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Geosite
Geoheritage is the geological aspect of natural and cultural heritage. A geosite is a particular geoheritage asset. The word is a blend of ''geological'' and ''heritage''. It is thus a heritage category comparable to other forms of natural heritage, such as biodiversity. History of the concept The first reference to geoheritage as such was at a 1993 conference held in the UK, the Malvern International Conference on Geological and Landscape Conservation. The term geological heritage was first mentioned at the First International Symposium on the Conservation of our Geological Heritage at Digne, France in 1991. The matter is further discussed in 2002 by Sharples. Conceptually, geoheritage derives from various writings of Busby et al. 2001 and Hallam 1989). In Sharples 1995 the original concept of geoheritage further developed to include the protection of dynamic geological processes and geodiversity. In Sadry 2021 the concept of geoheritage have more developed to include the ...
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Geosite
Geoheritage is the geological aspect of natural and cultural heritage. A geosite is a particular geoheritage asset. The word is a blend of ''geological'' and ''heritage''. It is thus a heritage category comparable to other forms of natural heritage, such as biodiversity. History of the concept The first reference to geoheritage as such was at a 1993 conference held in the UK, the Malvern International Conference on Geological and Landscape Conservation. The term geological heritage was first mentioned at the First International Symposium on the Conservation of our Geological Heritage at Digne, France in 1991. The matter is further discussed in 2002 by Sharples. Conceptually, geoheritage derives from various writings of Busby et al. 2001 and Hallam 1989). In Sharples 1995 the original concept of geoheritage further developed to include the protection of dynamic geological processes and geodiversity. In Sadry 2021 the concept of geoheritage have more developed to include the ...
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Geological And Mining Institute Of Spain
The Geological and Mining Institute of Spain (Spanish: ''Instituto Geológico y Minero de España'') is a research institute located in Madrid, Spain. It is run under the auspices of the Ministry of Science. In collaboration with the Spanish Geological Society (''Sociedad Geológica de España'' or SGE), the Institute has drawn up a list of internationally important geosites in Spain. This work, which began in 1999, is part of the Global Geosites project promoted by IUGS in the 1990s and subsequently supported by UNESCO. History The origins of the institute go back to the nineteenth century when a commission was established to work on the geological map of Spain. The building which houses the institute is on Ríos Rosas street in the Chamberí district of Madrid. Next door is the School of Mining Engineering of Madrid, which was built in 1893, whereas the institute building, designed by Francisco Javier de Luque, was formally opened in 1926. The opening took place during the In ...
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Indonesia
Indonesia, officially the Republic of Indonesia, is a country in Southeast Asia and Oceania between the Indian and Pacific oceans. It consists of over 17,000 islands, including Sumatra, Java, Sulawesi, and parts of Borneo and New Guinea. Indonesia is the world's largest archipelagic state and the 14th-largest country by area, at . With over 275 million people, Indonesia is the world's fourth-most populous country and the most populous Muslim-majority country. Java, the world's most populous island, is home to more than half of the country's population. Indonesia is a presidential republic with an elected legislature. It has 38 provinces, of which nine have special status. The country's capital, Jakarta, is the world's second-most populous urban area. Indonesia shares land borders with Papua New Guinea, East Timor, and the eastern part of Malaysia, as well as maritime borders with Singapore, Vietnam, Thailand, the Philippines, Australia, Palau, and India ...
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Wonosari
Wonosari ( jv, ꦮꦤꦱꦫꦶ, translit=Wanasari) is the administrative centre of Gunung Kidul Regency, in the Special Region of Yogyakarta on Java, Indonesia. Wonosari District is bordered to the north by the district of Nglipar, to the east by the districts of Karangmojo and Semanu, to the south by the district of Tanjungsari, and to the west by the districts of Paliyan and Playen (to the west of Yogyakarta). It had a population of 87,454 as of 2020 Census.Badan Pusat Statistik, Jakarta, 2021. Education There are many schools in the town of Wonosari. The most popular ones are Wonosari Baru Elementary School, Wonosari 1 Junior High School, and Wonosari 1 High School. There is also Wonosari 2 High School. The education level is mid-high depends on the school quality (like the teacher ability, the student's impact, facility, etc.) The schools in Wonosari are mostly managed by Disdikpora Gunungkidul or Dinas Pendidikan dan Olahraga Gunungkidul, located in Jl. Pemuda No.227, Rejosa ...
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Bioturbation
Bioturbation is defined as the reworking of soils and sediments by animals or plants. It includes burrowing, ingestion, and defecation of sediment grains. Bioturbating activities have a profound effect on the environment and are thought to be a primary driver of biodiversity. The formal study of bioturbation began in the 1800s by Charles Darwin experimenting in his garden. The disruption of aquatic sediments and terrestrial soils through bioturbating activities provides significant ecosystem services. These include the alteration of nutrients in aquatic sediment and overlying water, shelter to other species in the form of burrows in terrestrial and water ecosystems, and soil production on land.Shaler, N. S., 1891, The origin and nature of soils, in Powell, J. W., ed., USGS 12th Annual report 1890-1891: Washington, D.C., Government Printing Office, p. 213-45. Bioturbators are deemed ecosystem engineers because they alter resource availability to other species through the physical ch ...
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Gunung Kidul Regency
Gunungkidul Regency is a regency in the southeast part of the province of Yogyakarta Special Region, Indonesia. It is located on the island of Java. The regency (the name of which means South Mountains in Javanese) is bordered by the Sleman Regency to the north west, Bantul Regency to the west, the Indian Ocean to the south, Wonogiri Regency to the east and Klaten Regency to the north. It covers an area of 1,485.36 km2 and had a population of 675,382 at the 2010 CensusBiro Pusat Statistik, Jakarta, 2011. and 747,161 at the 2020 Census.Badan Pusat Statistik, Jakarta, 2021. The traditional snacks and meals from Gunungkidul include "Gathot" and "Thiwul". They are made from Fermentation Cassava and Dry Cassava. The southern coast of Gunungkidul has several beaches: Baron, Kukup, Krakal, Drini, Sepanjang, Sundak, Siung, Wediombo, Jungwok, Greweng, Sedahan and Sadeng. Some of these beaches provide fresh fish and other sea product supplied by local fisherman. The most notable is Ba ...
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Kulon Progo Regency
Kulon Progo Regency ( jv, Kulon Praga, , ) is one of the four regencies within the Yogyakarta Special Region, Indonesia. It is located on the island of Java. The regency's name stems from the fact that it is situated to the west (in Javanese "kulon") of the Progo River. The capital is Wates. The greatest part of the population of the regency work as farmers. Kulon Progo Regency is surrounded by the Menoreh Hills. The area of the regency is 586.27 km2, and the population was 388,755 at the 2010 census and 436,395 at the 2020 census. History In 1674, Keraton Mataram, Yogyakarta was attacked by Trunojoyo who received assistance from Macassar, resulting in damage to the palace and the king Amangkurat I had to flee and asked the Netherlands for help, till he died in Tegal during flight. To anticipate attacks from Trunojoyo's followers, in 1677 the palace of Mataram led by Amangkurat II as the crown prince of Amangkurat I asked for the regent Ponorogo to obtain the palace protec ...
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Parangtritis
Parangtritis Beach is a tourist beach on the southern coast of Java in the Bantul Regency within the province of the Yogyakarta Special Region. There is a road to the area which is about 30 km south of the Yogyakarta, city of Yogyakarta. This beach is located south of :id:Pantai Parangkusumo, Parangkusumo Beach, which is also a mainstay of tourism in Bantul Regency. This beach is often visited by local and foreign tourists. Facilities and attractions Quite large crowds of mainly local tourists visit Parangtritis over weekends and at holidays. Larger tourist buses as well as various types of cheaper minibuses ply the route to the beach from Yogyakarta. There are local tourist facilities at Parangtritis including parking arrangements, modest hotels which provide visitors with places to change and shower, and small restaurants. Often small ponies or horse-drawn carts can be hired for rides along the beach. Tourists also visit some of the various caves and Spring (hydrology), sprin ...
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Bantul Regency
Bantul ( jv, ꦧꦤ꧀ꦠꦸꦭ꧀; ) is a regency located in the Special Region of Yogyakarta, Indonesia. It is located on the island of Java. The regency's population was 911,503 at the 2010 Census, but has risen to 985,770 at the 2020 Census. Like many regencies on the island of Java, it is densely populated with roughly 1,945 people per square kilometre in 2020, although this is largely because the north of the regency partly surrounds the city of Yogyakarta and contains many suburban communities, notably in the densely-populated districts of Banguntapan, Sewon and Kasihan. The regency is bordered by the city of Yogyakarta and Sleman regency to the north, the regency of Kulon Progo to the west, the Gunung Kidul Regency to the east and the Indian Ocean to the south. The town of Bantul is the administrative centre. The village of Kemusuk in the Sedayu District in the northwest of the regency is the birthplace of former Indonesian President, Suharto. 2006 earthquake On 27 May ...
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Candi Ijo
Ijo temple ( id, Candi Ijo) is a Hindu candi (temple) located 4 kilometers from Ratu Boko or around 18 kilometers east from Yogyakarta, Indonesia. The temple was built between 10th to 11th century CE during the Mataram Kingdom period. Location The temple compound is located in Groyokan hamlet, Sambirejo village, Kecamatan Prambanan, Sleman Regency, Yogyakarta. The temple's name derived from its location, the Gumuk Ijo hill. The temple compound stood on western slope of the hill, in a quiet region east of Yogyakarta, around 4 kilometers southeast from Ratu Boko archaeological compound. The temple elevation is 410 meters above the sea level. The western hill of Gumuk Ijo overlooks rice paddies, villages and Adisucipto International Airport. The temple compound measures 0.8 hectares, however the original temple compound is estimated to be far larger. On the hill foot and slopes on western sides there are some archaeological artifacts and temple ruins which suggest the larger com ...
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Prambanan
Prambanan ( id, Candi Prambanan, jv, ꦫꦫꦗꦺꦴꦁꦒꦿꦁ, Rara Jonggrang) is a 9th-century Hindu temple compound in Special Region of Yogyakarta, Indonesia, dedicated to the Trimūrti, the expression of God as the Creator (Brahma), the Preserver (Vishnu) and the Destroyer (Shiva). The temple compound is located approximately northeast of the city of Yogyakarta on the boundary between Central Java and Yogyakarta provinces. The temple compound, a UNESCO World Heritage Site, is the largest Hindu temple site in Indonesia and the second-largest in Southeast Asia after Angkor Wat. It is characterized by its tall and pointed architecture, typical of Hindu architecture, and by the towering central building inside a large complex of individual temples. Prambanan temple compounds originally consists of 240 temple structures; which represents the grandeur of ancient Java's Hindu art and architecture, also considered as a masterpiece of the classical period in Indonesia. Prambanan ...
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Pillow Lava
Pillow lavas are lavas that contain characteristic pillow-shaped structures that are attributed to the extrusion of the lava underwater, or ''subaqueous extrusion''. Pillow lavas in volcanic rock are characterized by thick sequences of discontinuous pillow-shaped masses, commonly up to one meter in diameter. They form the upper part of Layer 2 of normal oceanic crust. Composition Pillow lavas are commonly of basaltic composition, although pillows formed of komatiite, picrite, boninite, basaltic andesite, andesite, dacite or even rhyolite are known. In general, the more felsic the composition (richer in silica - resulting in an Intermediate composition), the larger the pillows, due to the increase in viscosity of the erupting lava. Occurrence They occur wherever lava is extruded underwater, such as along marine hotspot volcano chains and the constructive plate boundaries of mid-ocean ridges. As new oceanic crust is formed, thick sequences of pillow lavas are erupted at the ...
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