Avrig Lake
Avrig Lake ( ro, Lacul Avrig) is a glacial lake situated in the Făgăraș Mountains of Romania, in the northeastern corner of Vâlcea County. It is situated at an altitude of . The lake surface is about and the deepest point reaches . The lake has an approximately trapezoidal shape, with its length reaching around from east to west, and a maximum width of around from north to south. It is the origin of the Avrig River The Avrig is a left tributary of the river Olt in Romania. It discharges into the Olt in the town Avrig. [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
Făgăraș Mountains
The Făgăraș Mountains ( ro, Munții Făgărașului ; hu, Fogarasi-havasok) are the highest mountains of the Southern Carpathians, in Romania. Geography The mountain range is situated in the heart of Romania, at . The range is bordered in the north by the Făgăraș Depression, through which the Olt River flows, and in the west by the Olt Valley (Valea Oltului). Despite its name, Făgăraș, located to the north, is not the nearest town to the mountain range, which has no major settlements. Other important surrounding cities are Brașov and Sibiu. Glacier lakes include Bâlea (2,034 m, 46,508 m2, 11.35 m deep), the largest. The highest lake is in the Hărtopul Leaotei glacial valley. The deepest glacial lake is Podragu (2,140 m, 28,550 m2; 15.5 m deep). Other lakes are Urlea (2,170 m, 20,150 m2) and Capra (2,230 m, 18,340 m2). The highest peaks are: *'' Moldoveanu'' — *'' Negoiu'' — *'' Viștea Mare'' — *''Lespezi ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
Glacial
A glacial period (alternatively glacial or glaciation) is an interval of time (thousands of years) within an ice age that is marked by colder temperatures and glacier advances. Interglacials, on the other hand, are periods of warmer climate between glacial periods. The Last Glacial Period ended about 15,000 years ago. The Holocene is the current interglacial. A time with no glaciers on Earth is considered a greenhouse climate state. Quaternary Period Within the Quaternary, which started about 2.6 million years before present, there have been a number of glacials and interglacials. At least eight glacial cycles have occurred in the last 740,000 years alone. Penultimate Glacial Period The Penultimate Glacial Period (PGP) is the glacial period that occurred before the Last Glacial Period. It began about 194,000 years ago and ended 135,000 years ago, with the beginning of the Eemian interglacial. Last Glacial Period The last glacial period was the most recent glacial period ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
Glacial Lake
A glacial lake is a body of water with origins from glacier activity. They are formed when a glacier erodes the land and then melts, filling the depression created by the glacier. Formation Near the end of the last glacial period, roughly 10,000 years ago, glaciers began to retreat. A retreating glacier often left behind large deposits of ice in hollows between drumlins or hills. As the ice age ended, these melted to create lakes. This is apparent in the Lake District in Northwestern England where post-glacial sediments are normally between 4 and 6 metres deep. These lakes are often surrounded by drumlins, along with other evidence of the glacier such as moraines, eskers and erosional features such as striations and chatter marks. These lakes are clearly visible in aerial photos of landforms in regions that were glaciated during the last ice age. The formation and characteristics of glacial lakes vary between location and can be classified into glacial erosion lake, i ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
Romania
Romania ( ; ro, România ) is a country located at the crossroads of Central, Eastern, and Southeastern Europe. It borders Bulgaria to the south, Ukraine to the north, Hungary to the west, Serbia to the southwest, Moldova to the east, and the Black Sea to the southeast. It has a predominantly temperate- continental climate, and an area of , with a population of around 19 million. Romania is the twelfth-largest country in Europe and the sixth-most populous member state of the European Union. Its capital and largest city is Bucharest, followed by Iași, Cluj-Napoca, Timișoara, Constanța, Craiova, Brașov, and Galați. The Danube, Europe's second-longest river, rises in Germany's Black Forest and flows in a southeasterly direction for , before emptying into Romania's Danube Delta. The Carpathian Mountains, which cross Romania from the north to the southwest, include Moldoveanu Peak, at an altitude of . Settlement in what is now Romania began in the Lower Pale ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
Vâlcea County
Vâlcea County (also spelt ''Vîlcea''; ) is a county ( județ) of Romania. Located in the historical regions of Oltenia and Muntenia (which are separated by the Olt River), it is also part of the wider Wallachia region. Its capital city is Râmnicu Vâlcea. Demographics In 2011, it had a population of 355,320 and the population density was 61.63/km2. * Romanians - over 98% * Roma, others - 2% Geography This county has a total area of . The North side of the county is occupied by the mountains from the Southern Carpathians group - The Făgăraș Mountains in the east with heights over , and the Lotru Mountains in the west with heights over . They are separated by the Olt River valley - the most accessible passage between Transylvania and Muntenia. Along the Olt River Valley there are smaller groups of mountains, the most spectacular being the . Towards the South, the heights decrease, passing through the sub-carpathian hills to a high plain in the West side of ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
Avrig (river)
The Avrig is a left tributary of the river Olt in Romania. It discharges into the Olt in the town Avrig. e-calauza.ro The upper reach of the river is also known as ''Râul Mare''. Its source is the in the Făgăraș Mountains. Its length is and its basin size is . There is a dam on the Avrig river for the water supply of the town Avrig and the village of Mârșa
Mârșa is a commune located in no ...
[...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
Lakes Of Romania
This is a list of lakes of Romania. Notable lakes include Lake Sfânta Ana, the only crater lake in Romania, and Lake Razelm, the largest liman in the country. Major natural lakes Glacial lakes In volcanic craters Karstic lakes Behind natural dams In depressions On river banks On river-maritime banks Lagoons In river valleys In Danube Delta Major reservoirs Major mountain lakes Other (minor) mountain lakes Other lakes * Lake Sărat: "Sărat" = "Salty"; at its bottom is still a crust of salt. Near Brăila. A small beach. * Lake Someșu Rece: it is located in Cluj County See also * List of lakes in Bucharest * Ocna Sibiului mine#Lakes of the salt mine References External links * Paul Decei, ''Lacuri de munte'', Editura Sport–Turism, 1981 * Anuarul 2004 al Institutului Naţional de Statistică {{Romania topics * Romania Lakes A lake is an area filled with water, localized in a basin, surrounded by land, and distinct from any river o ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
Glacial Lakes
A glacial lake is a body of water with origins from glacier activity. They are formed when a glacier erodes the land and then melts, filling the depression created by the glacier. Formation Near the end of the last glacial period, roughly 10,000 years ago, glaciers began to retreat. A retreating glacier often left behind large deposits of ice in hollows between drumlins or hills. As the ice age ended, these melted to create lakes. This is apparent in the Lake District in Northwestern England where post-glacial sediments are normally between 4 and 6 metres deep. These lakes are often surrounded by drumlins, along with other evidence of the glacier such as moraines, eskers and erosional features such as striations and chatter marks. These lakes are clearly visible in aerial photos of landforms in regions that were glaciated during the last ice age. The formation and characteristics of glacial lakes vary between location and can be classified into glacial erosion lake, ice ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |