or place, e.g. the "Sonoran Desert fauna" or the "Burgess Shale fauna". Paleontologists sometimes refer to a sequence of faunal stages, which is a series of rocks all containing similar fossils. The study of animals of a particular region is called faunistics. Etymology ''Fauna'' comes from the name Fauna, a Roman goddess of earth and fertility, the Roman god Faunus, and the related forest spirits called Fauns. All three words are cognates of the name of the Greek god Pan, and ''panis'' is the Greek equivalent of fauna. ''Fauna'' is also the word for a book that catalogues the animals in such a manner. The term was first used b ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Endemic
Endemism is the state of a species being found in a single defined geographic location, such as an island, state, nation, country or other defined zone; organisms that are indigenous to a place are not endemic to it if they are also found elsewhere. For example, the Cape sugarbird is found exclusively in southwestern South Africa and is therefore said to be ''endemic'' to that particular part of the world. An endemic species can be also be referred to as an ''endemism'' or in scientific literature as an ''endemite''. For example '' Cytisus aeolicus'' is an endemite of the Italian flora. '' Adzharia renschi'' was once believed to be an endemite of the Caucasus, but it was later discovered to be a non-indigenous species from South America belonging to a different genus. The extreme opposite of an endemic species is one with a cosmopolitan distribution, having a global or widespread range. A rare alternative term for a species that is endemic is "precinctive", which applies to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rawa Pening
Rawa Pening (literally meaning 'Clear Swamp', from the Javanese ''Bening'') is a lake in the Ambarawa Basin in Central Java, Indonesia. It serves as a source of power, irrigation, and flood control, and is used for fishing. Due partly to high numbers of aquatic plants, it may dry out by 2021. Location and description Rawa Pening is located in the volcanic Ambarawa Basin in Central Java, between Ambarawa and Salatiga. It covers a total area of . It is shallow and swamplike, with muddy banks. History Rawa Pening is estimated to have been formed between 18,000 and 13,500 BC after a period of increased precipitation. It reached its largest size from 11,000 to 9,000 BC, but shrank until it reached its current size around 6,000 BC. In order to protect Rawa Pening, the local government has enacted a green belt policy. Several establishments, such as the tourist attraction Kampoeng Rawa, were controversial owing to their construction within this belt. Role One of the majo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gedong Songo
__NOTOC__ Gedong Songo ( id, Candi Gedong Songo) is a group of Hindu temples located near Bandungan, Semarang Regency, in north Central Java, Indonesia. It is variously dated between the 8th and 9th-century. Built around a hill near Mount Ungaran, it consist of five ''Gedong'' (temple group) – two on the east side of the hill, two towards the north and one to the west. These total nine temples, all dedicated to Shiva and Parvati.Veronique Degroot (1972), Candi Space and Landscape: A Study of the Distribution, Orientation and Spatial Organization of Central Javanese Temple Remains, Geboren te Charleroi Belgie, Leiden University, pp. 12–14 The Gedong Songo complex is one of 110 sites in central Java with Hindu temple structures or remains, and one of 21 in Semarang area, states Veronique Degroot. The site was originally built during the early period of the Mataram Kingdom of Central Java. Similar to the Dieng temples on the Dieng Plateau, Gedong Songo was erected out of volcani ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ungaran
Ungaran (Dutch: ''Oengaran'') is a town in Central Java, Indonesia and the administrative centre of the Semarang Regency in the province of Central Java. Ungaran is located at -7° 8' 17", 110° 24' 18" at an elevation of 319 metres. It encompasses two districts (''kecamatan'') within the Regency - Ungaran Barat (West Ungaran) and Ungaran Timur (East Ungaran). In the 19th century, defensive posts were established between Semarang and Surakarta to control the trade route between the two cities. A fort known as Fort Ontmoeting was established in Ungaran. Climate Ungaran has a tropical rainforest climate A tropical rainforest climate, humid tropical climate or equatorial climate is a tropical climate sub-type usually found within 10 to 15 degrees latitude of the equator. There are some other areas at higher latitudes, such as the coast of southea ... (Af) with moderate rainfall from June to September and heavy to very heavy rainfall from November to May. References Rege ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fumarole
A fumarole (or fumerole) is a vent in the surface of the Earth or other rocky planet from which hot volcanic gases and vapors are emitted, without any accompanying liquids or solids. Fumaroles are characteristic of the late stages of volcanic activity, but fumarole activity can also precede a volcanic eruption and has been used for eruption prediction. Most fumaroles die down within a few days or weeks of the end of an eruption, but a few are persistent, lasting for decades or longer. An area containing fumaroles is known as a fumarole field. The predominant vapor emitted by fumaroles is steam, formed by the circulation of groundwater through heated rock. This is typically accompanied by volcanic gases given off by magma cooling deep below the surface. These volcanic gases include sulfur compounds, such as various sulfur oxides and hydrogen sulfide, and sometimes hydrogen chloride, hydrogen fluoride, and other gases. A fumarole that emits significant sulfur compounds is some ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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