1 TÜRKİYE PROFESYONEL LİGLERİNDE GÖREV ... - Spor Bilim

In Çanakkale, there is a transition climate of Mediterrenaen and Black Sea. In
spring and winter there is much more rain. In tourism season, the temperature of the sea
water reaches the maximum level in July and August. Daily air temperatures are 35 as
the maximum level and 25 at the minimum in the season and at the night it has been 10
degrees at the minimum level for many years. During the year, the dominating wind in
Çanakkale is northern but the southern wind is the most effective. Devlet Meteoroloji
İstasyonu (Çanakkale) İklim Verileri (DMİ-1930-2002).
Geological Structure:
The geological structure of Çanakkale includes schists with clay and marbles
that were formed at the 1 st time; limestones, clay, stone and schists formed at the 2 nd
time; stone, sand formed at the 3 rd time; alluviums and volcanic rocks formed at the 4 th
time.
1 st Time Grounds ((Paleozonik): The west of Karabiga is the best sample of this
kind of grounds. This area is, especially, formed with marbles and schists with clay.
2 nd Time Grounds (Mezozoik): These grounds are formed with limestones, sand,
stone, clay and schists. It covers the Anafartalar Harbour and Kireçtepe regions. This
kind of grounds are seen between Biga and Gönen, around the Göre mountain and in the
neighborhoods of Yiğitler, Bayramiç, Ezine and Geyikli. Limestone is mined in this
region. There are also 2 nd time mines such as bullet, zinc, iron and marble.
3 rd Time Grounds (Neozoik): The areas that are covered with this kind of
grounds are in the Hamdibey sub-district which is on the northwest of the county Çan,
and the parts that covers the both collars of the Dardanelles and not higher than a
hundred meters. The stones in this area are sandy and with clay. There are also some
parts where limestones are dominant.
4rd Time Grounds (Kuvaterner): These are the grounds which are surrounded
by the alluviums that were carried by the brooks and were sprinkled at two sides. These
areas get wider where the brooks arrive the sea. Since they are very rich in point of sole
water, they form water sources in some regions such as Çardak.
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