Kızılcahamam kuzeyinde fiziki coğrafya araştırmaları
Başlık çevirisi mevcut değil.
- Tez No: 25906
- Danışmanlar: YRD. DOÇ. DR. ALİ FUAT DOĞU
- Tez Türü: Yüksek Lisans
- Konular: Coğrafya, Geography
- Anahtar Kelimeler: Belirtilmemiş.
- Yıl: 1993
- Dil: Türkçe
- Üniversite: Ankara Üniversitesi
- Enstitü: Sosyal Bilimler Enstitüsü
- Ana Bilim Dalı: Coğrafya Ana Bilim Dalı
- Bilim Dalı: Belirtilmemiş.
- Sayfa Sayısı: 152
Özet
10- SUMMARY A big cavity, which is the working site is in between Bolu- Ankara and old base of Sakarya, is filled with volcanic materials, which were come from faults of Alpin movements. In this region at the end of Eosen, volcanism was increased its effect as a result of violence of Orogenic movements. At middle Miocene, as a result of collision of continents, faultines, rising of mountains, lowering of basins were occured Miocene lakes were filled and dried with volcanic intermediate layers of lacustrine sediments with the increasing volcanic activities. At the end of upper Miocene, in the Miocene lakes accumulated flat places, and at the mountains de veloped corrosion surfaces as pediment shape were occured. These Upper Miocene corrosion surfaces are lie and elevated from south to north, 1350 to 1750 m. around the working site. Corrosion was refreshed at the end of Pliosen as a result of epirogenic movements. In this way lowlands and cavities, which formed Pliosen topography and which were occured by the effect of tectonism, were filled at the end of Upper Pliosen. Upper Pliosen continental depos its must be the lower corrosion surfaces correlated which occur by re freshing. These lower corrosion surfaces are lie and elevated from south to north around 1000 to 1400 m., around the working site. 108At the north boundary of working site existence of North Anatoli an Mountains altitudes and at the south boundary existance of Middle Anatolian basins cause lowering up these corrosion surfaces from north to south. These lower corrosion surfaces have an inclination in its sur face systems and they show parallel but different extensions in every surface systems. The region that was occured by the tectonic movements at the Pliosen and filled with continental deposits at the upper Pliosen, is emptied by Gürcü River today. This Upper Pliosen filling basin was cracked at the lowest Pleistosen and at the top coarse conglomerates was gave it its top shape, as a result of tectonic movements at the end of Pliosen and also as a relief result of changes in climatic conditions. At the Gürcü River Valley upper terrace has a height of 50-60 m., which is most obvious here, and at the Hamam River Valley this terrace has a height of 60-70 m. At the lowest Pleistosen ı recracking was occured and lower terrace surface was took form. Upper portion have a height of 15-20 m. at Gürcü River Valley. This lower terrace step is not very obvious. Corrosion surfaces were cut into parts by the steep and narrow base valleys of the working site.. The climate of the working site shows a transitional climatic condi tions between the Blacksea climate and Middle Anatolian Region's step climate. Kızılcahamam precipitation regime is the“Middle Anatolian Transition Type”,. As a point of precipitation activity, climate shows 109transition between Middle Anatolian semi arid areas and Blacksea coast moist areas. Therefore Kızılcahamam has“semi- moist”climate. In study zone, in general dentritic drainage pattern is seen. The most important river is Kocaçay which is enlarging by the addition of side branches, at the northern part of Kızılcahamam and a branch of Kirmircayi which is added to Sakarya River later. Cracks, which were occupied by the tectonic movement, provided finding of hot water sources at Kızılcahamam, Acısu, and Sey village, Regional soils, which are not calcareous brown forest soils, cover a huge area in study zone and a narrow area is covered by non regional soils of brown forest soils in the southwest of the study zone. Precipitation is increasing by the rise in the elevation, while going to the north of Kızılcahamam. Abundant forest was grown up at the northern parts as on influence of classing to Blacksea. At the north ern parts of study zone above the 1500 m. level forest has moist charac teristics and consist of yellow pines and firs. At the southern parts especially at corrision surfaces, which are very suitable to citizens, forest zones were destroyed and by the effect of Middle Anatolian cli mate at forest zones were widespreaded here. 110
Özet (Çeviri)
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