Puncak Trikora
Puncak Trikora (literally "Peak People's Triple Command") is a 4,730 or mountain in the Highland Papua province of Indonesia on New Guinea. It lies in the eastern part of the Sudirman (Nassau) Range of the Maoke Mountains. Behind Puncak Jaya (Carstensz Pyramid) at , it is either the second or third highest mountain on the island of New Guinea and the Australasian continent. As such it appears on some Seven Second Summits lists, although SRTM-data support that Puncak Mandala (Juliana Peak) in the Jayawijaya (Orange) Range is higher with .See for example the lists apeaklistSeveral other summits of Mount Carstensz besides Carstensz Pyramid, like Ngga Pulu (4,862 m) and Carstensz East (4,820 or 4,840 m) are higher than both Mandala and Trikora, but because of their low prominence (200-300 m) and isolation (2.2-2.6 km) these are usually not regarded as separate mountains. Name The Dani living near lake Habbema call the mountain Ettiakup. Around 1905 the mountain was named a ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Maoke Mountains
The Maoke Mountains is a mountain range in the province of Central Papua and Highland Papua. It extends over 692 km and is composed of the Sudirman and Jayawijaya ranges. It is part of the larger New Guinea Highlands The New Guinea Highlands, also known as the Central Range or Central Cordillera, is a long chain of mountain ranges on the island of New Guinea, including the island's highest peak, Puncak Jaya, Indonesia, , the highest mountain in Oceania. The r ... or Central Cordillera. Although ''Maoke'' means 'snow' in the local language, the glacier on Puncak Trikora in the Maoke Mountains disappeared completely some time between 1939 and 1962. References External links UGSG Satellite Image Atlas of Glaciers of the World* Mountain ranges of Western New Guinea Geography of New Guinea {{HPapua-geo-stub Mamberamo basin ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Dani People
The Dani (also spelled Ndani) are an ethnic group from the New Guinea Highlands, Central Highlands of Western New Guinea in Baliem Valley, Highland Papua, Indonesia. Around 100,000 people live in the Baliem Valley, consisting of representatives of the Dani tribes in the lower and upper parts of the valley each 20,000 and 50,000 in the middle part (with a total of 90,000 people). The areas west of the Baliem Valley are inhabited by approx 180,000, representatives of the Lani people, incorrectly called "Western Dani". All inhabitants of Baliem Valley and the surrounding areas are often called ''Dani'' hence they are also sometimes conflated with other highland tribes such as Lani in the west; Walak in the north; Nduga people, Nduga, Mek people, Mek, and Yali people, Yali in the south and east. They are one of the most populous tribes in the highlands and are found spread out through the highlands. The Dani are one of the best-known ethnic groups in Papua, due to the relatively nume ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Summit Of Wilhelminatop (P
A summit is a point on a surface that is higher in elevation than all points immediately adjacent to it. The topographic terms acme, apex, peak (mountain peak), and zenith are synonymous. The term (mountain top) is generally used only for a mountain peak that is located at some distance from the nearest point of higher elevation. For example, a big, massive rock next to the main summit of a mountain is not considered a summit. Summits near a higher peak, with some prominence or isolation, but not reaching a certain cutoff value for the quantities, are often considered ''subsummits'' (or ''subpeaks'') of the higher peak, and are considered part of the same mountain. A pyramidal peak is an exaggerated form produced by ice erosion of a mountain top. For summits that are permanently covered in significant layers of ice, the height may be measured by the highest point of rock (rock height) or the highest point of permanent solid ice (snow height). The highest summit in the world ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Wilhelmina Top New Guinea 1913 From South By P
Wilhelmina may refer to: *Wilhelmina (given name), a given name and list of people with the name People * Wilhelmina of the Netherlands (1880–1962), Queen of the Kingdom of the Netherlands from 1890 to 1948 * Wilhelmine Amalie of Brunswick (1673–1742), empress consort of the Holy Roman Empire, Queen of Germany * Wilhelmine of Bayreuth (1709–1758), German princess (the older sister of Frederick the Great) and composer * Wilhelmina of Prussia, Princess of Orange (1750–1820), German princess * Princess Wilhelmina of Schwarzburg-Rudolstadt, (1751–1780), Princess of Nassau-Saarbrücken * Wilhelmine of Prussia (1774–1837), German princess and later Queen of the Netherlands * Princess Wilhelmine of Baden (1788–1836), German Grand Duchess of Hess and the Rhine * Wilhelmina of Hesse-Darmstadt (1755–1776), German princess and Tsarevna of Russia Places * Queen Wilhelmina State Park, a park in Arkansas *Wilhelmina Bay, Antarctica *Wilhelmina Mountains, Suriname *Wilhelmi ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Geological Society Of America
The Geological Society of America (GSA) is a nonprofit organization dedicated to the advancement of the geosciences. History The society was founded in Ithaca, New York, in 1888 by Alexander Winchell, John J. Stevenson, Charles H. Hitchcock, John R. Procter and Edward Orton and has been headquartered at 3300 Penrose Place, Boulder, Colorado, US, since 1967. GSA began with 100 members under its first president, James Hall. In 1889 Mary Emilie Holmes became its first female member. It grew slowly but steadily to 600 members until 1931, when a nearly $4 million endowment from 1930 president R. A. F. Penrose Jr. jumpstarted GSA's growth. As of December 2017, GSA had more than 25,000 members in over 100 countries. The society has six regional sections in North America, three interdisciplinary interest groups, and eighteen specialty divisions. Activities The stated mission of GSA is "to advance geoscience research and discovery, service to society, stewardship of Ear ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Limestone
Limestone is a type of carbonate rock, carbonate sedimentary rock which is the main source of the material Lime (material), lime. It is composed mostly of the minerals calcite and aragonite, which are different Polymorphism (materials science), crystal forms of calcium carbonate . Limestone forms when these minerals Precipitation (chemistry), precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly Dolomite (rock), dolomite, a closely related rock, which contains a high percentage of the mineral Dolomite (mine ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Melanesian Orogeny
Melanesian is the adjectival form of Melanesia. It may refer to: * Melanesians * Melanesian mythology * Melanesian languages In linguistics, Melanesian is an obsolete term referring to the Austronesian languages of Melanesia: that is, the Oceanic, Eastern Malayo-Polynesian, or Central–Eastern Malayo-Polynesian languages apart from Polynesian and Micronesian. A ty ... See also * {{disambiguation Language and nationality disambiguation pages ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Miocene
The Miocene ( ) is the first epoch (geology), geological epoch of the Neogene Period and extends from about (Ma). The Miocene was named by Scottish geologist Charles Lyell; the name comes from the Greek words (', "less") and (', "new") and means "less recent" because it has 18% fewer modern marine invertebrates than the Pliocene has. The Miocene followed the Oligocene and preceded the Pliocene. As Earth went from the Oligocene through the Miocene and into the Pliocene, the climate slowly cooled towards a series of ice ages. The Miocene boundaries are not marked by distinct global events but by regionally defined transitions from the warmer Oligocene to the cooler Pliocene Epoch. During the Early Miocene, Afro-Arabia collided with Eurasia, severing the connection between the Mediterranean and Indian Oceans, and allowing the interchange of fauna between Eurasia and Africa, including the dispersal of proboscideans and Ape, hominoids into Eurasia. During the late Miocene, the conn ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Ice Cap
In glaciology, an ice cap is a mass of ice that covers less than of land area (usually covering a highland area). Larger ice masses covering more than are termed ice sheets. Description By definition, ice caps are not constrained by topographical features (i.e., they must lie over the top of mountains). By contrast, ice masses of similar size that ''are'' constrained by topographical features are known as ice fields. The ''dome'' of an ice cap is usually centred on the highest point of a massif. Ice flows away from this high point (the ice divide) towards the ice cap's periphery. Ice caps significantly affect the geomorphology of the area they occupy. Plastic moulding, gouging and other glacial erosional features become present upon the glacier's retreat. Many lakes, such as the Great Lakes in North America, as well as numerous valleys have been formed by glacial action over hundreds of thousands of years. The Antarctic and Greenland contain 99% of the ice volume on earth, ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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West Papua (region)
Western New Guinea, also known as Papua, Indonesian New Guinea, and Indonesian Papua, is the western half of the island of New Guinea, formerly Dutch and granted to Indonesia in 1962. Given the island is alternatively named Papua, the region is also called West Papua (). It is one of the seven geographical units of Indonesia in ISO 3166-2:ID. Lying to the west of Papua New Guinea and geographically a part of the Australian continent, the territory is almost entirely in the Southern Hemisphere and includes the Biak and Raja Ampat archipelagoes. The region is predominantly covered with rainforest where traditional peoples live, including the Dani of the Baliem Valley. A large proportion of the population live in or near coastal areas. The largest city is Jayapura. The island of New Guinea has been populated for tens of thousands of years. European traders began frequenting the region around the late 16th century due to spice trade. In the end, the Dutch Empire emerge ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Yogyakarta
Yogyakarta is the capital city of the Special Region of Yogyakarta in Indonesia, in the south-central part of the island of Java. As the only Indonesian royal city still ruled by Hamengkubuwono, a monarchy, Yogyakarta is regarded as an important centre for classical Javanese culture, Javanese fine arts and culture such as ballet, ''batik'' textiles, drama, Javanese literature, literature, music of Java, music, Javanese poetry, poetry, silversmithing, visual arts, and ''wayang'' puppetry. Renowned as a centre of Education in Indonesia, Indonesian education, Yogyakarta is home to a large student population and dozens of schools and universities, including Gadjah Mada University, the country's largest institute of higher education and one of its most prestigious. Yogyakarta is the capital of the Yogyakarta Sultanate and served as the Indonesian capital from 1946 to 1948 during the Indonesian National Revolution, with Gedung Agung as the president's office. One of the districts in s ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |