Düzce ilçesinin coğrafyası
Başlık çevirisi mevcut değil.
- Tez No: 22323
- Danışmanlar: DOÇ. DR. EJDER KALELİOĞLU
- Tez Türü: Yüksek Lisans
- Konular: Coğrafya, Geography
- Anahtar Kelimeler: Belirtilmemiş.
- Yıl: 1992
- Dil: Türkçe
- Üniversite: Ankara Üniversitesi
- Enstitü: Sosyal Bilimler Enstitüsü
- Ana Bilim Dalı: Belirtilmemiş.
- Bilim Dalı: Belirtilmemiş.
- Sayfa Sayısı: 84
Özet
Özet yok.
Özet (Çeviri)
81SUMMARYThe county Düzce formations investigation area in the northwestof Turkey in Bolu.Investigation area forms in the two foundation geolo-gic structure.In the plain Düzce places fault lines restricted the bendditch and the plain sides upland area.The uplands more Mesozoik area andespecially upper cretaceous formation,but the plain Düzce has lake areawhile the quartemary beginning positions alluvial fill result in today's.Uplands generally in the investigation area on 400 m. formationthe plateau areaJn the south, there are some upland mountains area on1500 meters and for the most part of plateau splits deep valleys morethan 10 km.These valleys to enter into point piled up the materials for-mationed the accumulation cones.In the southwest,Eft eni Lake sides Düzceplain's formation not upland.And then,cause in naturewater heightly,-thispart,there is formation the reed-bed and quagmire.In the investigation-area,sees the transition climate character-istics in West Black Sea.The yearly average warm is 13»3°C.In January isthe most cold month with 3»2°C while in July is the most warm with 22,4“CoThe frost days are 38,8 days and they formations from in November toin April.The strong wind directions are southwest and northeast so yearlyrainfall is 845 mm0 in Düzce.Especially,in winter and spring months morerainfall months in Düzce,but in summer rainy,too.Snowing from in Novemberto in April and total days are 11,8 days «In addition to this, sees thetransition climate characteristics in West Black Sea and humid climate incategories.Because,of the rainfall,those lakes? and rivers(in summer) decrea-ses the levels and flowes when in spring they increases level.In the northGülle Deresi,in the northeast Kurtsuyu Deresi»Küçük Melen ÇayxBin theeast Aksu Deresi,in the southeast Asar Suyu,in the south Uğur Suyu and inthe southwest Efteni Lake.Especially,fault lines and underground springwater rich in thisside and the plain area formations alluvial characteristics soil.The up-lands widespread podsol and the brown forest soil.More density being forest covered in county Düzce,not that weknow of first settle down beginning before 2000 year.Especially,the agri-cultural activity go in speeds steting from 17»century so that side be-gins get to migrate from outoThe side of speed population sees with the agricultural improveand mechanization.In the investigation area,the great settle down unitis in Düzce center and population 62 000.The last of 25 years,the industrycity characteristic gets in Düzce and densities on the roadway E5.Today's,Konuralp and Kaynaslx is the small village center,but this places havejust on the small town and every last day you can see cities activity inDüzce.In this side,the tradional country houses built with wooden ma-terials connected with the forest covered.These houses are most one ortwo stories and mansion form in small towns;however,especially,the lastof 15 years,builds modern residance0In 1935 total population is 78 220 and this population's 6476lives in Düzce.In 1990 total population is 155 855 and this population's62 606 lives in Düzce.In Düzce,the population density more or less 175persons.The average agricultural administer at large environs 15 acrein Düzce and patatoes,corn and white beet formation production areas.In this side,especially the. cattle and poultry in the important.In the end,Konuralp historical place and natural sides,tourismactivities in Düzce. ^ _ -,-*&_» ”- __-POKÜMAMÎASYOisi Mfi*i&£ZS
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