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Maja E Thatë
) , photo_size = , elevation_m = 2406 , elevation_ref = , prominence_m = , prominence_ref = , listing = , range = Albanian Alps , location = Albania , map = Albania#Montenegro , range_coordinates = , map_caption = , map_size = , label_position = bottom , coordinates = , coordinates_ref = , type = dolomite, Limestone , age = Triassic , first_ascent = , easiest_route = Rock climbing , language = Albanian , module = Maja e Thatë is a mountain peak of the Albanian Alps (Accursed Mountains) in Albania.Military topographic map of Albania (1:25 000): K-34-52-D-a (M. JEZERCES) It is located within Valbonë Valley National Park, roughly nort ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Albanian Alps
The Accursed Mountains ( sq, Bjeshkët e Nemuna; sh-Cyrl-Latn, Проклетије, Prokletije, ; both translated as "Cursed Mountains"), also known as the Albanian Alps ( sq, Alpet Shqiptare), are a mountain group in the western part of the Balkans. It is the southernmost subrange of the Dinaric Alps range (Dinarides), extending from northern Albania to southern Kosovo and northeastern Montenegro. Maja Jezercë, standing at , is the highest point of the Accursed Mountains and of all Dinaric Alps, and the fifth highest peak in Albania. The highest peak in Montenegro, Zla Kolata at and the second-highest in Kosovo, Gjeravica at are also part of the range. One of the southernmost glacial masses in Europe was discovered in the Albanian part of the range in 2009. Name Ptolemy mentioned , which has been connected to the Accursed Mountains. Bertiscus lives on artificially in the form ''bertiscae'' in the scientific names for endemic species that have their ''locus classicus'' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rosni Peak
Rosni Peak ( sr, Росни врх, Rosni vrh; sq, Maja e Rosit) is the highest peak of the Bjelić mountain, which is part of the Accursed Mountains range and located on the Montenegrin–Albanian border. It is 2,524 m (8,280 feet) high, making it the third highest mountain peak in Montenegro ) , image_map = Europe-Montenegro.svg , map_caption = , image_map2 = , capital = Podgorica , coordinates = , largest_city = capital , official_languages = M .... References External links Rosni Vrh (Maja Rosit) SummitPost.org. Mountains of Albania Mountains of Montenegro Accursed Mountains Albania–Montenegro border {{Montenegro-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Periglacial
Periglaciation (adjective: "periglacial", also referring to places at the edges of glacial areas) describes geomorphic processes that result from seasonal thawing of snow in areas of permafrost, the runoff from which refreezes in ice wedges and other structures. "Periglacial" suggests an environment located on the margin of past glaciers. However, freeze and thaw cycles influence landscapes outside areas of past glaciation. Therefore, periglacial environments are anywhere that freezing and thawing modify the landscape in a significant manner. Tundra is a common ecological community in periglacial areas. History Periglaciation became a distinct subject within the study of geology after Walery Łoziński, a Polish geologist, introduced the term in 1909. Łoziński drew upon the early work of Johan Gunnar Andersson. According to Alfred Jahn, his introduction of his work at the 1910 International Geological Congress held in Stockholm caused significant discussion. In the field trip ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Trough (geology)
In geology, a trough is a linear structural depression that extends laterally over a distance. Although it is less steep than a trench, a trough can be a narrow basin or a geologic rift. These features often form at the rim of tectonic plates. There are various oceanic troughs on the ocean floors. Examples of oceanic troughs * Benue Trough * Cayman Trough * Kings Trough * Hesperides Trough * Nankai Trough * Northumberland Trough * Okinawa Trough in the East China Sea * Rockall Trough and others along the rift of the mid-oceanic ridge * Salton Trough * South Shetland Trough * Suakin TroughDinwiddie, Robert et al. (2008) ''Ocean: The World's Last Wilderness Revealed'', London, Dorling Kindersley, page 452. in the Red Sea * Timor Trough See also * Walker Lane * Oceanic basin In hydrology, an oceanic basin (or ocean basin) is anywhere on Earth that is covered by seawater. Geologically, ocean basins are large geologic basins that are below sea level. Most ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Carbonate Rock
Carbonate rocks are a class of sedimentary rocks composed primarily of carbonate minerals. The two major types are limestone, which is composed of calcite or aragonite (different crystal forms of CaCO3), and dolomite rock (also known as dolostone), which is composed of mineral dolomite (CaMg(CO3)2). Calcite can be either dissolved by groundwater or precipitated by groundwater, depending on several factors including the water temperature, pH, and dissolved ion concentrations. Calcite exhibits an unusual characteristic called retrograde solubility in which it becomes less soluble in water as the temperature increases. When conditions are right for precipitation, calcite forms mineral coatings that cement the existing rock grains together or it can fill fractures. Karst topography and caves develop in carbonate rocks because of their solubility in dilute acidic groundwater. Cooling groundwater or mixing of different groundwaters will also create conditions suitable for cave ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Anticline
In structural geology, an anticline is a type of fold that is an arch-like shape and has its oldest beds at its core, whereas a syncline is the inverse of an anticline. A typical anticline is convex up in which the hinge or crest is the location where the curvature is greatest, and the limbs are the sides of the fold that dip away from the hinge. Anticlines can be recognized and differentiated from antiforms by a sequence of rock layers that become progressively older toward the center of the fold. Therefore, if age relationships between various rock strata are unknown, the term antiform should be used. The progressing age of the rock strata towards the core and uplifted center, are the trademark indications for evidence of anticlines on a geologic map. These formations occur because anticlinal ridges typically develop above thrust faults during crustal deformations. The uplifted core of the fold causes compression of strata that preferentially erodes to a deeper st ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Maja Grykat E Hapëta
Maja Grykat e Hapëta is a mountain located in northern Albania in the Bjeshkët e Namuna. It is found to the southeast of Maja Jezercë, south of the upper Valbonë valley. It is one of the highest mountains in the mountain range at high. In fact, it is the third highest after Maja Jezercë at in Albania and Gjeravica at in Kosovo Kosovo ( sq, Kosova or ; sr-Cyrl, Косово ), officially the Republic of Kosovo ( sq, Republika e Kosovës, links=no; sr, Република Косово, Republika Kosovo, links=no), is a partially recognised state in Southeast Euro .... Like many of the other mountains surrounding it, Maja Grykat e Hapëta has a stony texture near its summit. Maja Grykat e Hapëta belongs to the group of peaks called Majet e Zabores where there are 10 peaks that are higher than . summitpost.org Refe ...
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Monocline
A monocline (or, rarely, a monoform) is a step-like fold in rock strata consisting of a zone of steeper dip within an otherwise horizontal or gently-dipping sequence. Formation Monoclines may be formed in several different ways (see diagram) * By differential compaction over an underlying structure, particularly a large fault at the edge of a basin due to the greater compactibility of the basin fill, the amplitude of the fold will die out gradually upwards. * By mild reactivation of an earlier extensional fault during a phase of inversion causing folding in the overlying sequence. * As a form of fault propagation fold during upward propagation of an extensional fault in basement into an overlying cover sequence. * As a form of fault propagation fold during upward propagation of a reverse fault in basement into an overlying cover sequence. Examples * Waterpocket Fold in Capitol Reef National Park, Utah *Comb Ridge in southern Utah * Grandview-Phantom Monocline in Grand Can ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Montenegro
) , image_map = Europe-Montenegro.svg , map_caption = , image_map2 = , capital = Podgorica , coordinates = , largest_city = capital , official_languages = Montenegrin , languages2_type = Languages in official use , languages2 = , ethnic_groups = , ethnic_groups_year = 2011 , religion = , religion_year = 2011 , demonym = Montenegrin , government_type = Unitary parliamentary republic , leader_title1 = President , leader_name1 = Milo Đukanović , leader_title2 = Prime Minister , leader_name2 = Dritan Abazović (acting) , leader_title3 = Speaker , leader_name3 = Danijela Đurović , legislature = Skupština , sovereignty_type = Establishment history , established_event1 = Principality of Duklja , established_date1 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Vusanje
Vusanje ( sq, Vuthaj; cnr, Vusanje/Вусање) is a village in Gusinje Municipality, Montenegro. According to the 2003 census, the town had 648 inhabitants. Geography Vusanje is located within the Plav municipality, below the town of Gusinje. It is located in the geographical region of Prokletije mountain, in the basin of the Lim river. There is a notable waterfall Grlja. History The village was settled by ancestors of the Kelmendi region of Albania, by Gjonbalaj and Nik Bala family. Until 1912, it was part of Ottoman Empire. During the First Balkan War in 1912 it became part of the Kingdom of Montenegro. The village is made up of two settlements, Katundi i siper (upper village) and katundi i ulet (lower village). Also there is a hamlet called Zarunic. Post 1913, the village was subjected to repression and discrimination from the Montenegrin and Yugoslavian governments. The result was the expulsion of the 90% of the population to the United States, mostly in the New York area. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ordinal Direction
The four cardinal directions, or cardinal points, are the four main compass directions: north, east, south, and west, commonly denoted by their initials N, E, S, and W respectively. Relative to north, the directions east, south, and west are at 90 degree intervals in the clockwise direction. The ordinal directions (also called the intercardinal directions) are northeast (NE), southeast (SE), southwest (SW), and northwest (NW). The intermediate direction of every set of intercardinal and cardinal direction is called a secondary intercardinal direction. These eight shortest points in the compass rose shown to the right are: # West-northwest (WNW) # North-northwest (NNW) # North-northeast (NNE) # East-northeast (ENE) # East-southeast (ESE) # South-southeast (SSE) # South-southwest (SSW) # West-southwest (WSW) Points between the cardinal directions form the points of the compass. Arbitrary horizontal directions may be indicated by their azimuth angle value. Determination Addi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
