TRABZON PROVİCE
TRABZON RESİMLER
TRABZON FOTOĞRAFLAR
TRABZON MANZARALAR
TRABZON GÖRÜNTÜLER
TRABZON TANITIM
TRABZON TARİH
TRABZON COĞRAFYA
TRABZON KÜLTÜR
TRABZON KİLİSE
TRABZON MANASTIR
TRABZON KARADENİZ
TRABZON RESİMLER
TRABZON FOTOĞRAFLAR
TRABZON MANZARALAR
TRABZON GÖRÜNTÜLER
TRABZON TANITIM
TRABZON TARİH
TRABZON COĞRAFYA
TRABZON KÜLTÜR
TRABZON KİLİSE
TRABZON MANASTIR
TRABZON KARADENİZ
The city center from the sea in the north, south, rises in terraces are not as smooth as on Boztepe. Degirmendere, Kuzgundere (or Tannery) and placement Zagnos streams from south to north, divided the deep straits. Tannery and Zagnos between streams and a high table in the form of non-uniform over an area of the city known eneski settlement remains have been identified. for this reason that the name of the former Trabzon Grekçe table or trapezoid / trapezium format as for "Trapezos" word view that is gaining weight. Trabzon, on behalf Trapezos the first time, the Greek commander, penned by Kesnophon, BC 4. Century, the events described in the "Anabasis" by the ancient sources are found.
BC Western Anatolia after the ion-based Miletoslular 7. The Black Sea coast in the coming century, colonial cities have set up. Trabzon, Sinop, which is the center of these colonies, and many researchers have considered, as the dryness of the city's first show of this period. But Kolkhlar, Driller, the macro from the indigenous tribes, such as has been previously lived in the vicinity of Trabzon.
BC Macedonian King Alexander the Great All in Anatolia in 334 put an end to the domination of Persia.
BC I. Century, the occupation of Anatolia by the Romans in the west have begun to strength. Pompeius, the King of Pontus, the Roman king of the V. Kelkit valley defeat inflicted on the Kingdom of Pontus Mithridates distributed. Thus, Trabzon, BC Roman rule in 66 years, has entered. BC with Rome Avgustus'la Since 27 started the Empire period. Augustus as a result of administrative arrangement of Trabzon, have formed part of the Pontic Polemoniacus called vassalage, the emperor Tiberius (AD 14-37), the other an administrative department of the State of which remained within the borders of Cappadocia. In the period of the emperor Nero (54-68) has been acquired the privilege of being free city. During this period of Trabzon "famous" and "rich" definition, the city is located in the books of historians. Emphasis on the defense of the Roman Empire, the eastern limit of the time of Vespasian (69-79) in Trabzon, have been included in the state of Cappadocia-Galatia.
The famous Roman emperor Hadrian Era (117-138) as well as the entire empire in Trabzon, the major construction activities, HAS, many religious and military buildings and roads, aqueducts, and, until recently, an artificial port that can be seen the ruins of Hadrian was built after the Trabzon s heyday ended, 244 were deprived of jurisdiction in the printing of money. Trabzon printed on the front of the coins of the emperors of the Roman Period yüzlerindeRoma bust, but the reverse side has prevailed since the time of the kingdom of Pontus and his mythological figures given in the script has been used Grekçe.
The Roman empire was divided into two in 395, Trabzon, Istanbul center of the Eastern Roman / Byzantine Empire remained within the borders. Byzantine emperor Justinian (527-564) restored the city walls in Trabzon ettirerek launched a new development activity. The time of Heraclius (610-641) the empire started to leave the military areas, Trabzon, Teophilos time (829-842) has been established Khaldia central theme.
I. After receipt of the Kingdom of Trabzon Komnenos in 1398 Bayezid Samsun region to the Ottoman Empire were forced to pay an annual tax. David Komnenos, during his reign (1458-1461), pay taxes, by stopping the advance paid back through the Akkoyunlu State asked Sultan Uzun Hasan, the alliance made a proposal to the great states of Europe against the Ottomans. Forces led by the Ottoman Sultan Mehmed II laid siege to this region, conquered Trabzon in 1461 and put an end to the sovereignty of Komnenosların.
During the First World War, the Russians attacked Trabzon (April 14, 1916). Trabzonlulardan of the strike forces (militia), give the guerrilla warfare during this attack. This time, the ammunition to the front to be sent to the port of Trabzon Trabzon support Hamidiye battleship gençlerce Macka moved to pour in with great enthusiasm.
Valleys formed by rivers, especially the arms and the second-order streams, where the side sections very dardırlar involved in them. This feature is dominated by the majority of the site. Character of the area's humid climate, watersheds, and more freight transport is a fast-flowing, deep-abrasive played a major role. Which is vulnerable to wear tuff, agglomerate and limestone buildings, on the one hand konsekant vertical erosion accelerated in the arms perpendicular to develop "V"-shaped valleys formed, on the other hand, this also occurred on the slopes of the valleys and slopes of the secondary arms thoroughly slaugh increased their discharge activity. So today, in the field of vaccine dantritik drainage system consists of the valley descending towards the sea, sat a uniform. Even though you have moved into a small area of erosion debris near the base of valley slopes, the accumulation of low-, low-sloping plains formed part. At the same time suitable for carrying any of these areas.
East of the west of the province of Trabzon Değirmendere Karadere Folder and resources, and gutters Solakli Horos, Onions, and is Haldizen Mountains. Folder, Degirmendere, Karadere and Solakli creek basins in the south up to each other reaping the smaller river basins in the form Kalenima, Yambol Creek, Küçükdere and Manahos River, a short length and very narrow valleys meydaa bring fast flows. The occurrence of different rocks in the slope, roughness is a factor which reinforces the other. Sedimentary and volcanic sediment character, easy to carry aşınırken surfaces, volcanic rocks, exposing the normal slope along the slope surfaces have formed a high level.
Rivers into the Black Sea, during the Pleistocene sea-level rise due to lower altitudes, significant effects were found on coastal erosion and deposition activities. Beds, 90 m yarmışlar up to the last post-glacial period, sea level rise depending on the aktıkları boşulmuş valleys, the sea, the valley mouths indentation made towards the land. Then silt brought by rivers, has led to the development of the shape of a valley filled. The most important of these is the length of the coast about 4 km from the Degirmendere Delta today., A 3.5 km extension into the valley. km2 and is close to area 7. In other deltas Vakfıkebir Fol Creek, Star Creek Greenhouse, Kalenima Söğütlü Creek, Yomra Yomra creek, creek, Yalıboyu Yambol, Karadere Arakli, Small Dere Cavuslu Down, Toggle Creek Manahos Of near the creek and created a more narrow alluvial düzlüklerdir Solakli.
Trabzon Province in the north polar air masses, the transition area is located on the south, tropical air masses. In winter, the Sun in the apparent movements, depending on the tropical south, falling Basınç'ın Yuksel, usually come from the north who had settled in Anatolia on the high point of land north of Siberia and Eastern Europe, located on the polar Antisiklonu'nun cava under the influence of the mass of property is a convergence area. However, the area close to the earth, winter temperatures, the presence in the north of the Black Sea and the coast extending from as close to the set because of the presence of the Eastern Black Sea Mountains, it becomes temperate latitudes when compared to other fields. Rainfall, near-shore areas, rain, snow is usually the middle and high areas.
In summer, sections of the atmosphere close to earth, the Azores High Pressure Low Pressure Centre Area extensions developed between the north and Basra sector carried moist air flows over the land masses and the Black Sea, coastal areas leads to precipitation orografk, from time to time inserted into the cool air raids in the north with the cold front also frequently seen torrential rains, the cold air drops in cases of high levels with plenty of great instability and unpredictable developments in the fall yağıılar. The average temperature during this season in the region around 18.8 ° C
frequencies of wind direction in our province, area of contact centers, movement of the pressure, in the shape of features and is under the influence of the Black Sea. Winds blowing from the north and south by land and sea breeze winds dominance feels way. Close to the sea areas south and southwest winds are more effective. Winds blow-dry February, March and April, are seen and may find an annual average of twelve days.
Rates are high relative humidity in summer, especially in the area and observed limit to expanding inland. This season the Black Sea north of the evaporation, when the air is calm and keep close to the shore segments under the influence of the low pressure center over time, moving towards the southern areas of high winds, thanks to Mary, moved here because of the moisture directly from the highland areas, which often continues until noon on a clear open- valleys throughout the state of the weather, then rising water vapor, completely covering the pitch, and sometimes for days çekilmemektedir.
One moves towards the glacial valleys of the peaks showing the distribution of almost every valley, about twenty, some of them one by one after another gideşenle interconnected glacial lakes located in areas ranging from 100-1900 m2 wide. Karagol, Sarigöl, Fish Lake and Stallion can be considered as the most important of lakes. Demirkapı, North slopes of these mountains are right and Multat streams resources. Each one of the board of the glacial valleys of the rivers undersized. Side starts to receive streams of approximately 2000 m. To the north, with the increasing levels of fluvial topography from the moving forces begin to announce themselves thoroughly. Important tributary creek to the east Solakli Haldizen Creek, Demirkapı, right, and brooks, with the participation of the North, 1,150 m. Multat Uzungöl reaches levels. Continuing on from here under the name Black Creek Solakli confused.
Further west of the fault is a thrust from the mass of bulbous mountains between the Upper Cretaceous-Eocene oil rhyolite and dacitic lava porfiridasitlerin infiltrate occurred. That make up the Great River Creek Creek Solakli Haldizen with an average of 2,500 m. High level of the plateau is located in a very large, bulbous mountains alçaldığı connecting these areas inland of the coast-Çaykara-Bayburt road is the gateway. Belt section of water line to the west, Mount (2746 m) and Visit Peak (2850 m) and continues. This line is also part of the water line in the south constitutes Karadere. Sector, which extends inland to the north junction of the right arm of Karadere Yağmurdere watershed, extending to the southwest to encompass the handle portion of the water line reaches Degirmendere Basin. Black Sea coast road south, along the left Karadere Dağbaşı Arakli-road, falling water, part of the area around Stone Bridge to the south line reaches Gümüşhane.
One of the geomorphological elements of the province of Trabzon in the mass movements. These are based on the size of landslides, earth flows and soliflüksiyondur. Trabzon province is extremely important in shaping the basic reason for the formation of mass movements of soil structure. The lavas and tuffs are the dominant materials are slit and their bodies because of the cracks are more or less water conduction. Although still common in the tuffs contain pores large extent. Receive more precipitation in the region is quite hot and humid fact, decomposite cause rocks to the depths, while the overall slope, slopes of 25 ° - 30 ° on the fact that the total rainfall in the months and year-end values in the specific amounts to reach close to the mass movements are encouraged. To date, the most important of landslides that have occurred; Çaykara-Grand Mosque (1929, 146 dead), Greenhouse (1949), Macka-Catak (1988, 63 dead), Sındıran (1990) and King and Poplar Landslide.
The vertical dimension of the field variable in all seasons in temperate and rainy climate, the vegetation of different species, gave rise to generations of vegetation of different species. Accordingly, 0-300 m. yükseltilerinden psöudomaki infiltrate into the Mediterranean plant species (persimmon, maple, boxwood, cherry laurel, laurel, prekanta, medlar, juniper tar, strawberry ... etc.) showing distribution of elements, circles close to the shore from the broad-leaved forests located in the skirt (alder, chestnut, oak species , ash, linden, common hazel, white willow, poplar, east, such as Plane Tree ...), on the floor leaves a large wide-dominated mixed coniferous forests (European chestnut, common alder, hornbeam, common hazel, eastern horn, oak, maple , rowan, ÇİTLENBİK, laurel, purple flowered rhododendron, beech, spruce and fir) and also above the forests dominated by conifers (pine, spruce, rhododendron, and some of the purple flowering shrub species) shows that distribution.
According to the 2000 census the total population as of the 19th of the 81 cities of Trabzon, as population in the province center 25'incidir.
The population ages 6 and up (874 962) according to the 2000 Population Census, 439,142 women? By 356,316 percent (81.13%), 435,820 to 417,933 men-third (95.88%), reading and writing is fluent. Accordingly, the read-write the number of those who knew the 774,249 (88.49%), and the illiteracy in the 100,702 (11,51%), dir.
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