Bâsca Chiojdului River
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Bâsca Chiojdului River
The Bâsca ( ro, Bɨs'ca), also called ''Bâsca Mare'' in its upper course, and ''Bâsca Roziliei'' in its lower course, is a left tributary of the river Buzău, in Romania. It discharges into the Buzău near Nehoiu. Geographic position Positioned in the external region of the curvature of Carpathians (subunit of Eastern Carpathians), the Bâsca drainage basin has an area of . Its length is . It lies at an average altitude of 1,081 m between the LăcăuÈ›i Peak (1,777 m altitude) and the confluence with the Buzău River (385 m altitude). Geology From the geological point of view, the Bâsca River Catchment overlaps the orogenic unit of the Eastern Carpathians, where the external Paleogene flysch is predominant, including: sandstones (Tarcău sandstones Facies), marl, conglomerates. This area is characterised by tectonic uplift and by severe seismicity related to the Vrancea Epicentral Area, being affected by deep-seated landslides (Ielenicz, 1984). Lithology i ...
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Covasna County
Covasna County (, hu, Kovászna megye, ) is a county ( județ) of Romania, in eastern Transylvania, with the county seat at Sfântu Gheorghe. Demographics In 2011, it had a population of 210,177, making it the second least populous of Romania's 41 counties and the population density was . In 2002 the ethnic composition of the county was as follows: * Hungarians – 73.58% (or 164,158) * Romanians – 23.28% (or 51,790) * Romani – 2.68% (or 5,973) According to the 2011 census, the composition of the county was: * Hungarians – 73.74% (or 150,468) * Romanians – 22.02% (or 45,021) * Romani – 4.05% (or 8,267) * Others - 0.19% Covasna County has the second-greatest percentage of Hungarian population in Romania, just behind the neighboring county of Harghita. The Hungarians of Covasna are primarily Székelys. Geography Covasna county has a total area of . The main part of the relief consists of mountains from the Eastern Carpathians group. Most localities can be found ...
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Conglomerate (geology)
Conglomerate () is a clastic sedimentary rock that is composed of a substantial fraction of rounded to subangular gravel-size clasts. A conglomerate typically contains a matrix of finer-grained sediments, such as sand, silt, or clay, which fills the interstices between the clasts. The clasts and matrix are typically cemented by calcium carbonate, iron oxide, silica, or hardened clay. Conglomerates form by the consolidation and lithification of gravel. They can be found in sedimentary rock sequences of all ages but probably make up less than 1 percent by weight of all sedimentary rocks. In terms of origin and depositional mechanisms, they are closely related to sandstones and exhibit many of the same types of sedimentary structures, e.g., tabular and trough cross-bedding and graded bedding.Boggs, S. (2006) ''Principles of Sedimentology and Stratigraphy.'', 2nd ed. Prentice Hall, New York. 662 pp. Friedman, G.M. (2003) ''Classification of sediments and sedimentary rocks.'' In G ...
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Milei
The Milei (also: ''Milea'' or ''Pârâul Milei'') is a left tributary of the river Bâsca in Romania Romania ( ; ro, România ) is a country located at the crossroads of Central Europe, Central, Eastern Europe, Eastern, and Southeast Europe, Southeastern Europe. It borders Bulgaria to the south, Ukraine to the north, Hungary to the west, S .... Its length is and its basin size is . References Rivers of Romania Rivers of Buzău County {{Buzău-river-stub ...
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Cernat (Bâsca)
The Cernat is a left tributary of the river Bâsca in Romania Romania ( ; ro, România ) is a country located at the crossroads of Central Europe, Central, Eastern Europe, Eastern, and Southeast Europe, Southeastern Europe. It borders Bulgaria to the south, Ukraine to the north, Hungary to the west, S .... Its length is and its basin size is . References Rivers of Romania Rivers of Buzău County {{Buzău-river-stub ...
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Pătac
The Pătac is a left tributary of the river Bâsca in Romania Romania ( ; ro, România ) is a country located at the crossroads of Central Europe, Central, Eastern Europe, Eastern, and Southeast Europe, Southeastern Europe. It borders Bulgaria to the south, Ukraine to the north, Hungary to the west, S .... Its length is and its basin size is . References Rivers of Romania Rivers of Buzău County {{Buzău-river-stub ...
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Slobod
The Slobod is a left tributary of the river Bâsca in Romania Romania ( ; ro, România ) is a country located at the crossroads of Central Europe, Central, Eastern Europe, Eastern, and Southeast Europe, Southeastern Europe. It borders Bulgaria to the south, Ukraine to the north, Hungary to the west, S .... Its length is and its basin size is . References Rivers of Romania Rivers of Covasna County {{Covasna-river-stub ...
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Ghiurca Mare
The Ghiurca Mare is a left tributary of the river Bâsca in Romania. It discharges into the Bâsca near Comandău Comandău ( hu, Komandó, Hungarian pronunciation: ) is a commune in Covasna County, Transylvania, Romania. It is composed of a single village, Comandău. It formed part of the Székely Land region of the historical Transylvania province. It ser .... Its length is and its basin size is . References Rivers of Romania Rivers of Covasna County {{Covasna-river-stub ...
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Delușor
The Delușor (also: ''Holom'' or ''Cuțan'') is a left tributary of the river Bâsca in Romania. It flows into the Bâsca near Comandău Comandău ( hu, Komandó, Hungarian pronunciation: ) is a commune in Covasna County, Transylvania, Romania. It is composed of a single village, Comandău. It formed part of the Székely Land region of the historical Transylvania province. It ser .... Its length is and its basin size is . References Rivers of Romania Rivers of Covasna County {{Covasna-river-stub ...
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Precipitation (meteorology)
In meteorology, precipitation is any product of the condensation of atmospheric water vapor that falls under gravitational pull from clouds. The main forms of precipitation include drizzle, rain, sleet, snow, ice pellets, graupel and hail. Precipitation occurs when a portion of the atmosphere becomes saturated with water vapor (reaching 100% relative humidity), so that the water condenses and "precipitates" or falls. Thus, fog and mist are not precipitation but colloids, because the water vapor does not condense sufficiently to precipitate. Two processes, possibly acting together, can lead to air becoming saturated: cooling the air or adding water vapor to the air. Precipitation forms as smaller droplets coalesce via collision with other rain drops or ice crystals within a cloud. Short, intense periods of rain in scattered locations are called showers. Moisture that is lifted or otherwise forced to rise over a layer of sub-freezing air at the surface may be condense ...
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Föhn
A Foehn or Föhn (, , ), is a type of dry, relatively warm, downslope wind that occurs in the leeward, lee (downwind side) of a mountain range. It is a rain shadow wind that results from the subsequent adiabatic warming of air that has dropped most of its moisture on windward slopes (see orographic lift). As a consequence of the different adiabatic lapse rates of moist and dry air, the air on the leeward slopes becomes warmer than equivalent elevations on the windward slopes. Foehn winds can raise temperatures by as much as 14 Â°C (25 Â°F) in just a matter of hours. Switzerland, southern Germany and Austria have a warmer climate due to the Foehn, as moist winds off the Mediterranean Sea blow over the Alps. Etymology The name ''Foehn'' (german: Föhn, ) arose in the Alps, Alpine region. Originating from Latin ''(ventus) favonius'', a mild west wind of which Anemoi, Favonius was the Roman personification and probably transmitted by rm, favuogn or just ''fuogn'', the te ...
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Continental Climate
Continental climates often have a significant annual variation in temperature (warm summers and cold winters). They tend to occur in the middle latitudes (40 to 55 north), within large landmasses where prevailing winds blow overland bringing some precipitation, and temperatures are not moderated by oceans. Continental climates occur mostly in the Northern Hemisphere due to the large landmasses found there. Most of northern and northeastern China, eastern and southeastern Europe, Western and north western Iran, central and southeastern Canada, and the central and northeastern United States have this type of climate. Continentality is a measure of the degree to which a region experiences this type of climate. In continental climates, precipitation tends to be moderate in amount, concentrated mostly in the warmer months. Only a few areas—in the mountains of the Pacific Northwest of North America and in Iran, northern Iraq, adjacent Turkey, Afghanistan, Pakistan, and Central Asia†...
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Climate
Climate is the long-term weather pattern in an area, typically averaged over 30 years. More rigorously, it is the mean and variability of meteorological variables over a time spanning from months to millions of years. Some of the meteorological variables that are commonly measured are temperature, humidity, atmospheric pressure, wind, and precipitation. In a broader sense, climate is the state of the components of the climate system, including the atmosphere, hydrosphere, cryosphere, lithosphere and biosphere and the interactions between them. The climate of a location is affected by its latitude/longitude, terrain, altitude, land use and nearby water bodies and their currents. Climates can be classified according to the average and typical variables, most commonly temperature and precipitation. The most widely used classification scheme was the Köppen climate classification. The Thornthwaite system, in use since 1948, incorporates evapotranspiration along with temperature ...
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