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Bogićevica
Богићевица; ) is a mountain area in the Accursed Mountains">Rops (peak)">Rops Bogićevica ( sr-Cyrl">Богићевица; ) is a mountain area in the Accursed Mountains (Prokletije) mountain range. It spreads over Montenegro, Kosovo and Albania. It is about 15 km long and 10 km wide. The mountain area has a number of peaks higher than 2000 m and two higher than 2500 m. Marijash (2533 m) and Maja e Ropës (2502 m) are both located in Kosovo. The towns of Deçan in Kosovo and Tropojë in Albania are located near the area. Geography, topography, and geology Bogićevica is located in the eastern part of the Prokletije (Accursed Mountains) system. It occupies a nodal geographic position on the main watershed of the Balkan Peninsula, situated between the Lim River valley to the west and the Metohija basin to the east. The main ridge has a sub-meridional direction extending from Čakor Pass in the north to Trekufiri (Trigranichni) Peak (2356 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Accursed Mountains
The Accursed Mountains (; sh-Latn-Cyrl, Prokletije, Проклетије, separator=" / ", ; both translated as "Cursed Mountains"), also known as the Albanian Alps (; sh-Latn-Cyrl, Albanski Alpi, Албански Алпи, separator=" / ", link=no), is a mountain range in coastal Southeast Europe adjacent to the Adriatic Sea. It is the southernmost subrange of the Dinaric Alps range (Dinarides), extending from northern Albania to western Kosovo and northeastern Montenegro. Maja Jezercë, standing at , is the highest point of the Accursed Mountains and of all Dinaric Alps, and the List of mountains in Albania, fifth highest peak in Albania. The range includes the mountain Zla Kolata, which, at , is the tallest mountain in Montenegro. The range also includes the mountain Gjeravica, which, at , is the second tallest mountain in Kosovo. One of the southernmost glaciers, glacial masses in Europe was discovered in the Albanian part of the range in 2009. Name The origin of the nam ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Trekufiri
Trekufiri (also known as ''Tromedja'' or Тромеђа in Montenegrin Cyrillic), is a mountain located in the Albanian Alps and the Bogićevica range. Perched at above sea level, its summit marks the border where Albania, Kosovo, and Montenegro intersect. The height of the three-country point varies, with Albanian maps recording the mountain's height as above sea level while official Yugoslavian sources state it as 2,366 m. After the dissolution of Serbia and Montenegro in 2006, followed by the establishment of the Republic of Kosovo two years later, a binational administrative three-point border emerged. Geology Trekufiri is situated in the heart of the Albanian Alps and Bogićevica range, where three ridges converge. The mountain ranges to the west on the Albania-Montenegro border are slightly less elevated. The ridge to the southeast, which forms the border between Albania and Kosovo, leads to Bogiçaj . The highest mountain in the region, Gjeravica , is located anoth ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Maja E Ropës
Rops is a mountain in Kosovo with a height of . It is a part of Bogićevica area in the Accursed Mountains. It is the second highest mountain in the Bogićevica area after Marijash at . References Mountains of Kosovo Accursed Mountains Two-thousanders of Kosovo {{Kosovo-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Marijash
Marijash (; , ''Marijaš'') or Bogdaš (Богдаш) is a mountain in Kosovo in the Accursed Mountains. At high, it is the highest peak of the Bogićevica Богићевица; ) is a mountain area in the Accursed Mountains">Rops (peak)">Rops Bogićevica ( sr-Cyrl">Богићевица; ) is a mountain area in the Accursed Mountains (Prokletije) mountain range. It spreads over Montenegro, Kosovo an ... area and one of the highest peaks in the Accursed Mountains in Kosovo. The mountain is located near the Montenegrin border. References Mountains of Kosovo Accursed Mountains Two-thousanders of Kosovo {{Kosovo-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Granite
Granite ( ) is a coarse-grained (phanerite, phaneritic) intrusive rock, intrusive igneous rock composed mostly of quartz, alkali feldspar, and plagioclase. It forms from magma with a high content of silica and alkali metal oxides that slowly cools and solidifies underground. It is common in the continental crust of Earth, where it is found in igneous intrusions. These range in size from dike (geology), dikes only a few centimeters across to batholiths exposed over hundreds of square kilometers. Granite is typical of a larger family of ''granitic rocks'', or ''granitoids'', that are composed mostly of coarse-grained quartz and feldspars in varying proportions. These rocks are classified by the relative percentages of quartz, alkali feldspar, and plagioclase (the QAPF diagram, QAPF classification), with true granite representing granitic rocks rich in quartz and alkali feldspar. Most granitic rocks also contain mica or amphibole minerals, though a few (known as leucogranites) conta ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Schist
Schist ( ) is a medium-grained metamorphic rock generally derived from fine-grained sedimentary rock, like shale. It shows pronounced ''schistosity'' (named for the rock). This means that the rock is composed of mineral grains easily seen with a low-power hand lens, oriented in such a way that the rock is easily split into thin flakes or plates. This texture (geology), texture reflects a high content of platy minerals, such as mica, talc, chlorite group, chlorite, or graphite. These are often interleaved with more granular minerals, such as feldspar or quartz. Schist typically forms during regional metamorphism accompanying the process of mountain building (orogeny) and usually reflects a medium Metamorphism#Metamorphic grades, grade of metamorphism. Schist can form from many different kinds of rocks, including sedimentary rocks such as mudstones and igneous rocks such as tuffs. Schist metamorphosed from mudstone is particularly common and is often very rich in mica (a ''mica schis ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Quartz
Quartz is a hard, crystalline mineral composed of silica (silicon dioxide). The Atom, atoms are linked in a continuous framework of SiO4 silicon–oxygen Tetrahedral molecular geometry, tetrahedra, with each oxygen being shared between two tetrahedra, giving an overall chemical formula of Silicon dioxide, SiO2. Quartz is, therefore, classified structurally as a Silicate mineral#Tectosilicates, framework silicate mineral and compositionally as an oxide mineral. Quartz is the second most abundant mineral in Earth's continental crust, behind feldspar. Quartz exists in two forms, the normal α-quartz and the high-temperature β-quartz, both of which are chiral. The transformation from α-quartz to β-quartz takes place abruptly at . Since the transformation is accompanied by a significant change in volume, it can easily induce microfracturing of ceramics or rocks passing through this temperature threshold. There are many different varieties of quartz, several of which are classifi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Permian–Triassic Extinction Event
The Permian–Triassic extinction event (also known as the P–T extinction event, the Late Permian extinction event, the Latest Permian extinction event, the End-Permian extinction event, and colloquially as the Great Dying,) was an extinction event that occurred approximately 251.9 Million years ago, million years ago (mya), at the boundary between the Permian and Triassic geologic periods, and with them the Paleozoic and Mesozoic eras. It is Earth's most severe known extinction event, with the extinction of 57% of Family (biology), biological families, 62% of genera and 81% of marine biology, marine species, (previous estimates of 90–96% marine species extinction were due to historical conflation with the End-Capitanian mass extinction event, end-Capitanian mass extinction which occurred 7–10 million years earlier) and 70% of terrestrial vertebrate species. It is also the greatest known mass extinction of insects. It is the greatest of the "Big Five" mass extinctions of t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Paleogene
The Paleogene Period ( ; also spelled Palaeogene or Palæogene) is a geologic period and system that spans 43 million years from the end of the Cretaceous Period Ma (million years ago) to the beginning of the Neogene Period Ma. It is the first period of the Cenozoic Era, the tenth period of the Phanerozoic and is divided into the Paleocene, Eocene, and Oligocene epochs. The earlier term Tertiary Period was used to define the time now covered by the Paleogene Period and subsequent Neogene Period; despite no longer being recognized as a formal stratigraphic term, "Tertiary" still sometimes remains in informal use. Paleogene is often abbreviated "Pg", although the United States Geological Survey uses the abbreviation "" for the Paleogene on the Survey's geologic maps. Much of the world's modern vertebrate diversity originated in a rapid surge of diversification in the early Paleogene, as survivors of the Cretaceous–Paleogene extinction event took advantage of empty ecolo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Marble
Marble is a metamorphic rock consisting of carbonate minerals (most commonly calcite (CaCO3) or Dolomite (mineral), dolomite (CaMg(CO3)2) that have recrystallized under the influence of heat and pressure. It has a crystalline texture, and is typically not Foliation (geology), foliated (Layered intrusion, layered), although there are exceptions. In geology, the term ''marble'' refers to metamorphosed limestone, but its use in stonemasonry more broadly encompasses unmetamorphosed limestone. The extraction of marble is performed by quarrying. Marble production is dominated by four countries: China, Italy, India and Spain, which account for almost half of world production of marble and decorative stone. Because of its high hardness and strong wear resistance, and because it will not be deformed by temperature, marble is often used in Marble sculpture, sculpture and construction. Etymology The word "marble" derives from the Ancient Greek (), from (), "crystalline rock, shin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mesozoic
The Mesozoic Era is the Era (geology), era of Earth's Geologic time scale, geological history, lasting from about , comprising the Triassic, Jurassic and Cretaceous Period (geology), Periods. It is characterized by the dominance of archosaurian reptiles such as the dinosaurs, and of Gymnosperm, gymnosperms such as cycads, ginkgoaceae and Araucariaceae, araucarian conifers; a hot Greenhouse and icehouse earth, greenhouse climate; and the tectonic break-up of Pangaea. The Mesozoic is the middle of the three eras since Cambrian explosion, complex life evolved: the Paleozoic, the Mesozoic, and the Cenozoic. The era began in the wake of the Permian–Triassic extinction event, the largest mass extinction in Earth's history, and ended with the Cretaceous–Paleogene extinction event, another mass extinction whose victims included the non-avian dinosaurs, Pterosaur, pterosaurs, Mosasaur, mosasaurs, and Plesiosaur, plesiosaurs. The Mesozoic was a time of significant tectonic, climatic, an ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
